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                                 FOREWARD


The Environmental Protection Agency was established to coordinate administra-
tion of the major Federal programs designed to protect the quality of our
environment.

An important part of the Agency's effort involves the search for information
about environmental problems, management techniques, and new technologies
through which optimum use of the nation's land and water resources can be
assured and the threat pollution poses to the welfare of the American people
can be minimized.

The report contributes to the knowledge essential if the United States
Environmental Protection Agency is to meet the requirements of environmental
laws that it establish and enforce pollution control standards which are
reasonable, cost-effective and provide adequate protection for the American
public.

The Great Lakes National Program Office (GLNPO) of the United States Environmental
Protection Agency, was established in Region V, Chicago to provide a specific
focus on the water quality concerns of the Great Lakes.  GLNPO provides funding
for Great Lakes demonstration grants under Section 108(a) as well as provides
personnel support to the International Joint Commission activities under the
U.S.-Canada Great Lakes Water Quality Agreement.

Several land use water quality studies have been funded to support the
Pollution from Land Use Activities Reference Group (PLUARG) under the
Agreement to address specific objectives related to land use pollution to the
Great Lakes.  This report describes a methodology for integrating point and
diffuse source control practices and costs in both large and small watersheds.

The conference committee consisted of Ralph G. Christensen, Section 108(a)
Coordinator; Carl D. Wilson, Regional Nonpoint Source Coordinator; Clifford
Risley, Regional Research and Development Representative; Don Urban, USDA -
Soil Conservation Service; and Orville Macomber, Center for Environmental
Research Information.

We hope that the information and data contained herein will help planners
and managers of  pollution control agencies make better decisions for
carrying forward their pollution control responsibilities.

                                     Madonna F. McGrath
                                     Director
                                     Great Lakes National Program Office

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                                              EPA-905/9-80-009
                                              September 1980
SEMINAR ON WATER  QUALITY  MANAGEMENT TRADE-OFFS

   (Point Source  vs.  Diffuse Source Pollution)


                   Conference
                    Held  at
             Pick  Congress  Hotel
          520 South  Michigan Avenue
              Chicago,  Illinois
            September  16-17,  1980
             Conference  Assistance
                       by
Center for Environmental  Research Information
            -Technology  Transfer-
               Cincinnati ,  Ohio
            Sponsored  &  Published
                       by
            Section 108(a)  Program
     Great Lakes National Program Office
    U. S. Environmental  Protection Agency
       536 South Clark Street,  Room 932
           Chicago, Illinois  60605
                      U.S.  i:«vSr'onrrr-rtn!  '";•:•" :-:.'
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                      £,,j:'J  <.'..-"'-• I.'-  ',,•'-'  ,..- I W-^S.

                      Chicago, iiiinois  606U4  _

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                          Table of Contents                            page

Call to Order                                                               1
  Clifford Risley, JR. R&D Representative, USEPA, Chicago

Welcome                                                                     3
  John McGuire, Regional  Administrator, USEPA, Chicago

Congressional Intent of Clean Water Act and Amendments                       7'
  Jeff Nedelman, Administrative Assistant to Senator Gaylord Nelson

Water Quality Issues and Conference Overview                               13
  Madonna F. McGrath, Director, Great Lakes National Program Office
  USEPA, Chicago

Section 208 Program
  Peter Wise, Director, Water Planning Division, USEPA, Washington, D.C.
  (No paper submitted)

Prime Farmland and Water Quality                                           19
  Keith K. Young, Soil Scientist, USDA-SCS, Washington, D.C.

AST/AWT Policy Issues                                                      27
  Jeffery J. Gagler, Water Quality Policy Section, USEPA, Chicago

Federal Policy in Floodplain/Wetland Regulation                            33
  Ronald L. Mustard, Chief, EIS Review, USEPA, Chicago

U.S.-Canada Great Lakes Water Quality Agreement-Impact on U.S. Policy      37
  Kenneth Walker, Secretary, Great Lakes Water Quality Board, IJC
  Windsor, Canada (Dan Bondy)

State/EPA Agreements: A State/Federal Partnership                          43
  David Stringham, Assistant to Regional Administrator, USEPA, Chicago

WQM Plans, Status, Quality, Integration and Implementation                   47
  William G. Benjey, Chief, Ohio WQM Section, USEPA, Chicago

Water Quality Standards—Integration                                       53
  Michael MacMullen, Chief, Water Policy Section, USEPA, Chicago

Effects of Pollutants on Human Health                                      55
  Leland J. McCabe, Director, Health Effects Research Laboratory
  USEPA-Cincinnati

Sources of Pollutants to the Great Lakes                                   63
  W. Ronald Drynan, Senior Engineer, IJC, Windsor, Canada

Tributary Loads and Effects                                                75
  Nelson Thomas, Chief, Large Lakes Research, USEPA, Grosse He, MI

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                                                                             Page

Land Treatment of Municipal Wastewater                                        77
  Al Wallace, Dept. of Civil Engineering, University of Idaho
  Moscow, Idaho

Costs of Wastewater Treatment                                                 81
  James A. Hanlon, Chief, EEB, Water Division, USEPA, Chicago

A Management Technique for Choosing Among Point and Nonpoint Control          87
Strategies
  Part 1-Theory and Process Framework
  William Sonzogni, Water Resources Specialist, GLBC, Ann Arbor, MI

Recap of Previous Day's Program and Goals for Today                          125
  Carl D. Wilson, NPS Coordinator, USEPA, Chicago

A Management Technique for Choosing Among Point and Nonpoint Control         129
Strategies
  Part 2-A River Basin Case Study
  Timothy Monteith, Water Resource Engineer, GLBC, Ann Arbor, MI

BMP Cause and Effect Relationship  by Simulation                              163
  Larry Huggins, Agricultural Engineering,  Purdue University
  Lafayette, Indiana

Practical Uses of ANSWERS Model in BMP Planning                              177
  Daniel McCain, District Conservationist,  USDA-SCS,  Fort Wayne, IN

Water Quality: Sediment and Nutrient Loadings  from Cropland                  183
  Darrell Nelson and Ed Monke, Purdue University, Lafayette, IN

The Variety of On-Site Treatment System  Failure                              203
  Al  E.  Krause,  Environmental Scientist, USEPA, Chicago

Mill  Creek Pilot Watershed Study on Pesticide  Fate In An Orchard             207
Ecosystem: Development and Presentation  of  the Experimental  Data Base
  Matthew Zabik, Pesticides Research Institute, Michigan State  University,
  Lansing, MI

Livestock Inputs and Effects                                                 225
  Frederick Madison, Soil Scientist, University of Wisconsin
  Madison, WI

Upstream  Point Source  Phosphorus  Inputs  and Effects                          227
  David  Baker, Professor, Heidelberg College,  Tiffin, Ohio

Sediment  and Phosphorus Transport                                            241
  Stephen Yoksich  and  John Adams,  US Army COE, Buffalo,  NY

Bioavailability  of Phosphorus Sources to Lakes                               279
  Terry  Logan, Professor, Ohio State University,  Columbus,  Ohio

Water Monitoring Program-Planning  for 1981                                   293
  William Sanders,  III,  Director,  S&A Division,  USEPA,  Chicago

                                     iv

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                                                                            Page
Conservation Tillage Practices to Control Agricultural Pollution             301
  John Crumrine, Manager, Honey Creek Watershed Project, Tiffin, Ohio

Nonpoint Source Pollution in Urban Areas                                     309
  James Baumann and John Konrad, Wisconsin Department of Natural
  Resources, Madison, WI

(NURP) National Urban Runoff Program                                         323
  Douglas A. Ehorn,.  Chief, Michigan WQM Section, USEPA, Chicago

High Flow Water Quality Standards                                            329
  Lyman Wible, Chief Planner, SEWRPC, Waukesha, WI

Biological  Indices or a Measure of Water Quality                             355
  James Gammon, Professor, DePauw University,  Green  Castle, IN

Biotic Impact of Organic and Inorganic Sediments                             365
  James 0.  Bland, Ohio WQM Section, USEPA, Chicago

Conference  Summary                                                           377
  Clifford  Risley, Jr., Regional R&D Rep., USEPA, Chicago

List of Attendees                                                            383

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                             CALL TO ORDER

                          Clifford Risley, Jr.
                         Senior Science Advisor
                            US EPA, Region V
Good morning, Ladies and Gentlemen.  Welcome to the Seminar on Water
Quality Management Trade-offs.

I want to give you a few words of background regarding this seminar.  For
many years, Region V of EPA has been very much concerned with the problem
of evaluating and controlling non-point source pollution.  We have sponsored
many projects to give us a better understanding of each of the elements in
this problem.  This work ultimately led to a discussion among those involved
in non-point source pollution control regarding    the need to put it all
together into a process that we could use to evaluate non-point abatement
costs and compare them to conventional treatment or point source costs.  We
feel there is a great need for a method of doing this, in as simplified a
manner as possible, for all water quality managers.  As an outgrowth of
our discussion of this need, we decided that one of the best ways to pre-
cipitate this kind of product was to put together this seminar.  That is
the "why" of this particular seminar.

We have brought together here, today, many of the people who have been
working quite a few years on various parts of the problem; to give you an
idea of the kind of work that has been done; the kind of knowledge that is
available and the sources of this knowledge, so you will know who is who in
these complex studies.

It is now my pleasure to introduce to you, Ms. Madonna McGrath, Director of
the Great Lakes National Program Office, EPA Region V, who will be your
moderator for the first session.

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                            Welcome
                               by
                         John McGuire *
                    Regional Administrator
                    USEPA, Region V, Chicago

I am happy to welcome you to this seminar which we have entitled
"Seminar on Water Quality Management Trade-offs, Point Source vs.
Diffuse Source Pollution."  Our Region V Environmental Protection
Agency, Great Lakes National Program Office and the EPA Center for
Environmental Research Information have programmed this seminar to
address water quality issues and goalp that hopefully will help us all
to have a better understanding of how to plan and manage a water quality
control program.

The Great Lakes National Program Office, I speak of, became operational,
with headquarters in Chicago, in December 1977.  GLNPO's main function
is to conduct surveillance and coordinate research and special studies
in the eight Great Lakes States.  GLNPO also provides technical support
and remedial programs for EPA's nonstop fight against all forms of
pollution in the Lakes, the largest freshwater system in the world.

GLNPO coordinates its efforts and cooperates with other Federal agencies,
with State and local governments, and with university research programs.
GLNPO also works closely with these counterparts in Canada, which shares
the boundaries of and concern for the Great Lakes.

The Center for Environmental Research Information, headquartered at
Cincinnati is the Agency's technology transfer specialists.  We appreciate
their assistance in preparing this program.

The purpose of this seminar is to discuss a number of water quality
issues and policy issues related to control of both point source and
diffuse source pollution.  At present there is no accepted methodology
for integrating point and diffuse source controls and for comparing
the costs associated with them.
* Given by Madonna F. McGrath, Director, Great Lakes National Program
Office, for John McGuire.

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The legislative mandate given to the USEPA for protecting our water is
Public Law 92-500, and its amendments.  A responsibility to manage both
point source and diffuse sources of pollution are spelled out for us.
In addition to the U.S. mandate we have a responsibility to Canada for
our activities on the Great Lakes.  Under a U.S./Canada Great Lakes
Water Quality Agreement signed by the two countries in 1978 we share
a common concern for the pollution control of the international boundary
waters that includes all of the Great Lakes and their tributaries.

One of the reference of the Water Quality Agreement was directed by the
International Joint Commission to inventory land-use activities and
their pollution effects on the Great Lakes.

To do that task USEPA, through Region V, funded four major pilot water-
shed studies along with several other studies to prepare information
and remedial recommendations to best reduce and control diffuse source
pollutions to the Lakes.  Three major sediment control projects and one
urban drainage project were funded under Section 108(a) to provide data
for use in developing implementation programs in the Great Lakes basin.
The U.S. Army Corps of Engineers under Section 108(d), Lake Erie Waste-
water Management Study, has done extensive study and demonstration in
Lake Erie basin to reduce and or control sediment.  Approximately $19
million in addition to Section 208 Areawide Wastewater Management
Planning has been spent on diffuse source study and demonstration
since 1972 in Region V.

In the Great Lakes basin the USEPA has provided $5 billion of the
public funds to support additional State and local government funds
for treatment and control of municipal wastewaters.

The presenters at this seminar will provide you with data and information
that they have personally been involved with.  They will be able to
answer most of your questions.  We have a great amount of point and
diffuse source water quality data in Region V.  Based on the data we
have we are proposing a methodology that will help to evaluate cost

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effective trade-offs necessary to achieve a prescribed water quality
goal on a watershed basis.  This might tell us that in one watershed
diffuse source control is the most cost effective while in another-
watershed point source control is the most cost effective.  The
methodology will also help to evaluate what might be the best mix of
                                          I
point and diffuse source controls that together would be most cost
effective to achieve a water quality goal.

As we proceed through the two days of this| conference I hope you will
take advantage of the expertise and experience of the presenters to
help you with achieving our water quality |goals.

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                     CONGRESSIONAL INTENT OF CLEAN
                        WATER ACT AND AMENDMENTS

                              Jeff Nedelman
                      Administrative Assistant to
                         Senator Gaylord Nelson

It is always a pleasure to come back to Chicago.  I enjoy looking at
Lake Michigan and realizing that it is still a beautiful lake thanks
to the efforts of Region V of EPA.  I saw Madonna, several weeks ago,
when Senator Nelson and I were visiting your marvelous lab at Duluth.
We were getting a briefing on Great Lakes water quality issues, research
funding, programs under way, and a discussion of concerns which we both
share.  Madonna asked if Senator Nelson would be available to speak to
you today.  It was his desire to do so, but with the election only 15 days
away, the press of events has required him to reschedule his time day by
day and he was simply unable to get here today.

The Congressional Intent of the Clean Waters program as it applies to the
Great Lakes is my topic.  This is basically the third time I have had an
opportunity to speak about water quality issues.  The first time was
several years ago at an International Joint Commission (IJC) meeting in
Windsor, Ontario.  I delivered a speech which was euphemistically called
"Americas Great Lakes Programs and the Bureaucratic mess in the U.S."
which got quite a little bit of attention.   A year or so ago, Senator
Nelson spoke to the Great Lakes Fisheries Executive Meeting in Miluakee.
His speech was titled

          "Progress; albeit slow—New Problems on the Horizon"

He emphasized that progress was being made  but much too slowly.   He tried
to put this in perspective by taking us back a few years outlining some of
the trade offs that have to be made in contemplating the future.

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                                 - 2 -
The 1970's saw an enormous growth of public concern and public activity
regarding the environment.  There were a number of catalysts that came
to the fore.  For example, Gaylord Nelson happened to be invited to give
an address on Nuclear Power at Berkely right after the campus protests.
Flying back, he picked up a magazine that had a long piece about the
decried confrontations on the campuses about the Viet Nam War.  It de-
cried the energy and activity applied to the war and suggested that the
government should apply the same kind of energy and activity to domestic
issues.

The Senator made the logical comparison between the Educational and
Informational Programs on the war and the need for the same level of
effort on the Environment.  This led to Earth Day in April of 1970.
From the 70's we see a cry from the public for more legislation to
protect the environment.  EPA came along, Earth Day, Strip mine
legislation, Clean Air, SCOPE (Student Council on Protecting the environ-
ment) among many others.  When EPA was established in Chicago, I met a
lot of people who were working quietly and diligently to clean up the
environment and who were enormously helpful in supplying good informa-
tion to our office which helped us develop our legislative position.
I think, in all honesty, that in the late 60's and 1970's we were making
suggestions.  At the time when the legislation was created in Congress,
we were guessing at the scope of problems, we were guessing at the contri-
butions, we were guessing at the costs.  We did not really have any know-
ledge of how long it would take.  Nevertheless, we set a goal, we set a
deadline and we began.
                                  t

We set a goal of a quality environment; the fishable, swimmable, water
quality by 1985.  It still seems to us to be a reasonable goal.  However,
there are new considerations.  The 1980's, it seems to me, are like the
1960's.

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                                 - 3 -
There is a new vernacular, a new awareness on both sides that clean water
is desirable and attainable.  But we have new problems that we didn't know
existed before.  The question is not one of whether we shall have clean
water but the question is "How clean is clean?"  and "How quickly can we get
there?"  The Congressional staff is constantly discussing how much it is
going to cost and where is the money coming from?

In my judgment, the whole movement of the 60's toward a high quality environ-
ment remains today as the concern of the highest priority for the public,
second only to our national security.  What we are talking about 10 years
after Earth Day, are still questions affecting the productivity of our
oceans and our lakes.  These are of high concern, especially to the hundred
millions of people living around the Great Lakes.

We have seen sone progress but it has been slow.  For example, the Reserve
Mining situation where 67,000 tons of carcinogenic material were dumped
yearly into Lake Superior.  It took eleven years of court action to stop
the 20 years of dumping.  There are many other examples of slow but sure
progress.  We have been putting together all the parts of the clean up
process but I am not sure we understand all the parts.  The thrust of
EPA's program has been to gain a basic scientific understanding of how
these enormous bodies of water work.  Where is the pollution coming from?
What effects does it have?  How do we get it out?

What we have been seeing in Congress is, in my view, a lack of sensitivity
to these problems.  EPA is just not getting the money that is needed for
Great Lakes.  This year EPA spent $18,000,000 in travel and only $2,000,000
on the Great Lakes.  We have been going back and forth on this issue for
many years.  The Congressional supporters of the Great Lakes keep putting
items into the budget and the budget committee keeps knocking it out.
To members of Congress from the Great Lakes States and the Northeast, this
is recognized as a great problem.

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                                 - 4
Basically, we have about ten years If the degradation continues.   The Great
Lakes program is being funded very minimally.  By comparison, look at the
Sewage treatment plant construction program.   It is in the order of three
to four Billions of Dollars.  These programs  are decided by Congress and
the appropriations made and KPA hms little choice but to do those things
which Congress appropriates the money for.

William Proxmire, Chairman of the Budget Committee proposed taking 2 million
dollars out of Sec. 314 funds to pay for KPA salary increases.  We fought
against this and therefore we have bad news for those expecting a pay raise.
I don't think you are going to get it.

Section 108 program lias had no increases for  years.  The Office of Planning
and Management constantly refers to the billions of dollars in the Sewage
Treatment Plant Construction which goes in part to Milwaukee, Chicago and
Detroit and assumes this takes care of Great  Lakes needs.  But of course
it can't be used for the Great Lakes Research needs.

The Administration requested of Congress in April that 3.5 Billion dollars
of the Construction money be deferred.  We objected because this would hit
Wisconsin very hard; it would hit the Great Lakes very hard.  It took four
of five months of discussion and action but the motion to overturn this
appropriation deferment carried unanimously in the Senate budget committee
and it carried unanimously on the floor of the Senate.  Despite all the
talk of the necessity to tighten the belts and to batten down the hatches
in federal spending, Gaylord Nelson successfully led the fight to continue
this funding.  The support was there in the committee and in the Senate.
You just cannot get this support for 8.6 Billion dollars in these times with-
out the members of Congress and members of the Senate understanding that
there is wide base public support for these programs in their home states.
                                   10

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In terms of new problems and trade offs that are  facing Congress  in the
next year or so, Environmental  issues have heen constantly before Congress.
We have had fights over water policy but even more over public works pro-
jects.

Both the Clean Air Act and Amendments to the Water Quality Act come before
Congress next year.  From everything that T hear, we can expect 1981 to be
a major test of the nation's resolve to meet the  goals that were  spelled
out in the Water Quality Act.  Congress needs to affix the direction of
the enormous costs that have to be spent to achieve the goals.  It needs
to set the new round of time tables for moving ahead.

According to Kl'A estimates 54 Billion dollars will be needed to complete
all secondary treatment plants and advanced waste treatment projects.  With
inflation in the construction industry running to more than 50% we are not
making any real headway at all.   KPA itself estimates that with a /.ero
inflation rate it would take twenty years to complete all the mandated
projects.

That brings us to the second issue  "Can we wait  twenty years?"  The answer
is "No, we cannot."  The city of Milwaukee is an example of many other
cities which have needs beyond the current level of appropriations.  How
are we going to get these major cities to move along to meet their man-
dated time tables when the Federal funds come to the states on a much
slower time table?  How can the  cities come up with sufficient funds on
their own?

The third issue is "Why should Congress increase the appropriations when
about 50% of the plants on line  now operate inefficiently?"  The means of
achieving proper O&M should he a local responsibility.   Congress  is faced
with a difficult decision regarding funding of O&M costs.
                                  11

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                                 - 6 -
It seems to me that we only have one Great Lakes.   They are a national
treasure and a national resource that demand high priority.  They must
be viewed as a long term committment.  They cannot he reviewed on a year
to year budgetary basis.  Where the administration does have discre-
tion, it seems to me, they must exercise that discretion as positive
support for the Great Lakes.

I am optimistic about the future of the Rnvironmeental movement.  Part
of the dialog that takes place in Congress daily deals with clean air,
clean water and a safe environment.  We can all be thankful for that.

Congress is comprised of many members who, with their staffs, share your
concern about the Great Lakes and who are more aware than most what man
is doing to the environment.  Therefore, we have a very heavy responsi-
bility indeed, to make sure that the programs work, that they are run
efficiently, that the public understands the progress we have made and
the problems we face in the future.  We must be careful not to be
doomsayers but to be frank about the problems and the difficulites to
be faced and the costs required to solve them.
                                  12

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            Water Quality Issues and Conference Overview
                          Presented By
                        Madonna F. McGrath
          Director, Great Lakes National Program Office

Canada and the United States share a vast and valuable resource - the
five Great Lakes, which form the largest freshwater system on earth.
One-fifth of the U.S. population, one-quarter of the U.S. industry, and
more than one-third of Canada's population depend on the Great Lakes
for drinking water, transportation, industrial development, energy
production, fishing and recreation.  The water quality of the lakes must
be maintained or those uses will be lost or greatly impaired.

While many governments, states and agencies share the responsibility for
Great Lakes water quality, the prime pollution control efforts in U.S.
waters fall within the scope of the U.S. Environmental Protection Agency
and the various programs it administers.  The goal  of EPA's Great Lakes
program is to restore and enhance water quality in the Great Lakes basin
so that public health, welfare and the environment are protected.  To
achieve this goal USEPA established the Great Lakes National Program
Office.  The principal function of this Office is to plan, coordinate
and oversee EPA's pollution control programs as they affect waters of
the Great Lakes, acting as a catalyst with the EPA Divisions and the
States in identifying Great Lakes problem^ and recommending solutions
to them.

Since the U.S. and Canada share a common concern regarding pollution of
the lakes the two countries renewed the Great Lakes Water Quality Agree-
ment in 1978.  Historic precedent for both the 1972 and 1978 Agreement  is
the U.S. - Canadian Boundary Waters Treaty of 1909, which specified that
neither country is to do anything that would harm Great Lakes waters and
threaten the health of citizens of the other country.  The implementation
of the U.S. portion of that Agreement is the responsibility of my Office,
which also provides staff services to Region V's Regional Administrator,
John McCuire, in his capacity as Co-Chairman of the International Joint
Commission's Great Lakes Water Quality Board.
                                  13

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To accomplish both our national and international goals we conduct water
quality surveillance programs and special investigations and provide both
the public and other offices with scientific reports and policy recommen-
dations.  To assure that citizens are involved and well informed in matters
and decisions affecting the Great Lakes our staff prepares brochures,
technical reports and other educational materials.  The Great Lakes
National Program Office also serves as a focal point for communication
and cooperation with other groups and agencies involved in Great Lakes
activities, as evidenced by this Conference today.

We greatly appreciate the participation of the many agencies which are
represented by our speakers and guests in the audience.

The new definitive strategy for activities by the Great Lakes National
Program Office calls for concentration of most of our scientific and
technical resources on three key areas:
    1.  The revision and implementation of Great Lakes monitoring to
        emphasize toxic chemical and nutrient surveillance.
    2.  Special investigations of serious "hot spots" problem areas,
        and development of multimedia remedial control programs for
        them.
    3.  Increased State involvement in Great Lakes decision-making
        through the State/EPA Agreement process.
To understand why the Great Lakes National Program Office is concentra-
ting of these areas, it is important to understand the problems that
currently plague the Great Lakes.

The most serious threat to the Lakes is the existence of persistent toxic
chemicals in Great Lakes water, fish, wildlife and sediments.  These
substances affect all portions of the Great Lakes in varying degree.
Many have the capacity to bioaccumulate; they have been found in the
Lakes'  fish and wildlife in alarming concentrations.  Fish from Lake
Ontario are heavily contaminated by Mirex.  Lake Michigan fish cannot
be sold commercially because of high levels of PCB's.  Fish from Lake
St. Clair had high levels of mercury that restricted their use for several
years.
                                  14

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Toxic substances reach the aquatic environment through direct discharges
from industries, in runoff from agricultural and urban activities, and
from the atmosphere.  While the effect of toxic substances on aquatic
organisms is not well understood, severe adverse health effects on
mammals and birds are well documented.  But we need to learn very much more
about how and where these pollutants enter the lakes, how to identify
and locate them in the lakes and their tributaries, and to learn about
effective management programs to remedy their negative impacts.

While toxic chemcial pollution is receiving a great deal of attention,
there still remains the problem of accelerated eutrophication of the lakes
by nutrient enrichment.  If not controlled, this enrichment and the result-
ing loss of oxygen can lead to greatly increased costs for treating
drinking water, elimination of high-quality fish species, and loss of
recreational activities through fouling of beaches, elimination of sport
fisheries, and increased algal growths on the hulls of boats and ships
that sail the Lakes.

All of the Great Lakes are affected by this process in varying degree, but
Lake Erie and Lake Ontario and sheltered areas such as Green Bay and Saginaw
Bay are the most severely affected; they have suffered major deterioration
in the quality of their fish stocks.  Dissolved oxygen depletion in the
bottom water of the central basin of Lake Erie has a severe impact on
fish reproduction because of fish respiratory problems and changes in
chemistry.

Traditionally phosphate discharges to the lakes have been reduced through
more stringent requirements on direct municipal and industrial dischargers.
But nonpoint sources from rural land runoff, combined sewer overflows,
the atmosphere and urban storm runoff also contribute nutrients and
sediments to these waters.  What mix of point and nonpoint source
control measures are needed to slow down the euthrophical processes in
the Lakes?
                                 15

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In Region V over the past year we have been a mounmental water quality
planning effort come to fruition with the local, state and federal
approval of nearly all the regional and state 208 Water Quality Management
Plans.

As these plans become more fully developed and more fully utilized, we
will expect to see more integration of the Construction Grants 201
program with the implementation of nonpoint source abatement programs
so that the total water pollution in any area is regulated in the most
cost-effective manner to meet water quality standards.  New methodologies
for water quality modeling and distribution of wasteload allocations may
be needed to meet this goal.

Several types of pollutant source reductions - as opposed to structural
measures are often a feature of nonpoint pollution abatement plans.
Reductions may be proposed through implementation of appropriate best
management practices or better housekeeping practices such as storm
sewer cleanups or street sweeping.  Nonpoint source abatement may also
involve improved management practices of on-line construction - for example,
modifications of flow control devices to increase storage capabity and
attenuate flow surges in combined sewer systems.  What are the options
and alternatives in combining such nonpoint abatement techniques with
sewage treatment plant construction and other structural pollution
abatement technologies?

One source reduction and management method which is appropriate for reduc-
ing phosphate discharge to the Great Lakes is to ban the use of high
phosphate detergents.  Currently, all Region V states but Ohio restrict
phosphate detergents, and water quality has shown^ifiprovements where
restrictions have been effectively enforced.  Immediate reduction of
phosphorus loads to the Great Lakes may still be realized with an exten-
sion of detergent controls to States which have no such controls and
whose waste treatment programs are not in compliance with phosphorus
effluent limitations.
                                    16

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Although the need for further phosphorus control of the Great Lakes is
evident, clear directions of the extent, timing and type of additional
controls needed are not readily apparent.  The effectiveness of non-
point source controls, phosphorus bioavailability, and the cost of these
remedial measures can now only be quantified in a very incomplete
fashion.  While there are indications that additional tributary load
reductions will be required to meet the International Joint Commission's
1978 target loads, we need to assess the impact of presently recommended
controls for toxics and phosphorus and for point and nonpoint loads,
especially on Lake Erie and Lake Ontario, before recommending major new
programs.

Information shared in this conference about multimedia lake inputs,
agricultural demonstration watershed projects, model structures and
evaluations, target loading, phosphorus bioavailability, appropriateness
of institutional control measures - to name a few of the seminar topics
will be used to improve implementation of our present goals and to reduce
uncertainties about development of future goals for the Great Lakes.
Having this information is essential to your and our need to understand
the total Great Lakes ecosystem and the diverse interactions which
occur within its chemical, physical  biological and societal components.
As we develop this kind of understanding we can, together, develop
effective management and restoration of the Great Lakes.
                                  17

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                    PRIME FARMLAND AND WATER QUALITY

                                   by

                             Keith K. Young*


                             INTRODUCTION

     Food production involves a trade-off with water quality.   Whenever
the protective cover of vegetation is disturbed and the soil is tilled,
the potential for erosion is increased.  Increased erosion not only
lowers productivity but increases sediment in streams and lowers water
quality.

This paper discusses our supply of prime farmland, its effects on water
quality, and our need to preserve and conserve it.

                        WHAT IS PRIME FARMLAND?

     Detailed criteria for prime farmland were published in the Federal
Register on January 31, 1978.  Basically, prime farmland is the land that
is best suited to producing food, feed, forage, fiber, and oilseed crops.
It has the soil quality, growing season, and moisture supply needed to
economically produce a sustained high yield of crops when it is treated
and managed using acceptable farming methods.  Prime farmland produces
the highest yields with minimal imputs of energy and economic resources,
and farming it results in the least damage to the environment.

     Prime farmland can be cropland, pastureland, rangeland, forest land,
or other rural land but not urban and built-up land or water areas.  It
must either be used for agricultural production or be available for these
uses.  Certain drained wetlands also meet the criteria, but SCS does not
provide technical assistance for draining existing wetlands.

     Prime farmland usually has an adequate and dependable supply of
moisture from precipitation or irrigation.  In general, it also has
favorable temperature and growing season, acidity and alkalinity, and
salt and sodium content.  It has few or no rocks and is permeable to
water and air.  Prime farmland is not excessively eroded or saturated
with water for long periods and is not flooded during the growing season.
Slope ranges mainly from 0 to 5 percent.

* Soil Scientist, Soil Technology, Soil Conservation Service, Washington, D.C.
                                 19

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                  HOW MUCH PRIME FARMLAND DO WE HAVE?

     There are about 346 million acres of prime farmland in the United
States excluding Alaska.  Most of this land is in the Corn Belt, followed
by the Northern Plains, the Lake States, and the Southern Plains (1).
Figure 1 shows the acreage of prime farmland by state and farm production
region in 1977.  The amount of prime farmland in each state varies greatly,
ranging from 38 million acres in Texas to 81,000 acres in Rhode Island.

     From 1967 to 1975, about 8 million acres of prime farmland were lost
to other uses at an average rate of 1 million acres per year (3).  Of
this 8-million-acre loss, 6.5 million acres were converted to urban and
built-up areas and 1.5 million acres to water areas.

                         HOW IS IT BEING USED?

     Two-thirds of our prime farmland, or 230 million acres, was used for
cultivated crops in 1977 (1).  This accounts for more than one-half of
the 413 million acres of cropland in the United States.  Of the 166
million acres of prime farmland that were not in cultivated crops in
1977, there were 42 million acres of forest land, 40 million acres of
native pastures and pastureland, 23 million acres of rangeland, and 11
million acres of farmsteads, farm roads, feedlots, and similar lands.

     Prime farmland accounts for a large share of cropland in the major
farming regions of the United States.  In the Corn Belt, which has 22
percent of the cropland in the country, 74 percent of the cropland is
prime farmland.  By contrast, the Mountain Region has 10 percent of the
nation's cropland, only 21 percent of which is prime farmland (1).

     Prime farmland produces the largest share of the nation's total crop
production and a large portion of the commodities for export.  This land
significantly helps to reduce the foreign trade deficit.  In addition,
the use of prime farmland for crops helps to ensure that efficient food,
fiber, forage, and oilseed production will continue with the least damage
to the environment.  The loss of prime farmland to other uses means that
more pressure  is placed on nonprime lands to meet production demands.
Nonprime land  generally are  inherently less productive and are more
erodible, droughty, difficult to cultivate, and more damaging to the
environment.
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                        LAND USE AND POLLUTION

     The following table shows sheet and rill erosion by selected land
uses (1):

                         Tons per year            Tons per acre
Land use                   (millions)               per year

Cropland                     1,969         '            4.8
Pastureland                    274                     2.4
Native pasture                  72                     4.1
Rangeland                    1,392                     3.4
Forest land                    437                     1.2
     Total                   4,144                     3.1

     The erosion amounts represent tons of soil moved from the field—not
tons of sediment.  Some of the eroded soil is trapped before it reaches
the stream.  A strong relationship exists, however, between soil loss and
sediment delivery.  Generally, the greater the erosion, the greater the
amount of sediment delivered to a stream.  The table shows that cropland
accounts for nearly one-half of the total annual erosion in the U.S. and
also has the highest average per acre loss.

     Rangeland also accounts for large amounts of eroded soil, some of
which reaches streams.  Together, cropland and rangeland produce over 80
percent of sheet and rill erosion from agricultural land.

     Because relatively larger amounts of chemicals are applied on cropland
than on other agricultural lands, sediment from cropland is more
environmentally destructive than sediment from other agricultural lands.
The PLUARG study  (2) discovered that cropland accounts for higher loads
of sediment, total phosphorus, and, total nitrogen than land in all other
uses except urban developments.  The study concluded that intensively
farmed fine textured soils near watercourses contribute the major portion
of water pollutants.

                     PRIME FARMLAND AND POLLUTION

     Of  all U.S.  cropland, that which is prime farmland has the lowest
rate of  erosion.  By capability class, estimated average annual sheet and
rill erosion on U.S. cropland  is as  follows:

                    Capability
                    class and             Erosion
                     subclass            (ton/acre/yr)
                         I                   3.0
                        He                  5.0
                        Hie                  6.9
                        IVe                  8.7
                        Vie                  14.9
                        Vile                  15.4

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     Most prime farmland is in class I or II.   The average annual soil
loss for prime farmland is less than 5 tons per acre—assumed to be an
acceptable level under which soil productivity can be maintained for a
long period of time.   Nonprime cropland soils  have much higher rates of
erosion--at unacceptable levels that degrade the potential productivity
of the soil.   On a per-acre basis, the nonprime farmland soils furnish
the greatest amount of sediment and chemicals  to streams.

     Despite the benefits of prime farmlands,  however, they also produce
pollutants.  The prime farmland soils are naturally fertile but respond
well to commercial fertilizer so farmers apply it—along with pesticides--
for optimum crop production.  Because of the relative large acreage of
prime farmland under cultivation (two-thirds of the total cropland),
total erosion and sediment from prime farmland are significant.  Prime
farmland produces almost half the amount of erosion from all cropland.
Some prime farmland soils are flooded at times — though generally not
during the growing season—arid thereby contribute sediment and other
pollutants to streams.

     Prime farmland soils are more likely to have seasonal water tables
closer to the surface than nonprime farmland soils.  As a result, leachates
from chemicals applied to prime farmlands are  more likely to reach underground
water supplies.

     On some prime farmland that is irrigated, another water quality
problem arises from improper irrigation systems and water management.  If
more water is applied than the plants can use  or the soil can hold, the
excess runs off the surface or percolates through the soil, carrying
large volumes of salts to streams and rivers.

     Prime farmland underlain by coal or other valuable mineral deposits
presents another problem that could affect water quality.  Surface mining
can cause serious environmental damage unless  proper mining and reclamation
techniques are used.  Acid materias and rock fragments must be buried and
the soil replaced in such a way as to restore  the original soil productivity
and minimize water pollution from sediment and acid runoff.

                         PRIME FARMLAND POLICY

Preservation

Preservation of prime agricultural land is a federal policy.  The National
Environmental Policy Act  (NEPA) set the federal policy "to preserve
important historic, cultural and natural aspects of our national heritage
and maintain, wherever possible, an environment which supports diversity
and variety of individual choice."  This policy was restated  in a joint
memorandum to agency heads  from USDA  and the Council on Environmental
Quality.  The policy stated that prime agricultural land,  including prime
farmland,  should not be  irreversibly  converted to other uses  unless other
national  interests override the importance of preservation or  otherwise
outweigh  the environmental  benefits of protection.
                                  22

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     The Department of Agriculture is committed to assisting federal
agencies in the identification of prime farmland.   The Soil Conservation
Service has published about 400 prime farmland maps of high priority
counties.  The rest are scheduled for publication in the mid-80's.   The
prime farmland soils are identified in counties in which soil surveys are
available (about two-thirds of the 3000 counties in the U.S.)

     The Department of Agriculture also evaluates draft environmental
impact statements with respect to impacts on prime and other important
farmlands.

Conservation

Conservation of prime farmlands—and all other lands as well--is promoted
through policies of the Department of Agriculture.  In general, the Soil
Conservation Service (SCS) provides technical assistance to farmers, the
Agriculture Stabilization and Conservation Service (ASCS) provides cost
sharing, and Farmers Home Administration (FmHA) provides low-cost loans
for implementation of conservation work.  The Science and Education
Administration (SEA) provides research, demonstration, and education.

Salinity Control

Salinity control on certain irrigated lands that include some prime
farmland has been mandated by Congress.  The Colorado River Basin Salinity
Control Act of 1979 (P.L. 93-320) authorizes certain activities to reduce
salinity problem in the Colorado River Basin.  The first study completed
the 60,000-acre Grand Valley Unit, showed that a locally acceptable
program of improved onfarm irrigation practices could reduce salt loading
of the Colorado River gy 130,000 tons annually.

Prime Farmland Restoration

The Surface Mining Control and Relamation Act of 1977 (P.L. 95-87) set
forth procedures for minimizing environmental degradation.  The Department
of Agriculture was given responsibility for reviewing surface mining and
reclamation plans on all prime farmland and for making recommendations to
the state regulatory agency.
                                  23

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                                SUMMARY

     With all cropland there is a trade-off—food production for lower
water quality.   However, when prime farmland is used for crop production
the detrimental effects on water quality are minimized.   The loss of
prime farmland puts more pressure on marginal lands which are less productive,
more credible,  and produce more pollutants.

     Environmental policy provides emphasis on preservation and conservation.
Much remains to be done, however, to preserve out best cropland from
irreversible conversions, protect its productivity from erosion, and
minimize damage to the environment.
                                24

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                               References

(1)   USDA.   1978.   1977 National Resource  Inventories.

(2)   Sonzogni,  William C.  1980.   Environmental  Pollution from land runoff.
     Environmental Science and Technology  14(2):   148-153.

(3)   USDA.   1980.   Appraisal review draft,  Part I,  Soil and Water Resource
     Conservation Act (RCA).
                                  25

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                           AST/AWT POLICY ISSUES

                                    by

                               Jeff Gagler*



     With the institution of Public Law 92-500, ambitious water quality goals

were established.  These included meeting secondary treatment by 1977 and

"Fishable/Stfimmable" by 1983.  In the process of trying to meet these goals

we have become entangled in controversy over advanced waste treatment (AWT)

issues.  On March 9, 1979, EPA issued PKM 79-7, to more intensely review

advanced treatment projects in response to a directive issued by the Appro-

priations Conference Committee.  Suit was filed against EPA on December 28,

1979, by the State of Illinois.  In general, the suit claimed that the review

policy was preventing the State from achieving the goals of the Clean Water

Act.  A settlement agreement was signed between Illinois and EPA on April 22,

1980.

     Notwithstanding the fact that the Agency's initial review procedure was

successfully challenged by the State of Illinois and has been modified to

screen out low cost technologies form further review, the policy issues

raised from the initial review procedures will not go away by merely changing

those procedures.  These and other issues go to the very heart of the National

Water Quality Management Program.  The issues are as follows:

     A.  Water Quality Standards Issues

        1.  There is a need to have a clear definition for the term "Fishable/

        Swimmable" as it applies to water quality for protecting and preserving

        the ecology of aquatic communities as they exist in waters across this

        country.
* Environmental Scientist, Modeling Coordinator, Policy Section,
  U. S. Environmental Protection Agency, Region V.
                                   27

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   2.  Efforts must be made to provide procedures and guidance for




   establishing consistency in classifying our waters and applying




   designated uses.




   3.  A clear and concise guideline must be formulated to determine




   "attainability" of the receiving water use.




      a.  This guidance should require that the test for "attainability"




      be applied against the classification and designated uses of stream




      segments and not water quality criteria.  The water quality criteria




      should be based not solely on chemical,  but also physical and




      biological conditions necessary to support a receiving water use.




   4.  The "Red Book" presumptive applicability policy for water quality




   standards must be clarified.  There must be a clear understanding for




   accepting and supporting the State's rights to recommend more restrictive




   or less restrictive criteria as recommended by the "Red Book" when




   justifiable.




   5.  There is an urgent need to develop simplified procedures for adop-




   tions, approval, disapproval,  and promulgation of water quality




   standards and use designations.




   6.  We need a policy which ensures consistency in establishing water




   quality standards between EPA Regions and States while allowing enough




   flexibility for recognizing the uniqueness  of water quality requiements




   from Region to Region.




B.  Wasteload Allocation Issues




   1.  There is  need for simplified procedures for the adopting, approval,




   or disapproval of wasteload allocations.
                           28

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   2.   Clear and concise guidelines need to address water quality modeling




   techniques to include:




      a.   A clear understanding of what water quality models can and




      cannot do.




      b.   How to apply modeling results for conversion to effluent




      limitations.




      c.   Reevaluation of critical low flow as a base line in all cases.




      d.   Guidelines for defining




         1)  Conditions under which simplified water quality analysis




         techniques can be justified.




         2)  Requirements of model calibration and verification.




         3)  Transferability of water quality analysis from one receiving




         water to another based on similar characteristics.




      e.   Methods for taking into account other source contributors




      including nonpoint source, combined sewer overflow, and industrial.




      These need to be evaluated both seperately and collectively to




      determine major source of impact.




      f.   Methods for determining toxic pollution impacts.




C.   General Issues




   1.   We must address the use of flow maintenance to meet standards.




   2.   We need a mixing zone policy.




   3.   We need to relook at the antidegradation policy and possibly revise




   it.  At the same time we need methods for implementing that policy.




   4.   We should expand the use designation and classification scheme




   to  include wetlands
                            29

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        5.  We need to recognize the difference and values of intermittent



        streams and continuous flowing streams and apply policies and guidance



        accordingly.



     The practical significance of these issues is to avoid individual project



situations such as:



     Where a small community served by an existing lagoon several miles up-
                              y


stream of a lake proposes land application or chemical treatment solely



because the lagoon discharge does not meet an imposed phosphorus limit.



However, there are no studies to document the significance of the point



source discharge versus the nonpoint contribution or to suggest what benefit,



if any, might be achieved by controlling the point source phosphorus con-



tribution.



     Then there is the situation where a community is required to have an AWT



process to meet water quality standards when the receiving stream is chan-



nelized or channelization is proposed.  Channelization has probably had a



greater adverse impact on that stream ecology than could be offset by any



benefits gained by applying AWT.



     Another situation would be where a community would propose the use of a



tertiary sand filter following an existing secondary treatment process to meet



effluent limits of 15/20 EOD/SS.  What is lacking is a good evaluation of the



technical capabilities of the existing facility through fine tuning and improved



operations and maintenance.



     From an administrative standpoint, economics is the limiting factor for



attaining water quality and the focal point for the AWT controversy.  However,



if we at State and Federal levels can logically see the whole picture rather



than just parts and address and make decisions for the issues at hand, we will
                                 30

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probably find that there are many more cost effective approaches to meeting




the goals of water quality than we have realized.   It is the responsibility




of the State and Federal Agencies to act or we will surely jeopardize the




support of the Public and Congress for meeting the goals and programs of the




Clean Water Act.
                                   31

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                 FEDERAL POLICY ON FLOODPLAIN/WETLAND REGULATION




                                          by




                                     Ron Mustard







Federal Regulation of Wetland or Floodplain use is restricted to specific projects




that fall within the scope of regulatory or financial assistance programs admini-




stered by the various federal agencies.  Under these programs, the use of wetlands




or floodplains for development was, in the past, reviewed in the context of poli-




cies adopted by each individual- agency.  These policies were, as a rule, derived




independently from one another.  In spite of their independent origins, these




policies were, for the most part, similar in that they expressed the concerns then




current in the scientific community.  However, there was a wide degree of variance




in the manner in which these policies were applied, and as a consequence, there




was a great deal of confusion about the extent of the Federal Government's Com-




mitment to the concept of Wetland and Floodplain Regulation.






In order to establish a true national policy, and to encourage a more uniform and




active application of that policy, President Carter, on May 24, 1977, issued




executive orders 11988 on Floodplain Management and 11990 on Protection of Wet-




lands .






Executive order 11988 Established, as a Policy, that:




     "Each agency shall provide leadership and shall take action to reduce the




rick of flood loss, to minimize the impact of floods on human safety, health and




welfare, and to restore and preserve the natural and beneficial values served by




floodplains in carrying out its responsibilities for (1) acquiring, managing, and




disposing of federal lands and facilities; (2) providing federally undertaken,




financed, or assisted construction and improvements; and (3) conducting federal




activities and programs affecting land use, including but not limited to water





                                      33

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and related land resources planning, regulating, and licensing activities."






In carrying out this policy, each agency has a responsibility to identify pro-




jects with potential floodplain impacts, consider alternatives that would eli-




minate or minimize any  adverse impacts, and to provide opportunities for public




involvement in the process.






As instructed, the water resources council issued guidance on implementation




of the executive order on October 1, 1977.  Since then, all other federal agen-




cies have completed, or are in the process of completing, ammendments to their




regulations or operating procedures that will ensure compliance with the executive




order.






In language almost indentical to that used in the Floodplain Executive order,




Executive order 11990Established as a policy that:




     "Each agency ahall provide leadership and shall take action to minimize the




destruction, loss or degradation of wetlands, and to preserve and enhance the




natural and beneficial values of wetlands in carrying out the agencie's respon-




sibilities..."






The one exemption to the applicability of this policy is to the issuance by




federal agencies of permits, licenses, or allocations to private parties for




activities involving wetlands on non-federal property.  However, the programs




affected by this exemption all have strong wetland protection provisions in




their own right, and so, in practice, there is no discontinuity in the federal




response to proposed activities in wetlands.






In carrying out the policy established by executive order 11990, each agency
                                      34

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has a responibility to avoid unnecessary construction in wetlands, and to mini-




mize the impact of those activities that are necessary.  Each agency must also




provide for early public review of actions affecting wetlands.  Most federal




agencies amended their regulations or procedures to ensure compliance with this




executive order concurrently with the amendments undertaken for executive order




11988.






From the viewpoint of the general public, the most significant aspect of this




process is the requirement that federal agencies document the steps that have




been taken to comply with the requirements of the executive orders.  When a




proposed action will impact a floodplain or wetland area, the sponsoring agency




must clearly demonstrate that (1) there is no practicable alternative to the




proposed action, and (2) that the proposed action includes all particable mea-




sures to minimize harm to the affected resources.  By requiring that agency




compliance with the policies established by the executive orders be specifically




addressed and entered into the public records, interested parties are given ad-




ditional opportunity to review agency actions and to challenge decisions on the




grounds of erroneous application of policy.  This ability alone will encourage




federal agencies to•ensure that their decisions are based upon careful con-




sideration of all available information, and are arrived at in a consistant man-




ner.
                                     35

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       UNITED STATES-CANADA GREAT LAKES WATER QUALITY AGREEMENT —

                          IMPACT ON U.S. POLICY

                                    by

                           Kenneth  H. Walker*
    The quality of  the water  in  the Great Lakes  has  been  a matter  of
concern for many decades.   Intermittently since  1912,  the Inter-
national Joint Commission has undertaken investigations to determine
the extent of pollution  and degradation of  this  irreplaceable  resource,

    In 1964, the IJC was formally  asked by  the Governments of  the
United States and Canada, pursuant to  the Boundary Waters Treaty of
1909, to investigate Lake Ontario, Lake Erie  and the International
Section of the St.  Lawrence River  to determine the extent of inter-
national pollution, identify  the sources, recommend  remedial measures,
and estimate probable costs to carry out such programs.

    The IJC report  on the lower  lakes  was completed  and presented  to
the Governments in  1970.  It  represented a  combined  effort by  experts
drawn from the federal governments of  the two countries,  the Province
of Ontario, and the eight Great Lakes  states  —  New  York,
Pennsylvania, Ohio, Indiana, Michigan, Illinois, Minnesota, and
Wisconsin.  These experts served on the Boards and Committees  which
carried out the necessary scientific and field studies to enable them
to advise the Commission on the seriousness of the pollution problems
in the lower lakes.

    The Commission's report provided a detailed  assessment of  the
water quality and made comprehensive recommendations for  action by the
Governments of Canada and the United States.  One outcome of this
report was the Great Lakes Water Quality Agreement which  was signed on
April 15, 1972.

    In this Agreement, the two countries stated  their determination to
restore and enhance the water quality  in the Great Lakes  System.  They
were convinced that the best means to  achieve improved water quality
in the System was through the adoption of I common objectives, the
development and implementation of cooperative programs and other
measures, and the assignment of special responsibilities  and functions
to the International Joint Commission.

    The Agreement is unique in that while recognizing the rights of
each country in the use of the Great Lakes  and reaffirming the
obligation not to pollute,  it expressed the determination of each
country to restore and enhance the water quality.  Water  quality
objectives were enumerated.  Programs  and other measures  to achieve
the objectives were identified and were to  be completed or in  the
*Great Lakes Regional Office, International Joint Commission, Windsor,
 Ontario.

                               37

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process of implementation by December  31,  1975.  Additional  powers  and
responsibilities were given to the International Joint  Commission,
including:  collation, analysis, and dissemination  of data relating to
water quality, pollution, water quality objectives,  and effectiveness
of programs; tendering advice and recommendations to the Parties  and
to state and provincial governments; provision of assistance  in
coordination of joint activities and Great Lakes water  quality
research; and reporting at least annually  to the Governments  and  to
the state and provincial governments on progress toward the  achieve-
ment of the water quality objectives.

    The 1972 Agreement set into motion three major  activities:   (1)
the study of water quality of the Upper Lakes; (2)  the  study  of
pollution from land use activities in  the Great Lakes Basin;  and  (3)
the implementation of remedial measures to mitigate  pollution from
point sources.  These activities required  the interaction of  federal,
state, provincial, and non-government  officials.

    The 1972 Agreement also provided that a comprehensive review  of
its operation and effectiveness should be conducted  by  the Parties
during the fifth year after its coming into force.   This review was
carried out and resulted in the Great  Lakes Water Quality Agreement of
1978 which was signed by the two countries on November  22, 1978.

    The new Agreement reaffirmed the determination  of Canada  and  the
United States to restore and enhance the water quality  of the Great
Lakes System.  While the new Agreement continued many of the
provisions of the 1972 Agreement, it also provided  new  directions for
many of the activities, based on experience gained  from the  former
Agreement.

    The impact of the Agreement on policies and programs in  the United
States is extensive.  This is evident  from the commitment made in
Article II of the Agreement which states the purpose as  follows:

         The purpose of the Parties is to restore and main-
    tain the chemical, physical and biological integrity of
    the waters of the Great Lakes Basin Ecosystem.   In  order
    to achieve this purpose, the Parties agree to make  a
    maximum effort to develop programs, practices and tech-
    nology necessary for a better understanding of  the  Great
    Lakes Basin Ecosystem and to eliminate or reduce to  the
    maximum extent practicable the discharge of pollutants
    into the Great Lakes System.

         Consistent with the provisions of this Agreement, it
    is the policy of the Parties that:

    (a)  The discharge of toxic substances in toxic  amounts
         be prohibited and the discharge of any or  all
         persistent toxic substances be virtually eliminated;

    (b)  Financial assistance to construct publicly  owned
         waste treatment works be provided by a combination
         of local, state, provincial,  and federal participa-
         tion; and

                                 38

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    (c)  Coordinated planning processes and best management
         practices be developed and implemented by the
         respective jurisdictions to ensure adequate control
         of all sources of pollutants.

    There is a wide range of programs established by the Agreement,
many requiring action by specific dates.  The Agreement establishes
two Boards, a Great Lakes Water Quality Board and a Great Lakes
Science Advisory Board, to assist the Commission in the exercise of
the powers and responsibilities assigned to it under the Agreement.
It also calls for a Great Lakes Regional Office of the International
Joint Commission to provide administrative support and technical
assistance to the two Boards, and to provide a public information
service for the programs, including public hearings, undertaken by the
Commission and the Boards.

    The Agreement has an effect on the policies and programs of the
Federal Government as well as those in the states.  In addition to a
commitment by the Parties to support the many provisions of the
Agreement, in Article XI, the Parties specifically commit themselves
to seek:

    —   The appropriation of the funds required to implement the
         Agreement;

    —   The enactment of any additional legislation that may be
         necessary to implement the programs and other measures
         provided for in Article VI; and

         The cooperation of the State and Provincial Governments in
         all matters related to the Agreement.

    A review of the Agreement indicates that it specifically addresses
such topics as:  general and specific water quality objectives; water
quality standards; pollution from municipal and industrial sources;
eutrophication; pollution from agricultural, forestry and other land
use activities; pollution from shipping activities; pollution from
dredging activities; spills of oil and hazardous polluting substances;
hazardous polluting and persistent toxic substances; airborne
contaminants; and vessel wastes.

    These provisions impact on U.S. programs involving construction
grants, enforcement, NPDES permits, water quality standards, phos-
phorus control and removal, control of toxics, urban drainage, and
point and nonpoint sources of pollution.

    The Water Quality Board and the Science Advisory Board provide
additional opportunities for interrelationships between the United
States and Canada and between the federal, state, and provincial
governments.  The Water Quality Board was established as the principal
advisor to the Commission with regard to the exercise of all the
functions, powers and responsibilities assigned to the Commission
under the Agreement, except for those assigned to the Science Advisory
Board.  The Board has 18 members, nine from the United States and nine
from Canada.  Each of the eight Great Lakes states is represented by a


                                  39

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senior official of the state agency with environmental responsibility.
The United States federal government is represented by the Regional
Administrator of EPA Region V who is also the United States Cochairman
of the Board.

    This arrangement permits a beneficial exchange of advice on
programs and problems to take place between the Parties, the IJC, the
Board and the states and EPA.  Programs which are recommended  to  the
Commission are frequently implemented by the state members of  the
Board even before the recommendation is officially transmitted through
the Parties back to the state agencies.

    The Science Advisory Board structure differs radically from that
of the Water Quality Board.  Its membership contains federal,  state,
and provincial representation, but also draws its membership from
industry, university, and public environmental groups.  The Board is
the scientific advisor to the IJC and the Water Quality Board.  The
Board has 16 members plus two ex-officio members who represent the
International Association for Great Lakes Research and the Great  Lakes
Fishery Commission.  The U.S. Cochairman is associated with the U.S.
EPA Water Quality Laboratory at Duluth.

    Both of these Boards have supporting committees, work groups, and
task forces which provide additional input into the many Agreement
programs.  These organizations result in participation by over 216
people in intermediate and  senior professional and administrative
positions who serve a liaison role in impacting Agreement programs as
well as those of the organizations they represent.  This involvement
in the Agreement functions  represents a tremendous investment  of
manpower in both countries  and provides for an exchange of ideas  and
information among all the jurisdictions and organizations
participating.

    Time does not permit an examination of all the programs being
carried out under the Agreement.  I would  like to explore briefly two
of these programs — the water quality objectives and  their  impact on
water quality  standards, and the  significance of  the phosphorus
control programs.

    Water quality objectives were considered  the  foundation  for
achieving improved water quality  in  the Great Lakes  System  in  both  the
1972 and the  1978 Agreements.  The  concept of using water quality
objectives  as  guidelines for preserving or restoring the water quality
in the  lakes  is  one  of  long standing  for  the  IJC.  These  objectives
are goals to  be  maintained  and achieved in the boundary waters through
effective pollution  control programs  in both  countries.

    Article V (1)  in  the Agreement  states:   "Water  quality  standards
and other regulatory  requirements  of  the  Parties  shall be  consistent
with  the achievement  of  the General  and  Specific  Objectives.   The
Parties  shall  use  their  best efforts  to  ensure  that  water  quality
standards  and other  regulatory  requirements  of  the  state  and
provincial  governments  shall similarly be consistent with the
achievement of these  Objectives".
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    The  1978 Water Quality Agreement  contains  41  specific  water
quality  objectives.   These are  constantly  being reviewed by the
Aquatic  Ecosystem Objectives  Committee  of  the  Science  Advisory Board.
The Committee  is also developing  new  objectives on many problem
substances.

    At the request of the Water Quality Board, the Regional Office
just recently  completed a report  on "A  Review  of  the Impact of Water
Quality  Agreement Objectives  on Water Quality  Standards".   The purpose
of the review  was to  determine  if the Agreement Water  Quality
Objectives had been used by the jurisdictions  in  developing their
water quality  standards and if  not, why not?

    The  conclusion of the review  was  that  the  Agreement Objectives
have had a decided impact on  the  water  quality standards and
objectives adopted by the jurisdictions.

    For  example, New  York State has established a classification  of
Class A-Special for the International Boundary Waters.  In Ohio,  70
percent  of the values in the  water quality standards for 33 parameters
are equal  to or more  stringent  than the Agreement Objectives.   In
Pennsylvania for 30 parameters, 63 percent of  the state values are
equal to or more stringent than the Agreement  Objectives.

    Some jurisdiction have related their programs to the Agreement
more than  others.  In some states, the  last revision made  to their
standards  preceeded the 1978  Agreement  and therefore do not reflect
those objectives.  The revisions  now  under consideration will
recognize  the  Agreement and the objectives to  a greater extent.

    One  of the major  programs established  by the  Agreement is  the
control  of phosphorus to minimize  eutrophication  problems  and  to
prevent  degradation resulting from discharges  of  phosphorus to the
lake system.   Annex 3 of the  Agreement  deals with the  control  of
phosphorus.  Among other provisions,  the Annex establishes phosphorus
loads for  the  base year (1976)  and future  phosphorus loads.   It calls
for the  Parties, in cooperation with  the State and Provincial
Governments, to confirm the future phosphorus  loads and establish load
allocations and compliance schedules  within 18 months  after the
Agreement  is signed.   This date was passed last May and the Parties
have not yet established the  load  allocations  as  required.   However,
extensive discussions  are being carried  out. between the two countries
on this  matter.

    Another important  requirement  in  this  section on phosphorus
control  is that municipal waste treatment  plants  discharging more than
3,800 cu m/d (1.0 MGD) shall  achieve  effluent  concentrations of 1.0
mg/L total phosphorus  maximum for plants in the basins of  Lakes
Superior, Michigan and Huron  and  0.5  mg/L  total phosphorus  maximum for
plants in the  basins  of Lake  Ontario  and Lake  Erie where necessary to
meet the loading allocations  or to meet  local  conditions whichever are
more stringent.
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    The Annex also calls for a reduction of phosphorus in household
detergents to 0.5 percent by weight where necessary to meet the
loading allocations or to meet local conditions whichever are more
stringent.  All the Great Lakes states except Ohio, Pennsylvania and
Illinois have now instituted bans on phosphorus in detergents.  In
Ohio and Illinois, the Cities of Akron and Chicago, respectively, have
limited the phosphorus in detergents.

    The Agreement establishes two additional deadlines which will have
an effect on programs in the U.S.  Article VI calls for programs for
municipal sewage treatment facilities to be completed and in operation
no later than December 31, 1982.  Programs for the abatement, control
and prevention of pollution from industrial sources are to be
completed and in operation no later than December 31, 1983.

    Based on this brief review of some of the Great Lakes Water
Quality Agreement requirements, one can conclude that the Agreement
has had a decided impact on policy and programs in the United States
portion of the Basin and will continue to do so.  The Agreement has
been a positive factor in cleaning up the Great Lakes.  We have not
yet reached the point where we can sit back and congratulate ourselves
on completing the restoration and enhancement of the water quality in
the Great Lakes System.  However, we are making progress and every
effort, including the output from seminars such as the one we are
participating in here, moves us a little further down the road  towards
our goal of an improved Great Lakes System.
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                  State/EPA Agreements;  A State/Federal Partnership

                         by    David Stringham
Getting the EPA Region V Office and its State counterparts to agree on priority
environmental problems and ways to solve them is the objective of our new
planning process—the State/EPA Agreements.  The goals of the Agreement planning
process are:  (1) to make the  Federal and State governments partners in determining
priorities for State and Federal funding assistance and technical assistance;
(2) to bring important environmental problems to the attention of senior management
at both the Federal and State  agencies; and (3) to surface environmental  problems
that might not be covered by any individual environmental program and that may
demand a creative mixing of funds from a number of programs.  In addition, we
expect the Agreements, properly drafted in understandable English, to be an
important vehicle for communicating the direction of EPA and State programs to the
public.

The Agreements influence how environmental problems are addressed because they have
a direct bearing on how EPA and the States allocate millions of dollars to various
aspects of their environmental programs.  The major programs included in this year's
State/EPA Agreements cover a range of activities authorized by Federal  statutes,
including The Clean Water Act, The Safe Drinking Water Act, The Clean Air Act, The
Resource Conservation and Recovery Act, and The Toxic Substances Control  Act.

For the 1980 fiscal year, our first full year with this process, Agreements have.
been completed in all six Midwest States,  Implementation of SEA provisions, while
admittedly mixed, is generally proceeding.  Development of the FY 81  Agreements
began late last winter.  The process begins with each State and Region  V developing
their own list of environmental problems and priorities, air quality, water quality,
and solid and hazardous waste  are all considered.  And though there are many
different kinds of problems in each, the Agreement process usually identifies
a total of only a dozen or so of the most important issues for special  attention.
These issues range from concern over a particular type of pollutant to  concern
about a particular stretch of  river.  The lack of  pretreatment for industrial
wastewater or the need for programs to control pollution caused by farming
practices are examples.  In addition, the Agreements note significant program
operation problems, such as State/EPA work sharing or delegations oversight, needing
special study.

Once EPA and the States develop lists of these issues independently,  they meet to
resolve differences.   The next step then is to work out the general  solutions for
each issue.   The solutions usually relate to improved implementation  of EPA and
State environmental  protection programs.

In FY 1980 only one State in Region V, Michigan, had a specific Great Lakes issue
in its SEA and  received Great Lakes funding to conduct Great Lakes surveillance.
This activity included:  nearshore studies on  Lake St.  Claire,  Thunder  Bay,
St.  Ignace and  Cheboygan; Great Lakes loading  flow analysis and water intake studies;
and a salmon residue  monitoring program.

FY 1981 will  see three States (Michigan, Indiana and Ohio)  with Great Lakes SEA
issues.  An  additional  State, New York, may also develop a  Great Lakes  SEA
highlight in connection with a special  regulatory assessment and broad  scale
intensive survey of the Niagara River in New York.   Both the draft Indiana and Ohio
State EPA Agreements  focus attention on special  problems in nearshore areas of the
Great Lakes—estuaries, harbors and beaches which are seriously degraded  due to
combinations of point and nonpoint pollution.   These degraded waters, while small

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in relationship to the  total  lake  system,  are  a  portion of  the Great  Lakes  seen
and used by millions  of people.  The municipal,  industrial  and storm  runoff
loading concentrated  in these areas and  some upstream  urban industrial  areas
impact both local  use and the lakes as a whole and are a  logical  focus  for  control
efforts.

Industry has been  required to expend large amounts of  money for waste treatment
in these nearshore areas.  Also, large amounts of local,  State and  Federal  funds
have been expended in constructing municipal treatment works, and far more  funding
is being planned for  both treatment works  and  control  of  combined sewer systems.
Additionally, programs  for the control of  urban  storm  runoff are  being  developed
in an attempt to deal with pollutants  in urban storm water.  These  efforts  in  the
past have been  oriented toward conventional pollutant control, but our activity
under the SEA Agreements will also heavily emphasize control of toxic pollutants.

The benefit of these  past efforts, in  terms of impact  on  estuary  and  nearshore
areas, is not well known.  Conversely, it  frequently is not known what  controls
are needed to reach various levels of  ambient  water quality.  These problems exist
elsewhere on river systems but are less  critical than  in  harbor and estuary
localities.  Because  of the hydrologic complexity of estuaries, the Great Lakes
relatively long retention time, and the  intense  use for water supply  and recreation
associated with these water bodies, information  needs  for regulatory  efforts tend
to be greater in these  locations.  At  the  same time, many of these  areas have
already received extensive investigation,  making considerable regulatory progress
possible.

The focus of our initiative in the Ohio  and Indiana SEA's will be in  the vicinity
of the Urban/Industrial Gary-Indiana  Harbor and  the Toledo, Greater Cleveland
and Ashtabula areas.  The specific goals of these Urban-Industrial  elements of
the Agreements are to control pollution  in Lake  Michigan  and Lake Erie; to  protect
and enhance drinking  water, recreation,  commercial  and aesthetic  uses of these
waters; and to slow the eutrophication processes in the Great Lakes.

Initial sections in these SEA's summarize  these  specific  goals and  spell out
agreement on the priority problems as  perceived  by  the public, the  State, and  the
Federal government.  These initial sections are  followed  by a so-called "Problem
Solving Approach" (or PSA) that lays  out the key steps for  attaining  the jointly
perceived goals.  In both the Ohio and Indiana Great  Lakes  elements the first
step  toward solving the problem is to be a joint State-Federal review of all  avail-
able  information about the problem area; and this may  provide a  basis for immediate
implementation of remedial programs.   This initial  information base,  can also  serve
as a  basis for development of a pollution  control  strategy  which, when  combined
with  other activities to further define,the extent  and nature of the  problems, will
provide both the State and the Federal  government with the  basis  for  further remedial
program efforts as needed.

Key steps  in the supplementary assessment work will  be fish flesh and sediment
analysis for toxic contaminants, review of combined sewer overflow studies  and
the conditions around major  storm sewer outfalls,  location  and  evaluation of
major nonpoint sources of pollution (such as pits,  ponds, lagoons and landfills),
and process assessment of relevant industrial  dischargers.   Other data to be
reviewed will relate to  drinking water  taste and odor problems,  swimming bans
and beach  closings,  fish consumption warnings, incidents  of gross pollution,
recent performance of  sewage treatment  plants that discharge in these areas, and
major industrial  discharger  permit compliance.

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The final steps to address these Urban-Industrial Great Lakes issues focus on
performance of needed regulatory actions.  Among the actions expected in this
phase of the joint effort may be the evaluation of existing pretreatment and/or
sewer use ordinances as administered by local  sewage treatment plants, designation
of plan of study areas for development of regional sludge management plans,
development of plans to accelerate sewage treatment plant improvements, preparation
of a management plan for any in-place pollutants; development of pretreatment
and permit revisions and identification of necessary enforcement actions.

In response to national priorities and in recognition of the particular environ-
mental needs of the State of Ohio a second Great Lakes highlight element was
negotiated to promote control of phosphorus in Lake Erie, where the natural
ecosystem and the fishery supported by it have been disrupted by accelerated
eutrophication.  The discussion of phosphorus* induced problems in the Agreement
provides basis for the detailed objectives which are:  (1) that Ohio's industrial
dischargers attain maximum practicable reduction of phosphorus discharges  to
Lake Erie; (2) that Ohio's municipal dischargers attain effluent phosphorus limits
of 1 mg/1 for all plants discharging more than one million gallons per day,
(3) that Ohio's detergent phosphate limits be  reviewed in the light of Federal
evaluation of OEPA cost-benefit data and any applicable resolutions of the
U.S.-Canada Water Quality Board, and (4) control of agricultural  nonpoint  source
pollution through implementation of agricultural best management practices.

The problem solving measures for this phosphorus control  issue include review of
and high priority attention on municipal and industrial phosphorus dischargers  to
assure early compliance and an effective follow-up strategy for permit violators,
development of a method and schedule for periodic updating of the Great Lakes
phosphorus compliance and municipal point source loading  reports, and an exchange
of critiques between OEPA and USEPA about OEPA phosphate  detergent ban cost-benefit
data.  This Agreement includes a commitment from USEPA for financial  support for
two agricultural nonpoint source control projects on streams tributary to  the
western basin of Lake Erie, and a commitment from OEPA to participate in the
activities of the U.S.-Canada Water Quality Board and the IJC Great Lakes
Phosphorus Management Task Force.

The Michigan EPA Agreement will include two unique Great  Lakes issues for  the
coming year.   The first, named the Multimedia  Monitoring  Highlight, relates to
the fact that additional data and monitoring needs required for dealing with toxic
and hazardous materials will strain the State  monitoring  budget.

In an effort to more effectively utilize the limited State resources, the  Michigan
Department of Natural Resources and USEPA will  coordinate and evaluate monitoring
activities of all media in a selected problem  area.   The  goal  of this multimedia
monitoring activity is  not only improved monitoring  efficiency, the State  and
USEPA also hope that the new monitoring initiative will provide a more complete
environmental picture of a selected geographic area, so that a more balanced
response will be available from environmental  managers in remedying problems,
and citizens affected by environmental  problems might be  given a  better chance
to appreciate the scope of the problems under  consideration by environmental
agencies.

The work elements associated with this  highlight include  identification of the
geographic area for the study, a review of scheduled monitoring programs in the
area, specification of  monitoring or inspection data needed to identify inter-
related air,  water and  solid waste pollution problems, development of a study
plan, compilation of information from monitoring and study efforts, and identification

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of air, water and solid waste pollution  relationships.   Preliminary  conclusions
and recommendations will  be circulated among  State  and  Federal  program managers
and the published report on the outcome  of the monitoring  study will  be available
to the public.  A final  work element in the PSA calls  for development of remedial
measures to correct identified environmental  problems.

The second Great Lakes  Highlight in the  Michigan/EPA  Agreement  evolved from the
recognition that open waters of the Great Lakes still  receive unacceptable
loadings of numerous pollutants and that some nearshore, estuary and bay areas
in the State waters have been degraded with loss of beneficial  uses  due to intense
loadings  and limited dilutions.  The Agreement proposes that concentrating efforts
on these nearshore areas offers the opportunity to  restore beneficial  uses in
these localities and to reduce major Toadings which now enter the Great Lakes.
The goal of the work effort is to develop an integrated management system for
implementing planning,  remedial and monitoring programs to protect the Michigan
waters of the Great Lakes.

Key elements in the problem-solving approach are a  definition of common water
quality objectives; case study analyses  of problem  areas which  have been success-
fully addressed, as well as those which  presently do not meet the agreed upon
objectives; and identification and definition of appropriate monitoring programs.

In all of these State/EPA Agreements specific tasks are assigned to the State
and Federal partners, milestone schedules are established, and  funding and
responsible party assignments  are settled.  The FY 81  SEA documents have
been under review by appropriate State and Federal  agency  personnel, as well as
the public.  Final revisions, of the FY 81 draft documents  are underway, and EPA
expects that signing of these final documents by John McGuire,  the EPA Regional
Administrator, and the heads of the respective State environmental agencies will
be completed by the first of October, the beginning the next fiscal  year.

The purposes and uses of these State/EPA Agreements are ambitious.  The Agreements
are intended to be a decision document,  a management tool, and  a communications
device.  Their immediate purposes are to focus the attention of top officials
on integrated program management, to identify high priority environmental issues,
to guide the grants distribution process, to focus attention on tracking progress
toward  solving identified problems, and to inform the interested public and
agencies.  The implementation of the process will identify opportunities for
useful  reform in overall environmental program management.  This, in turn, should
result  in  the faster attainment of our environmental  objectives and assure our
goals  for  protection and improvement of our priceless heritage—The Great Lakes.
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           WATER QUALITY MANAGEMENT PLANS,  STATUS,

           QUALITY, INTEGRATION AND IMPLEMENTATION

                             by


                      William G. Benjey*
Good morning.  [As mentioned] I am Bill Benjey of  the  USEPA
Ohio Water Quality Management Section.  My purpose  today
is to give you an overview of the status and  implementation
of water quality management  (WQM) plans.  I would  also like
to discuss the need for emphasis on a balanced approach to
point and nonpoint water pollution abatement.  There are  220
WQM planning agencies nationwide and 37 within Region  V,  of
which 194 nationally, and 33 within the Region, are at least
conditionally approved, including the nonpoint pollution
portions.  Rather than regale you with statistics,  I will
restrict my observations to my perspective on Region v.   The
degree of specificity of WQM plans in identifying  and  ad-
dressing water quality problems is highly variable.  In many
cases point source based problems and recommended  solutions
are detailed (or discharge specific) relative to treatment
of nonpoint sources (which are often generalized to the level
of the State or a regional drainage basin comprising one-
quarter to one-third of the State).  The focus upon point
sources of water pollution under the water quality manage-
ment program dates from the designation of the original
urban-industrial complex planning areas in 1974 and 1975.
This is not too difficult to understand, given the  legal
priority then required for the immediate issuance  of NPDES
permits for point source dischargers, and the widespread
public awareness of flagrant and dramatic examples  of  point
source caused problems.  Consequently, much of the  emphasis
of the water quality management plans now approved  is  upon
point sources.


     However, as you know, during the past three years the
emphasis has shifted dramatically to nonpoint source pollu-
tion abatement planning and  implementation, as reflected  in
the fact that section 208 funds can no longer be used  for
point source work.  The rationale is that much of  the
initial point source planning work should be  accomplished
(although I will be the first to say much remains  to be
done), and that the benefits to be derived from reducing
pollution from diffuse sources have been relatively ignored.
*Supervisory Environmental Protection Specialist, United
States Environmental Protection Agency, Region V, Chicago,
Illinois
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     We have arrived at a point where  in  general,  point
source problems are usually known  and  addressed  with NPDES
permits and/or the section 201 municipal  construction
grants programs; while most of the nonpoint  problems are
known only in gross terms (for example, estimates  of sedi-
ment and phosphorus from the Maumee River  to Lake  Erie).
There are exceptions to this rule, such as the remaining
need for sound wasteload allocations and  for implementation
of industrial pretreatment to control  point  source  effluent
limitations.  There are also a limited number of detailed
nonpoint pollution control studies under  the National Urban
Runoff Program (NURP) and the testing  of  agricultural best
management practices (BMPs) in special studies such as Black
Creek in Indiana, Honey Creek in Ohio  and  the Red  Clay
Project in Wisconsin.  However, the results  are  not in from
the NURP projects, 6 of which are  in Region  V, and  the Rural
Clean Water Program (RCWP) and the new Agricultural Conserva-
tion Programs.  There are 3 RCWP's in  Region V,  including
Highland-Silver Lake, Illinois; Lower  Manitowoc, Wisconsin;
and Saline Valley, Michigan.

     A coordinated and integrated  approach to point source
and nonpoint source related aspects of pollution problems
in specific areas is one of the primary features missing
from current WQM plans.  We are all aware  of the uneven
and variable mix of water quality  problems;  urban,  construc-
tion and agricultrual runoff, feedlots, malfunctioning
septic tanks and package plants, and overloaded  and
inadequate municipal and industrial wastewater treatment
facilities.  Point sources are more easily addressed,  but
in many cases, a water quality problem has multiple causes.
Consequently, focusing only on point sources will  not
guarantee attainment of the 1983 goals of  the Clean Water
Act, particularly when the parameters  accumulate,  such as
phosphorus, heavy metals or toxic  chemicals.  It is at least
highly embarrasing to build an elaborate  treatment  plant
only to find that you have not significantly helped the
problem.  This is one reason for the AST/AWT reviews
discussed earlier by Mr. Chaiken.

     The lack of coordinated approaches can  be remedied by
taking all present pollution sources into  account  when
devising geographic priorities for future  study  and imple-
mentation.  Priorities recognize limited  resources.   By this
time, priorities should also be highly area  specific,  that
is, to the sub-basin level, and as problem specific as
possible.  In priority order, specific, tailored work plans
for additional refinement of problem identification and
implementation can be prepared for the sub-basins.   Only  in
this manner will we be able to successfully  approach the
problems of each area.  In any event,  it  is  inefficient to
attempt to implement structural or nonstructural abatement
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methods across the countryside regardless  of  the  variable
locations and magnitudes of the problems.   In most  cases
more detailed work is needed to pin down  che  actual,  as
opposed to broadly defined "potential" problems.

     The above process ought to be a part  of  an overall
State strategy for addressing priority water  quality
problems.  Often, States work upon-strategies which include
a section for point sources, and sections  for agricultural
nonpoint and urban nonpoint sources, etc.   In addition,
States have classified stream segments as  effluent  limited
or water quality limited based upon whether or not  advanced
treatment of point source discharges is needed to meet water
quality standards.  All of these parts of  the whole should
be considered when setting forth specific  priorities.

     Making a joint priority system requires  drawing  together
planning for programs which operate on vastly different fund-
ing and at different speeds.  Obviously the municipal con-
struction grants program has resources to  move much more
quickly than nonpoint pollution abatement.  Yet,  nonpoint
"tradeoffs" are supposed to be considered  in  construction
grants facilities planning.  In order to set  overall  State
priorities by sub-basins, any known characterization  of non-
point pollution problems in a given sub-basin could be made
a part of the "severity of problem" and other factors of the
municipal construction grants priority list prepared  by the
States.  Alternatively, a separate ranking  system could be
established into which the municipal construction grant
priorities feed.  Because of the need for  cooperation of
various agencies (agricultural, health, etc,), it is  advisable
to have their input on the problems with which they are most
familiar.

     Region V states have or are developing Statewide agri-
cultural strategies, often around the State sediment  control
laws, and groundwater strategies.  Groundwater quality, of
course, is affected by surface water pollution.   Statewide
problem area priorities are in different stages of  develop-
ment, with Wisconsin the most advanced at  this time in this
Region.  However, they are not yet integrated strategies.

     Current prototype nonpoint pollution  projects  a~*e, of
course, limited in geographic coverage.  The  question arises;
how can we get effective nonpoint pollution abatement with so
much area, and so little money available?   Here again, a State
strategy is important.  The immediate reaction is often to
propose additional Federal, State or local  funding, or all
of the above, usually as some variety of a  cost-sharing program,
such as in Wisconsin and Illinois.  This is certainly a valid
approach.  However, we all know that the prospects  of expanding
limited sources of money from any level of  government in the
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current economic situation  is  not  good.   Additional  regula-
tions may help  In some circumstances.   However,  they too
often prove unwhieldy as well  as locally  unwelcome  in deal-
ing with nonpoint problems.  Most  States  have  a  sediment
control law as  a basis, in  any event.   Our  next  tactic must
be to selectively work upon nonpoint problems  in order of
the degree of severity of the  water pollution  problem to
which they contribute, in accordance also with overall sub-
basin priorities.   Even so, it is  necessary to pool  the
resources of all State, Federal and local agencies,  in order
to concentrate  upon specific,  identified  areas with  water
quality problems.   For example, a  water quality  management
plan may place  a priority order upon sub-basins  with water
quality problems largely induced by agricultural runoff.  In
this event, USEPA,  the U.S. Department  of Agriculture and
the State water quality and agricultural  agencies should
cooperate in focusing their water  quality efforts and funds
upon the sub-basins in priority sequence.   Their actions must
be in cooperation with each other  and the local  landowners
through the designated management  agency  (often  a soil and
water conservation district).   If  septic  tanks are a problem,
a health department may be  involved.  There will usually be
several actors  involved.

     The primary intermediate  water quality problem  objective
which is heard  incessantly  is  implementation,  improved water
quality of course being the final  objective.   Implementation
requires more than just a concerted effort  by  agencies,  as
we all know.  In agriculture,  landowners  and soil and water
districts must  see the specific water quality  problem and
the benefit of  BMPs and cleaner water for themselves.   In
addition to demonstrating the  general value of soil  and
nutrient retention, it is important to demonstrate the
presence of problems and importance of water quality in  a
specific area,  in order that water quality  be  made signifi-
cant and tangible to landowners.   Cities  and counties must
see the importance of clean and abundant  water in relation-
ship to their current and future needs  in water  supply and
recreation.  This again ties in with the  need  to concentrate
on specific, known, high priority  problem areas.  It is  also
increasingly important that the State and areawide water
quality agencies provide necessary data to  the designated
management agencies to assist  and  document  implementation
of BMPs and the effects on water quality.   This  represents
a change in role from the initial  days of water  quality
planning, when  local agencies  provided  information to State
and areawide agencies to demonstrate perceived problems.

     I have mentioned five  items which are  complementary
approaches to water quality abatement.  They are: (1)
following integrated sub-basin priorities,  (2) interagency
cooperation, (3) costsharing,  (4)   regulation and (5)  provision
                             50

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of more direct information and  assistance  to  specific imple-
menting agencies.  These  items  should  all  be  parts of State
strategies.  The strategies should  result  in  concerted
efforts in selected areas and more .effective  and  demonstr-
able results in terms of  water  quality.
                             51

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                          WATER QUALITY STANDARDS
                            by Michael MacMullen

Water Quality Standards consist of two general parts:  (1) biological uses
to be protected, and (2) specification of criteria necessary to attain the
designated use.  Standards are enforceable through NPDES permits.

Section 101 of the Water Pollution Control Act Amendments (P.L. 95-217)
establishes a national water quality goal for accomplishment wherever
attainable (emphasis supplied) of a water quality providing for the pro-
tection and propagation of fish, shellfish, and wildlife, and also providing
for recreation in and on the water by July 1, 1983.  It is precisely this
aspect of attainability, however, which has not been dealt with in a sys-
tematic manner up until the present time.  Henceforth, water quality standards
activities will be conducted through the focus of prioritized attainability
analyses.U

Under the new focus of attainability analyses, the principal emphasis of the
water quality standards activities will be shifted from the three-year review/
adoption cycle previously utilized, to one year standards program plans
designed to provide the necessary water quality, technologic and socio-
economic data necessary to make sound decisions.  In EPA-Region V, the
priorities for acquisition of  the necessary attainability information will
be negotiated between the individual States and appropriate Regional Office
staff in consideration of the  need to reissue major permits and to make
supportable decisions regarding the level of treatment beyond secondary
which may be needed by municipal sewage treatment facilities.  Results of
the negotiations will be confirmed in the State/EPA Agreements.

Pending acquisition of attainability information in accord with the priori-
tized schedule, EPA will not require upgrading of any Water Quality Standard
to the level specified in Section 101.  Similarly EPA will not approve of
downgrading actions without the necessary attainability information.  NPDES
effluent limitations would be  set at levels consistent with operation of
existing treatment facilities  or application of categorical effluent limi-
tations, whichever is more restrictive, prior to completion of attainability
analyses for the receiving water in question.  Following  completion of the
attainability analysis, the NPDES permit limitations will be set at whatever
level is necessary to achieve  compliance with the attainable Water Quality
Standard.
                                   53

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                  EFFECTS OF POLLUTANTS ON HUMAN HEALTH
                             Leland  J.  McCabe
                    Health  Effects Research  Laboratory
                         Cincinnati, Ohio  45268
      The  EPA's  two  health  effects  laboratories  conduct  research  to provide
 data  for  standards  setting purposes.   These  data  and  the  results  of
 other research  are  used  by the  Office  of  Health and Environmental Assess-
 ment  in Washington  to  provide risk assessments  for  the  regulatory programs.
 In  some cases there is a close  working relationship between  the  laboratory
 and the regulatory  program and  information is provided  directly  on a
 continuing  basis.   In  my experience this  has been true  in the  drinking
 water program.   But interaction between the  research  laboratories and
 the regulatory  programs  is being enhanced by the  Research Committee
 structure.   The Regional Offices have  a more reciprocal method of making
 these research  needs known in the  Research Committees.

      The  HERL in North Carolina has specialized in air  pollution  and the
 HERL  in Ohio on water  problems,  but not exclusively,  and  there are smaller
 programs  on other environmental problems  at  each  laboratory.   The majority
 of  our research in  Cincinnati is concerned with drinking  water, but I
 will  review these activities that  may  be  more germane to  point vs.  diffuse
 source pollution.

 Bathing Beaches

      The  Agency has a  criteria  for recreation water quality  in the Red
 Book  (1)  of a mean  of  200  fecal  coliforms per decaliter.   The  bases for
 the criteria were a series  of studies  conducted in the  early 1950's and
 were  from data  on freshwater with  considerable  extrapulation.  For the
 past  eight  years we have conducted microbiological methods research and
 a series  of epidemiological studies  at  saltwater  beaches.  This illus-
 trates that research on  health  effects  does  not provide fast answers to
 complex problems.

      The  concept was to  develop  a  relationship  between  water quality and
 illness experienced by swimmers.   A decision could then be made on ac-
 ceptable  risk of illness and from  the  relationship the  necessary  water
 quality would be determined.  A  report  on these marine  studies has  been
 completed (2) and the  figure shows  the  relationship.

      The  study  design  called for measurement of water quality  by  as many
methods as  possible, including  currently used methods,  and then seeing
which water  quality parameter best  correlated with illness related  to
 sewage, fecal pollution.   Both pathogens and indicator  organisms  were
 considered  and  a series of  facile methods developed.
For presentation September 16, 1980.  Seminar on Water Quality Management
Trade-Offs, Chicago, Illinois

                                    55

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     The epidemiological protocol developed used a more rigorous defini-
tion of exposure than had been used in past studies; the head had to go
into the water.  The study areas were selected to provide a beach with
"barely acceptable" water quality—that is, a beach not posted as
"Swimming Not Allowed", and a beach that was relatively unpolluted.  The
beach user population also had to be large enough to provide an adequate
study population.  Families were interviewed at the beach on Saturday
and Sunday as to exposure and then called on Monday, 9 to 10 days later
to obtain information on additional midweek swimming and illness ex-
perienced during the week following the exposure trial being studied.
The statistic used was the illness difference between swimmers and non-
swimmers and thus control was achieved over the many other factors that
could affect illness rates.  Adjustments were made on the demographic
variables of age, sex, race, and socioeconomic status.

     The figure shows the relationship develop for the illness defined
as highly credible gastrointestinal symptoms.  That is an illness syn-
drome involving vomiting or diarrhea with a fever or disabling enough
for an individual to remain home, remain in bed or seek medical advice,
or stomachache or nausea accompanied by a fever.  Data points from three
areas were combined for this graph; New York City, Lake Pontchartrain,
Louisiana, and Boston Harbor.  Some confirmatory information was also
obtained from an Alexandria, Egypt study.

     The best indicator to fit the illness data was the Enterococcus
density as measured by a method developed in the study (3).  For an
increased illness rate of 1 percent, the Enterococcus density would be
13.6 per decaliter and for 5 percent increased illness, 906 per 100 ml.

     A generalization of the data from the New York City beaches would
equate 30 Enterococcus to about 200 fecal coliform with an increased
illness rate of 1.8 percent.

     Studies of the freshwater relationship were continued this summer
in Oklahoma and at Lake Erie beaches.  We would like to find a beach to
study nonpoint source pollution.

Aerosols

     Another problem area we were asked to study was the health effects
of siting of sewage treatment plants.  Region 5 asked us to determine if
health effects could be demonstrated in persons living near a sewage
treatment plant so a decision could be made about the necessity of aerosol
suppressive devices at the O'Hare plant.  Construction was allowed to
continue if research would provide data for evaluation before the plant
went on line.

     Fortunately, we had some research underway on the health of sewer
workers and additional projects were started and completed within the 3
1/2 years provided.  A symposium was held at Cincinnati in September
                                   56

-------
 1979  where  study results  were  presented  and  discussed.   The report on
 the  symposium is at  the printers  (4).  We  participated  in writing the
 final environmental  impact  statement  for the O'Hare  plant and  it started
 operation in  May of  this  year.

      I am not completely  satisfied  that  we developed adequate  methodo-
 logies for  the studies, but our assessment was  that  despite the  fact
 that  some microorganisms  are emitted  by  aeration  basins  of a sewage
 treatment plant,  there is no detectable  increase  of  disease in persons
 exposed to  the aerosols.  This is true not only with persons living or
 going to school near a treatment  plant,  but  also  with sewage treatment
 plant workers who normally  have a higher exposure than  the nearby residents.

      As we  have in the bathing water  studies, it  is  reassuring to have a
 dose  response relationship  that can be then  extrapulated back  to a no
 effect level  or acceptable  effect level.   This  was not  possible  in the
 aerosol studies because adequate numbers of  new sewage  treatment workers,
 exposed before immunities had developed, could  not be studied  and our
 serological epidemiological techniques could not  focus  on the  correct
 etiological agents.

 Toxic Effluents

      When the Agency finally got serious about  providing the Criteria
 Documents in  the  spring of  1978 our laboratory  was given three months to
 produce the human health  effects portion of  20  of the 65 consent decree
 documents.  We met our deadline and the  criteria  were published  for
 review in the Federal Register (5).  The final  documents are expected to
 be available  this month.  This illustrates that assessment of  current
 knowlege  on health effects  can be made quickly  at any time,  but  may lead
 to protracted controversy in the review  process.

      Our  own  research, both inhouse and  extramural,  contributed  more
 heavily  to  the  chloroform and asbestos documents.  The Environmental
 Criteria  and  Assessment Offce in Cincinnati  is  now in charge of  producing
 the documents,  but members  of our laboratory  staff have  continued  to
 serve  as  many of  the committees developing the  total  set of  criteria
 documents.

     Most critical to the Great Lakes will be the toxic  pollutants that
 have  significant bioaccumulation.    The methodology has been  changed from
 that used in  the review documents.  Previously,  the weekly  consumption
 was assumed to  be 18.7 grams of edible aquatic  products.   This estimated
 consumption has been reduced to include  only  freshwater  and  coastal
 fish/shellfish  and many of  the bioaccumulation  factors have  been revised.
 In 38 of  the  review documents the intake from both water and fish was
 considered.    In 15 (39%)  the fish intake dominated,  in 22  (58%)  the
 water intake  dominated,  and  in one  case  the  impact was equal.  The final
 documents should be reviewed to see where the fish intake  dominates or
makes a significant contribution.    Because of the Great  Lakes  fishery
                                   57

-------
resource such toxic pollutants will require the most close surveillance.
There will also be populations where the average fish consumption is
greatly exceeded and their health studies should be evaluated.

     In several cases limits could not be set for some of the consent
decree chemicals.  The table lists the six chemical for which it was not
possible to set limits because the health effects data base was inadequate.
For 13 other chemicals the limit was set only on organoleptic effects,
taste or odor, and no health effect limit was set.  In two additional
cases both a organoleptic and health effects limit was considered for
review.  Our laboratory is conducting research to fill the data gaps at
the projected rate of 10 chemicals per year.  New chemicals are, of
course, developed at a faster rate but our research on testing metho-
dology should assist in covering this problem by premarket testing under
the Toxic Substances Control Act.
                                   58

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References

1.   U.S.E.P.A. Quality Criteria for Water, Washington, D.  C.  (1976).

2.   Cabelli, V. J. Health Effects Criteria for Marine Recreational
     Water.  EPA-600/1-80-031,' September 1980.

3.   Levin, M. A. Fischer, J. R. and Cabelli,  V. J.   Membrane  Filter
     Technique for Enumeration of Enterococci  in Marine Waters.   Appl.
     Microbiology, 30:66 (1975).

4.   Pahren, H. R. and Jakubowski, W. (eds.).   Wastewater Aerosols and
     Disease.  Proceedings of a Symposium,  EPA 600/9-80-028,  U.S.E.P.A.
     Health Effects Research Laboratory, Cincinnati, Ohio,  June  1980.

5.   E.P.A. Water Quality Criteria.  Federal Register 40 (52)  15926
     (March 15, 1979).
                                  59

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CONSENT DECREE POLLUTANTS

Could not set health limit.

     2,4-dimethylphenol
     Chlorocresol (Chlorinated Phenols)
     Haloethers
       Chlorophenyl phenyl ethers
       Bromophenyl phenyl ethers
       Polychlorinated diphenyl ethers
     2,6-dinitrotoluene

Criteria based on organoleptic effects.

     Copper                          1    mg/1
     Zinc                            5    mg/1
     Acenaphthene                    0.02 mg/1
     Hexachlorcylopentadiene         1.0  yg/1
     Nitrobenzene                    0.03 mg/1
     Chlorinated Phenols

       a)  Monochlorophenols
           2-chlorophenol            0.3  yg/1
           3-chlorophenol           50    yg/1
           4-chlorophenol           30    yg/1

       b)  Dichlorophenols
           2,4-dichlorophenol        0.5  yg/1         371 yg/1 H.E.
           2,5-dichlorophenol        3.0  yg/1
           2,6-dichlorophenol        3.0  yg/1

       c)  Trichlorophenols
           2,4,5-trichlorophenol    10    yg/1
           2,4,6-trichlorophenol   100    yg/1

     Chlorinated benzenes
       Monochlorobenzene            20    yg/1         450 yg/1 H.E.
       Trichlorobenzene             13    yg/1

-------
                  SOURCES  OF  POLLUTANTS  TO THE GREAT LAKES

                                     by

                             W. Ronald Drynan*
    Pollutants are introduced to the Great Lakes principally through
municipal and industrial point source wastewater discharges, atmospheric
deposition, and urban and agricultural land runoff.  In the lower Great
Lakes, interlake transfer via the connecting channels can also be a
significant source of contaminants.  The relative importance of each
source, in terms of its contribution to the total load of a given
pollutant, varies depending upon the specific lake and pollutant under
consideration.

    The point sources being relatively easy to locate, sample, and obtain
flow measurements for are generally more adequately monitored than
nonpoint sources.  The diffuse nature of nonpoint sources make them
extremely difficult to monitor and the fact that any pollutant loads
transported to the lakes are influenced by highly variable hydrologic and
atmospheric phenomena make it difficult to estimate annual loadings and
discern changes from year to year.

    Pollutants can be generally classified in five groups: oxygen
demanding substances, suspended solids, nutrients, trace metals, and
toxic organic substances.  The classical parameters, BOD and suspended
solids, used to measure the strength of domestic sewage, and estimate the
impact of wastewater discharges on dissolved oxygen and sedimentation
problems in estuaries and tributaries, have relatively little
significance in terms of the Great Lakes.

    Many of the water quality problems of the Great Lakes have been
associated with eutrophication with phosphorus being implicated as the
major nutrient contributing to eutrophication.  Concern of the
deteriorating water quality of the lakes and the need for joint efforts
to restore and enhance them led, in 1972, to the signing of the Great
Lakes Water Quality Agreement between Canada and the United States.  A
major focus of the Agreement was on programs to reduce the total loadings
of phosphorus to the lakes.  The most complete information on the total
annual loadings of any pollutant to the lakes and their sources is
available for phosphorus.

    In the late 1960's point source discharges, particularly municipal
wastewater, were identified as the major sources of phosphorus loadings.
Programs to reduce phosphorus loadings have been directed primarily at
the municipal sources.  As these programs, primarily chemical
precipitation of phosphorus at municipal sewage treatment'plants, have
been implemented nonpoint sources have become an increasingly significant
    *Senior Engineer, International Joint Commission, Great Lakes
     Regional Office, 100 Ouellette Avenue, Windsor, Ontario N9A 6T3
                                     63

-------
proportion of the total residual loads.  Table  1 shows  the  present
phosphorus loadings to each lake from the various  sources.   Current
analysis indicates that achievement of desirable water  quality  conditions
in Lakes Erie and Ontario will require further  reductions in total
phosphorus loadings which can only be achieved  by  implementing  controls
in both point and nonpoint sources (1).
TABLE 1
TOTAL PHOSPHORUS LOADS TO THE GREAT LAKES
(metric tons per year)
Direct Direct
Lake Municipal Industrial
SUPERIOR
MICHIGAN
HURON
ERIE
ONTARIO
72
1,041
126
6,292
2,093
* Tributary loads
tributaries
Sources -
103
38
38
275
82
Tributary
Total (Diffuse*)
2,455
3,596
2,901
9,960
4,047
minus estimates of point
(2,222)
(1,891)
(2,428)
(8,718)
(3,257)
Atmosphere
1,566
1,682
1,129
774
488
(1976)
Urban Upstream
Direct Load Tot£
16 - 4,212
- 6,35-
16 657 4,86/
44 1,080 18,42!
324 4,769 11,802
source loads discharged upstream to the
Final Reports of Pollution from Land Use
and the Phosphorus Management Strategies
Activities
Task Force
Reference Group(2)
Final Report(1)
    In recent years, water quality concerns have shifted to problems
associated with heavy metals, such as lead and mercury, and toxic organic
substances.  The methylation of mercury discharged to the lakes and its
subsequent bioaccumulation to levels of concern in fish and the
possibility that discharges of other metals, such as lead, may lead to
similar problems has focussed interest on the sources of these
contaminants.  Identification of significant levels of toxic organic
substances, such as PCB, DDT and mirex, in fish and herring gulls has
also created an interest in determining the sources of these contaminants
to the lakes.  The information available on sources of these micro
contaminants is very incomplete and any assessment of the relative
importance of possible sources is much more speculative than for
conventional pollutants such as phosphorus.
                                      6'4'

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                               POINT SOURCES

    Information on point source dischargers to the Great Lakes is
maintained in an "Inventory of Major Municipal and Industrial Dischargers
in the Great Lakes Basin"(3) and reported annually to the IJC by the
Great Lakes Water Quality Board.  An-annual estimate is made of the flow
and total loads of BOD, suspended solids, and total phosphorus discharged
by municipal point sources discharging more than 3,800 cu m/d (1MGD) and
all those discharging directly to the lakes.  Most other parameters of
concern are not measured routinely at municipal wastewater treatment
plants and in any case data on these are not routinely reported to the
IJC.

    The U.S. EPA is presently funding a survey of some 50 cities in an
effort to evaluate the extent of the 129 priority pollutants in
wastewater entering municipal wastewater treatment plants, their sources,
removal efficiencies, and amounts accumulating in sludges.  Preliminary
information indicates nine of the thirteen heavy metals (Cd, Cr, Cu, Pb,
Mn, Hg, M, Ag, and Zn) and six organic pollutants (benzene, chloroform,
methylene chloride, bis (2 ethylexyl) phthalate, tetrachloroethylene, and
toluene) were found in nearly all wastewaters.

    Estimates of the amounts of four heavy metals (Pb, Zn, Cu, and Cd)
discharged to the Great Lakes via municipal wastewater, based on the
levels detected in treated effluents and the total flow from treatment
plants(1), are shown in Table 2.
TABLE 2
MUNICIPAL DISCHARGES OF TRACE METALS TO THE GREAT LAKES*
(metric tons per year)
Metal
Zn
Pb
Cu
Cd
Superior
7.9
1.8
1.8
0.5
LAKE

Michigan Huron
103.0
22.9
22.9
6.9
* Based on 1978 reported municipal wastewater
following assumed effluent concentrations in
discharged: Zn - 90 ug/L, Pb - 20 ug/L,
Cd - 5 ug/L.
23.9
5.3
5.3
1.6
discharge(
municipal
Cu - 20
Erie
228.2
50.7
50.7
15.2
3) and the
wastewater
ug/L, and
Ontario
146.3
32.5
32.5
9.8

                                     65

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    The present criterion for reporting industrial pollutant loading
information, other than total phosphorus, to'the IJC is based on a
determination by each jurisdiction of those parameters which may be of
significance to the Great Lakes.  A great deal of self-monitoring and
compliance monitoring by regulatory agencies is carried out for
industrial discharges to satisfy U.S. NPDES and the Ontario Ministry of
the Environment industrial waste control monitoring requirements.
However, these data are not all reported nor analyzed in any
comprehensive manner to obtain total industrial loading of any
pollutants.  Reported industrial inputs of the four heavy metals (Zn, Pb,
Cu and Cd) are shown in Table 3 based on the information reported in the
1978 "Inventory of Major Municipal and Industrial Point Source
Dischargers in the Great Lakes Basin"(3).
TABLE 3
INDUSTRIAL DISCHARGES OF TRACE METALS TO THE GREAT LAKES*
(metric tons per year)
LAKE
Metal Superior Michigan Huron Erie
Zn 10.2 50.0 32.5 148.6
Pb - 0.6 - 38.2
Cu 1.0 9.7 11.0 43.4
Cd - 0.02 - 0.3
* Reported by Great Lakes Water Quality Board in 1978. (3)


Ontario
64.4
7.8
15.5
1.8

    An additional point source, for which little or no information is
currently available, is combined sewer overflows.  These highly variable
discharges are difficult to sample and obtain flow measurements in order
to make estimates of the total quantities of pollutants they introduce
into the lakes.  In some of the major metropolitan areas, such as Detroit
and Cleveland, with combined sewers these discharges may be significant,
particularly in terms of local water quality impacts.  Their impact on
total pollutant loadings and whole lake water quality remain to be
determined.
                                     66

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                              NONPOINT SOURCES

    Estimates of nonpoint source pollutant loadings  to  the  lakes  are
based on measurements of flow and pollutant concentrations  in  samples
taken at the mouths of major tributaries to the Great Lakes.(4,5,6)
Estimates of annual pollutant loadings transported by tributaries  are
difficult to make due to the variability of the flows and pollutant
concentrations throughout the year.  Determining the relative
contribution of various land use activities to the pollutant load  carried
by the tributaries is complicated by questions of delivery  to  streams,
transport in streams and effect of the upstream point source discharges.

    The most extensive attempt to assess the  relative contributions of
urban and agricultural runoff, and streambank erosion,  and  other  land use
activities to the total pollutant loads to the Great Lakes  was  the IJC's
International Reference Group on Great Lakes  Pollution  from Land Use
Activities (PLUARG).  The PLUARG Final Report(2) and the technical report
series(7) provide a great deal of information on types  of pollutants and
unit area loads from specific land use activities in specific  locations
throughout the basin.  Using an Overview Model,(8) PLUARG extrapolated
this information for phosphorus to estimate whole-lake  loadings from land
drainage.  The overview model is presently being developed  by  the  Great
Lakes Basin Commission to make estimates of other parameters.(9)

    Runoff from agricultural land, particularly erosion from row crop
production on fine-textured soils, was identified as a  major contributor
of phosphorus to the Great Lakes.  Urban and  rural runoffs  were also
identified as possibly significant contributors of other contaminants.
However, very little data are available upon  which to make  any  estimates
of the amounts of toxic organics or heavy metals which  may  be  transmitted
to the lakes from these sources.

    Shoreline erosion is another nonpoint source which  potentially
contributes a large amount of pollutants to the lakes.  Estimates  of the
total sediment and total phosphorus loads from shoreline erosion  in each
lake are given in Table A.  The whole lake impact of these  loadings is
considered to be quite minimal in that the phosphorus and other
pollutants are not considered to be biologically available  and  are
generally associated with larger particles which settle in  nearshore
areas.  In any event, shoreline erosion has been occuring in the Great
Lakes since their creation and any efforts by man to control the
phenomenon would not likely result in reductions in pollution  of the
lakes commensurate with the expenditure of funds required for  any
significant control of shoreline erosion.
                                     67

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TABLE
SHORELINE EROSION AS A SOURCE OF
LOADINGS TO THE
(metric tons
Lake
Superior
Michigan
Huron
Erie
Ontario
Notes:

Tributary
(suspended solids)
1,378,260
706,540
1,052,960
6,531,800
1,597,000
Shoreline Erosion
(total sediment)
11,279,000
21,778,000
1,763,000
11,131,000
3,206,000
4
SEDIMENT AND TOTAL PHOSPHORUS
GREAT LAKES
per year)
Total Phosphorus
Shoreline2 Total
Erosion All
3,800 1
3,700
794
10,536 3
1,280


1976
Phosphorus
Other Sourci
4,212
6,357
4,867
18,425
11,803
1. U.S. load only
2. PLUARG reports on U.S. and Canadian shoreline erosion.
3. Canadian estimate for short term used (1972-1973) @ 9512 t/yr -
Canadian long term estimates (1953-1973) @ 5912 t/yr.
                            ATMOSPHERIC SOURCES

    Preliminary work carried out during the Upper Lakes Reference
Group(lO) and PLUARG Studies(ll) indicated that atmospheric inputs may be
a significant source of pollutants to the lakes particularly for toxic
organics and some heavy metals.  Work has continued in the difficult task
of measuring dry and wet deposition and estimating annual atmospheric
loads.  Recently, contracts funded by the IJC's Great Lakes Science
Advisory Board(12,13) summarized the available information on atmospheric
inputs of organic and inorganic constituents to the lakes.  These data
are summarized in Tables 5, 6 and 7 for the nutrients and major elements,
trace metals, and trace organics, respectively.  While much of the data
are preliminary in nature, and the sampling methodology and analytical
techniques are still in early stages of development, the data indicate
that the atmospheric pathway is a very significant input for total loads
for parameters such as PCBs and lead, and it may be significant for some
of the other organics, total phosphorus, aluminum, cadmium, copper,
chromium, iron and nickel.  For example, available data of loadings of
lead from the various sources, as summarized in Table 8, indicate the
dominance of atmospheric inputs for that parameter.
                                      68

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TABLE 5
TOTAL DEPOSITION OF AIRBORNE NUTRIENTS AND MAJOR ELEMENTS TO THE GREAT LAKES
(metric tons per year)
Element
so4
NO 3 /NO 2
Ca
Na
Cl
K
Mg
Si
Superior
205,000
41,000
#
32,800
41,000
24,600
16,400
24,600
Michigan
259,000
46,000
173,000
28,800
t
11,500
28,800
11,500
Total Phosphorus # #
& Estimate not
possible from
available
LAKE
Huron
179,000
41,700
#
17,900
29,800
17,900
11,900
11,900
1,190
data.
Erie
113,000
25,100
50,200
12,600
20,100
12,600
12,600
7,540
754

Ontario
85,300
19,000
28,400
19,000
9,480
3,790
7,580
948
379

TABLE 6
TOTAL DEPOSITION OF AIRBORNE TRACE METALS TO THE GREAT LAKES
(metric tons per year)
Metal
Zn
Pb
Cu
Cd
Ni
Fe
Al
Mn
# Estimate not
Superior
8,210
1,230
821
82
328
8,210
14,000
1,640
possible from
LAKE
Michigan Huron
# #
1,730 596
575 298
58 60
575 89
# 4,770
28,800 #
1,150 #
available data.
Erie
#
754
151
75
75
3,270
#
#

Ontario
948
379
95
28
76
1,520
#
#

69

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TOTAL DEPOSITION OF
Compound
TOTAL PCB
TOTAL DDT
a-BHC
y-BHC
DIELDRIN
HCB
p,p' -METHOXYCHLOR
a-ENDOLSULFAN
B-ENDOSULFAN
TOTAL PAH
ANTHRACENE
PHENANTHRENE
PYRENE
BENZ(a) ANTHRACENE
PERYLENE
BENZO(a) PYRENE
DBP
DEHP
TOTAL ORGANIC
CARBON
Superior
9.8
0.58
3.3
15.9
0.54
1.7
8.3
7.9
8.0
163
4.8
4.8
8.3
4.1
4.8
7.9
16
16
2x105
TABLE 7
AIRBORNE TRACE ORGANICS TO THE GREAT LAKES
(metric tons per year)
Michigan
6.9
0.40
2.3
11.2
0.38
1.2
5.9
5.6
5.6
114
3.4
3.4
5.9
2.9
3.3
5.6
11
11
1.4xl05
LAKE
Huron
7.2
0.43
2.4
11.6
0.55
1.2
6.1
5.8
5.8
118
3.5
3.5
6.1
3.0
3.4
5.8
12
12
1.5xl05
Erie Ontario
3.1
0.19
1.1
5.0
0.17
0.53
2.6
2.5
2.5
51
1.5
1.5
2.6
1.3
1.5
2.5
5.0
5.0
.66xl05
2.3
0.14
0.77
3.7
0.13
0.39
1.9
1.8
1.9
38
1.1
1.1
1.9
0.94
1.1
1.8
3.7
3.7
.46xl05
70

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                                     TABLE 8

                 SOURCES OF LOADINGS OF LEAD TO THE GREAT LAKES
                             (metric tons per year)
Lake
Superior
Michigan
Huron
Erie
Ontario
Municipal
1.8
22.9
5.3
50.7
32.5
Industrial
0
0.6
0
38.2
7.8
Atmospheric
1,230
1,730
596
754
379
    Several intermittent potent
Lakes, which are not well docum
the transportation and handling
dredging activities which may r
disposal of dredged materials
operations such as drilling for
   OTHER SOURCES

 Lai  sources of pollutants to the Great
 ;nted,  include spills which occur during
  of  toxic  or hazardous substances,
 ^distribute pollutants in sediments,
in open waters, and resource recovery
  gas in Lake Erie.
                                  SUMMARY
    The Great Lakes are subject
variety of sources.  In the pas
 ;d to pollutant loadings from a wide
    the major problems were attributed to
municipal and industrial wastewater discharges of conventional
pollutants.  Concerns have now
 shifted to persistent, toxic substances
that bioaccumulate, and find their way into the lakes via many different
pathways and from as yet unidentified sources. While efforts need  to
continue to improve the estimates of total loadings of pollutants  of
concern such as phosphorus in order to provide direction for control
programs, it is not practical tc
input/output analysis for all pollutants, and particularly the  toxic
organics.  It is important that
creating problems in the lakes be identified and efforts to identify
various sources be directed at these.  Methodologies are being developed
to enable one to make first-cut
pollutants from various sources.
since trying to monitor everything everywhere is not practical.
   attempt  complete mass balance
  the specific pollutants which are
  estimates of the relative inputs of most
    These efforts need to be continued
                                   71

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    Improvements are needed in sampling and monitoring programs for both
the tributary and atmospheric inputs.  A coordinated program is required
to identify atmospheric airborne contaminants and provide an adequate
assessment of the loads from this pathway to compare with municipal and
industrial and tributary loadings.
                                      72

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                            REFERENCES

1.   Phosphorus Management for the Great Lakes - Final Report of the
     Phosphorus Management Strategies Task Force to the IJC's Great
     Lakes Water Quality Board and Great Lakes Science Advisory
     Board.  Windsor, Ontario (July 1980)

2.   Environmental Management Strategy for the Great Lakes System -
     Final Report of the Pollution from Land Use Activities Reference
     Group, Windsor, Ontario (July, 1978)

3.   Inventory of Major Municipal and Industrial Point Source
     Dischargers in the Great Lakes Basin - Great Lakes Water Quality
     Board, Windsor, Ontario (July, 1979)

4.   Annual Tributary Loadings - Great Lakes Water Quality Board
     Annual Report Appendix B, Windsor, Ontario (1975-1979)

5.   United States Great Lakes Tributary Loadings - Pollution from
     Land Use Activities Reference Group, Windsor, Ontario (January,
     1978)

6.   Land Use, Water Quality and River-Mouth Loading: A Selective
     Overview for Southern Ontario - Pollution from Land Use
     Activities Reference Group, Windsor, Ontario (March, 1978)

7.   Annotated Bibliography of PLUARG Reports - International
     Reference Group on Great Lakes Pollution from Land Use
     Activities - Windsor, Ontario (1979)

8.   Management Information Base and Overview Modelling - M.G.
     Johnson, J.C. Comeau, T.M. Comeau, T.M. Heidtke, and W.C.
     Sonzogni - PLUARG Technical Report, Windsor, Ontario - August
     1978.

9.   U.S. Heavy Metal Loadings to the Great Lcikes: Estimates of Point
     and Nonpoint Contributions - T.M. Heidtke, D.J. Scheflow, and
     W.C. Sonzogni, Great Lakes Basin Commission, GLEPS Contribution
     No. 12, Ann Arbor, Michigan (January 1980).

10.  The Waters of Lske Huron and Lake Superior - Report to the
     International Joint Commission by the Upper Lakes Reference
     Group. 3 Vol. Windsor, Ontario.  1976.

11.  Atmospheric Loadings to the Great Lakes - A Technical Note
     prepared for the International Reference Group on Pollution of
     the Great Lakes from Land Use Activities, IJC Great Lakes
     Regional Office, Windsor, Ontario (September, 1977)

12.  Assessment of Airborne Inorganic Contaminants in the Great Lakes
     - Great Lakes Science Advisory Board, Windsor, Ontario (1980)

13.  Assessment of Airborne Organic Contaminants in the Great Lakes -
     Great Lakes Science Advisory Board, Windsor, Ontario (1980)
                                 73

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                        TRIBUTARY LOADS AND EFFECTS
                Summary of a Speech by Nelson A.  Thomas  on
      "Biological  Effects of Chloride and Sulfates on  Lake  Michigan"
                          September 16-17, 1980
                            Chicago, Illinois
Many of the Great Lakes water quality problems  can  be associated with  the  poll-
utant inputs from various tributary sources.  Since  the Great Lakes  differ  greatly
in their trophic state, the impact of pollutants  is highly varied and  dependent
upon type. Water quality problems can arise from  sediment input; algal  nutrient
additions, such as phosphorus; heavy metals;  and  organic toxins, both  industrial,
agricultural. Many of the effects are related to  each other because particulate
matter carries much of the pollutant load to  the  lakes.

Sediment plays a vital role in the ecosystem  of the lake. It has both  delet-
erious and beneficial impacts. When present in  sufficient quantities it blocks
out the light to rooted aquatic plants,  inhibits  photosynthesis by  phytoplank-
ton, burys benthic animals, and covers fish spawning grounds.  It may be benef-
icial in the sorption and removal of certain  heavy  metals and  organic  toxins.
The sediments of the Great Lakes are the ultimate disposal sites of most of
the persistent, non-conservative pollutants entering the Great Lakes.

It is important to quantify the effects  of tributary inputs on the  uses made
in the Great Lakes. When determining the load reductions required,  estimates
can be made regarding the benefits to be derived  from pollution control prog-
ams, when a cause and effect relationship can be  established.  To do this,  it
is important to: 1) know the magnitude of the input, 2)  quantify the processes
that reduce the pollutant, and 3) the relationship  between pollutant conc-
entration and water use. This approach has been used in  the estimating of  the
target phosphorus loads cited in the 1978 Water Quality  Agreement between
the U.S. and Canada. Phosphorus loadings were related to taste and  odor prob-
lems in Saginaw Bay, hypolimnic dissolved oxygen  concentrations in  Lake Erie,
and the restoration of more desirable phytoplankton and  zooplankton populat-
ions in Lake Ontario.
Nelson A.  Thomas,  Large Lakes  Laboratory,  USEPA,  Grosse  He,  Michigan

                                       75

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                 LAND TREATMENT OF MUNICIPAL WASTEWATER

                                   by

                             A. T. Wallace*
     The topic suggested by the title, presented within the framework of
this seminar on water quality management trade-offs, provides its author
an interesting challenge.  The seminar organizers correctly recognize
that trade-offs may often be required and that decisions relating to
water quality management cannot take place in a vacuum if any meaningful
results are to be expected.  Examination of point source control prac-
tices jointly, given a set of realistic objectives and a finite budget,
is a logical, acceptable concept,  Quite certainly it will prove to be in
our best professional interests to have the tax-paying public understand
at least the rudiments of this management approach.

     Land treatment systems are only one subset of management tools
which, under certain circumstances, can yield substantial water quality
benefits with low capital expense and low O&M and energy commitments.
However, utilization of this technology definitely involves consideration
of trade-offs and often requires considerably more pre-design analysis
than does the employment of conventional technologies.  As land treatment
technology frequently transforms a potential point source into a diffuse
source, its discussion at this seminar seems especially apropos.  Some
materials pass through the soil, comingling with native groundwater;
some are incorporated in growing plants which may be removed from the
site.  In some systems, such as overland flow (OF) or wet lands, contami-
nants may runoff to various collection or discharge points to again be-
come point sources.  Proper design and operation limits the percentage of
applied contaminants which subsequently leave the site boundaries.  Most
importantly, a substantial mass of potential environmental pollutants are
either permanently immobilized or transformed to less objectionable
materials.  I have insufficient time to expound on the technical aspects
of land treatment.  Also, there are a number of recent books and manuals
which do an excellent job of this and some of these are listed in the
references (4, 5).  It should prove more worthwhile to discuss the topic
philosophically.
                            THUMBNAIL HISTORY

     We are speaking of ancient, rather than modern technology as most of
you are aware.  An EPA Water Program Operations Technical Report, "A
History of Land Application as a Treatment Alternative", (1) provides
clear insights into the reasons for the early acceptance, later rejection
and current reemergence of the use of land treatment technology.

     The impact of Federal legislation, beginning with PL 92-500 has been
traced and analyzed by Thomas and Reed (2).   Their review deals in par-
ticular detail with the Clean Water Act (CWA) of 1977 and subsequent EPA
policy statements which carry a strong message that land treatment
*Professor of Civil Engineering, University of Idaho,  Moscow, ID 83843

                                 77

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deserves serious consideration within the spectrum of wastewater manage-
ment alternatives.  Congress, as you may be aware, "loaded" the CWA with
financial incentives for selecting "alternative" technologies, of which
land treatment is the prominent example.  Chief among these are:

     1.  The federal share of a construction grant may be increased from
         75% to 85%.

     2.  The federal government may participate with full grant funding
         in projects which are up to 15% more costly than the most cost-
         effective conventional alternative.

     3.  Projects which fail to meet design criteria are eligible for
         100% federal grants for modification or replacement.

     4.  Land used as part of the treatment system is a grant eligible
         item and further, appreciates at a rate of 3% per year.  (All
         other costs of course are calculated in constant dollars).

     Evaluation of land treatment systems as a Best Practicable Waste
Treatment Technology (BPWTT) in accordance with PL 92-500 requires that
the groundwater quality criteria established by the Interim Primary
Drinking Water Standards mandated by the Federal Safe Drinking Water Act,
PL 93-523,  be met.  In addition, land treatment alternatives must be
fully coordinated with on-going area-wide planning under section 208 of
the Act.  An October, 1977 memo from EPA Administrator Costle specified
that section 208 agencies should be involved in the review and develop-
ment of land treatment options.
               LAND TREATMENT VS. CONVENTIONAL TREATMENT
                       COMPARISONS AND TRADE-OFFS

     The uniqueness of the design procedure for land application of
wastewater affords an opportunity for far better control of most contami-
nants than does the utilization of conventional technology.  In the
design of conventional systems, one usually begins with the permit condi-
tions and assembles, on paper, collections of sub-systems which can meet
these objectives.  The costs of qualifying systems are then estimated to
see which meets the cost-effectiveness criteria of section 212(2)c of
PL 92-500.  This is the approach suggested in EPA1s own guidance document
(3).  Obviously, this approach will produce systems which just meet the
discharge limitations for the permitted parameters.  Such systems may
accomplish more or (generally) less removal of other parameters, not
covered by the permit as written, for example the nutrients, nitrogen and
phosphorus.

     The design of land treatment systems on the other hand, proceeds by
attempting to identify the land limiting constituent, which may include
the liquid load (4, 5).  Under this approach, better than minimal manage-
ment of all other (foreseeable) contaminants is automatically assured.
Of course this apparent advantage is not gained without some compensating
disadvantages.  Foremost among these is the sacrifice of the substantial
dilution and dispersion mechanisms normally associated with surface water
discharge.  These are no longer available when contaminants reach flowing
groundwaters via percolation.  A related disadvantage concerns the impact

                                 78

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of a temporary treatment dysfunction  (fairly common for conventional
technologies while rare, but possible, for land treatment).  Similar
problems may arise upon the arrival of an unusual "slug" of contaminant
which cannot be attenuated to safe levels in passage through the system.
In the case of conventional technology with end-of-pipe discharge, the
impact upon the receiving water, although possibly severe, is usually
temporary and rapid recovery is possible.  Water intakes may be closed
if the dangers warrant and ecological upsets are generally mitigated by
natural repopulation from upstream or tributary sources.  Planned re-
stocking programs may be called for.  In any event, the original water
quality conditions can usually be restored in a fairly short time frame.
Not so in the case of the land based treatment system.  The relatively
ineffective dilution and dispersion mechanisms, together with low velo-
cities, permit the groundwater, once polluted, to remain so for a long
while unless natural decay or adsorption mechanisms act to attenuate the
contaminant(s).

     Some other important differences are:

     1.  Land treatment systems can be designed for flows closer to
         average daily flow than conventional systems which generally re-
         quire consideration of a peaking factor.

     2.  Provided that the necessary additional land is available, land
         treatment systems can be expanded much more easily and rapidly
         than most conventional systems (6).

     3.  Land treatment systems do not necessarily impose any significant
         aesthetic change on the receiving location,  or require changes
         in existing land use.   It may, for example,  preserve agricultur-
         al or timber production, or a unique wildlife habitat.  If
         technological changes should make all or a part of the system
         obsolete in future years, the site should have considerable
         salvage value (7).
                               CONCLUSION

     Something worth remembering, and in fact the premise of an entire
treatise on the subject (5) is that almost without regard for either the
source and type of wastewater and the type of soil or site conditions,
there is some safe loading which will control all contaminants and still
not degrade the terrestrial receiver to the extent that any future uses
are irrevocably precluded.  It may be of course that this loading is too
low to be economical and thus conventional technology provides a better
solution.  However, there have been many realistic exercises in compara-
tive economics performed (5, 8, 9, 10, 11) and these tend to show sub-
stantial economic incentives for land treatment systems under a wide
range of site conditions.
                               REFERENCES

1.   Jewell,  W. J. and B.  L.  Seabrook.  June, 1978.   A History of Land
     Application as a Treatment Alternative.   U. S.  Env.  Prot. Agency
     430/9-78.   83 p.

                                 79

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2.    Thomas, R. E. and S. C. Reed.  1980.  EPA Policy on Land Treatment
     and the Clean Water Act of 1977.  J. Water Pollution Control.  52:
     452-459.

3.    Van Note, R. H. et_ _al.  July, 1975.  A Guide to the Selection of
     Cost-Effective Wastewater Treatment Systems.  Office of Water
     Programs Operations, U. S. Env. Prot. Agency 430/9-75-002.

4.    Loehr, R. C., _et _al.  1979.  Land Application of Wastes, Vols. I &
     II.  Van Nostrand Reinhold Co.  739 p.

5.    Overcash, M. R. and D. Pal.  1979.  Design of Land Treatment Systems
     for Industrial Wastes - Theory and Practice.  Ann Arbor Science
     Pub., Inc.  684 p.

6.    Reed, S. C. and T. Buzzell.  1975.  Land Treatment of Wastewaters
     for Rural Communities in Water Pollution Control in Low Density
     Areas.  W. J. Jewell and R. Swan (Eds.)  University Press of New
     England,  p. 23-40.

7.    McGowan, F. M.  1975.  Water and Land Oriented Wastewater Treatment
     Systems in Water Pollution Control in Low Density Areas.  W. J.
     Jewell and R. Swan (Eds.)  University Press of New England,  p. 3-14.

8.   Jewell, W. J.  1979.  Personal communication.

9.   Reed, S. C.  1980.  Personal communication.

10.  Gulp, G., Williams, R. and T. Lineck.  Oct. 1978.  Costs of Land
     Application Competitive with Conventional Systems.  Water and
     Sewage Works 125:49-53.

11.  Crites, R. W., Dean, M. J. and H. L. Selznick.  Aug., Sept. 1979.
     Land Treatment vs. AWT - How Do They Compare?  Water and Wastes
     Engineering 16:16-19, 51-53.
                                     80

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               COSTS FOR WASTEWATER TREATMENT

                            by

                     James A. Hanlon
     During the next few minutes this afternoon I would like to share
with you some of the experiences we have gained over the last seven
to eight years here in Region V in the construction grant program re-
garding the subject of the cost for wastewater treatment.  As you
might well by now recognize, the seven to eight year time span put us
back generally to the point in time when the Federal Water Pollution
Control Act of 1972 was passed by Congress in October of that year.
As we all know it was that statue, public law 92-500, that gave us
the set of water planning programs with which we continue to deal with
today.  These include the section 201 facilities planning program under
Step 1 which then subsequently leads to Step 2 design and Step 3 con-
struction projects, the section 208 water quality management program
and the section 303 water quality standard program.  These programs re-
sulted in a framework or process which produced literally thousands of
national pollutant discharge elimination system permits requiring speci-
fic levels of treatment for mun icipally owned wastewater treatment fa-
cilities and then, through the process described above, a set of facili-
ties plans recommending treatment solutions to the defined problems.

     The Federal Water Pollution Control Act also gave us the first com-
prehensive involvement in the cost of wastewater treatment services at
the local level.  Section 204(b)(l) of the statue established the re-
quirement for user charges to be developed for all municipal grantees
receiving construction grant funding for wastewater treatment facilities.
Briefly, Section 204 required that each applicant for a waste treatment
construction grant has adopted, or would adopt, a system charges to as-
sure that each recipient of waste treatment services within the applicant's
jurisdiction would pay its proportionate share of the cost of operation
and maintenance  (including replacement) of any waste treatment services
provided by the applicant.

     Section 204 of the Law represented a recognition by Congress that
the cost for managing waste treatment facilities are in intregal part
of the agency's management of the construction grant program and that
a system for proportionately distributing the cost of waste treatment
services must be established in conjunction with each Step 3 construc-
tion grant.  It should also be noted that the user charge requirement
applied to all facilities within the applicant's jurisdiction, not only
the facilities being affected by a given grant project.
                                81

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      To put in perspective the numbers of municipalities and the
number of revenue systems that have been approved under the re-
quirements of Section 204, let us briefly look at where the con-
struction grant program has come under Public Law 92-500.  To
date congressional appropriations for the construction grant pro-
grams, through fiscal year 1980, total in excess of $31.5 billion
dollars.  Correspondingly, actual obligations, in the form of grant
awards to cities, towns and villages across the country presently
total in excess of $25.7 billion dollars.  This $25 billion dollars
in obligations represent approximately 18,000 individual grant
awards.  It is therefore evident that the cost of waste treatment
services, the construction grant prpgram and user charge systems
have impacted very significant portions of the opoulation within
Region V and nationwide.  It is currently estimated that on the
order of $7 billion dollars is currently collected annually in
user charges by local municipal treatment authorities.

      Allow me to clarify the definition of user charge systems
for the purposes of our discussion.  By definition, user charge
means: the cost for operation, maintenance and replacement of the
treatment facilities.  The cost for local debt retirement or the
local share of the capital cost are not included in user charge
numbers which will be discussed due to the complicating factors
of interest rates, methods of bond payback and long term out-
standing bond issues.

      Subsequent to the passage of Public Law 92-500 it was ap-
proximately the end of 1974 until the first user charge system
was approved in Region V, that being the first nationwide.  Since
that time, approximately 700 municipal revenue systems implementing
the user charge requirement have been approved in Region V.  Those
numbers extrapolated to the national level indicates that on the
order of 3000 to 3500 user charge systems have to date been re-
viewed and approved for construction grant projects.

      As the program moved through the years of 1975, 1976 and
1977, it became apparent that the process which had been set up
was working very well.  Hundred of construction grants were
awarded, dozens of user charge systems developed under those grant
projects were reviewed and approved.  It also became apparent,
however, that the cost impacts at the local level of these waste
treatment construction projects were significant.  The impact of
these cost considerations was especially large on the very small
communities.  It should be noted that of the 18,000 existing
grant awards that I mentioned earlier, approximately 48% of those
grants have been made to communities with populations less than
3500.  Another recognition that took place at about the same
time was that the process which had been set up, as described
                               82

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earlier, the process of: water quality standards leading to NPDES
permits leading to facilities plans, leading to central waste treat-
ment facilities with conventional collection systems had become the
order of the day.  The potential for these central treatment and col-
lection systems to have significant economic impacts was further com-
pounded by an interest rate which has averaged in the construction in-
dustry, and particularly in the waste treatment construction industry,
approximately 1% per month.  In addition the subject facilities are
capital intensive, using large amounts of bricks and mortar and are
also energy intensive in terms of necessary killowatts to power
aeration blowers, pumps etc.

     We have maintained a file of the approximately 700 approved user
charge systems in Region V which until recently was in manual form
and which has recently been updated and placed on data file in our
Regional computer.  A data file now named "File of Approved Municipal
Revenue System", and nicknamed FOAMRS, is, to the best of our knowledge,
the only data file of approved revenue system information of its kind
in the country.  What that file tells us is that the costs for waste-
water treatment vary significantly from community to community.  The
largest swings are observed between the larger establish municipalities
and sanitary districts which have constructed and maintained facilities
over the past thirty to forty to fifty years versus the small communities
who are attempting to construct new treatment systems using todays in-
flated construction market

     Shown below in table I is a list of municipalities which may be
familiar to many of you.  These are the larger and older communities
around the Region.  Listed in the table in addition to the location is
the date the revenue system was approved and the annual estimated user
cost per connection of per household.  It should be remembered that the
annual user charge given is for operation, maintenance and replacement
and does not include debt retirement which would serve to further in-
crease the total annual charge.

Table I	

                           Date Approved      Estimated Annual Cost
Location
Aurora S.D., Illinois
MSD of Greater Chicago, 11
Springfield S.D., 11
City of Indianapolis, IN
Washtenaw Co. /Ann Arbor, MI
Metro Waste Control
Comm Serving Minn/St. Paul,
Northeast Ohio RSD
serving Cleveland, OH
6/79
1/80
12/79
9/77
7/79
MN 9/77
4/76
$44.00
$45.00
$65.00
$47.00
$119.00
$55.00
$59.00
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     The annual charges shown above should appear typical to most of
us here today, and are probably what we expect most people pay for
wastewater treatment services.  However, these figures can be contrasted
with those shown below in table II which are at the other extreme of
the cost scale.  These are all small communities which have recently
undertaken the construction of a new wastewater treatment system or
major additions to an existing system.  As you can see, the projected
annual user cost, per connection, is several times higher than that
being experienced in our larger communities.  It should be noted that
the estimated annual charge of $287.00 is equivalent to almost $24.00
per month, a significant charge in almost anyone's budget.

Table II

                                Estimated Annual Cost     Population
Location
Village of Elwood, Illinois
Town of Elnora, Indiana
Town of Freemont, Indiana
Village of Cass City, Michigan
Gross lie Sanitary Drainage
District, Michigan
Village of Butler, Ohio
Village of Rock Creek, Ohio
$
$
$
$
$

$
$
215
216
232
278
278

243
287
783
873
1090
2469
—

1018
800
     In response to these spiraling service costs, the Agency first at-
tempted to approach the concern in the form of better publicizing the
anticipated cost of wastewater treatment works projects which were still
in the planning phase.  In this direction, Program Requirements Memoran-
dum  (PRM) No. 76-3 entitled,  "Presentation of Local Government Cost of
Wastewater Treatment Works in Facility Plans" was published in August of
1976.  The principal purpose of this document was to ensure that the anti-
cipated costs of the waste treatment alternatives being analyzed in the
facilities plans be estimated and displayed clearly for all interested
parties to note.  The four categories of cost presentation required by
the  PRM were  (a) an estimate of total capital cost,  (b) a discussion of
the  anticipated method of financing,  (c) an estimate of the annual
operation, maintenance and replacement and a estimate of the monthly
charge for debt service retirement.

     In addition to the above, a current effort being initiated in the
Region is to use the FOAMRS file to close the loop between the cost pro-
jections being made in facilities plans and the actual approved costs
being identified in the context of approved user charge systems.  This
will allow for a level of consistency in the cost estimates which has
not  previously existed.
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     In addition to highlighting the cost of the proposed treatment
facilities, the Agency has also moved to investigate the technological
reasons behind these spiraling costs in small communities.  One of the
most significant advances in the effort to control cost at the small
community level was the enactment of the Clean Water Act Amendments
of 1977 which included a provision which established the eligibility
of on-site treatment systems.  Prior to this time, if it was shown
that the cost effective solution for a given community was to simply
upgrade or improve their existing septic tank based system of treat-
ment, the cost for doing so was entirely a local matter.  The Clean
Water Act Amendments of 1977 provided the ability to fund, under the
construction grant program, the upgrading or necessary replacement of
failing  septic systems or other on-site treatment methods where it
was shown to be cost effective.  This initiative of the Clean Water
Act has been carried out through the detailing of the necessary pro-
cedures to implement on-site system alternatives in PRM 79-8, titled:
"Small Wastewater Systems" published in May of 1979 and subsequently
in a step-by-step guidance document developed here in Region V during
the Spring of this year.

     The intent of this effort has been to give on-site treatment
systems every chance of working in order to provide reliable treat-
ment services at a reasonable cost to the local home owner.

     In addition to the on-site systems initiative for the smaller
communities, the program has also strongly encouraged systems in the
mid and large size municipalities which focus on energy conservation
and other forms of innovative and alternative technology.  A good
example of this is a current project in Muncie, Indiana where some
25 municipal vehicles will be powered by the methane gas produced
in the anarobic digesters at the wastewater treatment facilities.

     This, for the most part, summarizes where the Agency and the
construction grant program have come in terms of the issue of costs
for wastewater treatment services.  What I would like to do now is
to briefly outline what our current concerns are and where we see
ourselves moving during the years to come.

     Currently underway at the National level and at the direction
of Chris Beck, the Assistant Administrator for Water and Waste Manage-
ment is what is termed the 1990s study.  The purpose of this effort
is to identify where the construction grant program should be in
1990.  The format for the effort focuses on five major tasks within
which approximately 60 issue papers will be developed, each outlining
an array -of options being considered.
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     One of the major papers being prepared under the 1990 effort is
one addressing the issue of the financial management of publicly owned
treatment works funded under the construction grant program.  The pri-
mary focus of that paper is the long term economic self sufficiency
of publicly owned treatment works including the subject of local re-
sponsibilities relative to reconstruction or recapitalization.  Matters
being considered within the analysis include: (a) what should be re-
quired in terms of a thorough financial analysis during Step 1 facili-
ties planning, (b) user charge systems which include reconstruction/
recapitalization recognition, (c) fixed asset and preventive maintenance
management systems developed as a intergral part of construction pro-
jects arid  (d) follow-up by State or Federal program representatives
to monitor the financial management of constructed facilities by
grantees.  It is expected that the 1990s study will be completed by
the end of this calendar year.

     In conclusion, the issues related to the costs of wastewater
treatment have evolved over the last seven to eight years in the
context of the construction grant program and will continue to
undergo further analysis and refinement as we move into the 1980s
and approach 1990.
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             A MANAGEMENT TECHNIQUE FOR
CHOOSING AMONG POINT AND NONPOINT CONTROL STRATEGIES

       PART 1 - THEORY AND PROCESS FRAMEWORK
                         by

                William C.  Sonzogni
                Timothy J.  Monteith
                 Thomas M,  Heidtke
                Rose Ann C.  Sullivan

        Great Lakes Basin  Commission  Staff
                To be presented at

          U.S. EPA, Region V, Seminar on
       WATER QUALITY MANAGEMENT TRADE-OFFS
            September 16 and 17, 1980
                       87

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                    A MANAGEMENT TECHNIQUE FOR!

        CHOOSING AMONG POINT AND NONPOINT CONTROL STRATEGIES

              PART  1 - THEORY AND PROCESS FRAMEWORK

                          *,-.    by   ,                    ,

             William C. Sonzogni, Timothy J. Mohteith, ^
            Thomas M, Heidtke, and Rose Ann C. Sullivan,
       Abstract;   To  assist water quality managers and planners
       in  formulating  cost-effective   pollution  control
       strategies,  a methodology was  developed  for evaluating
       alternative point  and nonpoint  source  control  within a
       drainage   area.    The  methodology  — referred  to  as
       WATERSHED  —  allows  the  user(s)  to  estimate  loadings
       from each  major  pollutant  source  and to  examine  load
       reductions and  costs  associated with  control  options.
       Point  and  nonpoint source control strategies can then be
       ranked on the  basis  of  cost  per  unit  reduction  in
       pollutant  loading to  the receiving  water.   From  this
       ranking,  an optimum mix  of programs  can be identified
       which  will achieve  a  required  load  reduction  at least
       cost.    Strategies  can  be  staged,  that  is,   they  may
       consist  of several levels of control.

       In evaluating  loadings and control programs for a given
       drainage  are.a, WATERSHED  considers  the hydrologic,
       physiographic  and  demographic  characteristics  of  the
       basin, pollutant losses  or  entrapment during  transport
       from  source  to   river   mouth,  as   well  as   the
       bioavailability  of  the  pollutant(s) under  study.   The
       approach  is flexible and able  to  accommodate   a variety
       of techniques  for estimating loadings  from municipal and
       industrial point  sources  and   land  runoff.   Although
       WATERSHED is  primarily a  data integration and accounting
       system (rather than  a technique to  generate  point  and
       nonpoint  loads), some methods  for estimating  loads are
       specifically addressed.   Calculating  cropland loads
       based  on  potential  gross  erosion  determined  from  the
       Universal   Soil  Loss  Equation  (USLE) was  found to  be
       particularly useful,  since  the  effect  of  control
       programs  can  be  evaluated  based  on changes  in  the
       factors   governing  the  USLE.    A  case   study  of  how
       WATERSHED can be applied to the Sandusky River basin in
       northcentral  Ohio  is  presented  in  a  companion paper.
Great Lakes Basin Commission Staff.   Water  Resources  Scientist, Water
Resources  Engineers,  Regional  Planner/Policy Analyst, respectively.
Great Lakes Basin Commission, Ann Arbor,  Michigan.

                               88

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                              INTRODUCTION
    Water  quality managers  and  planners  are  faced  with  difficult
decisions on how to best reduce point and nonpoint pollutant inputs to
water  bodies.    Given  the  economic  realities  of  today (reduced
government spending,  inflation and high energy costs), these decisions
must be cost-effective.  Decision-makers must,  therefore, be careful to
select  the  combinations of  point  and  nonpoint  water  quality control
measures which will most efficiently solve  their  pollution  problems.

    Recognizing the  difficulty in  choosing  among point  and  nonpoint
control  strategies  within  any  given  drainage  basin,  the  U.S.
Environmental Protection Agency (Region V) asked the Great Lakes Basin
Commission staff to assist  them in  devising  a straightforward technique
for  choosing  among  river  basin management  options.   This  paper
describes the technique developed.   A companion paper will  show how the
technique can be  applied using  a  simple worksheet system  (Monteith et
al. ,  1980).    To  complete  the  effort  a  handbook  will  be  prepared
(summer, 1981)  to facilitate  application of  the technique.

    The  management  technique developed,  called  "WATERSHED",  is
basically an accounting  system for  assessing and  comparing alternative
management  strategies  to  control  point  and nonpoint  (excluding
atmospheric) source pollution inputs to  a  receiving water.  . It provides
a  means  for  evaluating the  fraction  of  the total  pollutant  input
attributable to any particular source,  as well as  how  cost-effectively
this input can be  controlled relative to the input from  other sources.
WATERSHED  utilizes  information  on   the  geophysical  and  demographic
characteristics of a  drainage  area,  along with  the  costs  of remedial
measures, to generate  the least-cost  program (or  sequence  of programs)
for attaining a required level of pollutant  load  reduction.  WATERSHED
is unique  in that  it  integrates  a wide range  of  technical information
on both point and  nonpoint pollution  control.  It  attempts to quantify
and practically apply  information generated  from years of  research and
demonstration.

    WATERSHED has evolved from  several studies, including the Pollution
from Land Use Activities Reference Group (PLUARG)  study, the Lake Erie
Wastewater Management Study (LEWMS);  the Black  Creek  (Ohio), Washington
County  (Wisconsin),  and  Red  Clay  Erosion  (Wisconsin)  demonstration
projects conducted under Section  108  of Public Law  92-500; a  host of
studies  conducted  under Section  208 of  Public  Law  92-500;   and  the
innovative Wisconsin  Fund program.   The interrelationships among these
studies, as well  as  details  of the1 studies  themselves, are summarized
in Sullivan et al. (1980a and b).

    Although all  of  the   above  studies  have  contributed  to  the
development of WATERSHED, its  foundation  lies  in the "overview
modeling"  process  developed  as part  of the PLUARG  study  (Johnson et
al., 1978; Heidtke,  1979;  Heidtke  et al.,  1979).   PLUARG was a multT1
million dollar  cooperative  investigation  of nonpoint  source pollution
in  the  Great Lakes basin.   In PLUARG, overview  modeling  was  used to
identify the most  cost-effective mix  of point  and  nonpoint controls in
                                 89

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each  of  the  Great  Lakes  basin  watersheds.     The  process  provided
detailed estimates of  pollutant  inputs from each major  source  in each
of the drainage areas  or  streams  discharging  to the lakes.  Because of
the  large  number  of  computations frequently  involved  in  arriving  at
these estimates, a computer program was used to simplify the accounting
procedure.

    The  overview  modeling  process  considers  factors  such  as  varying
land use  (such  as farmland,  forest  and wetlands)  and  land form (soil
texture  and  slope),  as well  as  different types  of urban  areas.   The
modeling process is dynamic, enabling one to take into account changing
conditions such as  population growth, urbanization of  rural  areas,  or
the natural removal of pollutants from the water as it moves downstream
to the lake.

    The value of  the  process is  fully  realized when  pollution control
information  is  introduced  into  the computations .   Alternatives  for
reducing phosphorus inputs  from  each source can  then be  tested.   Then
those measures  which  produce  the  greatest pollutant reduction at least
cost can be easily identified.

    Although  the   overview model  provides  the  basis   for WATERSHED,
WATERSHED  is much  more flexible  and  easier  to use.  PLUARG's overview
model is basically  a  research tool,  while WATERSHED  is designed to be
more user-oriented.

    While  WATERSHED is applicable to many nonpoint pollutants,  it has
been  developed  with   phosphorus  and  suspended sediment  primarily  in
mind.   Some  slight modifications  to  the  approach  may  be  necessary to
accommodate  the unique  characteristics of  other pollutants.   For an
example  of how  the  basic approach can  be  applied to  other parameters,
see Heidtke et  al., 1980) .
                  SYNOPSIS OF THE "WATERSHED" PROCESS

    The  initial  step in WATERSHED  is division of  a river or drainage
basin  into  sub-basin units.    Point  and  nonpoint  sources  in  these
sub-basins  are  then  identified  and  their  respective pollutant  inputs
are estimated.  An  accounting  system is  then  used  to route the  inputs
downstream  to  the receiving water.   This  accounting  can be  performed
manually  or with  the  aid of a computer.   Transmission  losses,  which  may
occur  due to a reservoir  or  other  obstruction,  are estimated  through
the application of  "transmission coefficients" in various stretches  of
the tributary.    The  percent  of the  pollutant  that  is likely to  reach
the  receiving  water in  a  biologically  available   form  can  also   be
factored  in.   Remedial measures can be  compared  in terms of cost  per
unit reduction  in pollutant input at the  receiving water  to  account  for
differences  between  upstream   and  downstream  sources.     This  basic
"accounting  system"  is  readily  adaptable  to  large  or small watersheds
and can be  as general as the user desires.

    Techniques  for  estimating pollutant  loads  (when  these loads  are  not
already  monitored)  are  based   on   the  most  accurate  and up-to-date
                                 90

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information available.  For  agricultural  land,  the  Universal  Soil  Loss
Equation  (USLE)  is used in  evaluating  the effect  of various management
techniques, such as conservation tillage, on loadings from agricultural
land.    This  allows  load  reductions  to  be related  to  a series  of
established  factors  that  affect  soil  erosion  losses  from land.
Widespread use  of  the USLE  in  the field  has established  its  validity
and utility for this purpose.

    The WATERSHED approach  can next  be used to  choose the  best  mix  of
point  and nonpoint management  techniques  to  achieve  a certain  load
allocation for  a receiving water  body.   Through a cost-effectiveness
ranking  scheme,  WATERSHED  shows the  order in which remedial  measures
should  be implemented  to  achieve  the  greatest   water  quality
improvements at the least  cost.

    Thus, WATERSHED provides planners and managers with a logical guide
to select  among  point  and nonpoint water  quality  control  programs.   It
will  be  most  valuable if  used  with the  assistance of  individuals  or
agencies  familiar  with the specific characteristics of  the hydrologic
basin  under  study.   WATERSHED'S  straightforward  accounting should  be
applicable to  most  river  basins,  but  its application should  be
customized through the use  of local  information and expertise  whenever
possible.
                  CONCEPTUAL LAYOUT OF THE STUDY AREA

    To  proceed  with  the WATERSHED process,  a  drainage basin is  first
divided  into a set  of  sub-basins.    Urban  areas  and  point   source
discharges within  each  sub-basin  are identified, as well  as  locations
along  the  main  channel where  the point  source and diffuse  pollutant
loadings are  assumed  to enter.   Physical characteristics  of  the  river
which may cause pollutant transmission losses are then  identified.   The
resulting  framework  conceptualizes  a drainage  basin  as  a series  of
discrete pollutant loadings proceeding in sequence from  the  headwaters
downstream  to  the river  mouth  (see  Figure   1).    A  more detailed
discussion of this layout process  follows.

Constructing Sub-Basins

    The initial  step in establishing  sub-basins  for  a  particular  study
area is to divide  the region into  smaller hydrologic units.   These  may
be defined from Conservation Needs Inventory hydrological maps or  from
analysis of  any  available  physiographic maps of  the drainage  area.
Once  the  boundaries  of  individual  hydrologic  units  have  been
delineated,  each  is  then  further divided  into areas  with  relatively
homogeneous  surface soil  texture  and topography.   Information on  soil
textures and  distrib.utions  can  generally be obtained  from county  soil
surveys  published  by  the  U.S.  Soil  Conservation   Service  (SCS)  and
through the assistance of local  SCS personnel.   The  resulting  divisions
are referred to  as "sub-basins"  of the drainage area  under  study.

    If desired,  the sub-basins  may be further broken down  on  the  basis
of land use  intensity  (i.e., cropland,  pasture, grassland, forest  and
                                91

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ro
                                                     FIGURE 1

                                     RIVER BASIN AND ITS SCHEMATIC REPRESENTATION
                                                                Rural
                                                                inputs
Urban
inputs
                             Lake

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wetlands).    However,  this  level  of  refinement  is  unnecessary  for
application of the WATERSHED process.

Components of the Sub-Basins

    After  establishing  sub-basin  boundaries,  it  is necessary  to
identify  and  define critical  characteristics of  the  urban and  rural
land contained within each sub-basin.  This information is  necessary to
accurately assess pollutant  loadings  and the  effect  of remedial
measures.

    Point Source Discharges:  All significant point sources discharging
to surface waters of the  sub-basin must  be identified.   For each point
source,  the following data are required:

    1) Pollutant load,  or
    2) Average wastewater  flow and  average  effluent  concentration for
       the pollutant(s) under study.

    For  municipal wastewater treatment  plants,  it  is  also  important  to
obtain an estimate of  the  population  served  by  the facility as well as
data  on  performance   history,   type  of  treatment  system  in  effect
(primary, secondary, or tertiary) and plans  for  future  expansion.   All
of  these  factors  are  useful  in evaluating point  source  pollutant
loadings and control programs within each sub-basin.

Urban Land:  Urban areas within each WATERSHED sub-basin are identified
and separated from the rural  land.   For each urban area, the following
statistics should be determined:

    1) total area
    2) area served by combined sewers
    3) area served by separate sewers
    4) unsewered area.

For  small cities  it  is  generally  sufficient  to  only determine  the
boundaries of the urban  land.   However,  to ensure  an accurate  analysis
of pollutant loadings and control measures in larger urban  areas (e.g.,
populations exceeding  10,000) ,  it is desirable to obtain  estimates of
combined, separate and unsewered areas.   Information on urban areas may
be  obtained  from  the  Bureau  of   the   Census,  "208"  water  quality
management plans, or other  state,  county and local  sources.   The U.S.
Environmental  Protection  Agency (1977)  has compiled   information  on
areas served by different types of sewer systems in large cities.

    To more  accurately describe an  urban  area,  additional information
should be obtained on the degree of industrialization and the amount of
urban  development.   Industrial  activity can significantly  affect the
concentration of  pollutants in  urban  runoff, whereas  developing  land
generally  contributes  the  largest  suspended solids  loading  per  unit
area.

    Rural Land:   After the areas of urban  land have been identified for
a  given  sub-basin,  the  remaining  rural  area  is  broken  down  into
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different land use categories (e.g., row  crop, mixed  farming,  pasture,
grassland,  forest  and  wetlands).    Because  agricultural  areas  are
generally responsible for the greatest diffuse pollutant  load  per unit
area of  rural  land  and  represent the focus  of nonpoint  source control
programs on rural land,  it  is critical  that these  areas  be  accurately
identified.    Here,  again,  information  on rural  land  uses  may  be
obtained from "208"  water quality management plans,  the U.S.  Department
of Agriculture's  Conservation Needs Inventory and  its system  of Land
Capability Units, or other appropriate  sources.   Within the Great Lakes
basin,  remote sensing techniques have been  used  to  classify  hydrologic
areas  according  to  different  land  covers  including   forest,  wetland,
grassland and agricultural land.   This  information has been compiled by
Monteith and Jarecki (1978).

Points of Entry and Transmission Coefficients

    Once  the  sub-basin  boundaries   have  been  defined and  the  major
sources  of  pollutant loadings have  been identified  and  characterized
(i.e.,  urban and rural runoff and municipal and industrial point source
discharges), locations where these loadings enter the  main channel must
be determined  (see  Figure 1).  The  WATERSHED methodology assumes that
all point and diffuse pollutant  sources within a given sub-basin enter
the  main  channel  at  discrete   positions  referred  to as  "points  of
entry".   Loadings from  several  sub-basins may  discharge to  the same
point  of entry.   There  is  no  fixed  rule  for  identifying points  of
entry;  this particular step requires sound judgment  in combination with
knowledge  of  the  pollutant(s)   under  study   and  the  physical
characteristics  of  the  main  river  or  stream.   In general, points  of
entry  correspond to  intersections   of  feeder  streams with  the  main
channel,  or to  positions  upstream  and  downstream of river  features
which  could retain  material moving  downstream (e.g.,   a reservoir or a
low-gradient flood plain).

    Each river stretch — a  section  of river between  any  two points of
entry  — has  a transmission  coefficient  associated with it .   For any
river  stretch,  this  coefficient  represents  the  fraction  of  pollutant
which  is transmitted from the upstream point of entry  to the downstream
point  of entry in the river  channel.  This  feature  of WATERSHED allows
the user to account for pollutant losses within the  river.
                    CHARACTERIZATION OF POLLUTANT LOADS

    Once the hydrologic basin has been characterized geophysically, the
loads of pollution sources must be  determined.   In  many cases the load
emanating  from  a  particular  pollution source is not  monitored.   Below
are  different   methods  of estimating  pollutant  loads  from  different
sources.   The methods  take into  account  the key factors that have been
identified  as  affecting  loads   from  various   sources  and  represent
state-of-the-art knowledge in the nonpoint source pollution field.  The
methods  were  specifically  developed  for  estimating   phosphorus  and
suspended  sediment  loads, but  can  be customized  for use with  other
pollutants.
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Measured Loads

    Whenever  possible  measured  loads,  based on  properly designed
sampling  programs,  should be  used to  determine  loads  from point  or
nonpoint sources.  In most cases,  however, such information will  not  be
available, although  sampling  programs have  been  established near  the
mouths of many  large  river basins (river mouth loads  are  particularly
helpful  for  calibrating results.   This  will  be  discussed  in  a
subsequent section).

    Where information from sampling programs is available,  loads  should
be  determined  (from  flow and   concentration  measurements)  using  a
calculation technique  that accounts  for  the  importance  of high  flow
events.   An  example  of  one  such technique  is  the  ratio  estimator
technique (IJC, 1976).

    River mouth  loads used in WATERSHED  should  always be  adjusted  to
historical average flows.  A technique  for  adjusting river mouth loads
to base year conditions is given in Sonzogni et al.  (1979).

Point Source Loads

    Municipal Point  Sources:    In  most cases,  data  on municipal  point
source  effluent  loadings  will  be available  for  parameters  such  as
phosphorus  and  suspended  solids.   The  U.S.  Environmental  Protection
Agency, state governments  and many regional  planning agencies maintain
inventories of  point  sources.   While  these inventories do  not  always
contain annual  loads  for  point sources, they  usually  provide flow and
chemical concentration data which can be used to calculate  loads.

    If sufficient data  are not available to permit calculation  of the
annual  load  from a  point  source,  an  estimate  can often  be made  if
certain characteristics of the point  source  are known.   Such estimates
are  most  readily made  for municipal   sewage treatment  plant  point
sources.  Municipal  point source  loads  can be estimated  from  typical
per  capita  flows  and typical  concentrations  for  different  degrees  of
wastewater treatment  reported  in  Sonzogni  et al.  (1978)  and Heidtke  et
al. (1979).

    Industrial Point Sources:    Industrial  point  sources,   which  often
have complex wastewaters and highly specialized treatment technologies,
are difficult to  estimate  without  empirical  data.   However, industrial
inputs  are,  in  many  cases,   a   small   part  of  the  total  load  of
pollutants.   For  phosphorus inputs  in particular, it has been  shown  in
the  Great Lakes  basin  that   industrial  phosphorus inputs are  small
relative  to  loads  from  other  sources   and  can  generally  be  ignored
(PLUARG,  1978;  Heidtke  et  al. ,  1979;  Sonzogni  et  al. ,  1980).  Further,
it has been  found that industrial  toxic  metal loads  to Lake  Michigan
currently comprise a very small percentage of the  total input of  metals
from  all  sources  (Sullivan et al. , 1980).   Consequently,   the lack  of
industrial loading data may not be a severe constraint  for  many  basins.
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Urban Nonpoint Loads

    One  approach  for estimating loads  from  urban nonpoint  sources if
measurements  cannot  be made,  is to use  urban  storm  runoff models such
as "STORM"  (U.S.  Army Corps of Engineers, 1975)  or  "LANDRUN" (Novotny
et al.,  1979).   If a lack of data  precludes the  use of such models or
if   a  simpler  approach  is  desired,  annual  unit  area  loads  (UALs)
(amount  of  pollutant  delivered  per unit area  of  basin)  may be used to
estimate loads.   Typical  UALs  for  different classes  of  urban land are
presented in Table 1.  Note that the UALs are dependent on (1) the type
of sewerage system in place, and (2) the degree of industrialization.

    Table  1 presents UALs  of  total  phosphorus attributable  to  urban
runoff.    These  values  were  used  in  the  Pollution   from  Land  Use
Activities  Reference  Group  (PLUARG)  study  (PLUARG,  1978;  Johnson et
al. ,   1980) and were  derived  from  extensive data  collected  during
several pilot  watershed studies within the Great Lakes basin.

    As  shown   in  Table  1,   the UALs  from  combined  sewer   areas  are
considerably higher than those from separate and unsewered areas.   This
is because  total  phosphorus  loadings  from  combined sewer overflows are
incorporated  into the UAL estimates  for  these  areas.   To confirm these
high values,  information on  combined  sewer  areas  and overflow loadings
within  southeast  Michigan was  examined.   According  to  SEMCOG (1978),
combined sewer  overflows discharge approximately 450-600 metric tons of
total phosphorus  annually  to lakes and  streams in southeast Michigan.
The approximate urban area served  by  combined  sewers  in this region is
650-800  km  .   This converts  to a  UAL ranging  from  600-900 kg/km /yr,
and  is  consistent with the  700-800  kg/km /yr  difference  between  UALs
presented in Table 1 for combined and separate  sewered areas.

    The  effect  of industrialization  on  UALs  from  urban  land  is  also
noted in Table  1.  Because industrial activity  is  generally accompanied
by accumulations  on  the  land surface of  particulate  matter  from  stack
emissions and heavy  transportation, UALs  of  several  pollutants tend to
be higher in these areas (Marsalek, 1978).

    Developing  urban land  (construction sites)  represents  a special
case in  that  UALs of  sediment  and sediment-associated  pollutants are
generally  several times  greater  than  those  from other  urban  areas.
Johnson  et  al.  (1978)  reported a  value of 225  mt/km   of  suspended
solids per year for developing land which is 3-5 times greater than the
UAL  from   separate,  combined  or  unsewered  areas.    Similarly,
compartively  high  contributions from  developing  urban  land  have  been
reported by Chesters  et al.  (1980)  in  their   extensive study of the
Menomonee  basin  in  metropolitan  Milwaukee.   Developing urban  land
generally comprises a small portion of the total urban area, but can be
important if extensive construction is occuring.

    Table 1 gives  UALs  for urban  lands  that are  typical  of  the  Great
Lakes  area.    For  areas  of  the country where  the annual  rainfall is
significantly  different  from the  Great  Lakes   region,  UALs  should be
adjusted accordingly.
                                   96

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                                                              TABLE  1




                                                 TOTAL P110SP110RUJ  UNIT AREA LOADS




                                                          FOR URBAN  LAN!)3
i-O

URBAN LAND
a A 9°, TFTTATTOM

Combined Sewered Areas
Separate Sewered Areas
Uasewered Areas
Small Urban Areas (Sewer
system not differentiated)
Urbanizing Land
TOTAL PHOSPHORUS UAL ( kg/km2 /yr)
DEGREE OF INDUSTRIALIZATION

Low
900
125
125

250
2,500
Medium
1,000
250
—

250
2,500
High
1,100
300
—

250
2,500
                  Adapted  from PLUARG (1978).

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Rural Runoff Loads

    Ideally, runoff loads  from  each  sub-basin should be based on actual
measurements.  However,  such  data  are  usually unavailable.  Further, it
is usually not possible to distinguish the individual contributions of
different  sub-basin  land  uses  (e.g., cropland,  woodland,  grassland,
urban land) from the load  measured at  the  mouth of  the sub-basin.

    A variety  of  techniques exist  for estimating rural  runoff loads
when  direct  measurements   of  loads  are  not  available.    Various
deterministic mathematical models exist  that allow  generation of
various runoff parameters  (Heidtke, 1979;  Heidtke and Sonzogni, 1979).
These  models  —  for  example   "ANSWERS"  (Beasley  et al. ,   1977)  and
"CREAMS"  (Knisel,  1980)  —   are  applicable  only to  very  small areas.
Typically  the  models require detailed  data  that  do not  exist  for many
basins.

    Many  of  the  models  that  have been developed to  date  are based on
the  Universal  Soil  Loss  Equation  (USLE) .    The USLE  groups   factors
influencing  erosion  under   six   major  terms  that  can   be  expressed
numerically.    The numerical  values  for these  terms,   derived   from
several decades of information-gathering and  research,  have  been
established  for  specific  sites  throughout the  United States .   Several
references  exist which  explain the USLE  (e.g.,  Wischmeier  and Smith,
1978) .

    Because  the  USLE  is established  and  widely  used,  particularly in
the  evaluation of rural runoff control strategies, it is desirable to
utilize  it in  estimating  loads.   One  of  the major problems with using
the  USLE  is that it provides an  estimation of potential  gross  erosion
of  sediment  rather than  sediment yield (or  load).   Sediment  yield is
the  amount of  sediment that actually reaches the  main  channel.
Potential  gross  erosion  must  be multiplied  by  a  factor,  termed the
delivery  ratio (DR), to estimate sediment  yield.

    Unfortunately,  no  agreed-upon method  has  been derived to  estimate
sediment  delivery  ratios.   Stewart  et  al.  (1975)  indicate that the
delivery  ratio has been  observed to be roughly  inversely  proportional
to  the 0.2  power of the drainage  area  (in acres).   However, such  a
relationship,  because   of  its  exponential nature,  makes  little
distinction  in delivery ratios  for  basins over about 40  to  50  acres in
 size.   Other  factors, such  as  surface soil texture, drainage  derisity
 and  slope may  have  a more significant effect on the delivery  ratio  than
 area drained.

     The surface  soil texture may  be particularly important to delivery.
 In  the  Great  Lakes  basin,   it  has been  found  that areas   with
 predominately  clay surface   soils  often  have relatively  low potential
 gross  erosion  rates but  high  yields  of sediment  and  associated
 pollutants (PLUARG,  1978).   Although  McElroy  et al .  (1976)   have
 attempted to relate  soil  texture  to delivery ratio, the  relationship is
 not  readily usable.   Clearly,  development  of  a  widely  applicable
 equation  for  sediment  delivery  ratios to allow direct  calculation of
 sediment yield from potentional  gross erosion  remains a  major  research
 question.
                                 98

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    Potential gross erosion, as calculated from the USLE, also does not
provide  information  on  chemical  pollution  (e.g.,  phosphorus)  from
runoff.   The  amount  of pollutant  delivered is  often  calculated  by
multiplying  sediment  yield  by the  proportion  of  chemical contained in
the  sediment  and then  by  an enrichment  ratio.   The  enrichment ratio
accounts  for  the fact  that the  pollutant  yield is often  a different
percentage of  the  sediment  yield than  the  average  percent  composition
of the  pollutant in  the sediment.   Taking phosphorus as an example, an
enrichment ratio  can be used  to account for  preferential  delivery of
clay-sized particles  which,  because of their physical  properties, tend
to have more phosphorus  associated with them than larger particles.

    In  WATERSHED,  the  conversion  of  potential  gross  erosion  to  the
yield  of a  chemical  pollutant  is   accomplished  by multiplying gross
erosion by a single factor termed the "pollutant delivery ratio".  This
operationally defined coefficient groups  chemical enrichment, sediment
delivery and  other  factors  into  an overall term.   Its  use is  further
explained  in the  companion  case  study  of  the  Sandusky  River Basin
(Monteith et. al.,  1980).

    When it is not necessary or  desirable to relate pollutant yield to
USLE  factors, the  yield of a pollutant  can  be estimated directly from
UALs .   This  is  possible because a UAL  is,  in  fact,  an  estimate  of
pollutant yield, since delivery and enrichment are intrinsic to UALs.

    Several  procedures   for  estimating loads  or  yields  of pollutants
from  rural  land  are  presented in  the  following  section.    These
procedures are  based on the concepts  discussed  above.   Cropland  and
non-cropland  are treated separately.

    Rural Non-Cropland:  For  non-cropland rural  areas  such  as forests,
grasslands and  marshland,  pollutant  yields are  best   estimated  from
UALs  such as  those shown in Table 2.  The area of a particular land use
(or  use intensity)  is   simply multiplied by  the  appropriate UALs  to
estimate  the  load.   The non-cropland UALs  in  Table  2  are  based  on
Johnson et. al. (1980)  and  PLUARG (1978), but should be representative
of most areas of the  United  States  since  studies  of non-cropland areas
show  consistently  low land  drainage loads.    For  example,  in PLUARG it
was concluded that forested  and  idle  land contribute one to two orders
of magnitude  fewer  pollutants per unit area than cropland or urban land
(Sonzogni et. al.,  1980).

Cropland

    As  mentioned  previously,   determining  loads  from cropland  is
especially important,  since management  of  cropland  will offer  the
greatest potential  for  pollutant reductions  from  land  runoff  in  many
areas.  Pollutant  losses from cropland,  especially land  in row crops,
also  tend to vary  from  site  to  site more than losses from  other types
of  land.    This  variability  has  been  illustrated  statistically  by
Reckhow et al.  (1980).

    One of the principal conclusions  from PLUARG was that  land  use is
not the  only variable influencing  pollution  from land runoff.   Other
                                   99

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                                                           TABLE 2



                                              TOTAL PHOSPHORUS UNIT AREA LOADS



                                                       FOR RURAL LAND*'1
LAND USE INTENSITY

Rural Cropland
Cultivated Fields -
row crop (low animal
density)
Cultivated Fields -
mixed farming (medium
animal density)
Rural Non-Cropland
Pasture/Range - dairy
Grassland
Forest
Wetlands
TOTAL PHOSPHORUS UAL (kg/km2/yr)
TYPE OF SOIL

Sand

25

10
5
5
5
—
Coarse
Loam

65

20
5
5
—
—
Medium
Loam

85

30
10
10
—
—
Fine
Loam

105

55
40
15
—
—

Clay

125b

85
60
25
ioc
—

Organic

—

—

—
—
0
o
o
          Adapted  from PLUARG (1978).


          Unit  area  loads  may be  higher  when  soil has an unusually high  clay  content.


          Unit  area  loads  may be  higher  in  certain unique forested areas with clay  soils.

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factors  which  often  explain the  large  range  in  contributions  from
single land uses are:   land form (characteristics of  the  land  itself,
such as surface soil texture, slope  and the chemical  characteristics of
the  soil),  land  use  intensity,  materials  usage  and  meteorology
(Sonzogni et al.,  1980).  The impact that some  of these factors  have on
phosphorus losses from cropland can be  seen  in  Table  2 where UALs  from
various land uses and soils are presented.

    As can be seen  from Table 2,  surface soil texture  was  found  to  be a
particularly important  determinant.   Some  factors,  such  as  materials
usage (e.g., amount  and technique of fertilizer  application),  are  not
easily quantified for the general case,  so the values  in  Table  2  must
be tempered with  the users'  judgment and knowledge of  the  study  area.

    It is  also possible  to adjust the UALs  in  Table  2 to  account  for
differences in the  slope  of the  land.  The  effect of  slope  on  UALs is
shown in a more detailed UAL table in Johnson et al.  (1980).

    While Table 2 could be used to estimate loads directly, it is often
desirable  to  relate  cropland  loads  to  potential  gross  erosion
calculated from the USLE  (for reasons discussed  previously).   In order
to establish this  relationship,  the  pollutant  delivery ratio must  be
estimated  for  the  cropland  under consideration.   Since an  acceptable
technique for directly determining delivery ratios for cropland  has not
been established (see  previous  section), they must be  estimated using
erosion and loading data.

    Procedures  for  estimating delivery ratios under two different river
basin data packages follow:

    1.  Pollutant Yield of Sub-Basin Known (measured)

        If the load  (yield) of a pollutant  from a sub-basin is known
        from a monitoring  program,  the  pollutant delivery ratio for a
        cropland  area  is   calculated  by  first  subtracting  from   the
        monitored  load  the total  non-cropland  contributions   (point
        sources,  urban  runoff  and  rural  non-cropland runoff).    The
        resulting  cropland  pollutant   load  is  then  divided  by   the
        potential gross erosion  calculated for cropland area to get a
        pollutant  delivery  ratio.    The  following  equation  describes
        this process:

      cropland     total  sub-basin    total non-cropland          ^ '
     PDR         =  L cropland                                    (2)
        cropland    E cropland
     where:

         Lcropland ~ p°llutant l°ad (yield)  from cropland (mt/yr)

         L    n    ,  .   .   = Total  pollutant  load from sub-basin
          total  sub-basin   ..   ,   f
                            (mt/yr)
                                 101

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     L.  .  ,          ,   ,  = Pollutant load not attributable  to
      total  non-cropland        i   .  /•   /   \
                           cropland  (mt/yr)

     PDR    ,   ,  = Pollutant Delivery Ratio  for cropland
        cropland    , ,.     •   ,    \
                   (.dimension less;

     E    1   ,  =  Potential gross  erosion  for total  cropland area
      crop an    (mt/yr)
                    i   j,  which  includes  contributions  from  such
           non—cropland
    sources as point sources, urban runoff  and  rural  non-cropland,
    may be  estimated  (when  not known)  from techniques  described
    earlier.

2.   Pollutant Yield of  Sub-Basin Not Known

    In the majority  of cases,  loads  from sub-basins will  not  have
    been measured.   In these situtions  several  techniques can  be
    used for  estimating delivery ratios.

    Perhaps  the  simplest  means of  getting a  pollutant  delivery
    ratio  is  to  use the  value from  a  monitored  sub-basin  with
    similar characteristics.  If the  pollutant  delivery ratio can
    be calculated  for  one sub-basin using  the  procedure  described
    above, this delivery  ratio  could  be  used for other  sub-basins
    which are expected  to behave similarly.

    Another straightforward technique  is  to  estimate cropland  loads
    based on  the  sub-basin cropland  area and  an appropriate  UAL,
    (for  example,  as given  in  Table  2).   The pollutant  delivery
    ratio is  then  calculated from equation 2.

    Finally,   it  is  possible  to calculate  a  cropland  pollutant
    delivery  ratio when  the  load for  the entire basin  (as opposed
    to  sub-basin)  is known.    Such  data  frequently  exist,  since
    monitoring programs  near river  mouths  are common.    In  this
    case,  the  total non-cropland  load  for the  entire  basin  is
    subtracted from the total known pollutant load  at  the  mouth to
    give  the cropland  load  for  the  basin.   The cropland  pollutant
    delivery  ratio is then calculated  by  dividing  the  cropland  load
    by the cropland  total  potential  gross erosion  (mt/yr).   These
    calculations  are analagous  to those  illustrated in  equations 1
    and 2  except  that  they  are carried  out for  the entire  basin
    rather than a  single  sub-basin.

    The resultant  pollutant  delivery  ratio  is  thus an  average for
    the entire basin.   This pollutant delivery ratio can  be  used
    for each  of the sub-basins,  provided  the characteristics of the
    sub-basins  (e.g.,   soil texture)  are   similar,  and  provided
    upstream  pollutant   inputs  do  not   undergo   significant
    transmission  losses before  reaching the  river mouth.
                            102

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Other Sources of Pollution

    Septic Tanks:  Private  waste  disposal  systems or  septic  tanks are
often implicated as  a  source of pollution in  rural  or unsewered urban
areas.  However, most field investigations have shown that only a small
percentage of  the  total  pollutant  input to  a river  basin  comes  from
septic tank discharges (Jones and Lee, 1979;  Krause and Pilling, 1979).
For  phosphorus  in  particular,  septic  tank  discharges  are  generally a
very small part of the phosphorus load from all sources, even in basins
with sandy soils.

     In  order   to  estimate  septic   tank inputs  of  pollutants for  a
sub-basin, an  annual per  capita  contribution should  be  multiplied  by
the  number of  residents  in  the sub-basin using  malfunctioning septic
tanks.   If the  private waste disposal units  are  used only seasonally,
an appropriate correction should be made.

    A  per capita  contribution of  about  1.5 kg/ha-yr  appears to  be
typical of most  septic tank operations (Reckhow et al., 1980).  Where a
detergent ban is in  effect, the per  capita  input may be  lowered by 30
to 40 percent.  Septic tank inputs are treated as a point source in the
WATERSHED process.

    Streambank Erosion:   Streambank  erosion  was extensively  studied
during PLUARG,  but  was found to  account for only a  small  part of the
total sediment  load  to the  Great  Lakes.  The  phosphorus contribution
was  found to  be even less  significant relative  to  other  sources since
Streambank materials tend to be lower in phosphorus than topsoil eroded
from fields.   Even the  Streambank erosion  sediment  contribution to the
Cuyahoga River,  once  thought  to be very  significant  relative to other
sources, has  been found to be small according to preliminary results of
a study of Streambank  erosion  along  the  river (Urban,  1980).   In  most
situations,  then,  Streambank erosion  should  be  ignored  as  a separate
pollutant source.

    Feedlots:   Feedlots  can  be a significant  source of  pollution  in
rural  areas  and should  be assessed  in a  basin  analysis.   Various
techniques exist to estimate   feedlot contributions,  which  depend  on
factors such as  the  number and types of  animals  using the feedlot and
its physical  layout.   Studies done on contributions  of pollutants from
feedlots  show  that  the  amounts  vary widely (Reckhow et  al. ,  1980).
When it is suspected that  feedlots in  a  sub-basin may be  important but
their contributions  are not  known, their relative importance can still
be assessed through WATERSHED by considering  a range of assumed values.
If, for example, the maximum  likely  value  (such  as might  be determined
from Reckhow et al.,  1980) is found to result in a low or insignificant
pollutant load compared to  other  sources, the contribution of feedlots
may  be  neglected.   Likewise,  if  the minimum UAL produces  significant
contributions,  then  feedlots  need   to  be given  more  attention  in  a
pollutant control program for the basin.   Feedlots should be considered
as point sources in WATERSHED.

    Miscellaneous Sources:  Additional sources of pollution  to a river
basin include landfills and other waste disposal  areas, sludge disposal
                                 103

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sites, mining  operations,  chemical  storage areas,  lagoons,  and  land
areas used  for  wastewater  application (e.g., spray  irrigation  sites),
recreational land, and wildlife (e.g.,  large geese  concentrations).   In
most  cases, loads  from  these  sources are small compared to loads  from
land  runoff  (PLUARG,  1978).    In  cases  where  one  or more  of  these
sources are suspected of being  significant, an estimate can be made  of
their pollution contribution and their relative importance assessed  in
the WATERSHED  process,  since  WATERSHED is flexible enough to consider
any sources desired.   When  an  estimate of a load  cannot easily be  made,
a  likely  range  of loads (maximum  and  minimum loads)  can be estimated
and the importance assessed under  either  extreme.  For example,  if  the
maximum load expected  is low  compared to that from  other sources,  the
source in question can be ignored.
                        BIOLOGICAL AVAILABILITY

    A  portion  of  the load of  certain  pollutants  may be in a  chemical
form  that  does  not  stimulate biological  growth.   In  the  case  of
phosphorus, a  substantial  portion  of the total phosphorus load may  be
in  a  form unavailable  for  biological  uptake.    Availability  is
especially  important  when  comparing the cost-effectiveness of  control
alternatives.   Otherwise,  funds  could be  wasted  on  controlling  a
pollutant that does not substantially affect  water quality.

    While  information  on  availability  is presently  incomplete,  enough
information  does   exist,   particularly  for  phosphorus,  to  make  some
generalizations that can  be  applied  in  WATERSHED.   Sonzogni  et al.
(1980) recently  reviewed the  existing  information on  phosphorus
availability.  Table 3 is based on their review.

    Table  3  shows  that the  bioavailability  of  phosphorus  in  runoff
water  is  consistently  low.   In contrast, phosphorus  in  municipal  point
source  discharges  is  largely available,  at  least  compared  to  other
sources.    Based  on  limited  data,  the  type  of   sewage  treatment  or
phosphorus  removal practices does not appear  to affect the  bioavailable
fraction  of phosphorus in the effluent.

    Because  the  bioavailability  of  phosphorus  between  point  and
nonpoint  sources  seems to differ  widely,  it  is  important  that  it  be
considered  in certain cost-effectiveness  factors.   In WATERSHED,  the
bioavailable  pollutant  load  from a  particular source is estimated  by
multiplying the  total  load  from  that  source  by  the  bioavailable
fraction.    Since  the  bioavailable  fraction will  almost  never  be
established for an  individual  source,  the value must be estimated.  In
most  situations,  it  is  advisable  to  assume  a  range  of  bioavailable
fractions  to ascertain  the sensitivity  of the  results  to  these
different  assumptions.
                                 104

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                            TABLE 3

       GENERALIZATIONS ON THE AVAILABILITY OF PHOSPHORUS

                 DERIVED FROM DIFFERENT SOURCES

              (Based Mostly on Great Lake Studies)
Form and Source

Particulate P in
River Water

Total P in River Water

Particulate P
in Urban Runoff

Total P in
Rural Runoff

Total P in Municipal
Point Source Discharges
Approx. % Available Phosphorus

      40 or less


      50-60 or less

      50 or less


      50 or less


      70 or more
                             105

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                        DOWNSTREAM TRANSMISSION

    Once the pollutant inputs have been  identified  and  quantified,  the
loadings from all  sub-basins  must  be routed downstream from  points  of
entry to the receiving water  (river  mouth).   As  discussed  previously,
each reach of the river (section of  river between two points  of entry)
has  a  transmission coefficient   (t)  associated  with  it.   This
coefficient represents  the fraction  of  pollutant  load  which  is
transmitted between  adjacent points  of entry.   For any given  entry
point, the  "effective transmission"  (T)  is  defined  as  the  fraction  of
the  total   pollutant  load  at that  point   which  is  delivered  to  the
downstream receiving water.   In other words, "T"  is the product of  all
downstream transmission  coefficients  "t".

    The concept of transmission is further  illustrated in  Figure 2.   If
the  transmission  coefficients  t,  and  t~   assume  the  values  0.5  (50
percent of  the pollutant  load entering  point  A is lost  by  the  time  it
reaches point B)  and 0.8 (20 percent  loss),  respectively,  the  effective
transmission of the  pollutant  load entering  at  point A  (T.) would  be
0.4 (T. = 0.5 x 0.8).   Thus,  if  the  pollutant load  introduced at point
A  were 100  mt/yr,   only  40  percent,   or  40  mt/yr,  would  reach  the
downstream  receiving water.    At   point   of  entry  B   the  effective
transmission T_ is the same  as  the transmission  coefficient (t_) since
there are no further downstream transmission  losses .    Thus ,  the total
load to the receiving water  in Figure 2 is  104 mt/yr.

    Importantly,   if  a control  program  reduced  the pollutant  load  at
point  A  by 50   mt/yr   (50  percent  reduction) ,  the  resultant  load
delivered to the  receiving water would  not  be reduced by  50 mt/yr.   As
the example in Figure 2  illustrates, the annual  load at  the  receiving
water would  be  reduced  by only  20 mt/yr.   The  new load,  as  shown  in
Figure 2, would be  84 mt/yr.  Accordingly,  if the  effectiveness of a
control is judged by the  amount of pollutant  reduction  achieved at  the
receiving water,  transmission is a salient  consideration.

    For some pollutants,  including phosphorus, transmission losses  are
often  small, especially  over the  long  term (PLUARG,  1978; Verhoff  et
al . ,  1978) .   This  is particularly true when  a  large  fraction of  the
pollutants under  consideration are associated  with  clay-size  particles
which are easily  suspended and transported.   In  most  cases, only those
tributaries with  large impoundments  or  large  flood  plains will  require
adjustments for transmission.

Summary of Load Calculation  Technique

    The load at the  river mouth  (or  some point  of  entry)  is  expressed
mathematically below.

    Pollutant Load at the Lake =
      N
      2t(L- x BF)    ,    , + (L. x BF)    ,          .    ,+  (L. x BF)  ,
            i      cropland     i      rural non-cropland   i      urban
                                                                  ran3
    1   1
          + (L. x BF)  .         ...+ (L. x BF)  ,           ]  x T.
              i      point source        i      other sources     i
                                         (3)
106

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                                  FIGURE 2
                  EXAMPLE  OF TRANSMISSION LOSS CALCULATION
        Load to River
                                 Points        Transmission        Effective
                                of Entry      Coefficient (t)  Transmission (T)
       L  = 100 mt/yr
        A
          = 80 mt/yr

1 VN
^

\

t
V

I
Receiving
Water
t.-O.S

t2 = 0.8


        RW
where   L
        L
         .,
         B
             (LA X V + (LB X TB)
             (100 x O.A) + (80 x 0.8) = 104 mt/yr
             Total Pollutant Load to Point of Entry A
             Total Pollutant Load to Point of Entry B
             Total Pollutant Load to Receiving Water
If control strategy reduces the L  by 50% (i.e., 50 mt/yr),
       then the new load (L_., ) is
                           RW,
      LRW  = (50 x 0.4) + (80 x 0.8) = 84 mt/yr
LRW   LRW,
             104 - 84 = 20 mt/yr
      .'. a 50 mt/yr reduction to entry point A produces only
          a 20 mt/yr reduction at the receiving water
                                      107

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    where:   L = loads  from  different  sources  to  a  specific point of
                entry,

           BF = Bioavailability  Factor,

           T. = Effective  transmission  from point  of  entry to mouth,
                and

            N = number of  points of entry.
    Note  that  more  than  one sub-basin  and  point  source may be
discharging to a single point  of entry.   For example,  the  cropland  load
to point  of  entry  "i" in equation 3 may  be the sum of cropland loads
from several  sub-basins.

Calibration

    One way  in  which  WATERSHED can be  calibrated  is  by  adjusting  the
transmission   coefficients  such that  the  calculated  loads  correspond
with  monitored  loads.   This  was done  successfully  in  the  overview
modeling  project  (Johnson  et  al.,  1978)  discussed earlier.   In  most
cases  (about 75 percent  of  the  time  for  U.S. waters),  transmission
adjustments  were  not  necessary.    However, when  they  were  necessary
(mainly for Lake Michigan),  an impoundment or lake-like  widening  of the
river was usually present.

    In order to account for  year-to-year differences in  pollutant loads
from a river basin  caused by meteorological  or  climatic  factors, loads
estimated through WATERSHED should  be calibrated  with  historical
average monitored loads whenever  possible.   Calibration  using data for
any  single year could be misleading if that year  was  a high- or  low-
flow year.

    Sonzogni et al. (1978)  have described a technique to adjust loads
for any one  year to "average"  conditions.   The  technique is based  on  a
historical  average  flow  computed   from  gaging  station  records.
Pollutant  loads are then adjusted to average conditions  in proportion
to flow.  The technique thus assumes that load  is proportional to flow.
This  approach  is  most  applicable  on  a  gross  scale  and  may not be
appropriate  for a  small  river basin.   However,  simply  considering the
range  in  annual flows  can  provide a  qualitative  appreciation of the
variability  expected   in  diffuse  inputs  due   to  meteorological  (and
runoff) conditions.   This may often be sufficient for  making WATERSHED
management decisions.

    In  calibrating results,  the  transmission  coefficient  is not  the
only  variable  that  can  be  adjusted.    The  values  of a  number  of
variables  used  in  the process  can be  changed to more  closely align the
calculated load with  the monitored  load.   Even  if  estimated loads  from
WATERSHED  cannot be easily  calibrated due to a  lack of monitoring data,
the  results  are still useful  for assessing  the relative importance of
different  pollutant inputs  and for determining  the sensitivity  of the
pollutant  loads to  different variables.
                                 108

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                           CONTROL STRATEGIES

Formulating Strategies

    At  this  point,  strategies  to reduce  pollutant  loads  can  be
developed.    Of the  different  strategies  identified for each  source,
one should  be  selected  for initial  testing.   Other strategies may  be
evaluated in subsequent WATERSHED analyses.  A  strategy may be  staged;
that  is,  it may consist of one  or  more incremental control  programs.
Similarily,  a control  program may  consist of  one or  more  specific
remedial measures.

    A  staged  approach,  whereby each program  builds upon the  previous
one,  is  designed to  allow for an  incremental  control  strategy.   For
instance,  a municipal  point   source  control  strategy  for  phosphorus
might  consist  of  three  stages  of chemical  phosphorus control.   Stages
I, II  and III might be  treatment  to the 1  mg/L, 0.5 mg/L and 0.3  mg/L
phosphorus  effluent  levels,  respectively.   Stage  III  could  not  be
implemented  before  Stage  II,  and  Stage  II could  not  be  implemented
before  Stage  I.  However,  it  is  possible that Stage  I and II  point
source control  programs  should be implemented before either a  Stage I
cropland or Stage I urban runoff control program.

    The  flexibility of  WATERSHED  also permits  the user  to  design  a
remedial  program  that   is comprised   of   several  different   specific
control measures, only some of which would  be used  at a  specific  site.
In combination, the control measures would  provide  an average  level  of
pollutant reduction at an  average cost.  Such  a combination of  control
measures  is likely  to  be  needed for  treating  runoff  in a  sub-basin,
since  "across-the-board" runoff control programs are more the  exception
than  the  rule.   For  example,  to  decrease the pollutant  contribution
from  a cropland  area, several  different tillage variations may  be  used
on  individual  farms  in the  area,   depending  on  factors  such  as  the
farmer's  preference,   type   of cropland,  and   the   site-specific
characteristics of the land.

    It  should  be apparent  that  considerable judgment  is required  in
formulating  strategies  on control programs that  are tailored  to
individual  situations.   It  is  important that  the water  quality  manager
be  familiar with  the  control measures  selected  for each strategy  and
know how the controls  relate to one another.

Costs  and Load Reductions

    In estimating the costs  of and  pollutant load  reductions  achieved
from  various  control  programs, only general  guidelines  can be  given.
The planner's or manager's judgment  and experience  is an  important  part
of  the process.    Studies  being conducted  should  soon  provide  more
information  on  the  cost  and  effectiveness of  controls.   The  authors
intend to  provide  a more  detailed  assessment  of  this  topic in  future
work.  In  the meantime,  the information given  below (predominately  on
phosphorus) summarizes much of the  current research.  The  information
will be applied in the companion case study (Monteith et  al.,  1980).
                                 109

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    Point Source:   Various  options  for  point  source  phosphorus  control
are  given  in  Table  4.    As  explained  in  the  previous  section  on
formulating   control  strategies,   som.e  of the  controls must  be
implemented in a hierarchical  fashion.   The load  reduction  achieved  by
these measures  will  depend  on  the  phosphorus  concentration  before
treatment.   In  the  Great  Lakes  basin,  the  average  phosphorus
concentration in treated municipal wastewater from  facilities  with  no
phosphorus control  program  is  about 4 mg/L P (Sonzogni et al.,  1978).

    Costs  for  point  source controls  are perhaps better defined  than
controls  for  other  pollution  sources.    Although  municipal and
industrial wastewater  treatment  plants  use  a  variety of  treatment
processes, most  have been  used  for a  number  of years  and are  well
defined  economically.   Consequently, reasonable  cost estimates  can  be
made for most treatment schemes.  Cost  data may  also be available from
information developed under Section 208 of  the  Federal  Water Pollution
Control  Act   of 1972  and  from   information developed  by  the  U.S.
Environmental Protection  Agency.

Urban Runoff  Controls

    Although many measures  have  been  identified for  controlling
pollutant  loadings  from  urban runoff  (IJC,   1977), the  cost and
effectiveness of most have  not been quantified.   Table 5 does,  however,
provide  some  cost-effectiveness data developed  for  PLUARG.  The  U.S.
Environmental Protection Agency is  currently  sponsoring the Nationwide
Urban Runoff Program (NURP) which  will determine  the effectiveness and
costs of various urban  control practices.  Initial results are  expected
within  the  year, although  it may  be  another  three years  before the
program  is completed.  This study  is  expected to provide  an excellent
source of information for use  in WATERSHED.  Studies done under  Section
208 of the Federal  Water  Pollution  Control Act of 1972 may also  provide
useful   information,  since  they  have  focused  on nonpoint   source
pollution during the  last few  years.

Rural Nonpoint Controls

    Most control measures for  rural land have focused on cropland, and
these,   rather  than  controls  for  rural  non-cropland  areas, are
considered here.

    One  of the  main  reasons for  relating  cropland  loads  to potential
gross erosion as calculated from  the USLE is the available information
on how control measures affect potential  gross erosion.  In particular,
an extensive literature exists on  how control measures  such as  tillage
practices  and  crop  rotation  affect  the   cover factor   (C).    Some
information  also  exists  on how measures  such  as contour  plowing and
strip-cropping will  affect  the practice  factor   (P)   and  how terracing
can affect the slope/length factor  (SL) .

    Table  6  provides  data  for  several  cropland  control programs
according  to  some  of the recent  findings  of studies  such  as  the Lake
Erie Wastewater Management Study  (Urban et  al.,  1978),  the Black Creek
                                110

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                                           TABLE 4

                                 COSTS OF PHOSPHORUS CONTROL

                          AT MUNICIPAL WASTEWATER TREATMENT PLANTS
                                                                      COST
CONTROL PROGRAM                                                    ($/cap/yr)

1.  Reduction of total phosphorus effluent concentration
    from a "no phosphorus treatment" condition ('v- 4 mg/L)
    to 1.0 mg/L by chemical treatment3                                2.4

2.  Reduction of total phosphorus effluent concentration
    from 1 mg/L  to 0.5 mg/L by chemical treatment"                   3.6

3.  Reduction of total phosphorus effluent concentration
    from 0.5 mg/L to 0.3 mg/L by chemical treatment/filtration        4.0
                                        (2
4.  Land treatment by rapid infiltration

5.  Land treatment by slow rate irrigation
    f\
      Estimate derived from Drynan (1978) .

      Estimate derived from Heidtke et al.  (1979).
    Q
      Because all other costs  assume  conventional secondary treatment
      facilities in place,  comparative costs  of  land application systems
      are not presented here;  for  further discussion see Heidtke et al.  (1980)

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                                                            TABLE 5




                                          COSTS AND TOTAL PHOSPHORUS LOAD REDUCTIONS




                                              FOR URBAN RUNOFF CONTROL PROGRAMS3
CONTROL
PROGRAM
Streetsweeping plus
Measures to Reduce Flow
Streetsweeping plus
Detention/Sedimentation
of Stormwater and
Combined Sewer Overflows





URBAN DIFFUSE SOURCES
COMBINED
SEWERED
AREAS
% UAL
Reduction
6


30
$/km /yr
7,400


32,100






SEPARATE SEWERED AREAS
HIGH INDUSTRY
% UAL
Reduction
20


40
$/knT/yr
7,400


16,000






MEDIUM INDUSTRY
% UAL
Reduction
25


45
$/km2/yr
7,400


16,000






LOW INDUSTRY
% UAL
Reduction
50


65
$/km2/yr
7,400


16,000
ro
           Adapted from Table 11, Johnson et al. (1978).

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                                                   TABLE 6

                                         COSTS AND LOAD REDUCTIONS

                                FOR RURAL RUNOFF PHOSPHORUS CONTROL PROGRAMS



CONTROL
PROGRAM
Voluntary Sound
Land Management
Chisel Plowing;
Mulch-Till; Winter
Cover Crops; Crop
Rotations
No-Till; Crop
Rotations













RURAL DIFFUSE SOURCE
CROPLAND
% Reduction
in Potential
o
Gross Erosion

—



50-60

60-90
Pollutant
Reduction
Efficiency

—



.6-. 9

.6-. 9
% Reduct ion in
Total Phos-
phorus Load

0-10



30-55

35-80


$/km2/yr

Minimal


A
65d

3,000e












OTHER AGRICULTURAL LAND
% Reduction in
Total Phos-
phorus Load

0-10



—

—


$/km2/yr

Minimal



—

—
Based on changes in average county "C" factors (crop management factor in the USLE) as given in Urban et al.
(1978).  Percent reductions assume all other USLE variables remain fixed.

Estimate of the extent that the phosphorus load is decreased from a given decrease in gross erosion; values
derived from LEWMS Preliminary Feasibility Report (U.S. Army Crops of Engineers, 1979).

These measures (properly incorporating fertilizers into soils; avoiding farming on slopes near streams) may
not affect erosion in cropland areas.

Estimated cost of providing technical  assistance and demonstration plots for education in new tillage practices.
Cost estimate derived from U.S. EPA (1979)  — a modeling study of the Black Creek watershed in northeastern
Indiana.

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Study  (Beasley et al.,  1977)  and  the  PLUARG  study  (PLUARG,  1978).
Losses  in potential  gross  erosion are  based on  changes  in  the  "C"
factor due to tillage or crop rotation practices.

    Note  that  the  first  control  program —   "voluntary  sound  land
management" — does not show an associated reduction in potential gross
erosion.    This  program  includes  measures,   such   as  properly
incorporating fertilizer into the soil, which  may have  little  effect on
potential gross erosion.

    For  the   second  program  in  Table 6   (chisel-plowing,  mulch-till,
winter  cover  crops,  crop  rotations),  the cost  is  based primarily  on
technical assistance.   Technical assistance  as  defined  here  includes
the  operation of  several  demonstration plots  to  illustrate  the
effectiveness  of  the new  practices.   Although  research continues  on
this  subject, it  is  assumed here  that  this  set  of  measures  can  be
implemented with no net  loss  of  income to the farmer.    The only cost,
therefore, is the technical assistance required to train  farmers  in new
tillage   methods.   The  Black Creek (Indiana)  and  Honey Creek  (Ohio)
demonstration programs haye shown how important technical assistance is
for these measures to  be  effective.   Technical  assistance would  likely
only be  required for  a  short  time  (three  to  five years), since farmers
would tend to  share their  experience with  other  farmers  in  the area if
it is successful.

    In  calculating the technical assistance program, it is assumed that
three   years  of  demonstration  and   intensive  assistance  would  be
sufficient to convince  farmers  to adopt the proposed measures.   It  is
also  assumed  that  the technical assistance program would affect about
35,000 ha.

    Table 7 further illustrates how costs  for  technical assistance were
derived.   Salary and overhead, demonstration plot  costs  and  equipment
rental  costs  are  all  estimated.   The  total cost is amortized over  25
years at  a 10 percent  interest  rate  to give  an annual  cost  of $23,000.
If  this cost   is converted to a  unit  area basis,  the annual cost  is
$0.65/ha  ($65/km )  assuming 35,000 acres are actually influenced  by the
technical assistance.   It  is  possible,  for example,  that up to 200,000
ha would  be  influenced at the above cost.  If  that were the  case, the
cost of technical assistance would be reduced  to $0.12/ha.

    The above  costs  were  generated  for  the  northwestern  Ohio area,
based  on preliminary data  for  this  area  (Honey Creek Joint  Board  of
Supervisors,  1980;  U.S. Environmental  Protection Agency,  1979).   The
cost  estimate is  admittedly only a first  approximation,  and  is  likely
to be modified when better data become available.

    The third  program  in  Table  6  involves  the  application of  more
intensive  conservation  tillage  practices (i.e.,  no-till  where soils
will  allow it) .  The  percent reduction in  total  phosphorus loading from
cropland  runoff — 85  percent — was also indirectly  estimated  from
changes in "C"  factors  specified for northwestern Ohio by the U.S. Army
Corps  of Engineers   (1979).   The estimated  incremental  cost  for
implementing  Stage  II control  is $3,000/km  /yr  (U.S.  Environmental
Protection Agency, 1979).
                                 114

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                 TABLE 7

ESTIMATION OF TECHNICAL ASSISTANCE COSTS
  FOR IMPLEMENTING THE MINIMUM TILLAGE
        AND CROP ROTATION PROGRAM
  - 125 ha of demonstration plots
  - 3-year program
  - Goal of 35,000 ha.converted to minimum till
           - Salary and overhead       $ 38,500/yr
           - Demonstration Plot Costs  $ 25,000/yr
           - Equipment rental          $  6,500/yr
                           TOTAL:      $ 70,000/yr

  3-year study     TOTAL               $210,000
  10% interest amortized over 25 years $ 23,000/yr
  Cost per ha considering only demon-
  stration plots $23,000/yr •* 125 ha   $ 184/ha-yr
  Cost per ha if 35,000 ha converted
  to minimum till $23,000/yr -t 35,000
  ha                                   $ 0.65/ha
                 115

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Pollutant Reduction Efficiency

    A  pollutant  such  as  phosphorus may  not  be  reduced  to  the  same
extent as potential gross erosion following implementation of a control
measure.   Some control  measures  could conceivably  result in  a  large
change in potential gross erosion with little change in pollutant load.
To account  for  this,  a new term, the  "Pollutant  Reduction Efficiency"
(PRE), is introduced in Table 6.  The pollutant reduction efficiency is
defined as the extent that a pollutant load (yield) is decreased from a
given decrease in potential gross erosion.

    In order  to calculate  the  effect  of  pollution reduction efficiency
on the load, the following equation is used:

    LR = LI - [(E].-ER) x PRE x PDR]                                 (4)

where:

    L  = reduced pollutant load (due to runoff controls),

    LT = initial pollutant load,

    E, = initial potential gross erosion,

    ER = reduced potential gross erosion,

   PRE = pollutant reduction efficiency,  and

   PDR = pollutant delivery ratio.

    The  use  of  equation 4  will be  demonstrated  in  the case  study
companion paper.

    According  to  studies  of  conservation tillage  in  the Lake  Erie
basin, the  relationship  between  potential  gross  erosion and phosphorus
load  as  affected  by  cropland  runoff  control  programs  can   only  be
estimated.    However,  based on  limited  information,  the  decrease  in
phosphorus  yield  from  a  given  decrease  in  potential gross  erosion
appears to  be between 60 to 90 percent  (U.S.  Army Corps of Engineers,
1979).  More research will have to be done on  this subject in  order to
expand the usefulness of the USLE as a water quality management tool.

    Control measures may also  have varying effects on the bioavailable
fraction  of  a given  pollutant.   For  example, two measures may cause
identical  decreases  in the  total  phosphorus  load but different
decreases in the available phosphorus fraction.  This could result from
one measure having a greater effect on the soluble phosphorus  fraction.
The difference  would  have to  be  accounted for  in the bioavailability
factor in the WATERSHED process.

    Presently, almost no field data exist  on how control measures might
affect  bioavailability.    About  the best  that can  be  done is  to  use
sound  judgment,  tempered with a  knowledge of how  the  control measure
may effect the chemistry of the pollutant.
                                 116

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    Substantial new  information  on the cost-effectiveness of  cropland
runoff control measures is expected soon,  especially with regard  to  the
economics  of  conservation  tillage  practices.   With rising fuel  costs,
many farmers may find it desirable to convert  to a conservation tillage
system,  making the  implementation  of  these systems easier than
originally  anticipated.    Further,  preliminary results  from the Lake
Erie Wastewater Management Study's  Honey  Creek Demonstration  Project
(Forester  et  al.,  1977;  Forester,   1978;  Honey Creek  Joint Board  of
Supervisors, 1980) show that costs can be  reduced and farm productivity
may  actually  be   increased  if  farmers  in   that  area  adopt   no-till
farming.  The net result could be an increased profit for farmers and a
concomitant reduction in the nonpoint loads  from their farm lands .

    It  should  be  clear  that  Tables 4, 5  and 6  are  only examples  of
programs that  can  be  formulated.  Options other than  those  given here
may be  appropriate  for  a  certain  location.   The tables  do  illustrate
the type of cost and  pollutant reduction  information  that is necessary
to characterize a control option or program.

Cost Effectiveness

    The  goal  of WATERSHED is  to compare  the  cost-effectiveness  (cost
per  unit  reduction   in  pollutant  load)  of   reducing  pollution from
different  point and nonpoint sources  in a basin.   The option with  the
lowest   cost   per  unit  reduction  in pollutant  load  is  the most
cost-effective.

    For  comparison  purposes, cost-effectiveness is generally best
measured  at  the   receiving water   (river  mouth).    Once   the   cost-
effectiveness  at  the receiving  water  is  known for  each stage of  a
control  strategy   developed  for  a  particular pollutant  source,  the
stages   of  the strategy  can be   ranked according  to their  cost-
effectiveness.  For example, if a control  strategy with three stages  of
control  were  devised  for  each  of  ten pollutant  sources in  a  river
basin,  a total of  30 different  control stages  could  be ranked.

    Note that  each staged  program  of a strategy can  consist  of  either
one control measure or a combination  of control measures.  For  a given
strategy, Stage II can never be  ranked higher than  Stage I,  Stage  III
can never  be  ranked  higher than Stages I or  II,  and so  forth,  due  to
the dependence  of a  stage on previous stages.   However, a Stage  II
point source  control  could be  ranked higher  than  a Stage   I  cropland
control.   In  other  words, WATERSHED  allows   for  comparing  different
stages  of point and non-point  control strategies.

Accounting Techniques

    To   simplify tracking  all   the  inputs  and  load  reductions,   and  to
ultimately rank the  cost-effectiveness of  different  strategies, some
kind  of  an  accounting  system  is  needed.    While  a  computerized
accounting  system  has  been  developed,  a  system  of  worksheets has
recently been  devised  which clearly  shows how to  apply  the WATERSHED
process.   This  approach  can be used efficiently with a calculator.   A
programmable  calculator  could  simplify  the  accounting  process even
more .
                                 117

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    The worksheets are  straightforward  yet  flexible,  and are  somewhat
analogous to an  income  tax  form.   Their use is demonstrated in  a  case
study of the Sandusky River  (Ohio)  in the companion paper by  Monteith
et al. (1980).

Long-Term Value of WATERSHED

    A major advantage  of  the WATERSHED  process  is  that  it   can
accommodate a  large  and  dynamic data base.   As criteria  change  or new
detailed information becomes available on such  factors  as  effectiveness
of control programs or the costs of remedial  programs,  WATERSHED may be
used  to  reevaluate  which  pollution  control  programs   offer  the  best
results  for  the tax  dollar.   Once  the  river  drainage basin has  been
mathematically described and  the  loads  from  all the pollutant  sources
mathematically  defined,   the  basic   information  exists  to  test   any
assortment of  remedial  strategies  or to  determine  the sensitivity of
the results to a modification of a given variable.   Thus,  the  WATERSHED
analysis is a  planning tool which will  have  many applications  and  will
form the basis  for long-term river  basin management.

Multiobjective  Analysis

    Currently,  the WATERSHED process  considers only one pollutant  at a
time.  However,  it is recognized that control  strategies  may,  in fact,
affect more than one  pollutant.  For  example,  removing  phosphorus  at a
municipal wastewater treatment plant may concurrently reduce discharges
of  biochemical  oxygen   demand,  suspended  solids,  toxic metals   and
viruses.   Ideally,  a multiobjective analysis  should  be  performed  so
that  the  cost  of  the   total  phosphorus  control  program   could  be
evaluated against benefits (or  costs) other  than just  those associated
with  phosphorus  reductions.   Simon  (1980) has  made an  initial  attempt
at  this  by modifying  the  overview  modeling  approach of  PLUARG
(discussed earlier) with a parametric nonlinear optimization  technique.
Consequently,   he  was   able  to  consider  the  control of  several
pollutants.  Further,  Chapra and Wicke  (1980)  have made some  initial
steps in this  direction.  The  authors intend to address multiobjective
analysis in upcoming work.

Load Allocations

    If a load  limitation has been  imposed on a particular river basin,
WATERSHED can  be used to  determine  the  most  cost-effective combination
of strategies  to achieve the desired  pollutant  load.   However,  in  very
few cases have pollutant loads been' allocated to river  basins .   Even in
the  Great  Lakes  basin,  where so-called  "target  loads"  have  been
suggested  for   the   individual  lakes,  there  has   been no  attempt  to
allocate portions  of the lake  loads  between  the  U.S.   and Canada, let
alone individual river basins.

    Although  load  objectives  may not  exist  for  a river  basin,  the
planner or manager may want  to  consider what control  strategies should
be  given priority  because  they produce  high  load  reductions  at low
cost .   Such  strategies  would  be  implemented   to  reduce  pollution in
general,  rather  than to achieve a  certain  allocated  load.   WATERSHED
can,  of  course, be  a very  useful  tool  for  the planner  or manager in
this  situation.
                                 118

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    If  water  quality  improvements  are  to  be  made  in  increments,
WATERSHED  can,  based  on  its  cost-effectiveness  ranking,  show  which
measures  should be  done first.   The planner or  manager  must  rely  on
information  other  than  WATERSHED,  since  control measures  will  have
benefits  and costs  other   than  those  considered  in  WATERSHED.    For
example, many  nonpoint control measures  improve  soil  conservation  as
well  as  water  quality.  Consequently,  some  nonpoint  control  measures
should  perhaps  be  implemented  as  a  soil  conservation  measure  even
though it has little effect on water quality.

    As mentioned above, so-called target loads for phosphorus  have been
suggested for the Great  Lakes.  However,  as discussed in Sonzogni  et
al. (1979),  these loads  are best used only  as  long-term  goals.   It  is
better  to make  water  quality  improvements  step  by  step,  based  on
economic  as  well  as  environmental  considerations.  One  rationale  for
this  approach is that water quality degradation is often reversible,  so
that  receiving waters often are  not irreversibly harmed  if all
pollutant inputs  are  not  immediately controlled.   This  is  especially
evident in the way lakes have responded  to  phosphorus input reductions.
The effects of some toxic  substances (for example, DDT) have  also been
shown  to  be reversible  (Sonzogni and  Swain,  1980).   The  reversible
nature  of  water  quality   degradation  is  of  great  significance  to
management,  particularly when funds for  pollution control  are  limited.
                                  1 19

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                               REFERENCES
Beasley, D.B.,  Monke,  E.J.,  and  L.F.  Huggins  (1977).   "The ANSWERS
    Model:   A Planning Tool  for  WATERSHED Research,"  American Society
    of Agricultural  Engineers,  Paper  No.  77-2532,  St. Joseph, Mich,

Chapra, S.C.,  and H.D.  Wicke (1980).   "Least Cost Optimization to Meet
    Phosphorus Objectives  in  the Lower  Great  Lakes,"  Contribution to
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    Environmental Research  Laboratory (NOAA), Draft.

Chesters, G.,  Konrad,  J.G., and G.V.  Simsiman (1980).   "Menomonee River
    Pilot WATERSHED  Study  -  Summary and  Conslusions,"  Draft Report,
    University of Wisconsin Water  Resources  Center, Madison, Wisconsin,
    77 pp.

Drynan, W.R.  (1978).   "Relative  Costs  of Achieving Various Levels of
    Phosphorus Control  at Municipal Wastewater Treatment Plants in the
    Great Lakes  Basin,"  International  Joint  Commission,  Great  Lakes
    Regional  Office, Windsor,  Ontario.

Forester, L.D. (1978).   "Economic Impact  of Changing Tillage Practices
    in  the  Lake Erie  Basin," U.S.  Army Corps of  Engineers, Buffalo
    District,  Buffalo,  New  York.

Forester, L.D.,  and G.S.  Becker (1977).   "Economic and Land Management
    Analysis  in  Honey  Creek  Watershed," U.S.  Army Corps of Engineers,
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Heidtke, T.M.  (1979).  "Modeling  the Great Lakes System:   Update of
    Existing  Models,"   Great Lakes Environmental  Planning  Study
    Contribution  No.   4,   Great  Lakes  Basin  Commission,  Ann Arbor,
    Michigan,  79 pp.

Heidtke, T.M., Monteith,  T.J., Sullivan,  R.A.,  Scheflow, D.J., Skimin,
    W.E., and W.C.  Sonzogni  (1979).   "Future  U.S. Phosphorus  Loadings
    to  the  Great Lakes:    An Integration  of  Water  Quality Management
    Planning  Information," Great  Lakes  Environmental  Planning  Study
    Contribution No.   11,  Great  Lakes   Basin  Commission,  Ann Arbor,
    Michigan,  71 pp.

Heidtke, T.M.,  Scheflow, D.J., and W.C.  Sonzogni  (1980).  "U.S. Heavy
    Metal Loadings  to the Great Lakes:   Estimates  of Point  and  Nonpoint
    Contributions,"   Great  Lakes   Environmental  Planning  Study
    Contribution  No.   12,  Great   Lakes  Basin  Commission,  Ann Arbor,
    Michigan,  34 p.

Heidtke, T.M.,  and  W.C. Sonzogni  (1979).  "Modeling  the Great Lakes
    System:   Ongoing  and  Planned  Modeling Activities,"  Great  Lakes
    Environmental Planning  Study Contribution No.  6, Great Lakes Basin
    Commission,  Ann  Arbor,  Michigan.
                                  120

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 Heidtke,  T.M.,  Sonzogni, W.C.  and  T.J.  Monteith (1979).   "Management
     Information  Base  and  Overview  Modeling:    Update  of  Projected
     Loadings  to  the Great  Lakes,"  Great Lakes  Environmental  Study
     Contribution  No.  7,  Great  Lakes   Basin   Commission,  Ann  Arbor,
     Michigan, 38 p.

 Heidtke,  T.M.,  Scheflow,  D.J.,  and  W.C.  Sonzogni (1980).   "Comparative
     Cost-Effectiveness  of  Land   Application of  U.S.  Municipal
     Wastewater:  Implications for Phosphorus Control in the Great Lakes
     Basin,"  Great  Lakes Environmental Planning  Study  Contribution  No.
     19, Great Lakes  Basin Commission, Ann Arbor, Michigan, 34 p.

 Honey  Creek  Joint  Board  of  Supervisors  (1980).   "Honey Creek Watershed
     Project  Tillage Demonstration  Results 1979," U.S.  Army Corps  of
     Engineers, Buffalo District, Buffalo, New York.

 International  Joint  Commission  (IJC)   (1977).    "Evaluation  of  All
     Remedial Measures to Control Nonpoint Sources of Water Pollution in
     the  Great  Lakes Basin,"  Great  Lakes Regional  Office,  Windsor,
     Ontario.

 International  Joint  Commission  (IJC)   (1976).    "Great  Lakes  Water
     Quality Board, Appendix B, Surveillance Subcommittee Report," Great
     Lakes Regional Office, Windsor,  Ontario.

 Johnson,  M.G.,  Comeau,  J.C., Heidtke,  T.M.,  Sonzogni, W.C., and B.W.
     Stahlbaum (1978).   "Management Information  Base  and Overview
     Modeling,"  prepared  for  the Pollution from Land Use  Activities
     Reference Group  (PLUARG), International Joint Commission,  Windsor,
     Ontario, 90 pp.

 Johnson,  M.G.,  Comeau,  J.C.,  Heidtke, T.M.,  Sonzogni, W.C., and B.W.
     Stahlbaum  (1980) .   "Modeling Effects  of  Remedial  Programs  to  Aid
     Great Lakes Environmental Management,"  J. Great Lakes Res.,  6 (1),
     p.8-21.

 Jones,  R.A.,  and G.T.  Lee  (1979).    "Septic  Tank Wastewater Disposal
     Systems  as  Phosphorus  Sources  for  Surface  Waters,"  Journal WPCF,
     51, 11, p.2764-2775.                                  	'	

Knisel, W.G., ed. (1980).   "CREAMS,  A Field-Scale Model  for  Chemicals,
    Runoff  and  Erosion  from  Agricultural Management  Systems," U.S.
    Department  of  Agriculture,   Conservation  Research   Report  No   26
    640p.

Krause, A.  and J.R. Pilling  (1979).   "Alternative  Waste  Treatment
    Systems  for  Rural  Lake Projects,"   U.S.  Environmental  Protection
    Agency, Region V, Draft.

Marsalek,  J.  (1978).  "Pollution Due  to  Urban  Runoff:   Unit Loads  and
    Abatement  Measures,"  National  Water  Research   Institute,   Canada
    Centre for Inland Waters,  Burlington, Ontario.

McElroy, A.D., Chin,  S.Y.,  Nebgen,  J.W.,  Aleti,  A.,  and F.W.  Bennett
    (1976).  "Loading Functions  for Assessment of Water Pollution from
    Nonpoint   Sources,"   U.S.  Environmental   Protection   Agency,
    Environmental  Protection Technology  Series  Report No.  600/2-76-151,
    Washington,  D.C.

                                 121

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Monteith,  T.J.,  and  E.A.  Jarecki  (1978).   "Land Cover  Analysis  for the
    United  States  Great  Lakes  Watersheds,"   Great  Lakes  Basin
    Commission  for  the  International  Joint  Commission,  Windsor,
    Ontario.

Monteith,   T.J.,  Sonzogni,  W.C.,  Heidtke,  T.M.,  and  R.A.C.  Sullivan
    (1980) .   "WATERSHED  - A  Management  Technique for Choosing  Among
    Point  and Nonpoint  Control  Strategies.  Part 2 - A River Basin Case
    Study," Great  Lakes Basin  Commission, Ann Arbor, Michigan.

Novotny, V., Balsiger, D., Cherkauer, D.S.,  Simsiman,  G.V.,  Chesters,
    G., Bannerman,  R.,  and  J.G.  Konrad   (1979).   "Simulation  of
    Pollutant Loadings and  Runoff  Quality,"   Menomonee  River  Pilot
    Watershed Study,  University  of Wisconsin  Water  Resources  Center,
    Madison, Wisconsin.
Pollution  from  Land Use  Activities  Reference Group  (PLUARG)  (1978).
    "Environmental  Management  Strategy for  the  Great  Lakes  System,"
    International Joint Commission, Windsor, Ontario, 115 p.

Reckhow,  K.H.,   Beaulac,  M.N.,  and  J.T.   Simpson  (1980).   "Modeling
    Phosphorus Loading  and Lake Response Under Uncertainty:   A Manual
    and  Compilation  of Export  Coefficients,"  Draft  Report  to  the U.S.
    Environmental   Protection   Agency,   Department   of  Resource
    Development, Michigan State  University,  East Lansing, Michigan, 214
    P-

SEMCOG  (1978).   "Regional Evaluation of a  Phosphorus  Detergent  Ban,"
    Southwestern Michigan Council  of  Governments, Detroit, Michigan.

Simon,  D.P.  (1980).   "A Parametric  Nonlinear  Optimization Approach to
    the Water  Quality  Problems  of  Southeastern  Wisconsin,"  Draft
    Report,  University of Wisconsin Water  Resources  Center,  Madison,
    Wisconsin.

Sonzogni,  W.C.,  Chapra,  S.C.,  Armstrong, D.E.,  and  T.J. Logan (1980).
    "Phosphorus  Availability   -   Significance   to  Modeling  and
    Management," in  preparation.

Sonzogni,  W.C.,  Jeffs, D.N., Konrad,  J.C.,  Robinson,  J.B., Chesters,
    G.,  Coote,   D.R.,  and R.C.  Ostry  (1980).   "Pollution  from Land
    Runoff,"  Envir.  Sci. and Tech. ,  _14_(2),  p.  148-153.

Sonzogni,  W.C., Monteith, T.J.,  tfach, W.N., and  V.G.  Hughes (1978).
    "United  States  Great  Lakes  Tributary Loadings,"  Great Lakes Basin
    Commission   for  the  International  Joint  Commission,  Great  Lakes
    Regional  Office, Windsor, Ontario.

Sonzogni,  W.C., Monteith, T.J.,  and  T.M.   Heidtke  (1979).   "Proposed
    Great Lakes Phosphorus  Target  Loads:   A  Synopsis and Some
    Perspectives,"   Great   Lakes   Environmental   Planning  Study
    Contribution No.  5,  Great  Lakes  Basin  Commission,  Ann  Arbor,
    Michigan, 9p.
                                 122

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Sonzogni, W.C., Monteith, T.J.,  Skimin,  W.E.,  and  S.C.  Chapra (1979).
    "Critical  Assessment  of  U.S.  Land  Derived Pollutant Loadings to the
    Great Lakes,"   Task  D Report, Pollution  from  Land  Use Activities
    Reference  Group, International  Joint  Commission, Windsor, Ontario.

Sonzogni, W.C.,  and W.R. Swain  (1980).   "Perspectives  on U.S.  Great
    Lakes Chemical  Toxic Substances Research," J. Great Lakes Res.,  in
    press.

Stewart, B.A., Woolhiser, D.A., Wischmeier,  W.H.,  Caro,  J.H.,  and M.H.
    Frere (1975).   "Control of Water  Pollution from Cropland  - Volume
    1,   A Manual  for  Guideline   Development," Agricultural  Research
    Services  Report No.  ARS-H-5-1,   U.S.  Department of  Agriculture,
    Hyattsville,  Maryland,  lllp.

Sullivan, R.A.,  Sanders, P.A., and W.C.  Sonzogni  (I980a).   "An Update
    of  Water Quality Planning Activities in the U.S. Great Lakes Basin
    - Review of State and Areawide  Agency Five  Year  Strategies and Work
    Programs," Great  Lakes  Basin  Commission  for  the  Great  Lakes
    National Program Office,  U.S.  Environmental Protection  Agency.

Sullivan, R.A., Sanders,  P.A.,  and  W.C.  Sonzogni (I980b).   "Post-PLUARG
    Evaluation of  Great Lakes  Water Quality  Management  Studies  and
    Programs," Great  Lakes  Basin  Commission  for  the  Great  Lakes
    National Program Office,  U.S.  Environmental Protection  Agency.

Sullivan, R.A.C.,   Scheflow,  D.J.,  and  W.C.  Sonzogni   (1980).   "The
    Relative Significance of U.S.  Industrial Heavy  Metal Loads  to the
    Great Lakes," Great Lakes  Environmental  Planning Study  Contribution
    No. 16,  Great Lakes Basin  Commission, Ann Arbor, Michigan, 42p.

Urban,  D.R.  (1980).   Personal  Communication,  U.S.  Environmental
    Protection Agency,  Region  V,  Chicago, Illinois.

Urban,  D.R., Logan,  T.J.,  and  J.R.  Adams (1978).    "Application of the
    Universal  Soil Loss Equation  in the  Lake Erie Drainage  Basin," U.S.
    Army Corps of Engineers,  Buffalo  District,  Buffalo, New York.

U.S. Environmental Protection  Agency (EPA) (1977).    "Nationwide
    Evaluation  of  Combined  Sewer  Overflows and  Urban  Stormwater
    Discharges Volume II:  Cost Assessment  and  Impacts,"  EPA Report No.
    600/2-77-064.

U.S. Environmental  Protection  Agency  (EPA)  (1979).    "Costs  and Water
    Quality   Impacts  of  Reducing  Agricultural  Nonpoint   Source
    Pollution," Office  of Research  and Development,  Athens, Georgia.

U.S. Army  Corps  of Engineers  (1975).    "Urban  Stormwater Runoff  -
    STORM,"  The Hydrologic  Engineering Center,  Davis,  California.

U.S. Army Corps of  Engineers (1979).   "Lake Erie Wastewater Management
    Study Methodology  Report,"  Buffalo  District,   Buffalo, New York,
    146p.
                                 123

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Verhoff,  F.H.,  Melfi,  D.A.,  Yaksich,  S.M.,  and  D.B.  Baker  (1978).
    "Phosphorus Transport  in Rivers,"  U.S.  Army  Corps  of  Engineers,
    Buffalo District, Buffalo,  New York.

Wischmeier, W.H.,  and D.D. Smith  (1978).   "Predicting  Rainfall  Erosion
    Losses,"   Agricultural  Handbook No.  537,  Science  and  Education
    Administration,  U.S. Department of Agriculture, Washington,  D.C.
                                 124

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                    RECAP OF PREVIOUS DAY'S PROGRAM
                                  AND
                            GOALS FOR TODAY
                                  BY
                            CARL D,  WILSON*

I WOULD LIKE TO REMIND THE AUDIENCE TO REGISTER AND GIVE THEIR ADDRESS
IF YOU WISH TO RECEIVE A COPY OF THE SEMINAR PROCEDURES ON  WATER
QUALITY MANAGEMENT TRADE OFFS,
f
I WOULD LIKE TO REPEAT THE OBJECTIVE OF THIS SEMINAR WHICH IS TO
PRESENT A METHODOLOGY TO EVALUATE NONPOINT AND POINT SOURCE POLLUTION
 N ORDER TO TREAT THE SOURCE OF THE LOADS IN A COST-EFFECTIVE MANNER,
 0 DATE, THE ENVIRONMENTAL PROTECTION AGENCY HAS APPLIED ITS EFFORTS
TO POINT SOURCE POLLUTION ONLY,

WE ORIGINALLY STARTED THE NONPOINT SOURCE PROGRAM IN 1971 BY
DEVELOPING THE BLACK CREEK PROJECT IN ALLEN COUNTY, INDIANA,
"BEST MANAGEMENT PRACTICES" WERE APPLIED ON A 12,000 ACRE WATERSHED
WHICH WAS PLANTED WITH CORN AND SOYBEANS, WHICH ALSO INCLUDED
EXTENSIVE AUTOMATED WATER SAMPLERS,  AFTER DATA WAS COLLECTED WE
INITIATED SEMINARS TO LET THE PUBLIC KNOW OF THE ANALYTICAL RESULTS,
THE SECTION 108 PROGRAM OF THE GREAT LAKES NATIONAL PROGRAM OFFICE
IS THE ORIGINAL SOURCE OF FUNDING FOR NONPOINT SOURCE PROGRAMS,
SEMINARS AND WORKSHOPS,

OUR OBJECTIVE, THEN AS IS NOW, IS TO DEVELOP A METHODOLOGY TO EVALUATE
BEST MANAGEMENT PRACTICES AS THEY EFFECT WATER QUALITY,  IN OTHER
WORDS GIVE THE CAUSE AND EFFECT IN A QUANTIFIED MANNER,

IN THE PAST THE CONSTRUCTION GRANTS PROGRAM USUALLY OBTAINED THE.
NONPOINT SOURCE LOAD BY SUBSTRACTION,   IN OTHER WORDS THEY ADDED UP
POINT SOURCE LOADS COMING OUT OF A PIPE AND SUBSTRACTED THAT NUMBER
FROM THE TOTAL RIVER LOAD TO OBTAIN NONPOINT LOADS,  WELL AT THE TIME
THAT WAS SUFFICIENT,  BUT WE HAVE ARRIVED AT A POINT WHERE THAT
SYSTEM IS NOT ACCEPTABLE,  WHY?  WE CANNOT MEET OUR WATER QUALITY
GOALS IN A COST-EFFECTIVE MANNER WITH THIS PROCEDURE,  THUS WE MUST
DEVELOP A NEW SYSTEM THAT IS MORE EQUITABLE AND EFFECTIVE,

OF COURSE PUBLIC LAW 92-500 HAD A SECTION CALLED 208 AND UNDER THIS
SECTION OF THE LAW, STATES AND AREAWIDE AGENCIES DEVELOPED 208 PLANS
TO ADDRESS ALL SOURCES OF POLLUTION AND DEVELOP A PLAN THAT CAN BE
IMPLEMENTED TO MEET WATER QUALITY GOALS,  PART OF THESE PLANS INCLUDE
THE CONSTRUCTION OF SEWAGE TREATMENT PLANTS WHERE EPA HAS PUT BILLIONS
INTO THIS PROGRAM,  AND AT THE SAME TIME EPA WAS PUBLISHING DATA
SAYING, IN FACT, WE WOULD NOT MEET OUR WATER QUALITY GOALS UNLESS
WE TREATED NONPOINT SOURCE POLLUTION,   So WHAT IS THE ANSWER?  THE
SEMINAR WILL PRESENT A METHODOLOGY TO RESOLVE THE PROBLEM,  FlRST
A FEW COMMENTS ON MODELING,

*CARL D, WILSON is A NONPOINT SOURCE COORDINATOR FOR REGION V, EPA,
PRESENTATION GIVEN AT THE PICK CONGRESS HOTEL, CHICAGO, ILLINOIS
SEPTEMBER 17, 1980,  SEMINAR ON WATER QUALITY MANAGEMENT TRADE-OFFS,
                                  125

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To EVALUATE NONPOINT SOURCE POLLUTION THE PROBLEM IS APPROACHED
FROM A WATERSHED BASIS,   AT THIS POINT I  AM ASSUMING THE MODELERS
ARE UTILIZING THE "STANDARD SOIL SURVEY"  CONDUCTED BY THE UNITED
STATES DEPARTMENT OF AGRICULTURE,   IF THE MODELERS ARE NOT USING
THIS SOIL SURVEY IN MY OPINION THEIR MODELS ARE TOTALLY USELESS TO
EVALUATE NONPOINT SOURCE POLLUTION FROM FARM AND RANCH LAND,  To
FURTHER SUBSTANTIATE MY POINT ALL TILLAGE SYSTEMS RESEARCH ARE ALSO
BASED ON THE STANDARD SOIL SURVEY, THIS INCLUDES MANAGEMENT SYSTEMS
IN GENERAL,  THUS.,  ALL PRACTICES TO CONTROL EROSION AND WATER
QUALITY HAVE TO RELATE TO THE SAME BASE TO MAINTAIN PRODUCTION AND
PROTECT WATER QUALITY,

THERE ARE SEVERAL MODELS THAT ARE AVAILABLE AND YOUR SELECTION OF
A MODEL DEPENDS ON THE SIZE OF AREA YOU WISH TO INVESTIGATE,  THE
INTERNATIONAL JOINT COMMISSION, THROUGH THEIR PLOARG STUDIES,
UTILIZED A  UNIT AREA LOAD  APPROACH AND  FOR GENERALIZED DATA THIS
SYSTEM CAN GIVE PROGRAM GUIDANCE,   BUT TO-BE MORE SPECIFIC AS TO
WHERE THE PROBLEM IS YOU WOULD HAVE TO SELECT A MODEL THAT IS MORE
SITE SPECIFIC SUCH AS THE ANSWERS MODEL,

THUS TO OBTAIN EVEN MORE DETAIL ON A FARM SIZE UNIT THE CREAMS
MODEL WOULD BE YOUR CHOICE,

BUT IN THIS SEMINAR WE WISH TO PRESENT A GENERALIZED METHODOLOGY
THAT CAN BE SOLVED WITH A DESK CALCULATOR AND IT IS CALLED WATERSHED,
YOUR COMMENTS ON THIS METHODOLOGY WILL BE APPRECIATED,

NOW TO BRIEFLY RESTATE WHAT THE SPEAKERS  SAID YESTERDAY,

ON WATER QUALITY ISSUES, MADONNA McGRATH  OF THE GREAT LAKES NATIONAL
PROGRAM OFFICE GAVE AN OVERVIEW WHICH INCLUDED PHOSPHORUS LOADS TO
THE GREAT LAKES,  SHE MADE THE POINT THERE ARE SOME WELL DEVELOPED
METHODOLOGIES AND THE NEED TO BE USED,

JEFF NEDELMAN REPRESENTING SENATOR GAYLORD NELSON'S OFFICE GAVE us
A BACKGROUND ON THE ENVIRONMENTAL MOVEMENT AND RESTATED THE IMPORTANCE
OF SETTING GOALS,  HE EXPRESSED CONGRESSIONAL CONCERN OVER COSTS AND
SUGGESTED PRIORITIES COULD BE A WAY TO BE MORE COST-EFFECTIVE IN
TREATING POLLUTION,  ALSO HE REITERATED  THEIR SUPPORT FOR THE PHOSPHATE
DETERGENT BAND,  HE ALSO RELATED HOW SLOW OUR SYSTEM IS TO RESPOND TO
CORRECTING POLLUTION PROBLEMS,  FROM HIS VIEWPOINT THERE IS A LACK
OF SENSITIVITY  IN CONGRESS FOR POLLUTION PROBLEMS,  EPA IS NOT GETTING
THE MONEY NEEDED FOR THE GREAT LAKES,  EXAMPLE EPA SPENT $13,000,"
ON TRAVEL AND ONLY $2,000,000 ON THE GREAT LAKES,  HE ALSO NOTED
EPA ESTIMATES 54 BILLION DOLLARS WILL BE NEEDED TO COMPLETE THE
SECONDARY TREATMENT PLANTS AND ADVANCED WASTE TREATMENT PROJECTS,
                               126

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 ETER WISE FROM EPA HEADQUARTERS WATER PLANNING DIVISION STATED
 08 PLANNING HAD DONE A POOR ASSESSMENT OF NONPOINT SOURCE POLLUTION,
..E ALSO STATED WE NEED CAUSE AND EFFECT DATA FROM NONPOINT SOURCES,
CONCERNS WERE EXPRESSED ABOUT MODELING,  PLANS NEED TO BE UPDATED
TO CORRECT DEFICIENCIES,  TRADE-OFFS BETWEEN POINT AND NONPOINT ARE
A PROBLEM,  SOME THOUGHTS HAVE BEEN SHOULD WE PAY FOR NONPOINT SOURCE
CONTROLS?  HOW TO ARRIVE AT TRADE-OFFS IS STILL A PROBLEM WITH THE
AGENCY,

KEITH YOUNG OF THE SOIL CONSERVATION SERVICE GAVE AN EXCELLENT
PRESENTATION ON PRIME AGRICULTURAL LAND,   FlY COMMENT, WE WILL SEE
THE DAY WHEN A LINE WILL BE DRAWN AROUND PRIME AGRICULTURAL LAND
AND THAT WILL BE ITS SOLE USE, AGRICULTURE,

JEFF GAGLER OF THE WATER QUALITY POLICY SECTioN-EPA GAVE AN IN
DEPTH LOOK AT ADVANCED SECONDARY TREATMENT AND ADVANCED WASTE
TREATMENT (AST/AWT),  HE POINTED PROBLEMS IN EVALUATION OF POINT
SOURCE VS, NONPOINT,  A BACKGROUND ON WATER QUALITY STANDARDS WAS
COVERED, INCLUDING WATER QUALITY GOALS,  HE POINTED OUT A NEED FOR
CLASSIFICATION  GUIDELINES WHICH WOULD ALSO INCLUDE BIOLOGICAL SYSTEMS,
CONCLUDED THE WHOLE ECONOMIC PICTURE NEEDS TO BE REVIEWED,

RONALD MUSTARD OF THE OFFICE OF ENVIRONMENTAL REVIEW COVERED THE
ISSUES CONCERNING WETLANDS AND FLOODPLAINS,  HE GAVE A BRIEF BACKGROUND
ON THE LAW,   NOTE AGRICULTURAL DRAINAGE IS 15% OF THE WETLAND PROBLEM
ACCORDING TO A RECENT REPORT,

)ON BUNDY OF THE INTERNATIONAL JOINT COMMISSION SPOKE ABOUT THE
:,S,/CANADA GREAT LAKES WATER QUALITY AGREEMENT AND ITS IMPACT ON U,S,
POLICY,  HE RESTATED THE IJC BOARDS MAJOR OBJECTIVE TO RESTORE THE
WATER QUALITY OF THE GREAT LAKES,  THERE HAVE BEEN MAJOR REVISIONS
IN THE WATER QUALITY STANDARDS,

DAVID STRINGHAM, REGIONAL PROGRAM COORDINATOR FOR REGION V-EPA GAVE
A PRESENTATION ON THE STATE/EPA AGREEMENTS,  THIS IS A METHOD TO
WORK WITH THE STATES TO ARRIVE AT PRIORITIES TO SOLVE PROBLEMS,
AND THIS WOULD GIVE GUIDANCE TO FUTURE EPA PROGRAMS,

WILLIAM BENJEY OF THE WATER QUALITY PLANNING BRANCH GAVE AN OVERVIEW
OF WATER QUALITY PLANS,  HE POINTED OUT THE PROBLEM OF BUILDING SEWAGE
TREATMENT PLANTS AND STILL NOT IMPACTING WATER QUALITY,  SUGGESTED
INTEGRATING ALL SOURCES OF POLLUTION BEFORE MOVING FORWARD WITH
TREATMENT,  HE STATED NONPOINT SOURCE TRADE-OFFS ARE SUPPOSED TO BE
CONSIDERED IN FACILITY PLANS,
MlKE MACFIULLEN FROM THE WATER QUALITY
WATER QUALITY STANDARDS,  REAFFIRMED [
   NDARDS AND GOALS,  HE ALSO STATED [
    PRIORITY POLLUTANTS,
'OLICY  SECTION  OF  EPA COVERED
DA'S  COMMITMENT TO WATER QUALITY
Y\ WILL PUBLISH STANDARDS ON
                                127

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LELAND ffcCABLE OF EPA's HEALTH EFFECTS LABORATORY GAVE THE RESULTS
FROM SOME CURRENT STUDIES ON EPIDEMIOLOGY RESULTS FROM BEACH STUDIES,

RONALD DRYNAN FROM THE REGIONAL OFFICE OF THE INTERNATIONAL JOINT
COMMISSION COVERED SOURCES OF POLLUTANTS TO THE GREAT LAKES,
HE STATED THE GREATEST SOURCE OF TOTALS LOADS COMES FROM NONPOINT
SOURCE POLLUTION,  POINT OUT WE NEED TO LOOK AT A MIX BETWEEN
POINT SOURCE AND NONPOINT SOURCE LOADS,

NELSON THOMAS OF USEPA RESEARCH LABORATORY DESCRIBED TRIBUTARY
LOADS AND THEIR EFFECTS ON THE GREAT LAKES,  HE STATED THERE IS A
NEED TO HAVE MANAGEMENT TRADE-OFFS BETWEEN POINT SOURCE AND NONPOINT,
GAVE DATA ON LOADS TO THE GREAT LAKES WHICH INCLUDED ATMOSPHERIC
LOADS OF PHOSPHORUS,   SPOKE ABOUT THE 11,000 METRIC TON LOAD
ESTABLISHED FOR LAKE ERIE AND WHICH SOURCES WILL HAVE TO BE CONTROLLED
TO REACH THIS AGREED UPON NUMBER,  FOOD CHAIN ACCUMULATION PROBLEM
WAS DISCUSSED,  PIIREX, TASTE AND ODOR PROBLEMS WERE ELABORATED
ON,

AL WALLACE FROM THE DEPARTMENT OF CIVIL ENGINEERING, UNIVERSITY
OF IDAHO SPOKE ABOUT LAND TREATMENT OF MUNICIPAL WASTEWATER,

JAMES HANLON FROM EPA's ENVIRONMENTAL ENGINEERING BRANCH SPOKE
ON COSTS OF WASTEWATER TREATMENT,  THERE WAS $31,5 BILLION APPROPRIATED
FOR SEWAGE TREATMENT PLANTS,

WILLIAM SONZOGNI OF THE GREAT LAKES BASIN COMMISSION PRESENTED A
PROPOSED METHODOLOGY TO INTEGRATE POINT SOURCE AND NONPOINT SOURCE
POLLUTION ASSESSMENT,  HY COMMENT ON THIS METHOD OR ONE SIMILAR
WILL BE USED IN THE FUTURE FOR WATER QUALITY MANAGEMENT TRADE-OFFS,
                               128

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             A MANAGEMENT TECHNIQUE FOR

CHOOSING AMONG POINT AND NONPOINT CONTROL STRATEGIES

         PART 2 - A RIVER BASIN CASE STUDY


                for presentation at

            U.S. EPA Region V Seminar on
        WATER QUALITY MANAGEMENT TRADE-OFFS
             September 16 and 17, 1980
                         by

                Timothy J.  Monteith
                William C.  Sonzogni
                 Thomas M.  Heidtke
                Rose Ann C. Sullivan

         Great Lakes Basin  Commission Staff
                  September,  1980
                       129

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              A MANAGEMENT  TECHNIQUE  FOR CHOOSING

           AMONG POINT AND NONPOINT CONTROL STRATEGIES

                PART 2 - A RIVER BASIN CASE STUDY


                                by

            Timothy J. Monteith, William C. Sonzogni,
           Thomas M. Heidtke,  and Rose Ann C.  Sullivan
      Abstract;   The  WATERSHED management technique  has  been
      designed to help water quality managers  select  the  most
      cost-effective pollution control  program for a drainage
      area.  WATERSHED has been  applied  to  the Sandusky River
      Basin in northern Ohio to demonstrate how it is used and
      how to interpret the results.  Programs to control total
      phosphorus loadings from  point  and nonpoint sources are
      evaluated  using  eight  worksheets  to  compile  the river
      basin data  and  carry  out calculations.    WATERSHED  is
      applied  in this manner:  the river basin physical layout
      is conceptualized and  all major total phosphorus sources
      are  identified.   Phosphorus  loads from  point  sources,
      urban runoff, rural  non-cropland  runoff  and  cropland
      runoff are calculated  for initial  conditions  and under
      different  stages  of  control.    Pro'gram  costs  are
      calculated and  used to estimate  the  cost-effectiveness
      of each  program.  The  forty programs identified are then
      prioritized  according  to their   cost-effectiveness  in
      reducing the total phosphorus load at the river mouth or
      receiving water.
Great Lakes Basin Commission Staff.  Water Resources Engineer, Water
Resources Scientist, Water Resources Engineer, and Regional Planner/
Policy  Analyst,  respectively.   Great  Lakes  Basin  Commission,  Ann
Arbor, Michigan.
                               130

-------
                               INTRODUCTION

     A companion paper (Sonzogni et al.,  1980)  discusses  the philosophy
 and  basic  components of the WATERSHED process.   This  paper presents an
 application of WATERSHED to  the  Sandusky River  in northern Ohio.   The
 case study  focuses  on  loadings  of  and  control  strategies  for  total
 phosphorus.

     This  case  study is intended  to  demonstrate  how  WATERSHED may be
 applied  to a  river  basin.   It is  not  intended to serve  as a rigorous
 analysis  of point and  nonpoint sources  in the  Sandusky basin.   Some
 simplifications of the Sandusky field  data have been made  in order to
 better  illustrate  the  process.  If a detailed  analysis of the Sandusky
 was  required,   individuals  intimately  familiar with the  Sandusky  River
 Basin would  need  to  be  consulted.

     Eight  different  worksheets have  been  developed  for   compiling  the
 river basin data  and making  the  necessary  calculations discussed  in
 Sonzogni  et al. ,  1980.   These  worksheets provide a simple,  sequential
 procedure  for  assessing  the importance  of point and nonpoint sources in
 a  river basin.    The  worksheets,   in  order  of  their  use,  are  listed
 below:

                   1.   Physical Layout
                   2.   Point  and Urban  Runoff  Loads
                   3.   Rural Non-Cropland Loads
                   4.   Cropland Loads
                   5.   Loading  Summary
                   6.   Program  Costs  '
                   1.   Cost-Effectiveness Analysis
                   8.  Program  Summary

     This paper illustrates:  (l)  how  these worksheets are  used in  an
 actual  river  basin  (i.e.,  the  Sandusky  River  Basin),  (2)  the  results
 which are obtained,  and  (3) how to  interpret  these results.
               EXAMPLE STUDY AREA - SANDUSKY RIVER  BASIN

    The  Sandusky  River Basin  was  selected for  this  WATERSHED example
because  it  contains  a  representative  mix of rural  and urban  land.   The
phosphorus  load  contributed by  this  basin  has  also  been extensively
studied  by  the  U.S.  Army Corps  of  Engineers  in  their  Lake   Erie
Wastewater Management Study (LEWMS) and by the  Water Quality  Laboratory
at  Heidelberg  College.   Hence,  considerable   data  exist  to  test  the
results of the WATERSHED analysis.

    The  Sandusky  River   drains   an   area  of   about  400,000  hectares
(980,000 acres) in northcentral Ohio.   The Sandusky flows north to  Lake
Erie, draining mostly  farmland.   There are  four cities  of significant
size  (population  greater  than  6,000)  that  discharge both  municipal
wastewater and stormwater  into  the Sandusky:   Bucyrus,  Upper Sandusky,
Tiffin and  Fremont.   For  a detailed  description of the  Sandusky  River-
system, see U.S. Army Corps (1975, 1979b) .
                               131

-------
PHYSICAL LAYOUT (WORKSHEET 1)

    The first  step  in  WATERSHED is  to  divide the Sandusky  basin  into
sub-basins.   The  Sandusky has a well-defined monitoring  network which
provides  excellent  loading  records  from  individual  hydrologic  areas.
These stations monitor sub-basins that each have relatively homogeneous
soils and land uses.  The resulting sub-basins are shown in Figure 1.

    The next  step  is to  develop  a schematic diagram of  the watershed
which delineates the key  components  along  the river  channel.   Figure  1
and Worksheet  1 show how  the Sandusky River  Basin was  divided for this
example, both physically and schematically.

Points of Entry

    As shown on Worksheet 1,  six points of entry  have  been defined for
the Sandusky River  Basin  (A-F).  Each receives  a  total  phosphorus load
from one  or more rural  sub-basins.   The urban  runoff and point  source
contributions  from  the cities  of  Bucyrus, Upper  Sandusky,  Tiffin and
Fremont are assumed to enter the main channel at  points A,  B,  D  and E,
respectively.

    The points  of  entry  were  selected  after inspection  of hydrologic
maps and  sampling station locations  within the  drainage  area.   In this
way the estimated total  phosphorus loads  to  the  main channel  from all
sources  can  be  compared  with  field measurements  obtained  from the
ongoing  sampling  program.   No  major  reservoirs,  lakes  or  other
significant physical influences were identified along the river system.
If present, however, their  locations would have also been considered in
defining  the points of entry  for this example.

    If  transmission  losses  were not  to be considered in a given section
of the  river  channel,  the  number  of  points  of  entry could be reduced.
For example,  if it  were known  that no transmission losses occur between
entry points A and  C, rural  positions 1, 3, 4, 6  and 7 as well as  urban
positions 2 and 5 could all  be  located at  entry point C.

Control Strategies

    In  this  case  study,  programs to reduce initial pollutant  loads are
evaluated.    For  each pollutant  source,  control  programs  are grouped
into  "stages"  of  implementation.   Any number of  stages can be selected
for  each  pollutant  source.   For  this  example,  two  stages of control
were  considered  for reducing the total phosphorus load from each  major
source  (rural  runoff,  urban runoff  and  municipal  point  source
discharges).   The stages  of control  have been formulated  as  incremental
levels  of treatment.   Thus, the costs and load reductions  presented in
the  following  worksheets  for  Stage  II  control  are  incremental (in
addition  to)  the  costs  and load reductions  associated  with Stage   I
control.

    This  staged approach  to control  of total  phosphorus loadings allows
 for  a  logical,  straightforward examination of the  level of  treatment
required  at  each   source.   Each  additional  stage  represents an
                               132

-------
Sandusky  Riven,  Ohio
                    FIGURE 1
                        £V"SANDUSKY
                                    Sub-Basin Boundaries

                                  1 )Position Number
                                    (Rural)
                                  2 | Position Number
                                    (Urban)
                   133

-------
                            PHYSICAL LAYOUT

                              SANDUSKY RIVER

                                 LAKE ERIE
                                                                                                                              WORKSHEET 1
                       Source
             Loss  Creek
             Bucyrus  City
             Broken Sword
             Upper Sandusky River
             Upper Sandusky City
             Tymochtee Cr
             Middle Sandusky
             Honey Creek
             Tiffin City
             Wolf  Cr
             Rock  Cr
             Fremont  City
             Lower Sandusky
CO
-pi
                                               Posit ion
 1
 2
 3
 4
 5
 6
 7
 8
 9
10
11
12
13
                                                               Point
                                                             of Entry
                                                                            Area
230
  8.5
217
325
  6.7
593
640
386
 17.4
385
464
 13.7
730
                                                                                      Surface  features
                                      Soils  Other
                                                                      Diagram
                                                                                                             Rural
                                                                                                                      LAKE ERIE
                                                                                                                                     Urban

-------
 incremental  level of treatment which can only be  implemented  subsequent
 to  the  previous  stage  of control.    In  other  words,  for  any  given
 loading  source, implementation of Stage II control  implies that  Stage  I
 control  is also implemented.  A more detailed discussion of the  control
 alternatives considered  in this example is given  below.

 POINT SOURCE AND URBAN RUNOFF LOADS (WORKSHEET 2)

    The  purpose of this  worksheet is to compile loading information  for
 all  of  the  significant  urban pollutant  sources,  including point
 sources,  stormwater runoff, combined sewer overflows, and other  sources
 such  as  construction  runoff  and runoff from unsewered  areas.  On this
 and all  subsequent worksheets,  reference  is  made  to column letters  and
 worksheet numbers.   For  example,  bn refers  to  column "b"  on worksheet
 lloll                                i

 Point Sources

    Municipal:  Within the Sandusky River Basin,  four  municipal  point
 sources  were  found  to  contribute the majority  of the total   phosphorus
 point  source  load.   The municipalities served by  these  point  sources
 are Bucyrus,  Upper  Sandusky,  Tiffin  and  Fremont.    For each of  these
 plants data were obtained on population served, flow  from the treatment
 plant, and the total phosphorus concentration in  the effluent.   Several
 small  point  sources  also exist, but  since the  cumulative  load  from
 these plants is very small, they are not considered in this example.

    Various  levels  of  phosphorus control  presently exist  at  the  four
 Sandusky  plants.  However, for example purposes it will be assumed that
 no phosphorus control  has  been  implemented at  these plants.   This will
 allow  for  a  comparison  of   several   control  options  among   plants.
 Initial  phosphorus  concentrations  in  the  discharge  water  is  thus
 assumed  to be  4  mg/L P.   This  value,  representative of many treatment
 plants  without  phosphorus control  (Drynan,  1978;  Sonzogni  e_t_ al. ,
 1978), is entered in column b«  for  all  four  plants.  The average daily
 flow  from each of the  municipalities  is  given  in column a. (million
 gallons  per  day).   The  average  annual  total phosphorus load in kg/yr
 (column  c2)  is calculated by multiplying  flow (mgd)  by  concentration
 (mg/L)  and  then  multiplying   this  product  by  a  conversion  factor
 (columns a2 x b2 x 1,382 = c2).

    The  next step  is  to enter on Worksheet  2  data which  describe the
 impact of selected  remedial  programs  on  total   phosphorus loads  from
municipal point sources.   Two  stages  of phosphorus control at  each of
 the four municipal wastewater  treatment   facilities  included in  this
case study are examined:

         Stage I Control:  chemical  precipitation to reduce   the total
                           phosphorus  effluent  concentration  to 1.0
                           mg/L.

         Stage II  Control: additional  treatment to  further reduce the
                           total  phosphorus effluent concentration  from
                           1.0  mg/L  to 0.5  mg/L.
                               135

-------
                                                          POINT AND  URBAN  RUNOFF  LOADS
                                                                     TOTAL P LOADS
                                                                                                                  WORKSHEET 2

Source
INITIAL CONDITION
Bucyrus City
Upper Sandusky City
Tiffin City
Fremont
TOTAL
STAGE I
Bucyrus City
Upper Sandusky City
Tiffin City
Fremont
TOTAL
STAGE II
Bucyrus City
Upper Sandusky City
Tiffin City
Fremont City
TOTAL
Column ->
Posi-
tion
2
5
9
12
2
5
9
12
2
5
9
12
a2

Flow
mad
2.5
1.5
3.2
5.1
2.5
1.5
3.2
5.1
2.5
1.5
3.2
5.1
b2
C2
Point
Cone.
H1R/L
4.0
4.0
4.0
4.0
1.0
1.0
1.0
1.0
0.5
0.5
0.5
0.5
Load
kg/vr
13,800
8,300
17,700
28,200
68,000
3,400
2,100
4,400
7.000
16,900
1,728
1,036
2,211
3,524
8,499
d2
e2
Storm
Area i UAL
km2 kk/km2/yr
1.3
0
7.0
1.4
9.7
1.3
7.0
1.4
1.3
7.0
1.4
250
250
250
188
188
188
140
140
140
f2

Load
ke/vr
320
1,800
350
2,500
240
1,300
260
1,800
182
980
196
1,358
82
h2
Combined
Area
km2 k
7.2
6.7
10.4
12.3
36.6
7.2
6.7
10.4
12.3
7.2
6.7
10.4
12.3
UAL
g/km2/yr
900
250
1,000
1,000
846
235
940
940
630
175
700
700
*2

Load
kS/yr
6,500
1,700
10,400
12,300
30,900
6,091
1,574
9,776
11.562
29,003
4,536
1,172
7,280
8,610
21,598
J2
*2
12
Un sewered »
Area
km2 kj
0
0
0
0
UAL
;/km2/yr

Load
ks/yr

        x  b  x 1,382 ->
f2 =
where 1,382  is  the conversion factor
       (mg/L x rngd x  1,382) = kg/yr.
  * Can include construction sites or  septic tank areas.
UAL >Unit  Area Load

-------
These new effluent concentrations are  entered  in  column b-  and used to
calculate a Stage I and Stage II controlled municipal load (column c.,).
The  cost  of implementing these programs  is  presented  later (Worksheet
6).

     Industrial:    No   industries  were  identified  as  discharging
significant levels of phosphorus to  the  Sandusky  River.  If industries
were  present,  they would be entered  on  Worksheet 2 as  point  sources.
Control measures may or may not be proposed and evaluated.

Stqrmwater Runoff

    For  the Sandusky  little data  were   available  on  the  urban  area
served  by  different  types  of  sewer  systems  (separate,  combined  or
unsewered).    As  a   result,  only   approximate  values  are  given  in
Worksheet 2 for the area served by all the sewer systems.

    The estimated area served by stormwater sewers for  each  of the four
cities  included  in this  analysis  are presented in column d_  (the City
of Upper  Sandusky  is served by  combined  sewers only  and thus has  an
entry of  "0"   in column  d_) .   These values are  then  multiplied  by  a
total  phosphorus unit  area load (UAL)  (from  the  companion  paper  by
Sonzogni  et al.,  1980)  representative of  stormwater sewer  areas,  and
the  products are entered as^ an initial condition in column f .   The UAL
applied here  —  250 kg/km  /yr  —  reflects medium industrial  activity
within  the  urban area.  The initial  condition  values entered  in column
f_  represent   runoff  loadings  assuming  no  remedial measures are  in
effect.

    The next step is to calculate the  reduced  loads  that result from  a
Stage I and Stage II  program for  controlling stormwater runoff.   In
this  example the following  separate  stormwater sewer  control  programs
are examined:

         Stage I  Control:  streetsweeping  at  7-day  intervals   with
                           vacuum sweepers.

         Stage II Control:  Stage   I   control   plus   detention   and
                           sedimentation  of stormwater  runoff.

These  and  other  programs  are  discussed  in  the companion  paper  by
Sonzogni et al. (1980).

    Implementing  the  Stage  I  program is  assumed to  result  in  a  25
percent  reduction in  the uncontrolled diffuse loading  from all  separate
sewered   areas.    Implementation  of  Stage   II  programs  will  realize
another 20  percent  total  phosphorus load  reduction  from the  initial
stormwater  load.   These  reductions  are  illustrated  in  the Stage  I  and
Stage  II  UALs  and  total   loads  contained  in  columns  e   and  f_,
respectively.
                               137

-------
Combined Sewer Overflows

    Estimates of diffuse  loadings  from urban areas served  by combined
sewers  are  obtained  in  a  manner  similar  to that  used for  separate
stormwater  sewers.   The  UALs  for  the  initial  loading condition
presented in column  h   are  taken from the  companion  paper  and reflect
combined sewer overflows typical  of cities in the Great Lakes region.

    The  following  combined  sewer  overflow  control programs  are
examined:

         Stage I Control:   streetsweeping  at  7-day  intervals  with
                           vacuum sweepers.

         Stage II Control: Stage  I control plus detention and treatment
                           of the combined sewer overflow.

The Stage  I  program results  in  about a  5  percent reduction  in total
phosphorus load, and Stage  II will result  in an  additional 25 percent
reduction in the total  phosphorus  loading (Johnson et al. ,  1978).   The
Initial, Stage I,  and  Stage  II UALs are  presented in column i~ .   These
values  reflect  medium  industrial  activity  within the  combined sewer
area.

    If other pollutant  sources,  such  as  septic  tanks  and feedlots (see
the companion  paper by Sonzogni  et al. ,  1980)  were  to  be  considered,
they would be included  in Worksheet  2.   These  sources would be  treated
as point sources.   In  many  cases,  loads  would be calculated separately
for these sources  and entered directly onto column c_ .

RURAL NON-CROPLAND AREAS  (WORKSHEET 3)

    The  purpose  of Worksheet 3  is to calculate  loads  for  rural  land
uses  within  each  sub-basin that  will not  be  treated  for phosphorus
reductions.  For the Sandusky River Basin, two main  land  uses of this
type were  identified:   grassland  and  woodlands.   If measured loads are
available, they would be  used directly.   In the  Sandusky,  loads  had to
be  estimated using  the  appropriate  UALs (as given  in the companion
paper).

    The  area of  each non-cropland  land use (columns  a.,, d,. and  g~) is
multiplied by the  appropriate unit area load (columns b-,, e_ and h,) to
provide  an estimate  of the  annual diffuse  total  phosphorus load.   The
results  are  presented  in columns  c^, f~  and  i~.   These  values are
subsequently summed  in column j~  to produce a total rural  non-cropland
load  for each  sub-basin.   This  load represents  a part of  the total
phosphorus budget  but will not be considered for  treatment measures.

RURAL CROPLAND AREAS -  (WORKSHEET 4)

    The  primary  tool used to  estimate  pollutant loadings and the effect
of  control  measures  in  cropland  areas   is  the  Universal  Soil  Loss
Equation (USLE).   The  components  and  the application of this equation
are discussed  in  detail  in the  companion  paper  and  in Wischmeier and
                                 138

-------
                                                                      RURAL NON-CROPLAND AREAS
                                                                              TOTAL P LOADS
                                                                                                                WORKSHEET  3
OJ
                       Source
Loss Creek
Broken Sword
Upper Sandusky River
Tymochtee
Middle Sandusky
Honey Creek
Wolf Creek
Rock Creek
Lower Sandusky (Soil  I)
Lower Sandusky (Soil  2)

             TOTAL
Column >•
'ositlon
1
3
4
6
7
8
10
11
13
13


a3
b3
C3
Grass
Area *
km2
11 .83
3.59
12.81
9 . 04
17.27
3.17
7.57
12.14
10. 00
8.25
95.67

UAL
kg/km /ye
10
10
10
25
10
10
10
10
25
10


Load
kg/yr
118
36
128
226
173
31
76
121
250
82

1 ,241
d3
63
f3
Woodland
Area *
km
25.04
18.17
34.38
47.13
67.96
44.07
22.89
56.47
74.54
-
390.65

UAL
kg/km /yr
10
10
10
10
10
10
10
10
10
10


Load
kg/yr
250
180
344
471
680
441
229
565
745


3,905
g3
h3
*3
Other **
Area
km










274.88 Wa

UAL
kg/km /yr










:er, Wetlan

Load
kg/yr










Is

J3
Total Non-
Cropland
Load , ,
kg/yr
368
216
472
697
853
472
305
686
1,077


5,146
c., = a... x b,.
f  _ ,1  V f>
f3 " d3 X 63
13 = g3 x 1,3
                                                                                     * Weighted Extrapolation
                                                                                    ** Includes septic tank failures
                                                                                   UAL »Unit Area Load
             j, =
        + f3 +

-------
                                                                 RURAL CROPLAND  AREAS
                                               UNIVERSAL SOIL LOSS EQUATION/TOTAL PHOSPHORUS  LOAD ESTIMATES
                                                                       WORKSHEET



Source
INITIAL
7
L.OSS Or
Broken Sword
Upper Sandusky
Tymochtee
Middle Sandusky
Honey Cr
Wolf Cr
Rock Cr
Lower Sandusky (Soil 1)
Lower Sandusky (Soil 2)
TOTAL
STAGE I
Loss Cr
Broken Sword
Upper Sandusky
Tymochtee
Middle Sandnsky
Honey Cr
Wolf Cr
Rock Cr
Lower Sandusky (Soil 1)
Lower Sandusky (Soil 2)
TOTAL
STACK II
Loss Cr
Broken Sword
Upper Sandusky
Tymochtee
Middle Sandusky
Honey Cr
Wolf Cr
Rock Cr
Lower Sandnskv (Soil 1)
S lu'-kv (So ' 1 '>)
TOTAL
Column •*


Position

1
3
4
6
1
8
10
11
13
13

1
3
4
6
1
8
10
11
13
13

1
3
4
6
7
8
10
11
13
13

a4
Cropland
Area

Universal Soil Loss Equations Coefficients
Rainfall
d Runoff
(ha) R
	 __ 	 j
18,984
18,719
27,460
52,840
54,236
34,355
34,311
40,990
24,355
10,000
316,250



















125
125
130
138
138
125
125
125
125
125


















Soil
Erodibility
K

.35
.38
.42
.32
.38
.35
.29
.34
.32
.28


















Topo-
graphic
LS

.402
.424
.426
.357
.381
.338
.256
.427
.410
.434


















Cover &
Management
C

.233
.233
.245
.260
.260
.237
.237
.237
.268
.237

.108
.099
.103
.108
.110
.101
.108
.105
.116
.099

.034
.035
.034
.032
.035
.034
.032
.033
.036
.0 13

Support
Practice
P

1
1
1
1
1
1
1
1
1
1


















b4
Soil
Loss
(T/ac/yr)
A

4.1
4.7
5.7
4.1
5.2
3.5
2.2
4.3
4.4
3.6
4.2

1.9
2.0
2.4
1.7
2.2
1.5
1.0
1.9
1.9
1.5
1.8

0.6
0.7
0.8
0.5
0.7
0.5
0.3
0.6
0.6
0.5
0.6
CA
Soil
Loss
Cmt/ha/yr)
A

9.3
10.5
12.7
9.2
11.6
7.8
5.0
9.6
9.9
8.1
9.5

4.3
4.5
5.3
3.8
4.9
3.4
2.2
4.2
4.2
3.4
4.0

1.4
1.5
1.7
1.2
1.6
1.1
0.7
] .4
1 .4
1. 1
1 .3
d4
Total
Gross
Erosion
(rot/yr)

176,551
196,544
348,742
486,128
629,138
267,964
171,555
393,504
241,114
81,000
2,992,250

81,269
84,756
146,494
203,721
265,887
117,017
75,938
171,635
102,601
34,468
1,283,786

27,196
27,692
47,388
65,143
86,613
38,678
25,309
56,460
33,572
11 ,278
419,329
e4
Pol-
lutant
}el iverv
Ratio "





.000105







.000105









.000105
f4
Pollutant
Reduction
Eff icienc;





NA

1.0
1.0
1.0
1.0
1.0
1.0
1.0
1.0
1.0
1.0
1.0

1.0
1.0
1.0
] .0
1.0
1 . 0
1 .0
1.0
1,0
1 . 0
i ."b
84
Total P
(mt/yr)
i Y

18.4
20.5
36.6
51.0
66.0
28.0
18.0
41.2
25.2
8.5
313.4

8.5
8.9
15.4
21.4
27.9
12.3
8.0
18.0
10.8
3.6
134.8

2.8
2.9
5.0
6.8
9.1
4.1
2.6
5.9
3.5
1.2
44.0
b^ = RIU.SCP


c. = b, x 2.243
 4    4

d, = c, x a,
Cj  >  PollutnnL  delivery  ratio  -  The  ratio of pollutant to total gross erosion for Initial Case.


f.  >  Pollutant  reduction cfl icienry  -  The extent  that a pollutant yield  i.s decreased from

     a Rivon  decrease  in potential jf,ross erosion.

-------
Smith (1978).  In this example, and in most WATERSHED applications,  the
USLE  will  be  applied to  large  areas.    Thus,  the  USLE coefficients
represent  averages  over  relatively  large cropland  areas.   If  large-
scale averaging  is  not appropriate  for  a particular  area (i.e., crop
types  differ significantly  within  portions   of  a  sub-basin),  it   is
possible to  further  divide the sub-basin.   In this example, the lower
Sandusky sub-basin, position No.  13,  is  broken into "Soil 1" and "Soil
2" areas because of a differance in the K, LS  and C factors.  The "Soil
1" area is composed of clay  surface material  while  "Soil 2" is made  up
of loam surface material.

    Ideally,  the  water quality manager  derives  unique  values  for  the
USLE  variables  which  reflect  the characteristics  of  the local study
area.  If  this cannot  be done,  some  generalized  values may be obtained
from the literature (e.g.,  Wischmeier and Smith, 1978).

    Most of  the USLE values  in  this  example  were  derived  from the U.S.
Army  Corps of Engineers' Lake  Erie Wastewater Management  Study  (LEWMS)
on the  Sandusky  basin (Baker,   1980;  U.S.  Army Corps,  1979b;  Urban _et
al.,  1978).    Because  these data do  not  exactly  fit  the  sub-basin
boundaries,  some modifications were necessary.

    Changes  in  the "C"  factor  reflect  changes  in the  cover  type  and
crop  rotation resulting  from control program  implementation.   The  "P"
factor is  1.0 for  this example,  which implies that very  little contour
or strip-cropping is used  in this basin.

    The USLE is applied to each sub-basin to generate a potential gross
erosion rate  for sediment  (in  tons/acre)  presented  in column b, .  This
value is then converted  to mt/ha  in  column c,.   Values in c,  are then
multiplied by the area (a^)  to  yield  the total potential  gross erosion
of sediment  in mt/yr (d,).   These erosion rates are then  summed for  the
entire  cropland  area, yielding  a total  load  of  2,992,250 mt/yr   (as
shown in d,).

    In this  example, a total river basin cropland load  is  calculated  by
subtracting  the  urban  loads  and rural  non-cropland  loads  from   the
monitored  river mouth  load.   The urban  loads  consist  of  the summation
of columns c_, f^  and  i_;  while the  rural non-cropland loads are found
in column  j~.  In  this example, 101,400 kg/yr of  total phosphorus  are
coming  from  urban  land (before  treatment)  and another  5,146  kg/yr  of
total phosphorus are coming from rural non-cropland.  Subtracting these
amounts from the  monitored river  mouth  load  of 420,000 kg/yr gives a
rural cropland total  phosphorus load of 313,454 kg/yr  from the  entire
river basin.   Note that these  loads  are average annual  loads and  not
indicative of any one year.

    The cropland total phosphorus  load  (313.4 mt/yr or 313,454 kg/yr)
and the cumulative  potential gross erosion (2,992,250  mt/yr)  are used
to estimate  the  total phosphorus  delivery  ratio  for  the entire river
basin.  This is  accomplished by dividing the  total  phosphorus load by
the total  gross erosion.   In  this case, a pollutant  delivery  ratio  of
0.000105 was obtained for  total  phosphorus.    This value,  entered   in
column e^,  is multiplied by all of the  potential  gross erosion values
                                  141

-------
in column d  to obtain cropland total phosphorus loads from each of the
sub-basins.  These are listed in column g, .   A more detailed discussion
of the  rationale for  calculating  the phosphorus  load in  this  way is
given in the companion paper.

    The next step is to determine what effect  the  Stage  I  and Stage II
control  programs  have  on reducing  soil  loss and  the  associated total
phosphorus  load.   Stage  I  and  Stage  II control  of  total  phosphorus
loadings attributable to cropland runoff are defined as follows:

         Stage I Control:  technical  assistance  to educate  fanners on
                           the  techniques  and  economic  advantages of
                           adopting conservation tillage practices.

         Stage II Control: Stage  I  control  plus  application  of  more
                           intensive conservation tillage  practices
                           (i.e., no-till where soils will support  it).

Both of  these programs include crop rotation.  A new cover factor ("C")
is then  calculated  for each of  these  programs.   The  Stage I and Stage
II "C" values were derived  from  the Corps'  study (Urban et al., 1978).
"C"  values  (and thus "A"  values)  decrease  under   the  new  tillage
practices because of increased cover on the cropland (see Worksheet 4).

    The  phosphorus load reduction  caused by  a remedial measure may not
necessarily  be  equivalent   to  the  reduction  in  gross  erosion.    To
account  for  this fact,  Worksheet  4 includes  column  f, ,   "Pollution
Reduction  Efficiency",  where the estimated  percent  reduction in total
phosphorus  relative  to gross  erosion  reduction can be  entered.    This
column only applies to the load  reduction analysis.

    In this example, the pollutant  reduction efficiency has been set at
1.0 (column f,).  This is done only to simplify the illustration, since
the  pollution  reduction efficiency  is  likely to  be  less  than 1.0 for
the cropland strategies chosen (U.S. Army Corps of Engineers, 1979a).

    If  the pollution  reduction  efficiency  were to be considered, the
Stage I  load (L,.) would be calculated  from the  following equation:


    LT = L. .  .  , -  [(E.  .  . , - ET) x PRE x PDR]
     I     initial      initial    I
    where:

                                                        Worksheet
                                                         Column

    LT = Stage  I  Total Phosphorus Load (mt/yr),             g,

    L-  •  •  , =  Initial Total Phosphorus Load  (mt/yr),       g,

    E-  •  •  ,=  Initial Gross Erosion  (mt/yr),               d,

    E.. = Stage  I  Gross Erosion (mt/yr) ,                     d,

    PRE  =  Pollutant  Reduction  Efficiency (unitless), and    e,

    PDR  =  Pollutant Delivery Ratio  (unitless)               f,


                                 142

-------
    For  example,  if the Pollutant Reduction  Efficiency for Loss Creek
in  Worksheet 4  was  0.8  for  the Stage  I  phosphorus  load  reduction
program, L-, would be calculated as follows:


    L. = 18.4 -  [(176,551 - 81,269) x 0.8 x 0.000105] =  10.4 mt/yr
By considering  pollutant  reduction efficiency to be  0.8  as opposed to
1.0,  the  Stage I  load  for Loss  Creek is  increased  from  8.5  to 10.4
mt/yr .

LOADING SUMMARY - (WORKSHEET 5)
    This  sheet  is  used to summarize  information  on pollutant loadings
to  the river  channel  with  and  without control  programs  in effect.
Column  a,, contains  the initial  "uncontrolled" total  phosphorus load
from  each of  the  21  major  sources  identified in  the  Sandusky River
Basin example.  Columns b,. and c,- contain the adjusted total  phosphorus
loads with  Stage  I and Stage II  control in effect, respectively.  All
values  in these first  three  columns  are obtained  from Worksheets 2, 3,
and 4.  Columns d,-  and e-  reflect the load reductions achieved through
the two stages of control.

Point Sources

    It  is  assumed  that   municipal   wastewater  treatment   plants  are
discharging  at  a  4.0 mg/L  total  phosphorus  effluent  concentration
without phosphorus  control programs in  place (column  a-).   Under this
condition, the four major  treatment  facilities  included in this example
— Bucyrus,  Upper  Sandusky,  Tiffin and  Fremont —  account  for a total
phosphorus load to  the river  channel of 68,000  kg/yr, approximately 15
percent of the total  for all sources.

    Under a  Stage I  control  program at  these  municipal  point sources
(total  phosphorus effluent concentration =1.0 mg/L), the load would be
reduced  to   17,000  kg/yr  —  a  decrease of  75  percent.    Subsequent
implementation  of  phosphorus  controls  to  reach  a  0.5   mg/L  total
phosphorus  effluent  concentration  would  reduce  the municipal  point
source  load  to 8,500  kg/yr.

Urban Runoff

    Assuming no programs  in  effect to control urban runoff  in the  four
urban  areas  identified  here,  the  total phosphorus  load entering the
river channel  from  this source (stormwater and  combined sewer  overflow)
is estimated  at  41,870 kg/yr (about  10  percent of the total  load from
all sources).  Approximately 75 percent  of  the  load — 30,900 kg/yr —
is associated with combined sewer  areas.

    Inspection  of Worksheet  5  shows  that  a  Stage I  control program
(streetsweeping  at  7-day  intervals)  would  reduce  the  urban   runoff
contribution  by 2,567  kg/yr.   Stage  II control  (streetsweeping plus
detention/treatment of stormwater runoff and combined sewer  overflows)
would reduce the  load  by another 7,847 kg/yr.
                                   143

-------
                                                             LOADING SUMMARY
                                                                   TOTAL P
                                                                                                                WORKSHEET  5

Source
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky - municipal
- storm
- combiued
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky
TOTAL
Column -»-
Position
1
2
2
2
3
4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13

35
Initial Load to
River Channel
(kfi/yr)
18,868
13,800
320
6,500
20,816
37,072
8,300
0
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34,877
420,416
b5
V
Load to River Channel
With Controls in Place
(kg/yr)
Stage J
8,868
3,400
240
6,091
9,116
15,872
2,100
—
1,574
22,097
28,753
12,772
4,400
1,300
9,776
8,305
18,686
7,000
260
11,562
15,477
187,649
Stage II
3,165
1,728
182
4,536
3,116
7,272
1,036
—
1,172
7,497
9,953
4,572
2,211
980
7,280
2,905
6,586
3,524
196
8,610
5,777
82,301
d5
65
Load Reductions
(kg/yr)
Stage I
10,000
10,400
80
409
11,700
21,200
6,200
—
126
29,600
38,100
15,800
13,300
500
624
10,000
23,300
21,200
90
738
19,400
232,767
Stage II
5,700
1,672
58
1,555
6,000
8,600
1,064
—
402.
14, 600
18,800
8,200
2,189
320
2,496
5,400
12,100
3,476
64
2,952
9,700
105,348
->- Initial:  municipal (c.,), storm (f ) ,  combined sewer  (i_) ,  rural  (j, +  84)-
->• Stage I:  municipal (c2>, storm (f „) ,  combined sewer  (!„) ,  rural  (j., +  g, ) .
-v Stage II: municipal (c2>, storm (fz>,  combined sewer  (i2>,  rural  (J3 +  g^).
= ar - b  -»• The loading reduction from the initial  condition  when Stage I is  implemented.
= bj - c,. -* The loading reduction from the Stage I  condition  when Stage II  is  implemented.

-------
Rural Runoff

    Rural  runoff  represents  the  major source of total phosphorus loads
to  the  Sandusky  River.    Nearly  75  percent  of  the   initial  total
phosphorus  load  to the  Sandusky River (column  a,-)  is  attributable to
rural runoff within the  nine sub-basins.  Of the 319,000 kg/yr entering
the river  channel  from this  source, approximately  98 percent or 313,400
kg/yr  (column  g,)  is   derived   from  cropland  areas.    As  discussed
earlier,  in  this  example  only  cropland   areas   are  considered  for
remedial  action.    Therefore,  the  diffuse  load  from non-cropland —
5,146 kg/yr —  is  not  affected by implementation  of Stage  I  and Stage
II control programs.

    Worksheet 5 shows that  a Stage  I  rural  runoff control program will
reduce  the total  phosphorus  load  to  the   Sandusky River channel  by
179,100  kg/yr.    This  is  more  than   three  times  the  load  reduction
achieved  through  Stage   I   control  of  both  urban  runoff  and  point
sources.   The  Stage  II  program  results  in  an additional  total
phosphorus load reduction of 89,100 kg/yr — over 5  times the reduction
from Stage II control of urban runoff  and point  sources.

    In considering the total load reductions which are achieved through
the control programs included  in  this  case study,  Worksheet 5 indicates
that  Stage I control  at all  major  sources within  the  Sandusky River
Basin would result in a  232,767 kg/yr  reduction  in the total phosphorus
load  to  the  river channel  (column  d_ total) .   This represents  a more
than 50 percent decrease in  the  initial  load (column a^  total).   Thus,
the total  phosphorus  input  to  the Sandusky  River under  Stage I control
at all sources is 187,649 kg/yr  (column be total).

    If  Stage  II  programs  were  in  effect  at   all  major sources,  an
additional load reduction  of 105,348  kg/yr  (column  e,- total)  could be
achieved.  This would yield  a  total  phosphorus  load of  82,301 kg/yr to
the river channel (column d,. total).

PROGRAM COSTS (WORKSHEET 6)

    Worksheet 6 is  used  to compute the costs  of implementing  remedial
measures to  control  pollutant  loads   from each  source.   In  this case
study, costs are estimated for Stage  I and  Stage II programs  to reduce
total phosphorus  loadings  from each of the  21 major sources  listed on
Worksheet 6.

Cropland Costs

    By summing2the rural land  area in  column a,  (Worksheet 6),  a total
of 3,163.6  km  is  obtained.  This  corresponds to  the  total area  of
cropland  contained  within   the   Sandusky  River   Basin  that  will   be
considered  for Stage  I and  Stage II control.

    The  estimated  cost  of implementing  a  Stage  I  rural  program
contained in  column  b^  —  providing  technical assistance to  encourage
mulch-till  or chisel  plowing  in  cropland  areas  —  is $65/km  /yr (see
the companion paper,  Sonzogni et al. ,  1980, for  a discussion of  how
                                     145

-------
                                                                              PROGRAM COSTS
                                                                             TOTAL P REDUCTIONS
                                                                                                                               WORKSHEET  6
cr>
                       Source
LOBS Creek
Bucyrus - municipal
        - storm
        - combined
Broken Sword Creek
Upper Sandusky River
Upper Sandusky - municipal
               - storm
               - combined
Tymocbtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
       - storm
       - combined
Wolf Creek
Rock Creek
Fremont - municipal
        - storm
        - combined
Lower Sandusky

                    TOTAL
                                                Column  -»-
PosJt_Lon_

   1
   2
   2
   2
   3
   4
   5
   5
   5
   6
   7
   8
   9
   9 >
   9
  10
  11
  32
  12
  12
  13
36

Area Treated
(kin")
189.8
	
1.3
7.2
187.2
274.6
—
0
6.7
528,4
542.4
343.6
	
7.0
10.4
343.1
409.9
	
1.4
12.3
343.6

b6
C6
N on point
Initial to Stage I to
Stage- I Stage II
($/kin /yr)
65
—
7,400
7,400
65
65
—
—
7,400
65
65
65
—
7,400
7,400
65
65
	
7,400
7,400
65

3,000
—
8,600
24,700
3,000
3 , 000
—
—
24,700
3,000
3,000
3,000
—
8 , 600
24,700
3 , 000
3 , 000
	
8,600
24,700
3 , 000

d6
6
f6
Point
Units
Served
__
13,500
—
—
—
—
6,250
—
—
—
—
—
26,000
—
—
—
—
19,730
—
—
	

Initial to Stage I to
Stage I Stage II
($/cap/yr)
	
2.4
—
—
—
—
2.4
—
—
—
—
—
2.4
—
—
—
—
2.4
—
—
—

	
3.6
—
—
—
—
3.6
—
—
—
—
—
3.6
—
—
—
—
3.6
—
—
—

86
h6
Total Cost of Program
Initial to Stage I to
Stage I Stage II
(S/yr)
12,337
32,400
9,620
53,280
12,168
17,849
15,000
—
49,580
34,346
35,256
22,334
62,400
51,800
76,960
22,302
26,644
47,352
10,360
91,020
22,334
705,342
569,400
48,600
11,180
177,840
561,600
823,800
22,500
—
165,490
1,585,200
1,627,200
1,030,800
93,600
60,200
256,880
1,029,300
1,229,700
71,028
12,040
303,810
1,030,800
10,710,902
        a   v a/ cropland, or d  or g? or j^, urban land.

        b,   -> Unit area cost of going from the initial cropland  condition to  a Stage I cropland program.
        c,   >• Unit area cost of going from tlie Stage I cropland  program to Stage II.

        d   > Units served (i.e., population served for municipal  plants).
         6
        e,   v Unit cost of going from tbe initial point source load to a Stage I load.
        f,   ->• Unit cost of going from the Stage I point source program to Stage II.
                 x bfi, or

-------
this value  was derived).   Multiplying  this  value by  the land  to be
treated in  each  sub-basin in column a,  yields  a total  annual cost for
Stage I control.

    The  estimated  cost  of  adding  a  further  level  of  rural  control
(Stage II — more intensive tillage practices) is another $3,000/km /yr
(column  Cg).   Again,  applying  this  figure  to  the  area subject  to
treatment results in  the  incremental annual  cost  for  Stage II control
of cropland runoff (column a, x c& = h&).   Thus,  if a Stage II program
were implemented on  cropland in a sub-basin  within the Sandusky River
Basin,  the  annual cost would  be  the  sum  of  columns  g,  and  h,  for
cropland sub-basins.

Cost of Urban Runoff Control

    In this case  study, the  cost of  urban  runoff control  can vary with
both the stage of  treatment and the type of  sewer system present.   As
shown in column  b^,   the  annual  cost per unit  area treated  through a
Stage I  program   is  the  same  for all  urban land  ($7,400).    This is
consistent  with the assumption that the Stage I program (streetsweeping
at  7-day  intervals)   is applied in  both separate  and combined  sewer
areas.

    If a Stage I  program is implemented on all urban land identified in
this example,  the  resulting total  annual cost  for  control  in separate
and combined  sewer  areas (column  g,)  is obtained  by multiplying each
urban area contained in column a, by the annual unit area cost of Stage
I control in column br.
                     b

    The  annual  unit  area cost  of  Stage  II  urban runoff control  is
significantly higher  for  combined  sewer areas  Uian for separate sewer
areas.  Column c, shows a unit cost of $8,600/km /yr for separate sewer
areas and $24,700/km  /yr  for combined  sewer  areas.   This  difference is
due  to  the  fact  that  Stage II control  in  the combined  sewer  areas
includes treatment of combined sewer overflows.   The  incremental cost
for  Stage  II  control  of  these  urban  runoff  sources  (column  h,)  is
obtained by multiplying  column  a,  x  c,.    A  total  Stage II  cost is
calculated by adding the values in column g,  to those in h,.
                                           D              O
Costs of Point Source Control

    The cost of a Stage I program to control  phosphorus loads from each
point  source  (column  g^)  is  obtained  by  multiplying the population
served  at  each  facility  (column  d,)  by  the  annual  cost per  capita
(column e,) .   Stage  I  control at  the  four  treatment plants considered
in  this  example  would  cost  $2.4/capita/year (Sonzogni  et al. ,  1980).
This  represents  the  cost  of  treatment to   achieve  a  1.0 mg/L total
phosphorus effluent concentration (Stage l).

    The incremental  cost  of Stage II  control at  all  treatment plants
(column hg) is obtained by  multiplying  the  population served  in column
dg by the  incremental  unit  cost  increase  in column  f, ($3.6/cap/yr) .
As noted above, a Stage II program is defined as treatment  to achieve a
0.5 mg/L total phosphorus effluent concentration.
                                  147

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COST-EFFECTIVENESS ANNALYSIS (WORKSHEET 7 — MASTER)

    The purpose of Worksheet 7,  the master worksheet,  is to consolidate
the loading  and  cost  information with downstream transmission  data  so
that  a cost-effective analysis  can be  performed.   The  previous
worksheets  have  been  designed   to  help  the manager  make  reasonable
decisions about  each  portion  of the drainage area.   Worksheet  7  draws
all those decisions together  so  that  the cost-effectiveness of  control
programs can be compared and ranked on a common basis.

    As discussed earlier, the value entered in column a., represents the
portion of  a pollutant  that is  transmitted  from  the  point of entry  in
the main channel to the receiving water (river mouth).  In  this  example
it is  assumed that all  pollutants  that  enter the main  channel of the
Sandusky River eventually reach  the mouth (Verhoff et  al.,  1978; Baker,
1980).   Thus, a "T"  of  1.0  is assumed  throughout the main  channel.
Transmission  coefficients  of less than  1.0 at  any  point along  the
channel   will  have  a  direct  effect  on  the  cost-effectiveness
calculations.  This effect will   be  discussed  in  a following section  on
WATERSHED modifications.

    Column  b_  provides  an  opportunity  for analyzing  the  biologically
available or dissolved form of a parameter.  In the case of phosphorus,
it may be very important to know the effect that a program  will  have on
the  biologically  available  fraction, as discussed  in the  companion
paper.  Using this column, various assumptions can be made  in regard to
the  portion of  the .total  phosphorus  that is biologically available.
For example, municipal wastewater  sources  could  be  assumed 100  percent
available,  while cropland  or rural runoff  could be set at 50  percent
(column b_ value of 0.5).  Again, to keep this example simple,  only the
total form is examined here.  Thus column b^ is not applicable  (NA) .

    Column  c-,  represents the total load  to the  main  channel  (surface
water).  This value is taken directly  from Worksheet 5, column  a,-.

    Column  d7  represents  the  calculated  load at  the  river mouth.   To
perform this  calculation, any losses  that occur  (or fractions  that are
not biologically available  if this were  applicable)  along the  channel
must be considered.   The load at the mouth  is given  as the product  of
columns a,,  b.,,  and  c-,.   For  example,  the effective  transmission  at
position  1  is  1.0  (column  a_).   In this  case, column b_ does not  apply
(because  only the  total phosphorus content  is considered).  The  value
of  the  total  load (column  c.,)  entering  the  river channel is 18,868
kg/yr.  Multiplying a-, by c, yields a river mouth load of 18,868 kg/yr.
In  this  example,  column  d7  always  equals  column  c-,  because  the
effective  transmission  equals   1.0.    By  summing all  values  in  d_
(420,416 kg/yr), a total river mouth load is computed.

    Load  reductions and  costs of the  programs are  used  to compute the
cost-effectiveness of the various  control  programs.    If  transmission
losses occur  (or if biological availability is being studied),  the load
reduction must  be adjusted  to  reflect  a load  reduction  at the  river
mouth  (the   point  at  which  the control  programs will  be evaluated).
Columns d,-  and e,-  (Worksheet 5)  represent the load reductions likely to
                                   148

-------
                                                             COST-EFFECTIVENESS ANALYSIS
                                                                         TOTAL P
                                                                                                                     WORKSHEET 7  -- MASTER

Source
STAGE 1
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky - municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
-- storm
- combined
Lower Sandusky
TOTAL

Column"*
Position

1
2
2
2
3
4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13


a7
Effective
Transmission

1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1


b7
Bio-
Available
Fraction

NA






















C7
Total Load
to
Surface Water
(kg/yr)

18,868
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34,877
420,416

d7
Load at
Mouth
(kg/yr)

18,868
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
] ,800
10,400
18,305
41,986
28,200
350
12,300
34,877
420,416
**Subtotal

e7
Load
Reduction
at Mouth
(kg/yr)
STAGE I
10,000
10,400
80
409
11,700
21,200
6,200
—
126
29,600
38,100
15,800
13,300
500
624
10,000
23,300
21,200
90
738
19,400

232,767 **

f7
Cost of
Program
($/yr)
STAGE 1
12,337
32,400
9,620
53,280
12,168
17,849
15,000
—
49,580
34,346
35,256
22,334
62,400
51,800
76,960
22,302
26,644
47,352
10,360
91,020
22,334
705,342

87
Cost
Per Unit
Removed
at Mouth
($/kg)
STAGE I
1.2
3.1
120.2
130.3
1.0
0.8
2.4
—
393.5
1.2
0.9
1.4
4.7
103.6
123.3
2.2
1.1
2.2
115.1
123.3
1.2


h7
Cost-
Effect ive
Rank

7
12
27
33
3
1
11
—
34
5
2
8
13
23
30
10
4
9
26
28
6


a?  -> Effective Transmission  from Source to River Mouth  (usually 1.0).
b7  -t- Portion of parameter  that is judged to be biologically available.
c?  = a5
d?  = a7 x b7 x c?  •*  Load  at the mouth with losses and  availability factored in.
e-7  = d5 x a? x b?  (Stage I), or  =  e5 x  a?  x b?  (Stage II).
fy  = gft  (Stage I), or h&  (Stage  II).
87  = f7 * e7
h?  -> The rank from smallest  to largest value in g? (cost-effectiveness):   NOTE -  A  Stage II program must follow a Stage  I  in the same position.

-------
                                                                    COST-EFFECTIVENESS ANALYSIS
Ul
o
TOTAL p WORKSHEET 7 -- MASTER (conf a.)

	 	



Source
STAGE 11
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky — municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky





Column -*-
•



To? it ion

]
2
2
2
3
'4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13




n7



Effect ivp
Transmission


























b7


15 lo-
Avall.ible
Fraction


























C7

Totjl Load
to
furfaco U.itrr
(ks/yrl























PHASE 1
PHASE II

- d7


Load at
Mouth
(ks/vr)






















**Subtotal
Subtotal
Subtotal
TOTAL


67

Load
Reduction
1 at Mouth
(kn/yt) .
STAGE II
5,700
1,672
58
1,555
6,000
8,600
1,064
—
402
14,600
18,800
8,200
2,189
320
2,496
5,400
12,100
3,476
64
2,952
9,700
105,348 **

232,767
105,348
338,115


£7


Cost of
Program
($/yr)
STAGE II
569,400
48,600
11,180
177,840
561,600
-823,800
22,500
	
165,490
1,585,200
1,627,200
1,030,800
93,600
60,200
256,880
1,029,300
1,229,700
71,028
12,040
303,810
1,030,800
'lO,710,902



87
Cost
Per Unit
Removed
at Mouth
($/kg)
STAGE II
99.9
29.1
192.7
114.4
93.6
95.8
21.1
—
411.7
108.6
86.6
125.7
42.8
188.1
102.9
190.6
101.6
20.4
188.1
102.9
106.3





h7


Cost-
Ef f ect ive
Rank

21
16
38
34
19
20
15
—
40
25
18
32
17
35
31
37
22
14
36
29
24




                   Effective Transmission from Sourrr  t<>  Ri"cr Month  (u'.n.jlly 1.0).

                   Portion of parameter that  is  judged to hc>  1> i o 1 oj; ir.i] 1 y  available.
             '-/
             ''•?
                   .'], x b_ x c   ->• Load at Ihc mouth wiLli  I tv, •.(•", .ind  .wailnhll ity fartored In.
Jr x a  x b   (Stage I), or = e,. x a? x b? (Stage II).

(fi (Stage I),  or hfi (Stage II).
f7 t ,-7

-------
occur at  the  point  of entry if Stage I and then  Stage  II programs are
implemented.   These  reductions  are  adjusted  to represent reductions at
the receiving water (river mouth) by multiplying d,- x a-, x b? for Stage
I, and  e5 x a7 x b?  for  Stage II.   The  results  are  entered in column
67.  Again, because  no transmission losses occur  in  this  example  (T =
1.0 in  column a^), the values  in column e7 for  Stage  I control equal
those  in  column  d,-,  while values  in  column  e7  for  Stage  II  control
equal those in column  e,.

    The costs  of the  control  programs,  computed  on Worksheet  6,  are
entered in  column f,.   These  are the  incremental costs  of  going  from
the initial load  to  a Stage I  load  (column g,) and then  to  a Stage II
load (column h,).
              o

    Column g7 represents  the cost per  unit  of  pollutant removed at the
receiving water  (river mouth).   These  values  are calculated  for  each
stage of  implementation by dividing  column f-  by  column  e7.   In other
words,  the  total cost of  the  control  stage  is  divided by  the total
reduction  achieved  at the  river  mouth.  This  allows   all  stages  of
remedial  effort  to  be compared on the  basis of  their effectiveness of
total phosphorus  load  reductions at the receiving water.

    The final  step on Worksheet 7  is  to rank  the  programs by cost-
effectiveness values.  In  instances  where  programs have the  same cost-
effectiveness value,  the maximum  load  reduction  at the  receiving water
is checked (column e?) and the program that removes the  most  phosphorus
at the mouth  is  ranked first  (the total cost  of the program  could  also
be the secondary consideration).

    Column h7  contains the cost-effectiveness  ranking.   The #1 (most
cost-effective)  program  is  the  one  that  has  the  smallest .cost-
effectiveness value.   As  shown on  Worksheet?,  the #1  program  in  this
example   is  Cropland  Stage  I—providing technical  assistance  for
converting  from  conventional  tillage practices  to minimum  or  chisel-
plow tillage—in  the   Upper Sandusky  sub-basin (position 4,   Stage  I) .
The annual cost of this program  would  be  $0.8/kg  of  phosphorus removed
at the  receiving water (column  g?) .   The load  at the  mouth  would  be
reduced by 21,200 kg/yr (column e?).

    Note  that a Stage  II  program  in column g.,  cannot  precede a Stage I
program (also in column g7) at the  same  position.  This is because all
Stage II  costs  and  load  reductions are incremental,  i.e., in addition
to  Stage   I  costs   and   load  reductions.    For  example,  the  cost-
effectiveness  (at  the river mouth)  of a  Stage  II program  to  control
runoff from combined sewered areas in the City of Fremont (position 12)
is $102.9/kg.    This  is  less  than the  corresponding Stage   I  program
($123.3/kg).   However, the Stage II combined  sewer program  is ranked
higher (#29) than the  Stage I  combined  sewer  program  (#28) because the
Stage II  cost-effectiveness calculations  are  based  upon  the  Stage  I
program being funded and in place.
                                 151

-------
SUMMARY OF PROGRAMS (WORKSHEET 8)

    All of the programs are arranged in their ranked order on Worksheet
8.  Worksheet 8  also  contains  the  load reductions (column a.,) for each
program.  A summation of the load reductions is given in column bg.   In
this example, selecting  programs ranked 1 through  10 would  reduce  the
total phosphorus load at the mouth - by about 200,300 kg/yr.  Moving down
the  list   in  column  a™,  fairly significant  load  reductions  can  be
achieved through programs  25.   Program 26,  it will be  noted,  reduces
the river month load by only 90 kg/yr.

    Columns  Cg   and  dg  present  the  costs  for   each  program  and  a
summation of costs.   The values in column  c»  are obtained from column
e_.  Column  dg  contains a running  summation  of column Cg.   Selecting
programs 1-17 would accomplish a 240,000 kg/yr (column bft) reduction at
a cost of $600,000/yr (column dg).

    It is interesting to note  that  selection  of one more  program (#18)
would reduce the river  mouth load another  18,800  kg/yr.   However,  the
additional cost  ($1.6 million) is almost three times the total cost  for
the first 17 programs.   This  implies  that,  after  program 17, costs  per
unit reduction begin to rise quite sharply.

    Using column bft and column  dg,  a manager  can  quickly estimate an
approximate  cost  for  any  level of  load  reduction,   or determine  a
reasonable load  reduction  for any  level  of funding within  a drainage
area.   For  example, a  300,000  kg/yr  reduction (if  items 1-24  are in
place) would cost about $6.5 million per year to operate.   On the other
hand, if $9 million per  year were available  to control  pollution,  the
first  31   programs  could  be  implemented  and  about a   320,000  kg/yr
reduction in the total phosphrous load could be achieved.

    Many trade-offs can be made  by managers  in deciding  which programs
to  implement.   Numerous  political   and  sociological  factors,  not
considered in this  example, can influence  decision-making.  The ranking
does, however,  give the manager an excellent perspective on the options
available in the Sandusky  River Basin and  provides  the  groundwork  for
further analysis.

EXAMPLE MODIFICATION #1 - Transmission Losses Occur

    To provide  some insight into the effect various assumptions have on
the  ranking  process,  the  effect  of  altering   several  variables  on
Worksheet 7  has been  examined.   First,  it will  be assumed  that  all
values in Worksheet 7 are  the  same  as those  presented  in the previous
Sandusky  River   Basin  example,  with   the  exception of   the  effective
transmission from  the Loss  Creek  sub-basin.   Modified   Worksheet  7,
column a-,, indicates  that  an effective transmission Of 0.5  should  now
be applied to the diffuse loading from Loss Creek.

    According to the  diagram presented on Worksheet 1, a shift  in  the
effective transmission to Loss Creek  would  imply  that  the transmission
coefficient  between  entry  points  A   and  B   has   also  shifted.
Consequently, to be consistent with the physical  representation  of  the
                                 152

-------
                                                                 SUMMARY OF PROGRAMS
                                                                       TOTAL P
WORKSHEET 8

Source
Cropland - Upper Sandusky
Cropland - Middle Sandusky
Cropland - Broken Sword
Cropland - Rock Creek
Cropland - Tymochtee
Cropland - Lower Sandusky
Cropland - Loss Creek
Cropland - Honey Creek
Municipal - Fremont
Cropland - Wolf Creek
Municipal - Upper Sandusky
Municipal - Bucyrus
Municipal - Tiffin
Municipal - Fremont
Municipal — Upper Sandusky
Municipal - Bucyrus
Municipal - Tiffin
Cropland - Middle Sandusky
Cropland - Broken Sword
Cropland - Upper Sandusky
Cropland - Loss Creek
Cropland - Rock Creek
Storm Sewer - Tiffin
Cropland - Lower Sandusky
Cropland - Tymochtee
Storm Sewer - Fremont
Storm Sewer - Bucyrus
Combined Sewer - Fremont
Combined Sewer - Fremont
Combined Sewer - Tiffin
Column ->•
Rank (h,)
f*
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15,
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30

Stage
I
I
I
I
I
I
I
I
I
I
I
I
I
II
II
II
II
II
II
II
II
II
I
II
11
I
I
I
II
I
a8
Load
Reduction
(kg/yr)
21,200
38,100
11,700
23,300
29,600
19,400
10,000
15,800
21,200
10,000
6,200
10,400
13,300
3,476
1,064
1,672
2,189
18,800
6,000
8,600
5,700
12,100
500
9,700
14,600
90
80
738
2,952
624
b8
£ Load
Reduction
(kg/yr)
21,200
59,300
71,000
94,300
123,900
143,300
153,300
169,100
190,300
200,300
206,500
216,900
230,200
233,676
234,740
236,412
238,601
257,401
263,401
272,001
277,701
289,801
290,301
300,001
314,601
314,691
314,771
315,509
318,461
319,085
C8
Cost of
Reduction
($/yr)
17,849
35,256
12,168
26,644
34,346
22,334
12,337
22,334
47,352
22,302
15,000
32,400
62,400
71,028
22,500
48,600
93,600
1,627,200
561,600
823,800
569,400
1,229,700
51,800
1,030,000
1,585,200
10,360
9,620
91,020
303,810
76,960
d8
£ Reduction
Costs
($/yr)
17.C49
53,105
65,273
91,917
126,263
148,597
160,934
183,268
230,620
252,922
267,922
300,322
362,722
433,750
456,250
504,850
598,450
2,225,650
2,787,250
3,611,050
4,180,450
5,410,150
5,461,950
6,491,950
8,077,150
8,087,510
8,097,130
8,188,150
8,491,960
8,568,920
Ul
GO
       b8 =

-------
SUMMARY OF PROGRAMS
      TOTAL P
WORKSHEET 8

Source
Combined Sewer - Tiffin
Cropland - Honey Creek
Combined Sewer — Bucyrus
Combined Sewer - Bucyrus
Storm Sewer - Tiffin
Storm Sewer - Fremont
Cropland - Wolf Creek
Storm Sewer - Bucyrus
Combined Sewer - Upper Sandusky
Combined Sewer - Upper Sandusky
Column ->-
Rank (hj
31
32
33
34
35
36
37
38
39
40

Stage
II
II
I
II
II
II
II
II
I
II
a8
Load
Reduction
(kg/yr)
2,496
8,200
409
1,555
320
64
5,400
58
126
402
b8
£ Load
Reduction
(kg/yr)
321,581
329,781
330,190
331,745
332,065
332,129
337,529
337,587
337,713
338,115
C8
Cost of
Reduction
($/yr)
256,880
1,030,800
53,280
177,840
60,200
12,040
1,029,300
11,180
49,580
165,490
d8
£ Reduction
Costs
($/yr)
8,825,800
9,856,600
9,909,880
10,087,720
10,147,920
10,159,960
11,189,260
11,200,440
11,250,020
11,415,510

-------
                                                                 COST-EFFECTIVENESS ANALYSIS
                                                                              TOTAL P
MODIFICATION #1
 WORKSHEET  7  -- MASTER

Source
STAGE 1
LOB'S Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky - municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky
TOTAL


Column •*
Position

1
2
2
2
3
4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13



a7
Effective
Transmission

1 ' o-S
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1



b7
Bio-
Available
Fraction

NA























C7
Total Load
to
Surface Water
(kg/yr)

18,868
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34,877
420,416


d7
Load at
Mouth
(kg/vr)
%43+
^1&T$33"
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34,877
&&-&Z
4-10, 
3.1
120.2
130.3
1.0
0.8
2.4
—
393.5
1.2
0.9
1.4
4.7
103.6
123.3
2.2
1.1
2.2
115.1
123.3
1.2



h7
Cost-
Ef f ective
Rank

X?" \i
12
27
33
3
1
11
- —
34
5
2
8
13
23
30
10
4
9
26
28
6



cn
01
        ->•  Effective Transmission from  Source to River Mouth  (usually 1.0).
        ->•  Portion of parameter that  is judged to be biologically available.
        =  a5
        =  ay x b7 x c7  -* Load at the mouth with losses  and availability factored in.
     a?  = d5 x a? x b?  (Stage I), or = e5 x a? x b? (Stage II).
     E7  = g6  (Stage I),  or hfe (Stage II).
     17  - f? * e?
     i7  -* The rank from smallest to  largest value  in g?  (cost-effectiveness):   NOTE - A Stage  II program must follow a Stage  I  in the same position.

-------
                                                               COST-EFFECTIVENESS ANALYSIS
                                                                           TOTAL P
                                                                                                           MODIFICATION #1
                                                                                                                              (cont'd.)
                                                                                           WORKSHEET 7 --  MASTER


STAGE II
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky — municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky





Column •*
Position

1
2
2
2
3
'4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13





a?
Effective
Transmission



























b7
Bio-
Available
Fraction



























C7
Total Load
to
Surface '.-atc-t
(k?/vr>
























PHASE I
PHASE II

d7
Load at
Moutl-























**Subtotal
Subtotal
Subtotal
TOTAL

e7
Load
Reduction
at Mouth
(kR/yr)
STAGE II
_5_<7-eO 2j85(
1,672
58
1,555
6,000
8,600
1,064
	
402
14,600
18,800
8,200
2,189
320
2,496
5,400
12,100
3,476
64
2,952
9,700
loz,4^?
les-^TS **

0^rT5T-»
-Le5T?gg'— >
3i*rrl5-»

f.
Cost of
Program
($/vr)
STAGE II
1 569,400
48,600
11,180
177,340
561,600
823,800
22,500
	
165,490
1,585,200
1,627,200
1,030,800
93,600
60,200
256,380
1,029,300
1,229,700
71,028
12,040
303,810
1,030,800

10,710,902
1*7,767
_L°ii!3!_
330,165
S7
Cost
Per Unit
Removed
at Mouth
($/kg)
STAGE II
,9>-9 111.'
29.1
192.7
114.4
93.6
95.8
21.1
—
411.7
108.6
86.6
125.7
42.8
188.1
102.9
190.6
101.6
20.4
188.1
102.9
106.3





h7
Cost-
Ef f ect ive
Rank

^f 33
16
38
34
19
20
15
—
40
25
18
32
17
35
31
37
22
14
36
29
24





en
          a^  -». Effective Transmission  from Source to River  Month (usually 1.0).
          b,  -». Portion of parameter  that  is judged to be  biologically available.
              - a- x b_ x c_
                                Load at the mouth with losses and availability factored in.
d. y. a? x b,  (Stage I), or
                                                    x b? (Stage II).
                   (Stage  I), or hfe  (Stage II).
                f-
                The rank from smallest to lart-f-sl vnl
                                                                -.t -if f ret iveness) :   MOTE - A St,is;e  II  procram must follow a Staze I in the snme nosition.

-------
Sandusky  River  Basin adopted in this  case  study,  the total phosphorus
loading from Bucyrus  City (position 2) would  also  be affected by this
modification.   However,  to simplify  the  anlaysis,  this  example only
considers the impact  of  a change in the effective transmission for one
pollutant source (Loss Creek).

    As shown on modified  Worksheet  7,  the  total phosphorus load  at the
river mouth  attributable  to Loss Creek would decrease to approximately
9,400  kg/yr as  a  result  of  the  aforementioned  change  in effective
transmission (column  d7 = a.- x b7 x c7) .  This implies that control of
cropland  runoff in Loss Creek would not be as  effective in reducing the
load  at  the river mouth.   For example, Stage  I  control  in Loss Creek
would now reduce the  river  mouth  load  by only 5,000 kg/yr (column e.-. =
a.-,  x b7  x  d,) .    The  Stage  I cost-effectiveness  in column  g, then
changes  from ?1.2/kg/yr  to $2.4/kg/yr (column  g_  =  &-.  x f_).   This
adjusted  cost-effectiveness value changes the  rank  of Stage I control
in Loss Creek from 7  to 12  (column h,).

    The change  in effective transmission  for Loss  Creek  becomes even
more  significant when evaluating  the Stage  II program.  As can be seen
in column e_,  the  load reduction attributable  to  Stage II control now
changes   from  5,700  Kg/yr  to  2,850   Kg/yr.    Therefore,  the  cost-
effectiveness of the  program changes from $99.9/Kg to  $199.8/Kg (column
e7).  Based  on  this  new  cost-effectiveness  value,  Stage  II control in
Loss Creek is ranked #38  (column h7).

EXAMPLE MODIFICATION #2 - Changes in Costs

    In this  modification  it is assumed that  the annual  costs  of the
streetsweeping programs within  the separate  and combined sewer areas of
Tiffin,  Ohio  (Stage  I  control)   have been  raised  to  $76,800  and
$108,139,  respectively.    The  effect  of   this  change   is  shown  on
Modification  #2,   Worksheet 7.   The  cost-effectiveness  of   Stage  I
control  within  the   separate   sewered  area  of  Tiffin  changes  from
$103.6/kg  to $153.6/kg,  while  Stage   I  control  in  the  combined  sewer
area has  an adjusted cost-effectiveness value of $173.3/kg (column g_).
As a  result, the cost-effectiveness  ranking  would  change from 23 to 35
for the  stormwater  program, and from  30 to  36 for  the  combined  sewer
overflow  program (column  h_).   This *also has an effect on the Stage II
rankings.   Because  the  Stage II programs follow Stage I,  the  rank of
the  Stage II stormwater  program would  change from  35  to 38  and  the
combined  sewer overflow program from 31 to 37.

SUMMARY OF EXAMPLE  AND MODIFICATIONS

    As is true  in most  all modeling applications,  the accuracy of the
results obtained from WATERSHED are dependent  on the accuracy of  the
input data  base.    Small  changes  in  transmission  coefficients,  cost
assumptions  or  loading  reduction values  can  have  marked  impacts  on
program  evaluations.    However,  WATERSHED   can provide  a  reasonable
first-cut  evaluation of programs using  a variety of data bases.
                                  157

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                                                                  COST-EFFECTIVENESS  ANALYSIS
                                                                              TOTAL P
MODIFICATION n
WORKSHEET 7 - MASTER

Source
STAGE 1
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky - municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky
TOTAL

Column -*•
Position

1
2
2
2
3
4
5
'5
5
6
7
8
9
9
9
10
11
12
12
12
13


a7
Effective
Transmission

1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1
1


b7
Bio-
Available
Fraction

NA





















C7
Total Load
to
Surface Water
(kg/yr)

18,868
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34.877
420,416

d7
Load at
Mouth
(kg/yr)

18,868
13,800
320
6,500
20,816
37,072
8,300
—
1,700
51,697
66,853
28,572
17,700
1,800
10,400
18,305
41,986
28,200
350
12,300
34.877
420,416
**Subtotal

e7
Loa.l
Reduction
at Mouth
(kg/yr)
STAGE I
10,000
10,400
80
409
11,700
21,200
6,200
—
126
29,600
38,100
15,800
13,300
500
624
10,000
23,300
21,200
90
738
19,400

232,767 **

£7
Cost of
Program
($/yr)
STAGE I
12,337
32,400
9,620
53,280
12,168
17,849
15,000
—
49,580
34,346
35,256
22,334
62,400
51,800
76,960
22,302
26,644
47,352
10,360
91,020
22.334
705,342

§7
Cost
Per Unit
Removed
at Mouth
($/kg)
STAGE I
1.2
3.1
120. Z
130.3
1.0
0.8
2.4
~
393.5
1.2
0.9
1.4
4.7
JJJ3-TS 163,
^2^3 173.
2.2
1.1
2.2
115.1
123.3
1.2


h7
Cost-
Effect ive
Rank

7
12
27
33
3
1
11
•"""
34
5
2
8
13
(f 2-y 35
3 ^ft 36
10
4
9
26
28
6


CO
      a,  -»  Effective Transmission from Source to River Mouth  (usually 1.0).
      b?  •*•  Portion of parameter that  is judged to be biologically available.
          » a7 x b_ x c?  •* Load at  the mouth with losses and availability factored in.
          = d5 x a? x b7  (Stage  I), or = 6j x a?  x  b?  (Stage II).
          = gfc  (Stage I),  or hfc  (Stage II).
          = f? * e?
          •* The rank from smallest  to  largest value in g7 (cost—effect iveness) :   NOTE -  A Stage II program must follow a Stage I  in the same position.

-------
                                                             COST-EFFECTIVENESS  ANALYSIS
                                                                         TOTAL  P
                                                                                                        MODIFICATION  #2   
WORKSHEET  7 ~ MASTER  (conf a.)

	 Source 	
STAGE II
Loss Creek
Bucyrus - municipal
- storm
- combined
Broken Sword
Upper Sandusky River
Upper Sandusky - municipal
- storm
- combined
Tymochtee Creek
Middle Sandusky
Honey Creek
Tiffin - municipal
- storm
- combined
Wolf Creek
Rock Creek
Fremont - municipal
- storm
- combined
Lower Sandusky




Column •*
Posit ion

1
2
2
2
3
4
5
5
5
6
7
8
9
9
9
10
11
12
12
12
13




87
Effective
Transmission








b7
SLo-
AvailjbLe
Fraction








i

.






























C7
Total Load
to
Surface Uatet
(kg/vrl























PHASE I
PHASE II

d7
Load at
Mouth
fki/vrl






















**Subtotal
Subtotal
Subtotal
TOTAL


e7
Load
Reduction
at Mouth
(kR/yr)
STAGE II
5,700
1,672
58
1,555
6,000
8,600
1,064
	
402
14,600
18,800
8,200
2,189
320
2,496
5,400
12,100
3,476
64
2,952
9.700
105,348 **
232,767
105,348
338,115


f7
Cost of
Program
(S/vr)
STAGE II
569,400
48,600
11,180
177,340
561,600
•823,800
22,500
	
165,490
1,585,200
1,627,200
1,030,800
93,600
60,200
256,330
1,029,300
1,229,700
71,028
12,040
303,810
1,030,800
10,710,902



g7
Cost
Per Unit
Removed
at Mouth
(S/kg)
STAGE II
, 99.9
29.1
192.7
114.4
93.6
95.8
21.1
—
411.7
108.6
86.6
125.7
42.8
188.1
102.9
190.6
101.6
20.4
188.1
102.9
106.3




h7
Cost-
Effective
Rank

21
16
38
34
19
20
15
—
.40
25
18
32
17
XT 3"S
Jl 37
37
22
14
36
29
24




cn
            •*  Effective  Transmission from Source  to River :!outh (usually 1.0).
            -»•  Portion  of parameter that is judged to be biologically available.

            =  a5
            =  a? x  b?  x  c?  -+ Load at the mouth with losses ^nd -ivailabil ity  factored  in.
            =  d   x  a,  x  b_  (Stage I),  or = e,. x a.  x  b-  (Stage  II).
        fy  =  g6  (Stage I), or hfe (Stage II).
        S7
        h_
              The  rant, from smallest to lar;'e<=t  valur in *• - 
-------
    There is a  great  deal of  flexibility  built into this  approach so
that managers may custom-fit  WATERSHED  to any  drainage  area.   It is
usually desirable  to  execute  WATERSHED  several times  using  different
assumptions  or  ranges  in costs  and  load  reductions  associated  with
different  programs.    The value  of  such  a  sensitivity  anlaysis  was
demonstrated in the  Sandusky  River  example,  where  different  results
were obtained under new assumptions involving transmission and costs.

    The  worksheets  can  be  used   to extract  more  information  than
highlighted  in  this  case study.    For  example,  cost  information on
Worksheet 6  can be  used  to  compare  the  total  control costs  for each
major  category  (cropland,  urban runoff, and  point sources).   Stage I
programs  over  the  entire  basin would  cost $200,000/yr  for  cropland,
$34Q,000/yr  for urban  land  and $160,000/yr  for  point  sources  (from
column gfi) .   The Stage II programs would  cost the amount  for  Stage I
control plus another  $9,500,000/yr  for  cropland,  $990,000/yr  for urban
land and $240,000/yr  for point sources.  This is typical of the type of
data that does  not  directly  assist the WATERSHED  process  but can help
the  managers  analyze  their  plans.     This  type  of  information  is
available from all worksheets.

    Natural variability in the behavior  of most river systems makes it
difficult  to  precisely  predict  pollutant  loads  and  the  effect  of
control programs  for  any  single year.  However, by compiling an input
information  base  which best  reflects  conditions  in or typical  of the
river  basin  under study,  WATERSHED provides a  logical, orderly way to
organize  and use  river basin  data  for  the  purpose of making pollution
control management decisions.
                                  160

-------
                               REFERENCES  CITED

Baker,  D.B.  (1980).  Personal  Communication.    Data on  the  Sandusky
     River.

Drynan, W.R.  (1978).   Relative  Costs  of Achieving  Various Levels  of
     Phosphorus Control at Municipal  Wastawater  Treatment  Plants  in  the
     Great Lakes  Basin,"  International Joint  Commission,  Great  Lakes
     Regional Office,  Windsor, Ontario.

Honey Creek Joint Board of  Supervisors (1980).   "Honey  Creek Watershed
     Project Tillage  Demonstration Results  1979,"  U.S. Army  Corps  of
     Engineers, Buffalo District, Buffalo, New York.

International  Joint  Commission  (1978) .     "Environmental   Management
     Strategy for  the Great Lakes System (PLUARG),"  Great  Lakes
     Regional Office,  Windsor, Ontario.

Johnson, M.G., Comeau, J.L.,  Heidtke,  T.M.,  and W.C. Sonzogni  (1978).
     "Management Information Base and Overview Modeling,"  International
     Joint Commission, Great Lakes Regional  Office, Windsor, Ontario.

Sonzogni, W.C.,  Monteith,  T.J.,  Bach, W.N.,  and V.G.  Hughes  (1978).
     "United States Great Lakes Tributary Loadings,"   Great  Lakes Basin
     Commission  for  the  International Joint  Commission,   Great  Lakes
     Regional Office,  Windsor, Ontario.

Sonzogni,  W.C.,  Monteith,  T.J.,  Heidtke,  T.M.,  and R.A.C.  Sullivan
      (1980).   "WATERSHED  - A  Management  Technique Tor Choosing  Among
     Point and Nonpoint Control Strategies.   Part 1 - Teory  and Process
     Framework," Great Lakes Basin Commission, Ann Arbor,  Michigan.

Urban,  D.R.,  Logan, T.J., and J.R.  Adams (1978).   "Application  of  the
     Universal Soil  Loss Equation in  the Lake  Erie Drainage  Basin,"
     U.S. Army Corps of Engineers, Buffalo District,  Buffalo, New York.

U.S.  Army Corps  of  Engineers  (1975).  "Preliminary Feasibility Report,
     Volume  III,  Appendix  B,  Lake Erie  Wastewater  Management Study,"
      Buffalo District, Buffalo, New York.

U.S.  Army Corps of Engineers  (1979a).  "Lake Erie Wastewater Management
      Study Methodology Report," Buffalo District, Buffalo, New York.

U.S.  Army Corps of Engineers  (1979b).  "Land Management Alternatives in
      the  Lake Erie Drainage  Basin,"   Buffalo  District,  Buffalo,  New
     York.

U.S.  Environmental  Protection Agency (1979).   "Costs and  Water Quality
      Impacts of  Reducing  Agricultural  Nonpoint Source Pollution,"
      Office  of Research and Development,  Athens, Georgia.

Verhoff,  F.H.,  Melfi,  D.A.,  Yaksich,  S.M.,  and  D.B.  Baker  (1978).
      "Phosphorus  Transport  in Rivers,"  U.S. Army  CDrps  of Engineers,
      Buffalo  District, Buffalo, New  York.

Wischmeier,  W.H.,  and D.D.  Smith (1978).   "Predicting Rainfall Erosion
      Losses,"   USDA,  Agricultural  Handbook  No.   537,  Science  and
      Education Administration, Washington, D.C.


                                  161

-------
            BMP CAUSE AND EB'FECT RELATIONSHIPS BY SIMULATION

                                   by

               L.F. Huggins, D.B. Beasley and E.J. Monke
     We  are  currently entering  a period  in which  many  questions are
being  raised about  the  effectiveness  and  the  cost efficiency  of our
national efforts  to  improve the quality of  our  water resources.   These
are  valid  concerns and  they cannot be easily answered.   The questions
are especially difficult when they deal with non-point source  (NPS) pol-
lution.  Much of this difficulty stems from fact that it is very hard to
quantify sources  of  such pollution and to determine cause-effect rela-
tionships between sources and possible treatment methodologies.

     Before presenting a technique to evaluate certain  classes of agri-
cultural Best  Management Practices  (BMPs),  some general  remarks about
the problem of identifying cause-effect relations for NPS  pollution are
in order.
                            BASIC APPROACHES

     Two fundamentally different approaches to establishing cause-effect
relationships between  NPS pollution  and possible control  measures are
field monitoring studies and simulation techniques which rely on models.
The  relative strengths  and  weaknesses  of  these two  methodologies are
quite different.  Obviously, when both approaches are  used concurrently
the strengths of each tend to overcome the other's weaknesses.

Cause-Effect or_ Correlation?

     Two or more variables are statistically correlated when the numeri-
cal value  or level  of one, the independent variable(s), infers a likely
value for the other, the dependent variable.  Two variables are related
by  cause-effect when  there  are governing  physical  laws  which require
that a  change  in level  of the independent  variable  directly  causes a
prescribed  change  in  the  dependent variable.   Variables  which  are
related by cause-effect considerations will certainly show a high degree
of  correlation.   However, statistical correlation does  not,  of itself,
permit one to infer that a cause-effect  relationship exists between the
correlated variables.

     Statistical correlation will occur because variables are related by
physical  cause-effect  considerations or because  both  variables  are
influenced  by  another   unconsidered  variable(s).   To  illustrate  the
latter  situation,  consider the statistical correlation  shown in Figure
1.  Assume a need exists to predict the level of consumption  of alcohol
1.  Respectively, Professor, Assistant Professor and Professor, Dept. of
    Agricultural Engineering, Purdue University, W. Lafayette, IN.
                                  163

-------
and  the  only readily  available data  pertains  to  average  professorial
salaries  (to  make the  illustration more  personal,  substitute your own
profession as the label for the independent variable, since the correla-
tion  can be  expected to  change  very  little).   Such a  correlation is
quite valid and useful for this purpose.

     Now consider  the  situation if this correlation  is  deemed to  be a
cause-effect  relationship and  a  national decision  is  made  to  reduce
total alcohol consumption.   It would  then follow that  the appropriate
course of action would be to reduce professorial salaries to attain this
goal.  Such action would rightly be considered  ludicrous,  especially if
it is your  profession's  salary that is used as the independent correla-
tion variable.
    o  «»
    —  Ul
    t  :
    *  c
       111
    V)
    z
    o
    u

    
-------
of the  scientific  and informed lay communities  believe the only way to
accurately assess impacts of a water quality improvement program is with
a  well-designed and  well-executed monitoring  program.  Unfortunately,
this is a false hope  as  it applies to NFS  pollution,  particularly on a
watershed scale.  While  it is certainly possible to precisely determine
the chemical  constituents  in a  water sample,  it  is  another  matter to
evaluate the true significance of these constituents and their origin.

     A well-designed, comprehensive non-point monitoring program is very
costly  and  time consuming.  Except for irrigated agriculture, non-point
water pollution is generated by rainfall and the resulting runoff.  Many
years of record are required to remove confounding influences due to the
many  combinations  of  rainfall  intensities and antecedent  conditions
which occur.

     If scale-up problems  of translating plot-scale studies to  a real
watersheds are  to  be avoided, it is necessary to monitor what occurs on
natural,  but non-uniform  and  only  partially   controlled,  watersheds.
However, lack of complete experimental control results  in reduced sensi-
tivity to treatments and statistical confounding.

     Finally, monitored  watershed  data are strictly applicable  only to
the area  being monitored.   We do attempt  to transfer results to other
"similar" areas, but all too often results  are  unwisely used under very
dissimilar  physiographic and climatic conditions.   This occurs because
reliable non-point source pollution data are quite scarce.

     For all  these  reasons,  one must conclude  that  it  is  not economi-
cally  feasible to  implement NFS monitoring  programs  which  will  yield
general relationships about  benefits  from  individual  BMPs  installed at
various locations within a watershed.  In fact, the monitoring situation
would be quite dismal were it not for modeling.

     Monitoring and modeling are  inseparably linked.  Concurrent model-
ing provides  a means of transforming  single practice  measurements into
watershed scale projections.  Unique  storm  patterns  during  a relatively
short monitoring  interval  can  be transformed  into  more nearly average
patterns.  On the other hand, concurrent monitoring  on a continuous and
comprehensive basis for relatively long time periods is absolutely vital
if modeling authenticity is to be improved.  Such storm related monitor-
ing is needed for watersheds in different geographic regions.  Monitored
data are the  very  foundation of model  evaluation and  development,  but
they are in dismally short supply.

Simulation

     Simulation is  an analysis  methodology which  uses a  mathematical
model, usually implemented in the form of a computer program, to predict
the behavior  of a  system.   The mathematical model  is a collection of
equations which are purported  to  represent the phyical laws governing
the system's behavior.
                                  165

-------
     Simulation studies allow  cause-effect questions to be  asked about
potential  pollution control measures  because both  naturally occurring
and hypothetical situations can be analyzed.  Results are available very
quickly and inexpensively.  The single, most important disadvantage with
models developed  to simulate  non-point pollution  is  that,   to  varying
degrees, they are all inaccurate.

     Inaccurate results are often obtained from models  which attempt to
simulate  non-point pollution  because  of  the  many complex  factors and
interactions  involved.   To  build a  practical model,   a  developer  is
required to to use relationships which only approximate the true govern-
ing physical  laws.  Approximations are necessary  for two reasons: (1)
inadequate  knowledge  about controlling   physical  processes  and their
interactions and  (2)  a desire to  reduce  data preparation and computer
time costs.

Model Selection

     Choosing a model with which to simulate non-point  pollution is not
simple.   Numerous  models exist.   This is a  direct consequence  of the
complexity of the problem and the varying  degrees of  accuracy which are
thought  necessary  for different  applications.  No  currently available
model is capable of even crudely approximating the vast  range of condi-
tions and physical processes  that fall under the broad heading of NFS
pollution.

     The  "best" model  is  entirely dependent upon which  subset from the
comprehensive list of non-point pollution problems  is  most  appropriate
for a given situation.  Primary factors to consider in selecting a model
are:  (1)  availability  and cost (both for  data preparation and computer
time), (2) applicability to pollutants of  primary interest,  and   (3) the
accuracy  and sensitivity with  which  proposed  treatment  measures are
simulated.

     Despite shortcomings of models  currently available for simulating
non-point  source   pollution,  simulation  is  the  only viable  means for
rational  planning  and  evaluation of'cost  effective  non-point pollution
control  programs.   Furthermore, while it  complicates the  user's selec-
tion process,  much effort  is  currently  underway to  improve the  more
promising models.

     There  are  two primary  impediments to more  rapid   progress toward
improving NFS models.   First,  there is a  severe  lack of reliable, con-
tinuous monitored  data  from test watersheds and  little  evidence of the
public patience  required for  such studies to be of value.  Secondly,
model predictions  are considered  'theoretical1  and  completely  unreli-
able.   This latter  attitude has  resulted from early  experiences  with
very  crude models  or current efforts  which  utilize  models that are
grossly inappropriate for a particular application.
                                  166

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                              CASE STUDIES

     One particular  simulation model designed  for application  to non-
irrigated,  row-crop  agriculture  is  called  ANSWERS  (Areal,  Non-point
Source  Watershed Environment  Response  Simulation)   (1).   ANSWERS  was
developed at  Purdue  University under the sponsorship of the Environmen-
tal Protection Agency,  coordinated by the Allen  County Soil  and Water
Conservation  District (Black Creek  Project)  and  the  Indiana heartland
Coordinating  Commission  (Model  Implementation  Project),  and  in close
cooperation with the Agricultural  Research  section of  the Science and
Education Administration, the Soil Conservation Service and the Agricul-
tural Stabilization  and  Conservation Service.  It simulates the produc-
tion and  transport  of water, sediment, nutrients  and  certain chemicals
from moderate-sized watersheds  (current experience ranges to 15,000 ha).

     Each individual watershed represents a unique combination of topog-
raphy, soils, land use and management.  The amount and spatial distribu-
tion of these resources strongly influence the generation  of non-point
pollutants.   ANSWERS is  a  "distributed  parameter" model,  which means
that it directly simulates impacts of the spatial  distribution of each
resource.  In addition  to  predicting storm flow rates and chemical con-
centrations  at   a  watershed's  outlet,  the model   also  simulates  what
occurs at every  point within a watershed.  This is accomplished by sub-
dividing the  watershed  into a grid of small  (.5-2 ha)  uniform "ele-
ments" whose  behavior is  then individually  integrated  together by the
model.

Planning Example

     As an example of using ANSWERS as a tool for  planning  BMP systems,
let us consider an actual situation, the Marie Delarme watershed located
in NE Indiana.   This  watershed  is composed of almost  500  ha of predom-
inately  (60  percent)  poorly drained Blount,  Crosby and  Hoytville silty
clay loams, with the remainder  being  moderately permeable  Haskins and
Rensselaer silt  loams.   Element slopes ranging from 1  to  6 percent and
with an average of 1.9 percent.  Because of the moderate relief, an ele-
ment size  of 2.6 ha (.1  mi.  sq.) was chosen as  adequate  for modeling
purposes.  The resulting watershed representation is shown in Figure 2.

     In order to rank  the effectiveness of  alternative control stra-
tegies, some  frame of  reference or  "baseline condition"  was required.
To remove effects of particular land use and management practices from
the  baseline condition,  all  tillable  land  (in  this case,  the entire
watershed) was assumed to be planted to conventionally tilled corn.

     In addition to choosing a land use pattern,  a  time  frame must also
be selected.  Average annual conditions are usually used.  Since ANSWERS
is an event-based model,  simulations are performed on  a storm-by-storm
basis.  While it is certainly possible to simulate all  the storms of a
"typical" year and then sum the results, this is  not  necessary in most
situations.   Many research results have shown that most of the sediment
and associated chemicals are  produced by the largest one  or two storms
for  the  year.   Monitored   data  from  the  Black  Creek watershed  in NE
                                 167

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                           STRATEGY
                                      MARIE DELARME WATERSHED
                                         ALIEN COUNTY, INDUNA
                                              0  1/4 Mil. 1/2 lilt.
                              PTO Terrace Area

                              Chisel Plow Area
                Figure 2.  Elemental watershed  representation.

Indiana also  indicate  that average  annual yields  can be  approximated,
for that  region,  by simulating a single  1.5 hr duration, B-distribution
storm which  has a  recurrence interval  of 8 years.   This  hypothetical
storm was  assumed  to occur approximately one month after  planting  with
antecedent soil moisture at field capacity.  Simulating  these conditions
will approximate average annual yields for sediment and  nutrients except
for soluble nitrogen.  Because this single storm  yields only 10  percent
of the  expected annual water yield, annual  soluble nitrogen yields was
not accurately predicted by the single storm simplification.

     Having decided upon a set of baseline conditions, the  next step was
to simulate  the response of the Marie Delarme  watershed to those condi-
tions.  The  result  of that effort  is  shown  in Figure 3.   It shows  the
distribution of net sediment transported  from each  element  for  the base-
line condition.  Note that the values, ranging  from a loss  in  excess of
5000  kg/ha to  deposition  of more than  1000  kg/ha, represent  net tran-
sport from each 2.6 ha element.  Local erosion  rates would  generally be
much higher that the rates of transported sediment.  These  net  transport
rates are predicted by  ANSWERS without  resorting to  a delivery ratio
concept  which  is  very difficult  to quantify.   Instead,  the  specified
watershed  topography, land use and surface runoff rates  determined tran-
sport capacity within the watershed.

     Figure 3 gives information  important for devising  alternative  con-
trol  strategies.   It  shows  that the  highest  sediment and associated
nutrient yields occur in the upper third  of  the watershed  and  gradually
decrease  toward the outlet.   While anyone knowledgeable about  soil  ero-
sion  and  familiar  with the watershed  could  have predicted  this  general
trend  without  a  simulation  analysis,   a  distributed  type  model  is
required  to  quantify actual  yields in  the  manner shown.   More  impor-
tantly, as the  following results demonstrate,  such a model can  predict
relative  impacts of alternative control strategies.
                                  168

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                                         MARIE DELARME WATERSHED
                                          ALLEN COUNTY, INDIANA
                              LEGEND

                           ! YIELD IN EXCESS OF V, TON.'ACRE

                           I VIELD IN EXCESS OF 1 TON/ACRE

                            AREAS INSIDE DASHED LINES SHOW
                             DEPOSITION OF SEDIMENT IN
                             EXCESS OF '/, TON/ACRE
      Figure 3.   Net sediment yield distribution  for baseline conditions.

Figures 4a  through  4d  depict four alternative control strategies.  While
many  other  strategies, possibly even more effective than those chosen,
could have  been  selected,  they illustrate the scope of information made
available and the manner  in which simulation can be  used as  an  effective
planning tool.

     Table  1 summarizes   simulation  results  from  all strategies con-
sidered.   It illustrates  the complicated nature of ranking alternative
programs for NFS pollution control.   The position of a particular stra-
tegy  is very dependent upon  the ranking  criteria  used.   For example,
Strategies  2-5 have been  listed in terms of decreasing effectiveness  for
reducing  sediment  yield  at the outlet of the watershed.   However,  the
ranking would be quite different if  annual unit cost of achieving  a sed-
iment  yield  reduction is  employed.   Still  different results  would  be
obtained  if nutrient yields or concentration levels in the stream  are
chosen.  All  of these  water  quality improvement criteria and others  are
valid  for developing  a  control  program.   Generally,  several  of them
would be given some consideration.  It is the ability of a comprehensive
simulation  model to provide information on such  a wide range of factors
that  makes  it  such an attractive and even essential  tool for planning
NFS pollution control.

     The ranking of strategies is also influenced by the choice of base-
line  conditions, as  illustrated in Table  1 by Strategy 6.   The only
difference  between  results for Strategies 5 and 6 is the severity  of  the
hypothetical  storm  used  to simulate the baseline  condition.   For Stra-
tegy 6, a storm with 25 percent lower intensities  and total volume  was
used.   This gave a sediment  yield of 640 kg/ha for  the same land  use as
in Strategy 1.   When simulation results from Strategy  5  are compared  to
that baseline instead  of  Strategy 1,  they show lower absolute reductions
(110 kg/ha  vs.   170 kg/ha), but an increased  percentage  reduction.   The
unit  cost  of  reducing  sediment  yield  was  also  higher when  the less
                                    169

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STRATEGY *3
               MARIE DELARME WATERSHED
                    ALtEN COUNTY, INDIANA
                                                                       STRATEGY #2
                                                                                      MARIE DELA3ME WATERSHED
                                                                                           ALLEN COUNTY, INDIANA
                                                                             PTO Terrace Area




                                                                             Chisel Plow Area    L.
                 (A)
            (B)
 STRATEGY *4
                MARIE DELARME WATERSHED
                     ALLEN CQLNTY, iHDIAKA
                                                                     STRATEGIES *5&6
      PTO Terrace Area





      Chise! Plow Area
                                                                                       MARIE DELARME WATERSHED
                                                                                            ALLEN COUNTY, INDIANA
PTO Terrace Are.





Chisel Piow Area
                  (C)
            (D)
                 Figure  4.   Location  of BMPs  for  alternative  strategies.




                                                  170

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                                Table 1.  Simulation Results for Alternative Strategies
--4
Area Affected


Strategy*








1.
2.


1
2
3
4
5
6
Baseline
by
PTO

(ha)
0
285
85
91
0
0
BMPs
Chisel

(ha)
0
104
213
272
321
321

Sediment

(kg/ha)
1530
650
1080
1220
1340
520
condition: Fall moldboard
Fro terraces installed
where most
Total Yield at Watershed Outlet
Total
P

(kg/ha)
2.1
.8
1.5
1.6
1.8
.6
plowed, no
Avail.
P

(kg/ha)
.6
.2
.3
.4
.4
.1
BMPs .
of the sediment yielc
Sed.
N

(kg/ha)
13
6
10
11
12
4

3 was in
Sol.
N

(kg/ha)
1.0
.6
.8
.8
.9
.4

excess of 2.;
Sediment
Reduction

(%)

57
29
20
13
19

>5 tonne/hec

Cost**
($/tonne
reduced)

34.70
22.00
35.30
7.50
11.60

'tare. In
          5.
          6.
addition, those  areas  with  sediment yield in  excess  of 1.12 tonne/hectare not benefited by ter-
races were chisel plowed.
PTO terraces installed in the upper 1/3 of the watershed only.  All areas  with sediment yield  in
excess of 1.12 tonne/hectare not benefited by terraces were chisel plowed.
PTO terraces installed in the lower 1/3 of the watershed only.  All areas  with sediment yield  in
excess of 1.12 tonne/hectare not benefited by terraces were chisel plowed.
All areas with sediment yield greater than 1.12 tonne/hectare chisel plowed.
Same as Strategy 5 except that a storm with  25%  lower intensity and total  volume was used.  The
"baseline condition" for this storm gave a total sediment yield of 640 kg/ha.
           Cost  information was based on  1979 construction  costs for  PTO terrace  systems in Allen  County,
          Indiana.   The cost  is based on  total  area benefited  (both  above and below terraces) .   The figure
          used  in these calculations was $510.80  per hectare benefited.   A 10-year  life  was assumed,  which
          yielded an annual cost of  $51.08  per hectare benefited. The  chisel  plow was also assumed to have a
          10-year life.  The average annual  cost  per hectare, based on the cost  of a  new plow,  was $2.17.
          Since  the "design storm" used in  this example produced approximately the annual  sediment yield, the
          cost per  tonne of reduced yield at the watershed  outlet is,  essentially, the annual  cost.  However,
          due  to simplifying assumptions and unique local conditions,  these cost figures should  not  be con-
          sidered to be generally applicable to other planning situations.   They were  included to  demonstrate
          the type  of analyses  which  can be  performed.

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intense baseline storm was used.  This  again illustrates the complexity
of analyzing NFS pollution and its control.
     Evaluation Example

     As  an example of  the use  of ANSWERS for  interpreting monitored
data,  let us consider  it use  in the  Black Creek Project  (2,3).   This
project was  initiated  in late 1972 by  EPA to evaluate the  contribution
of  agriculture  to pollution  of Lake  Erie and  to determine impacts of
selected  BMPs on  that pollution.  The  4900 ha study watershed,  located
in  NE  Indiana,  is composed of relative heavy  soils associated with  gla-
cial till and an  old glacial  lake.   The  land  use  is  almost  entirely
agricultural  except  for  a  small community of about  500 persons.   Its
soils and land use distribution are representative of those in  the  Mau-
mee Basin.

     The  Allen  County Soil  and Water  Conservation District,  with  the
technical  assistance  of  the Soil  Conservation  Service,  developed  a
cost-sharing  program to encourage  installation  of  appropriate BMPs.
Purdue  University and the  University of  Illinois were  responsible for
monitoring the physical/chemical and biological water  quality impacts of
installed  BMPs.   Figure  5 depicts  locations at which physical/chemical
monitoring has been conducted for periods  ranging  from 3  to  6 years. An
even more extensive network of biological monitoring  locations was esta-
blished.
                                      N
                                             O Single BMP
                                             • Rainfall
                                             • Runoff
                                             A Water Quality
                 Figure 5.  Black Creek monitoring  locations.

     The Black Creek project has utilized automated, continuous monitor-
ing  of  stream  water  conditions  near  the  outlet  and  at  selected
subwatershed  points  for about  5 years.   Results from  these  data  were
                                 172

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given in  another  presentation at this seminar.  This comprehensive data
base has  established  a reliable indication of  water  quality conditions
within  the watershed.   However,  it  is  impossible from  such  data  to
answer  the question:  "What  have  been  the benefits  from  individual
classes of  BMPs  installed during the project?"  This  is a result of the
many uncontrolled  factors which influence  levels  of NFS  pollution and
the diversity  of  BMPs, crops and annual  management changes which occur
on a watershed scale.  Such a question can  be  answered  using simulation
analysis  because  it  is  possible  to  hypothetically hold  all  factors,
especially  hydrologic  conditions,  constant and change only  the applied
BMPs.

     Figure 6  shows  the  Black  Creek watershed  subdivided  into  three
major subwatersheds of approximately  equal size.  A  deliberate effort
was  made to  encourage the  installation  of  BMPs within  the  western
subwatershed.  This decision  was made to more clearly differentiate BMP
impacts and to demonstrate the magnitude of water quality change which
was  feasible.  As  a  result,  a  pattern  of decreasing  practice density
occurs  as one goes eastward.   The initial  development of  the ANSWERS
model was undertaken  as  a part of  the  Black Creek Project as it became
apparent  that monitored data alone was inadequate to quantify impacts of
the combinations of installed BMPs.

     The  BMPs installed within Black Creek  were primarily structural in
nature: parallel  tile-outlet terraces (PTO), field borders, grass water-
ways and  livestock exclusion.   Despite  the demonstrated  water quality
benefits  of  reduced  tillage  systems,  only   limited  utilization  was
achieved.   This was the  result of  fanner concern about  wetness during
the spring on the heavy soils of the area.

     The  area of land directly affected by installed BMPs  ranged from 6
percent  in  the  western  subwatershed  to less  than  2  percent  in  the
eastern subwatershed.  ANSWERS  simulations,  using patterns of  land use
change  and  BMPs  installed between 1975  and 1978  with  assumed constant
hydrologic conditions, indicated that BMPs  installed within the western
subwatershed would reduce annual sediment yield about  30 percent.  The
reduction for  the  medium  density middle  subwatershed was  about 20 per-
cent, dropping to  only about 10 percent for the minimum treatment level
on the  eastern subwatershed.   Watershed  scale impacts  from  a single
installation are  also available, but such results are extremely location
dependent.

     One additional result of general  interest was determined.  When the
installed structural  BMPs for the  western  subwatershed  were hypotheti-
cally augmented with chisel plowing in selected critical areas, the pro-
jected reduction of annual sediment yield was increased to 50 percent.
                        SUMMARY AND CONCLUSIONS

     The manner in which a well-adapted simulation model can be utilized
as both a planning and evaluation tool for agricultural non-point source
pollution has been demonstrated with two case studies.  Such results are
                                 173

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                figure 6.  Primary i^lack Creek subwa tersheds.

a direct consequence of  using  a model which  is  constructed from  esta-
blished  cause-effect  relationships between governing  processes and  is
designed to analyze impacts of the type of control measures selected.

     A simulation model  that analyzes  cause-effect relationships  in  a
site  specific  manner  is the only methodology currently  available for
rational planning or evaluation of storm-induced  non-point source pollu-
tion  control.   While  additional  development work will  significantly
improve the accuracy and generality  of such models, the  current state-
of-the-art  is  adequate  to justify  using them  for many applications.
Improvement of current models  is severely hampered  by the  scarcity  of
reliable,  continuous  monitored  data  on  watershed  and   individual  BMP
behavior.
                                  174

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     The Marie Delarme  case  study demonstrated how  ANSWERS simulations
could be  employed in a planning  role to quantify BMP  impacts and rank
site specific BMPs.  Maximum benefits from simulation accrue  when it is
applied  at  the  earliest  project planning  stages.   Furthermore,  this
example illustrated how a  ranking of alternative control  strategies is
dependent  upon  the user  in  the selection of a baseline condition,  or
unit cost, used  and how certain  criteria are  very dependent  upon the
baseline condition that is used.

     The  Black  Creek  Study has  demonstrated  that, even  with  a  very
comprehensive program,  it  is impossible to quantify benefits from indi-
vidual BMPs  by monitoring  the outlet of  a natural, diverse  watershed.
The ANSWERS model did yield a quantitative estimate of BMP benefits.  As
anticipated, benefits were estimated to vary with the number and density
of installed BMPs.  The annual reduction in sediment yield ranged from
only 10 percent  from  the eastern third of the  watershed to  30 percent
from the western,  most  densely treated, third.  Furthermore,  simulation
studies indicated  that  a  reduction  of 50 percent   is  feasible  if  the
installed  structural  BMPs  had been  augmented with chisel  plowing in
selected critical areas.
                               REFERENCES
1.  Beasley,  D.B.  and  L.F.  Huggins.   1980.   ANSWERS  User's  Manual.
   Agric. Eng. Dept.  Purdue Univ., 35p.

2. Lake, J. and J. Morrison.  1977.  Environmental impact of land use on
   water  quality: final  report  of the  Black Creek  project—summary.
   U.S. Envir. Prot. Agency, Region V, Chicago, IL.  EPA-905/9-77-007-A.
   94 p.

3. Lake, J. and J. Morrison.  1977.  Environmental impact of land use on
   water  quality: final  report  of  the Black  Creek project—technical
   report.   U.S.  Envir.  Prot.  Agency,  Region V,   Chicago,  IL.   EPA-
   905/9-77-007-B.  274 p.
                              175

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   PRACTICAL USES OF THE ANSWERS MODEL IN BMP PLANNING:

                 AN ALLEN COUNTY EXPERIENCE

                             by

                        Daniel McCain*
     Other papers in this proceedings discuss the details of the
work done in water quality management and ongoing research of plan-
ning at the national, regional, or state level.  The focus of my
presentation will be practical local use of the ANSWERS computer
model that is now setting priorities for conservation work as
related to water quality in Allen County.  At this time, we are
past the 5 year EPA funded Black Creek (1972-1977) demonstrational
project and well into our second year of applying ASCS Special
ACP Water Quality money.

     To be successful and get conservation on the land to improve
water quality, we've had to involve people—not just agency per-
sonnel, but the people that do the farming.  Ultimately, it is
the farmers who carry out national objectives for conservation.
To gain their cooperation, field people have to bring them to-
gether on some mutual basis.  In the humid midwest (corn belt),
that mutual interest centers on drainage basins.

     In 1969, when I was assigned to work in Allen County, the
emphasis of conservation work in the county—by both the Soil
Conservation Service (SCS) and the Agricultural Stabilization and
Conservation Service (ASCS)—was on drainage.  More than a decade
later, this emphasis has shifted dramatically.  SCS and other
agencies of the U.S. Department of Agriculture have undergone
considerable change in how their appropriations are used, and
their programs have also changed.  In Allen County the difference
has not been due entirely to the earlier Black Creek experience,
but I'm certain that many local changes occurred as a result of
national trends interacting with our staff, the soil and water
conservation district supervisors, and farmers during the 1970's.
We have found ourselves on the "cutting edge" with our local adap-
tion of nationally conceived "non-point source" concerns.

     After the work in Black Creek was complete, a search was made
for other problem areas in the county.  On a critical area map,
targeted rural watersheds were located that had the worst water
quality problems.  The result was a list of 13 small watersheds
(1,000 to 3,000 acres) we call the "Dirty Baker's Dozen."  Using
the ANSWERS model and ranking these watersheds according to gross
soil loss per acre, the most important critical areas were pin-
pointed.  In 1979 special funds wera applied for and received
through the Agriculture Conservation Program (ACP) for a water qual-
ity project.  Most of the $75,000 in ACP funds received in 1979 has
gone into one of the 13 target watersheds, a 1,645-acre area called
the Brunson project.  In 1980, two more critical watersheds were
evaluated and the "Dirty Baker's Dozen" was reranked.  This year
$100,000 is spread into six  (6) of the thirteen (13) watersheds.

*District Conservationist, Soil Conservation Service, Ft. Wayne, IN

                             177

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     A primary reason for this special ACP funding was an innovative
approach to determine where planning is needed.  When a group of people
come to us for what they believe is simple-to-define technical assistance
with drainage, they don't realize that we're going to try our best to
develop their appreciation for water quality improvement, as well as
solve their drainage problems.  We are doubly fortunate in that the rela-
tionships that began emerging with Black Creek in 1972 and that exist
among other local decisionmaking.groups reflects a strong commitment to
attack problems head-on.

     Groups we are now working with in the Special ACP Project approach
are receptive. The ANSWERS model is a big reason why.  Planning with
ANSWERS involves the use of computer drawn maps such as the "erosion
contours" map.  This tool points out "hot-spots" or critical erosion
areas identified by location within the watershed.  A trained conser-
vationist might wonder why these areas cannot be located through field
work instead of using printouts from a computer model.  We can, but
that's not the point.  A computer-drawn map of erosion contours in the
watershed gives a focus for meetings with groups of farmers.  Talking
with them about the map helps them become more receptive to learning
where and when erosion occurs because of slope and concentrated runoff.

     In meetings with the group, we emphasized the proximity of erodible
lands to the drainage outlets.  When a conservation planner presents
the group with a few conclusions from this fact, farmers can readily
visualize where erosion is causing water quality problems.  The total
sediment yeilds computed by the model represent a net loss of topsoil
through the "month" of the watershed.

     A 20- by 40-inch blowup of the Universal Soil Loss Equation (USLE)
sliderule calculator has been used before several groups.  The calcu-
lator has not intimidated the groups:  by using such visual aids, high-
ly technical matters are comprehensible to farmers.  Our partnership
with the groups has to be educational—on both sides—to be effective.
Taking the group on a field trip to see opportunities and to recognize
potential benefits also helps.

     In conservation planning sessions with the groups we have tried not
to put all cur eggs in one basket, for example, with conservation tillage.
Success with conservation tillage depends on many variables.  It was
not possible to persuade many farmers to convert to conservation tillage
during the Black Creek era simply because of these variables.  For ex-
ample, climatic variability over a 4-year rotation might bring a wet
spring, a dry spring, an early spring, and a late spring.  Climate and
other variables require the farmer to make daily decisions that can
complicate  his tillage plans.

     Not that I'm negative about conservation tillage—in fact it's the
one practice that can touch every acre—but I've seen what can happen
when a farmer tries it  without fully understanding it.  It may require
him to adapt his equipment and make other changes.  Every spring day
the farmer can  face a different set of weather conditions, crop prices,
operating expenses, and other things which he has no control but on
which he must form decisions.  Therefore, it is important to offer the
farmer conservation alternatives that won't add to his burden of daily
decisionmaking.  Seen positively,  however, conservation tillage is  not
a burden at all but an investment in wise management that pays off in
savings in fuel, labor, time, water, and soil.

                                 178

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      Even so, practices such as  terraces serve as permanent  "reminders"
 of  conservation on  the landscape.  These practices  can be very  compat-
 ible  with conservation tillage;  most important, however, they  signal a
 "commitment to conservation"  and become symbols of the  group's progress
 in  understanding and dealing with erosion and sedimentation.  And  if na-
 ture  provides a disastrous spring for tillage, at least  part of the con-
 servation system will function.

      Permanent conservation practices require the farmer to make fewer
 decisions, although they won''t necessarily be any easier to make than
 decisions about tillalge.  For example, if a farmer wants to construct
 terraces and waterways and needs financial help, he requests cost-sharing
 assistance from the ASCS office.  SCS provides an engineering plan and
 gives him a cost estimate, and his thoughts come down to a one  time "yes
 or  no" decision.  If he decides  to go ahead with the practices, a  con-
 tractor builds them and they become a. permanent facility.  The  only ques-
 tion  remaining is whether the farmer will permanently maintain  the prac-
 tices.

      In all, then, there are three ways we can tackle cropland  erosion
 problems related to water quality.  First, we encourage  changes in TIL-
 LAGE  and in planting techniques.  Second, we encourage CROP ROTATIONS
 that  are compatible with the farmer's present tillage system.   Or  third,
 we  suggest permanent land treatment practices such  as TERRACES, which
 reduce slope length and increase temporary storage  capacity for runoff.
 If  the farmer selects any on of  these changes—or some combination of
 them—improved water quality should be the result.

     When we targeted critical areas in the Brunson project we  had to
 go  after the job from the top of the hill down.  We didn't want to re-
 peat an earlier experience in Black Creek; that is,  overselling the
 group on what they were already prepared to request—outlet development.
 Also, in Black Creek more streambank protection than necessary  may have
 been installed because of the farmers' concern about highly visible
 streambank erosion.  Black Creek findings showed that only about 7 per-
 cent of the sediment load entering the Maumee River  was  caused  by  stream-
 bank erosion.  However, the farmers noticed streambank erosion  more than
 they noticed sheet and rill erosion'on sloping cropland.

     In planing with the groups and in orienting them to the kinds of
 practices needed, ASCS  and SCS can provide farmers with cost sharing
 and technical help as far down the outlet as necessary to make  a pro-
 perly functioning project.   In the Brunson project,  individual  terrace
 outlets were safely taken down the watershed through tile beside group
 grass waterways, and into a protected mutual open outlet.  All  these
 practices helped as part of a protective scheme for  the  critical areas.

     It may also be necessary to study the channel  far enough through the
 critical areas to find the unstable segments.   In Black Creek,  we were
most successful with a practice we call "training," that is,  putting rock
riprap low on the channel banks in unstable soils and installing a 1%- to
 2-foot drop structure to lessen channel grade.

     From the top of the watershed down,  an opportunity and an obligation
exists to explain technical alternatives to .the  farmers.   The  ANSWERS mo-
del is useful for these explanations because it graphically depicts the
eroding areas.   An overlay  of the erosion contours map with an ownership

                                 179

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map lets the farmer see whether he has an erosion problem that requires
attention.  But don't tell him, "Look, you dirty farmer, you're causing
all these water quality problems and you're going to have to do something
to clean them up."  Instead, approach the group in a positive way by
showing them the beneficial things that they can do—both as a group and
as individuals—to improve water quality and reduce the sedimentation
on their neighbors' lands donwstream.

     In some cases, the approach to land treatment in the Brunson pro-
ject was turned 180 degrees from the previous approach in Black Creek,
where outlets were usually developed first.  In the Brunson project, we
started at the top of the watershed by securing commitments from farmers
for cropland  treatment.  Of the $75,000 allocated for the Dirty Baker's
Dozen in 1979, ASCS approved $60,000 for cost sharing of group parallel
tile outlet (PTO) basin terraces in the Brunson watershed.  To make the
terraces work, waterways were constructed and outlets developed to handle
the metered tile flow from the terraces.  Most of the job was completed
in 1979. ' A second smaller group—SOUTHWEST BRUNSON—with some of the
same farmers, completed additional terraces and a mutual waterway in the
summer of 1980.

     The ANSWERS model could prove even more valuable when used with the
analysis of BMP's on farms and as a group.  The hypothetical watershed
(figure 1) and reduction  estimates  (table 1) illustrate a means of using
the ANSWERS model in planning.  Perhaps the time will come when the pub-
lic will buy water quality improvement with "dollars spent for tons saved."
                               180

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Tablf 1 - Effect of BMPs in reducing sediment
GROUP
A

SUB
GROUP
B

SUB
GROUP
C




SUB
GROUP
D

SUB
GROUP
E

INDIVIDUALS
ALL PLUS
SAMUELS
SMITH
FRY
SHARP
JONES
GREEN
GRAY
JOHNSON
JONES
GREEN
GRAY
JOHNSON
CELLS
100
20
17
13
6
14
8
10
12
14
8
10
12
PRIMARY
BMP
APPLICATION
OUTLET
LIVESTOCK
EXCLUS,
NONE
NONE
WATERWAY
TERRACES
TILLAGE
TERRACES
NONE
TERRACES
TILLAGE
TERRACES
NONE
LEVEL (/
INITIALLY
1350
1500
2000
1000
700
1000
1200
900
1200
1000
1200
900
1200
WE/FARM)
WITH BMP'S
675
700
2000
1000
500
400
600
400
1200
400
600
400
1200
%
REDUCTION
50%
53%
0%
0%
28%
60%
50%
55%
0%
60%
50%
55%
0%
181

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SCS-223  <»-&«
                                              CONSERVATION PLAN MAP
                           UNITED STATES DEPARTMENT OF AGRICULTURE      SOIL CONSERVATION SERVICE
                                                        cooperating with
E OUR SOIL * OUR STRENGTH =
Owner _
Operator
                 County
                   Conservation District

 G£OUP  PtoOJCCT    Plan No..
	  Scale	
                                                                 Photo No.,
                                                   Stale
Date
Acres
                                                                                  Appioiimote
                          F/BURE1  -  HYPOTHETICAL
                                           182

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      WATER QUALITY:  SEDIMENT AND NUTRIENT LOADINGS FROM CROPLAND

                                   by
                                                              ft
         D. W. Nelson, D. B. Beasley, S. Amin, and E. J. Monke
     Public Law 92-500 passed in 1972 mandated that each state prepare
a water quality management plan which encompasses nonpoint as well as
point sources of pollution.  In attempting to prepare strategies and/or
plans for control of nonpoint pollution, most state and federal
planning/regulatory officials became aware that relative little is known
about the amounts of water pollutants originating from agricultural
land or the effectiveness of techniques to control or minimize pollutant
deliveries.  Preliminary studies suggested that the most significant
water pollutants originating from cropland are sediment, plant nutrients,
and pesticides (1).

     Although a number of small watersheds (<30 ha) at various locations
in the eastern U.S. had been periodically monitored during the past 20
years, no monitoring of a medium size (vLOOO ha) agricultural watershed
had been conducted.  Furthermore, the effectiveness of soil conservation
practices known to reduce erosion on small plots had not been evaluated
on a medium size watershed.  Therefore, a long term study of the effects
of agricultural activities on water quality was started in 1973 on a
5000 ha watershed in Allen County, Indiana.  The project was funded under
the Great Lakes Program, Region V U.S. Environmental Protection Agency
and involved coordinated efforts of the Allen County Soil Conservation
District, the Soil Conservation Service, the Agricultural Research
Service, Purdue University, and the University of Illinois.  The
objective of the project was to determine if water quality in the water-
shed and in the Maumee River could be improved by implementation of a
wide range of soil conservation practices in the drainage area.  For
details of the project consult Lake and Morrison (2).
                          MATERIALS AND METHODS

Study Area

     The 5000 ha Black Creek watershed (Figure 1)  was selected for study
because it was representative of the soils and land uses prevailing in
the Maumee River drainage basin.  Table 1 provides information on the
soils and land use in the watershed.  About two-thirds of the area
consists of nearly level lake plain and beach ridge soils, whereas
one-third of the area is gently sloping (3-6%) glacial till soils.
Land use in the watershed is about 60% row crops,  30% small grain and
pasture, and 10% woods, roads, and developed areas.  The drainage pattern
in the area consists of one natural stream (Black  Creek) running from
*Professor of Agronomy and Assistant Professor,  Research Associate,  and
 Professor of Agricultural Engineering, Purdue University,  W.  Lafayette,
 IN 47907.  Indiana Ag. Exp. Sta. Jour. Paper No.  	.
                                   183

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 APPROXIMATE  SCALE
        KILOMETERS
1/2      0      1/2
     Figure 1.  Map of the Black Creek study area.
                          184

-------
west  to east and discharging into the Maumee River  (Figure 1).  A
number of constructed drainage ditches intersecting with Black Creek
are used as outlets for surface and tile drains.  Most of the lake
plain soils in the watershed are tile drained.

Table 1.  Characteristics of the Black Creek watershed and two intensively
          studied drainage areas within the watershed.


      Characteristic        Black Creek     Smith-Fry       Driesbach
      unaracteris  cs         watershed   Drain  (Site 2)  Drain (Site 6)

Drainage area, ha              4950           942             714
Soils:
  Lake Plain & beach ridge       64%            71%             26%
  Glacial till                   36%           29%             74%
Land  use:
  Row crops                      58%           63%             40%
  Small grain & pasture          31%           26%             44%
  Woods                           6%            8%              4%
  Urban, roads, etc.              5%            3%             12%
Number of homes:                 —            28             143
Monitoring Systems

     Grab sampling stations were established at 14 sites within the
watershed and on the Maumee River to provide weekly data on the quality
of water originating from soils and land uses in the drainage area above
the site.  Automated sample  (PS 69) and flow measuring devices were
installed at three locations (Sites 2, 6, and 12) in the watershed
(Figure 1) to provide continuous flow data and to permit calculation of
loadings on a storm or time period basis.  Meteorological conditions in
the watershed were continuously monitored.  A complete hydrometeoro-
logical station with automatic data acquisition and remote transmission
capabilities was established at Site 6.  The amount of rainfall was
measured at seven other locations in the watershed and rainwater samples
were collected for chemical analysis at two locations.

     Temperature and dissolved oxygen concentration of water were
measured _in situ and shortly after collection pH, turbidity, and
alkalinity were measured in grab samples.  Water samples taken by grab
or automated methods were frozen soon after collection, transported to
the Water Quality Laboratory at Purdue University and analyzed for sus-
pended solids, NH^-N, NOl-N, soluble organic N,  sediment-bound N, soluble
inorganic P (filtered reactive P), soluble organic P, and sediment-bound
P.  Pesticides, alkaline earth cations, and heavy metals were measured in
selected samples.  Methods used for analysis of all samples were those
prescribed by the American Public Health Association (3) or the U.S.
Environmental Protection Agency (4).

Data Processing

     Loadings of sediment and nutrients were calculated by integration
of flow and concentration data on a storm, monthly, quarterly, or yearly


                                 185

-------
basis.  Flow weighted mean concentrations (monthly basis) were
calculated by dividing the monthly load of sediment or nutrient by the
monthly volume of runoff.  The average total N and P concentrations in
suspended sediment were calculated by dividing the monthly sediment-
bound N and P loads by the monthly sediment load.  The enrichment ratios
for total N and P were calculated by dividing the total N and P
concentrations in sediment by the average total N and P concentrations
in soils present in the drainage area.  Linear regression and correla-
tion techniques (5) were used to determine the relationships between
monthly or quarterly runoff volume, sediment losses, nutrient losses,
and nutrient concentrations in sediment.
                         RESULTS AND DISCUSSION

     Reconnaissance sampling within the watershed revealed that no
significant amounts of hexane-soluble pesticides were present in water,
sediment, or fish tissue.  Specific pesticides evaluated included
aldrin, dieldrin, DDT and metabolites, atrazine, trifluralin, and
2,4,5-T (2).  Analysis of weekly grab samples established that the
dissolved oxygen, temperature, pH, alkalinity, and alkaline earth
cations levels exhibited trends which were typical for medium size
agricultural watersheds (6).  Heavy metals were present in only trace
concentrations (6).

Sediment and Nutrient Loads

     Table 2 provides information on rainfall, runoff, and sediment
lost from the two major drainage areas in the Black Creek Watershed
during the period 1975 to 1978.  Precipitation was above normal in 1975,
below normal in 1976, and near normal in 1977 and 1978.  Runoff volumes
tended to be highest during years with greatest rainfall, however, the
percentage of precipitation appearing as runoff varied over the years
(26% in 1975, 17% in 1976, 20% in 1977, 26% in 1978, an average of 22%
over 4 years).  Sediment discharges from the watershed averaged 895
and 1279 kg/ha for Sites 2 and 6, respectively.  However, sediment
losses in 1975 were from 4 to 8 times higher than the average of the
other three years.  Sediment losses during 1977 and 1978 were low
(380 to 540 kg/ha) even though rainfall during these years was near
normal.  This finding suggests that best management practices implemented
in the watershed during 1975 and 1976 resulted in reduced sediment losses
in subsequent years.

     Data on amounts of sediment-bound N and P discharged from the two
drainage areas during 1975 to 1978 is also given in Table 2.  The
quantities of sediment-bound nutrients lost from the drainage areas
decreased markedly after 1975, generally in proportion to reductions in
sediment loss.  Application of best management practices in the water-
shed was, at least in part, responsible for reductions in amounts of
sediment-bound nutrients observed during the course of the study.

     Table 2 also provides data on the amounts of soluble nutrients
discharged from the two drainage areas during a four-year period.
Although the amounts of soluble inorganic P annually discharged from the
                                 186

-------
drainage areas were low (<0.7 kg/ha/year), there is no indication that
the amounts lost decreased with time during the study.  In fact, there
was a marked Increase in soluble inorganic P loss during 1978.  One
explanation for the increase in soluble P loss at Site 6 during 1978 is
that large volumes of untreated household wastewater was discharged into
the drainage ditches near Harlan during the time an interceptor sewer
was being constructed.  Previous studies have shown that septic tank
effluents were a major source of soluble P measured at Site 6 (7).  The
amounts of NHt-N, NOo-N, soluble organic N, and soluble organic P dis-
charged from the drainage areas each year were directly related to the
volume of runoff.  Losses of soluble organic P were very low (<0.13 kg/
ha/year) except at Site 6 in 1978 where septic tank effluent likely
contributed to the load.  Soluble organic N losses were significant
(0.74 to 2.89 kg/ha/year) during all years at each site and the higher
losses measured at Site 6 probably reflect septic tank inputs.  Losses
of NH^-N were relatively low (0.58-1.82 kg/ha/year) throughout the period
of study except for Site 6 during 1978.  Septic tank effluents likely
were responsible for higher NH^-N losses observed at Site 6 in 1978.
The amounts of NO^-N in drainage water appeared to be related to
amounts of rainfall in the watershed, i.e. losses of NO^-N were highest
in 1975 and 1977, the two years with highest rainfall.  Losses of NO^-N
were relatively large (average of 12 and 8 kg N/ha/year for Sites 2 and
6, respectively) and likely reflect the fact that the watershed is tile
drained and that the soils are maintained in a high state of fertility
by applications of manure and inorganic N fertilizers.  Although the
amounts of NOo-N discharged from the watershed were substantial, the
annual flow weighted mean NOo-N concentration never exceeded the U.S.
Environmental Protection Agency drinking water standard (10 mg/1).

     The data in Table 2 suggest that adoption of best management prac-
tices to control soil erosion has not resulted in a reduction in the
discharge of soluble forms of N and P from the watershed.  In fact,
there is an indication that losses of soluble N and P increased slightly
as soil conservation practices were implemented during the study.  In
future projects some attention should be given to implementation of
best management practices which minimize the transport in drainage water
of soluble nutrients originating from soils.

     The annual discharges of sediment, sediment-bound nutrients, and
soluble N from Site 2 (almost all cropland) were similar to those from
large river basins and some small watersheds (Table 3).  However, the
annual sediment losses measured at Site 2 tended to be lower than sedi-
ment losses reported for several small (<33 ha) watersheds planted to
row crops.  There is little sediment deposition in small watersheds, but
considerable deposition in the Black Creek area.  The soluble inorganic
P loadings measured at Site 2 were similar to those reported from both
river basins and for small watersheds.  Soluble N (NH^-N plus NO'o-N)
loadings at Site 2 were higher than those reported for many small water-
sheds.  This finding likely results from the NOo-N in tile drainage
water present in the Black Creek watershed, but absent in most of the
small watersheds previously studied.
                                 187

-------
Table 2.  Rainfall, runoff, and sediment and nutrient loss occurring
          in two drainage areas of the Black Greek watershed during
          the period 1975 to 1978.
Parameter
Rainfall, cm
Runoff , cm

Sediment loss, kg/ha
Sediment P
Sediment N
Sol. inorg.
kg/ha
Sol. org. P
NH^-N loss,
NO~-N loss,
Sol. org. N
loss, kg/ha
loss, kg/ha
P loss,
loss, kg/ha
kg /ha
kg/ha
loss, kg/ha
Site
no,
2 &
2
6
2
6
2
6
2
6
2
6
2
6
2
6
2
6
2
6
1975
1976
6 108
29
26
.1
.0
66
12.4
10.1
2126
3735
5.
4.
31
28
0
0
0
0
1
1
19
11
2
2
24
51
.25
.98
.14
.34
.11
.13
.51
.82
.01
.63
.33
.51
0
0
4
2
0
0
0
0
0
0
5
2
0
0
637
384
.98
.73
.82
.86
.06
.18
.04
.04
.60
.85
.55
.39
.93
.74
Year
1977

96
18.5
19.4

1
1
4
4
0
0
0
0
0
1
15
12
1
1
435
452
.67
.78
.55
.71
.14
.47
.06
.10
.58
.30
.42
.73
.10
.78
1978
77
18.5
21.3
380
544
0.65
0.79
6.10
6.91
0.21
0.68
0.08
0.35
0.75
3.06
8.27
5.96
1.66
2.89
Ave.
86
19
19
.8
.6
.2
895
1279
2.
1.
11.
10.
0.
0.
0.
0.
0.
1.
12.
8.
1.
1.
14
95
68
87
14
42
07
16
86
76
06
18
55
98
     Average monthly rainfall, runoff, sediment loss, and nutrient loss
values are given in Table 4.   Rainfall was reasonably well spread
throughout the year with April, June, and August having the highest
monthly average amounts.  Sediment losses were greatest in February,
March, May, and June, whereas sediment losses were very low (<14 kg/ha/
month) from July through November.  Sediment N and P losses paralleled
sediment losses in that the highest discharges of sediment-bound nutrients
occurred in May and June and low discharges were observed from July
through November.  The highest monthly losses of Nff£-N, soluble organic
N, soluble inorganic P, and soluble organic P were observed in the period
February through April.  This finding suggests that snowmelt runoff and
early spring rains were responsible for significant transport of soluble
N and P.  Some of the soluble N and P transported likely was leached
from residues from the previous crop present on the soil surface at the
time of snowmelt.  Substantial amounts (>1 kg N/ha/month) of NO^-N were
transported out of the Site 2 drainage area during February, March, April,
June, and December.  The finding that relatively high losses of NOo-N
occurred during months when sediment loss was not high (April and
December) suggests that a subsurface flow and tile drainage are major
transport means for NO-j-N in the Site 2 subwatershed.
                                  188

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          Table 3.  Annual sediment and nutrient loading from selected agricultural watersheds in the United States.
oo
Watershed
Location

Ohio (Maumee
River Basin)d
Ohio (Portage
River Basin)d
Ohio (Plot lll)d
Mich. (Ave. of
Plots)6
Georgia
(Watershed P2)f
Iowa
(Watershed 2)8
Oklahoma
(Watershed C3)h
N. Carolina
(Watershed 2)1

Ohio (Maumee) ^
Michigan
(Mill Creek) J
Ag Watersheds^

Size
ha
.639 x
111 X
3.2
0.8
1.3
3.3
17.9
1.5

-
-
-

i-rdliU
Use

106 Mixed
10 3 Mixed
Soybeans
Row
Crops
Corn
Corn
Cotton
Corn
Wheat
Pasture
Cropland
Cropland
Cropland

Sediment

950
658
—
12940
6022
9980
3900


80-5100
20-70
400-800
Pollutants
Sed. P Sol. Pa

1.53 0.29
0.84 0.30
1.09 0.13
0.71
—
0.09
5.6 1.1
0.27

0.7-4.3 0.05-0.3
0.1-0.3 0.1-0.3
0.6-0.9 0.3 -0.4
transported
Sed. N Sol. N Reference

13.4 9
13.1 9
12.3 9
25.8 2.8 10
10.3 3.7 11
14.8 1.4 12
9.7 1.9 13
12.08 14

1
4.3-10c 1
16-31° 1
          a, Sol.  P  is  soluble inorganic  P  (filtered  reactive  phosphate);  b, Sol.  N is (NH^-N + NOo)-N; c, Sediment-bound
          and  soluble  N  combined;  d, Average of  data  from  1975-1976;  e., Average of data from 1974-1975; f, Average of data
          from 1973-1975;  g.,Average of data from 1969-1975; h^Average of  data from 1966-1976; i^Average of data from
          1968-1972; ^ Average of  two years data from  1975-1977.

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Table 4.  Average monthly rainfall, runoff, and sediment and nutrient
          losses from the Site 2 drainage area during 1975-1978.
i,  4-u T, - .c 11 Total  Sediment NHt-N NOo-N Sediment Sol. inorg. Sedxment
Month Rainfall     ....   .  .     i4.,3              r, i  <-     T> i  <-
               runoff   lost    lost  lost  N lost    P lost     P lost


Jan.
Feb.
Mar.
Apr.
May
June
July
Aug.
Sep.
Oct.
Nov.
Dec.


3.0
4.7
7.5
10.4
8.0
10.9
5.2
10.9
7.2
4.9
5.7
5.6


1.16
2.66
5.38
3.19
1.64
1.86
0.18
0.13
0.43
0.14
0.40
2.44


30
167
109
80
236
168
8
2
13
1
9
72


0.05
0.18
0.21
0.14
0.11
0.07
0.01
0.00
0.01
0.00
0.02
0.08


0.94
1.51
2.87
2.34
0.82
1.26
0.14
0.02
0.16
0.02
0.13
1.87
Vo- /Via
Kg/ na
0.33
1.10
1.15
1.49
3.54
2.82
0.07
0.01
0.10
0.01
0.12
0.87


0.004
0.020
0.049
0.019
0.008
0.008
0.002
0.001
0.004
0.000
0.002
0.023


0.050
0.317
0.243
0.209
0.522
0.414
0.016
0.004
0.033
0.002
0.039
0.287
Total   84.0   19.8     895    0.88  12.08  11.99      0.140     2.174
Average Monthly Flow Weighted Mean Concentrations

     Average monthly flow weighted mean suspended solids and nutrient
concentrations are given in Table 5.  Suspended solids and sediment-
bound nutrients concentrations were highest in February, May, and June
and lowest in March, August and October.  Fortunately, the poorest water
quality from solids and insoluble nutrient standpoints occurred during
the annual period of highest flows.  Soluble organic N concentrations
were reasonably stable over the year varying from 0.56 to 0.95 mg/1.
Highest soluble organic N concentrations were observed in January and
September.  Ammonium N concentrations were highest in February and
May and lowest in August and October.  Low NH^-N concentrations in late
summer may reflect assimilation by the profuse algae and aquatic weed
growth present in the ditches from August to October.  Nitrate N
concentrations were very high (>7.5 mg/1) during January, July, and
December.  Relatively low N07-N concentrations (<2 mg/1) were observed
during August and October when tile drains were not running and little
water was present in the ditches.  Soluble inorganic P levels exceeded
0.09 mg/1 in March, July, September, and December.  Only October had a
flow weighted mean soluble inorganic P concentration less than 0.01 mg/1.
The fact that inorganic P concentrations remained relatively high
throughout the summer is surprising in light of the algae and weed
growth in the stream.  One possible explanation is that sediment present
on the stream bed maintained the inorganic P level in solution by
equilibrium processes.  Soluble organic P concentrations were relatively
constant over the year, although the highest concentrations (0.08 mg/1)
were measured in August and the lowest level (0.007 mg/1) was observed
in October.
                                   190

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Table 5.
Average monthly flow weighted mean sediment and nutrient concentrations in Site 2 drainage water
during 1975-1978.
Month


Jan.
Feb.
Mar.
Apr.
May
June
July
August
Sep.
Oct.
Nov.
Dec.
Overall
Suspended
solids


259
628
203
251
1439
903
444
154
302
71
225
295
452
NH+-N


0.43
0.68
0.39
0.44
0.67
0.38
0.56
0.08
0.23
0.07
0.50
0.33
0.44
N03-N


8.10
5.68
5.35
7.34
5.00
6.77
7.78
1.54
3.72
1.43
3.25
7.66
6.11
Sol. org.
N
.
— mg/1
0.95
0.75
0.82
0.72
0.79
0.75
0.56
0.77
0.93
0.71
0.75
0.62
0.76
Sediment
N


2.84
4.14
2.14
4.67
21.59
15.16
3.89
0.77
2.33
0.71
3.00
3.57
6.06
Sol. inorg.
P


0.034
0.075
0.091
0.060
0.049
0.043
0.111
0.080
0.093
0.007
0.050
0.094
0.071
Sol. org.
P


0.034
0.038
0.035
0.041
0.030
0.054
0.056
0.080
0.023
0.007
0.025
0.029
0.036
Sediment
P


0.431
1.192
0.452
0.655
3.183
2.226
0.889
0.308
0.767
0.143
1.925
1.175
1.099

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Nutrient Concentrations in Sediment

     The average monthly total N and P concentrations in suspended stream
sediments and nutrient enrichment ratios for the Site 2 subwatershed are
given in Table 6.  The four-year average total N and total P concentra-
tions in suspended sediment were 1.340 and 0.242%, respectively.
Sediment transported during April and June had the highest (> 1.6%) total
N concentrations, whereas sediment discharged in February and August
had the lowest (< 0.7%) total N contents.  Total P concentrations in
sediment did not vary greatly over the course of the year, however,
sediment discharged in November had the highest P content (0.433%)
and sediment transported in January had the lowest (0.167%) concentra-
tion.

Table 6.  Average monthly enrichment ratios and total N and P concentra-
          tions in suspended sediment in drainage water collected at
          Site 2.  (All data calculated from average monthly loadings).
===============;===:==========:=:=========:===:======:===========:=:==£============

                 Nutrients in sediment          Nutrient enrichment ratio
 Month          Total N         Total P        Total Na         Total Pb
 Jan.            1.100           0.167            6.6             2.5
 Feb.            0.659           0.190            3.9             2.8
 Mar.            1.055           0.223            6.3             3.3
 Apr.            1.863           0.261           11,1             3.8
 May             1.500           0.221            9.0             3.3
 June            1.679           0.246           10.0             3.6
 July            0.875           0.200            5.2             2.9
 Aug.            0.500           0.200            3,0             2.9
 Sep.            0.769           0.254            4.6             3.7
 Oct.            1.000           0.200            6.0             2.9
 Nov.            1.333           0.433            8.0             6.4
 Dec.            1.208           0.299            7.2             4.4

 Overall          1.340           0,242            8.0             3.6
 a Average  total N concentration in  drainage area  soils was 1670  ug/g.
 b Average  total P concentration in  drainage area  soils was 680 yg/g.

      The four-year average  total N  and  total P enrichment ratios were
 8.0  and 3.6,  respectively.  Highest total N enrichment was observed  in
 sediment transported in April  and June.  Sediment discharged  in  November
 had  the highest total P enrichment  ratio although the ratio did  not
 vary greatly  over the course of the year.

 Relationships Between Runoff,  Sediment  Loss and NutrientLoss

      Table 7  provides data  on  the degree of relationship between runoff,
 sediment loss, and nutrient losses  from the Site  2 drainage area over
 the  period 1975 to 1978.  Data from both monthly  and quarterly periods
 were used  in  the correlation studies.   Losses of  NH^-N, NOg-N, soluble
                                  192

-------
organic N, and soluble organic P were highly correlated (r  = >.79)
with the total volume of runoff when both quarterly and monthly data
was used (Table 7, Figures 2, 3, 4, 5,).  Soluble inorganic P losses
were correlated (r2 = .78 for monthly data) with total runoff, however,
losses of sediment and sediment-bound nutrients were not correlated
with total runoff.

Table 7.  Relationship between total runoff, sediment loss, and nutrient
          losses from the Site 2 drainage area during 1975-1978.
Variable 1

Total runoff
Total runoff
Total runoff
Total runoff
Total runoff
Total runoff
Total runoff
Total runoff
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment loss
Sediment N loss
Sol. org. N loss
Sediment N loss
Sediment N loss
Sediment P loss
Variable 2

Sediment loss
NH*-N loss
NO^-N loss
Sol. org. N loss
Sediment N loss
Sol. inorg. P loss
Sol. org. P loss
Sediment P loss
NH^-N loss
NCH-N loss
Sol.' org. N loss
Sediment N loss
Sol. inorg. P loss
Sol. org. P loss
Sediment P loss
Total N in sediment
Total P in sediment
Sediment P loss
Sol. org. P loss
NH^-N loss
NO~-N loss
Sol. inorg. P loss
Quarterly
data
- Correlation
0.56
0.89
0.81
0.96
0.44
0.61
0.92
0.49
0.64
0.44
0.50
0.95
0.12
0.67
0.94
0.07
0.00
0.95
0.93
0.52
0.36
0.09
Monthly
data
Coeff., r2 -
0.38
0.79
0.81
0.95
0.31
0.78
0.92
0.33
0.47
0.26
0.31
0.92
0.14
0.38
0.93
0.16
0.00
0.91
0.93
0.37
0.22
0.10
                                                                 •I
     Losses of sediment-bound nutrients were highly correlated (r  = >.92)
with sediment loss (Table 7, Figures 6 and 7).  However, losses of
NHT-N, NOl-N, soluble organic N, soluble inorganic P, and soluble organic
P were not correlated with sediment loss.  Loss of sediment N was highly
correlated (r2 = >.91) with sediment P transport as was soluble organic
                                 193

-------
      1.U5
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9... 2.
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LL
U.
O
i 4-6-

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.0


0 o
0
0
Q
00 °
0 B
°to
On
                8)0
             0        .15      .3       .45

               flMMONJUM  N  LOSS,  KS/Hfl

Figure 2. Relationship between monthly runoff and ammonium
        N losses over the period 1975 to 1978.
                   194

-------
      1.U5.
       9... 2..
 o
 U.
 U.
 O
 Z

 Of
        L9_
4-. 6.
       2.3.
                       O
            ]ff
Figure 3.
     0        1-5     3        4-5

        NJTRflTE N LOSS,  KG/Hfl

 Relationship between monthly runoff and nitrate
 N losses over the period 1975 to 1978.
                   195

-------
         U..5.
    o
    u.
    u.
    o

    ID
    Of
          9... 2..
                    o

                    e
4-6.
o
d
                        o
          2.3.
                    s
               0        -3      .6       .9       1

               SOL.  ORGflNI'D  N LOSS,  KG/Hfl


Figure 4.  Relationship between monthly runoff and soluble
        organic N losses over the period 1975 to 1978.
                   196

-------
   u
   u.
   U.
   O
        1.U5
             T
         a. 2..
6.. 9..
         4.6.
         2.3.
                   O
             r.
             0       .011    .022   .033

             SOL.  ORGflNJC P  LOSS> KG/Hfl
                                       . 044.
Figure 5.  Relationship between monthly runoff and soluble

        organic P losses over the period 1975 to 1978,
                   197

-------
1J000

x 800.
CD
$ 600.
o
_)
h-
£ 400.
Q
bJ
CO
200.
p

o
Q
a °
*.o
GU.B
    0
       0         4.        8         12.
          SEDIMENT  N  LOSS,  KG/Hfl
Figure 6.
 Relationship between monthly sediment losses and
 sediment-bound N losses during  the period 1975
 to 1978.
            198

-------
        1000.
    CE

    N
800.
    CO
    05
    O
600.
    UJ
400.
    a
    UJ
         200.
                     a
            0
               0        -55     1-1     1-65
                 SEDIMENT  P  LOSS,  KG/Hfl
Figure 7.  Relationship between monthly sediment losses
        and sediment-bound P losses during the period
        1975 to 1978.
                 199

-------
N loss with soluble organic P transport.  Ammonium N and NOo-N loss
were not correlated with sediment N loss.   Soluble inorganic and organic
P losses were not correlated with sediment P transport.

     These findings suggest that monthly or annual loadings of NHt-N,
NO~-N, soluble organic N, soluble, inorganic P, and soluble organic P
leaving a watershed can be approximated by multiplying the annual flow
weighted mean concentrations by the volume of runoff during the period.
This procedure predicted the four-year average monthly loadings with
reasonable accuracy.  However, when applied to individual year monthly
data significant deviations from observed values were obtained.  This
approach may prove useful in models of soluble nutrient transport from
watersheds.

     The above findings also indicate that monthly or annual loadings
of sediment-bound N and P leaving a watershed can be estimated by
multiplying the mean total N and P concentrations, respectively, in
sediment by the amount of sediment discharged.  This procedure pre-
dicted the average monthly sediment-bound nutrient discharges with
reasonable accuracy.  However, when used to calculate monthly losses
of sediment-bound nutrients for individual years significant differences
from measured values were obtained.  It is apparent that this approach
will be valid for use in models which predict transport of sediment-
bound nutrients.
                               REFERENCES

 1.  International Reference Group on Great Lakes Pollution from Land
     Use Activities.  1978.  Environmental management strategy for the
     Great Lakes system.  International Joint Commission,  Windsor,
     Ontario.

 2.  Lake, J. and J. Morrison.  1977*  Environmental impact of land use
     on water quality.  Final report on the Black Cteek Project (summary).
     U.S. Environmental Protection Agency, Chicago, IL.  EPA-905/9-78-001.
     p. 3-9.

 3.  American Public Health Association.  1971.   Standard Methods for
     Examination of Water and Wastewater.  13th ed.  Am. Public Health
     Assoc., Washington, B.C.

 4.  U*S. Environmental Protection Agency.  1971.  Methods for Chemical
     Analysis of Water and Wastes.  U.S. Environmental Protection Agency,
     Cincinnati, Ohio.  16020	07/71.

 5.  Steel, R.G.D. and J. H. Tortie.  1960.  Principles and Procedures
     of Statistics.  McGraw-Hill Book Co., Inc., New York.  482 p.

 6.  Nelson, D. W. and D. B. Beasley.  1978.  Quality of Black Creek
     drainage water:  Additional parameters.  In Environmental impact
     of land use on water quality-supplemental comments.  U.S.
     Environmental Protection Agency, Chicago, IL.  EPA-905/9-77-077-D.
     p. 36-83.
                                 200

-------
 7.  Nelson, D. W., E. J. Monke, A. D. Bottcher, and L. E. Sommers.
     1979.  Sediment and nutrient contributions to the Maumee River
     from an agricultural watershed.  In R. C. Loehr (ed.).   Best
     Management Practices for Agriculture and Silviculture.   Ann
     Arbor Science, Ann Arbor, MI.  p. 491-505.

 8.  Logan, T. J. and R. C. Stiefel.  1979.  Maumee River pilot water-
     shed study.  Watershed characteristics and pollutant loadings,
     Defiance Area, Ohio.  U.S. Environmental Protection Agency,
     Chicago, IL.  EPA-905/9-79-005-A.  135 p.

 9.  Ellis, B. G., A. E. Erickson, and A. R. Wolcott.  1978.   Nitrate
     and phosphorus runoff losses from small watersheds in Great Lakes
     Basin.  U.S. Environmental Protection Agency, Athens, GA.
     EPA-600/3-78-028.  84 p.

10.  Langdale, G. W., R. A. Leonard, W. G. Fleming, and W. A. Jackson.
     1979.  Nitrogen and chloride movement in small upland Piedmont
     watersheds.  II. Nitrogen and chloride transport in runoff.
     J. Environ. Qual. 8:57-63.

11.  Alberts, E. E., G. E. Schuman, and R. E. Burnell.   1978.  Seasonal
     runoff losses of nitrogen and phosphorus from Missouri Valley
     loess watersheds.  J. Environ. Qual. 7:203-208.

12.  Menzel, R. G., E. D. Rhoades, A. E.  Olness, and S. J. Smith.   1978.
     Variability of annual nutrient and sediment discharges in runoff
     from Oklahoma cropland and rangeland.  J. Environ. Qual. 7:401-406.

13.  Kilmer, V. J., J. W. Gilliam, J. F.  .utz, R. T.  Joyce and C.  D.
     Eklund.  1974.  Nutrient losses from fertilized grassed  waterways
     in western North Carolina.  J. Environ. Qual. 3:214-219.
                               201

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                      THE VARIETY OF ON-SITE TREATMENT SYSTEM FAILURE

                                               by

                                         A. E. Krause*


                                            OUTLINE


Although there are numerous and very real problems of on-site system failure, its
presumed but unproven presence has been the justification for a wide variety of central-
ized treatment systems,  some of doubtful utility.  New sensing mechanisms and
a variety of on-site studies  have helped to allow a broader and deeper understand-
ing  of this phenomenon.

A. Three Caveats

   1.  The subject involves the limitations of a wide range of systems,
       including privies, cesspools, drywells, septic tanks and fields,
       and even holding tanks.

   2.  It is important to distinguish between individual and collective
       failure impact.  Individual malfunctions can be found in any  large
       group of systems;   They are very different from area-wide health hazards,
       such as contamination of an aquifer.

   3.  A functional failure need not mean the presence  of a condition that the
       homeowner can clearly identify; in area of porous soils  many kinds of
       failure may occur without visible evidence.

B. Variety of Failures

   1. Surface (Clogging Mat) Failures  and Overland Flows.
      There failures are usually associated with clogging mat formation.  They
      may be complicated by tight soils or hydraulic system  overload, including
      external flooding.   They may also be caused or affected by quality of construc-
      tion, suffering  from soil compression or irregular pipe slopes.
      Principal manifestations include surface ponding, system backup,  or
      overland flows to lakes and streams.  Principal impacts include
      lake or stream nutrient enrichment, pathogenic contamination,
      and other public health problems.

   2. Groundwater Failures.
      These are most common  on soils of medium to high porosity, and are
      not usually associated with clogging mat formation.  Since the groundwater
      effluent plume often moves along the surfa3e of the aquifer, its effects
      are greatly complicated  by the direction  and spe
-------
       Manifestations and impacts of groundwater failures include localized lakeshore
       enrichment, algal growth (particularly at point of plume entry)  and situational
       well contamination(where the well may lie in the path of the effluent plume.

   3.  Special situation or Elective Failures
       These include such things as direct tile drainage, straight pipes to streams
       and 'midnight pumpout" of holding tanks— failures by design.  It also includes
       the relatively uncommon contamination of an entire aquifer by excessive on-site
       system loading.  One of the best-known examples of such a failure is found in
       Central Long Island, where high density use of  cesspools and drywells*.
       has . rendered an entice aquifer unusable due to nitrate contamination.

C. Pollutants and Impacts

   1. Nitrogen.
      The various forms of effluent nitrogen are soon converted to the form of nitrates.
      Nitrates are one of the most significant pollutants  in cases of well contamination
      causing methemoglobinemia (blue baby syndrome)  in concentrations over 10 mg/1.
      Nitrates are of great importance for high density  aquifer contamination, as
      on Long Island, and are also of marginal significance to lake and stream enrich-
      ment.  The great bulk of normal effluent nitrogen loading comes from human
      liquid wastes.  There is little or no nitrogen removal in conventional on-site syst

   2. Phosphorus.
      Phosphorus has little or no direct public health impact, but is well known as
      a major factor in lake and stream enrichment.   It can trigger algal growths,
      particularly at the entrance point of a groundwater effluent plume.  Soil
      conditions, particularly alkaline soils high in carbonates, can allow a high
      level of pliG^phorus removal.  Preliminary evidence suggests this may even occur
      under saturated soil conditions.

   3. Pathogens.
      Bacteria and viruses  usually enter bodies of water through overland flow;
      bacterial and viral well contamination is often associated with defective
      well construction and overland flow.  Normally any reasonable amount of
      soil will allow a high degree of adsorbition onto the surface of soil
      particles.

   4. Miscellaneous
      BOD and suspended soilds are almost unimportant in relation to on-site treatment
      except in cases of direct or overland flows.  Suspended solids may of course
      play an important role in causing surface failures.

      Other pollutant roles  remain to be defined; for some lakeshore algae vitamin
      B-12 may play as important a role as phosphorus.  USEPA Region V (in its
      Rural Lakes Generic EIS) has some important studies underway.

D.  Failure Sensing Methods

    1. Interview and Inspection.
       This approach, sometimes quite costly, has been the most common one in the
       past.   The classic rhodamine dye test can be reliab e for detecti   tile field,
       straight pipe and some overland flows.  The door-to-door interview survey is
       relatively cheap, and even when residents are not completely candid, can
       produce a useful profile of water consumption and hydraulic loading.
                                       204

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     2. Aerial Photography.
        Color and color/infrared aerial photography can provide a good, quick, and
        relatively cheap survey of conventional surface failures of septic systems
        and drywells.  The photographs should be taken at a height not exceeding
        6000 feet, at a time of limited tree cover (early spring or late fall),
        about five days  after the last rainfall.  Under these conditions the
        method can be very effective, sometimes even showing the cause of the
        failure.  It will have a relatively limited value where surface-type
        failures are uncommon.

     3. Septic Leachate Detector ("Septic Snooper")
        This device monitors conductance and ultraviolet fluorescence to detect
        the actual entrance point of an effluent plume reaching a stream or lake.
        It uses a wand-type probe and pump to vacuum up water from near-shoreline
        bottoms for continuous analysis by the instrument, which is normally carried
        in a small boat.  The leachate detector is very effective if properly used
        (wind  velocity should  not  exceed 5 miles per hour), and has detected some
        unique situations not accessible through other methods.   It has also
        made possible evaluations and refinements of conventional lake and stream
        models to reflect, actual contributions and loading from on-site treatment
        systems.  This is because, once  the plume entry point is known, spot samples
        can be taken from the lake or (using a portable well point) from the
        groundwater itself.  Miscellaneous uses of the device include quick cheap
        screening of  of drinking water samples for marginal septic effluent
        contaminationB

     4.  Groundwater Flow Meter.
         This device uses small heat pulses to provide a three dimensional readout of
         groundwater flow direction and speed, when lowered into the water table.
         It does this in about three minutes.  In soils with possible rock or other
         inclusions, multiple measurements are needed.

         It is thus possible to have frequent and very site-specific measurements
         of groundwater flow direction.  When used in concert with a leachate detector
         the flow meter allows tracking  of individual effluent plume back to their
         sources.  On old construction it shows the possible direction from which
         well contamination may be coming.  One new construction it allows the
         treatment system to be placed "downstream" from the well; with a filter field
         the long axis can be placed perpendicular to the groundwater flow, minimizing
         effluent concentration at any one point.

E. Results

Using the new sensing approaches it is now possible and cost-effective to determine
which of a group  of on-site treatment  systems may be causing water quality problens,
and if an areawide problem actually exists.  On seven sample rural lake  environmental
impact statements  (copies available on request) it proved possible to cut treatment
costs by an average of two thirds  (over a twenty year period) using on-site treatment
where appropriate.

In responding to identified system failures there are literally dozens of alternatives
available, including: on-site repair, mound systems, cluster systems; field dosing;
water conservation and flow reduction, and greywater/blackwater separation.  In addition
modular combination of these alternative may  useful; this was the case on most of
the seven lake projects and the recent waynesville, Illinois facilities plan  (recently
approved for Step 2+ 3 funding ).

                                          205

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F. Work in Progress
The Environmental Engineering Branch of tiae USEPA Region V Water Division has several
projects now underway  that may help to further understanding of  the problems and
appropriate responses to on-site system failure.  Among these are:

      1. Soil Map Reinterpretation.
         Existing  U.S. Department of Agriculture soil map interpretations are
         being revised.  Instead of the simple four-way hazard system for conventional
         tanks and filter fields, there will be a flexible rating system for a variety
         of on-site treatment approaches, together with an estimate  of the mitigative
         measures needed (with their approximate cost) to overcome the soil limitation,
         This work, which will first be completed for ten northern Indiana counties,
         will allow a much more flexible use of the existing SCS soil surveys.

      2. Water Conservation.
         On several dozen presently failing on-site systems in northern Indiana,
         USEPA has contracted with the State of Indiana and Purdue University to insta]
         advanced water conservation and flow reduction devices (two-quart flush
         toilets, two quart per minute air compressor shower heads, front-loading
         washing machines)  to monitor the exact effect on such devices on effluent
         quality, and to find just how far water conservation  can go in rehabilitat-
         ing failed systems, especially surface failures.

      3. Greywater/Blackwater Separation.
         On other failing Indana system, especially those with groundwater contaminatic
         problems, the same team will install a new kind of greywater/blackwater separ-
         ation.  This uses  an extremely low volume flush toilet  (two quarts to one cuj
         per flush) together with a holding tank for the toilet wastes only.  The syst«
         require pumping at interval of six months to two years and results in at least
         an 80 per cent reduction in nitrate loading to groundwater.

      4.  Generic Rural Lakes Environmental impact Statement.
          This document will use the seven rural lake impact statements, among others,
          to assess wastewater planning techniques and sensing methods to produce
          a cookbook for rural on-site wastewater planning, particularly for rural
          lake areas.

For information on this and other work in progress, as well as copies of  forthcoming
papers, please write U.S. Environmental Protection Agency, Region V, Environmental
Engineering Branch (5WEE), 230 South Dearborn, Chicago, Illinois 60604.
                                           206

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                  MILL CREEK PILOT WATERSHED STUDY ON

                PESTICIDE FATE IN AN ORCHARD ECOSYSTEM:

      DEVELOPMENT AND PRESENTATION OF THE EXPERIMENTAL DATA BASE

                                  by

                      M. J. Zabik, J. J. Jenkins
                                   a                 b
                 R. Kon, L. Geissel  and Erik Goodman

a Pesticide Research Center, Michigan State University, East Lansing,
  Michigan.

b Department of Electrical Engineering and Systems Science, Michigan State
  University, East Lansing, Michigan.
                                      207

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                  INTRODUCTION TO MILL CREEK STUDIES

     A study of Mill Creek, a subwatershed of the Grand River basin was
begun in 1974 as part of the Task C Pilot Watershed Studies of PLUARG.
Mill Creek represents a watershed typical of the large fruit growing region
of southwestern lower Michigan.  Since fruit orchard farming utilizes some
of the most intensive pesticide application rates of any agricultural prac-
tices in the Great Lakes Basin, it seemed particularly appropriate at the
initiation of these studies to emphasize pesticide transport processes.
Studies of nutrient exports were also included but not emphasized.

     The pesticide transport process can be divided into two categories:
(1) pesticide transported in solution, and (2) pesticide adsorbed to par-
ticulate matter and convected along with the sediment load of the stream.
This distinction is necessary if one is to accurately identify the source
of the problem.

     The removal and subsequent transport of agricultural non-point source
pollutants are directly related to the rainfall-runoff process.  Overland
flow is responsible for the initial movement of pollutants from the land
surface to the stream.  Once in the stream, the pollutant may be transpor-
ted considerable distances by the stream flow.  In the particular case of
pesticides the quantity transported is related to the solubility and adsorp-
tive characteristics of the pesticide considered.  The translocation of
pesticides that are adsorbed to or coated on sediment particles depends on
the many variables influencing the capability of a stream to transport sed-
iment, whereas those that are water soluble will be convected in amounts
that are directly proportional to their concentration level and the stream
discharge.

     In view of the above description of the processes responsible for the
transport of pesticides, the major objective of our research effort was to
determine the relative amount of pesticide transported on the suspended
solids and in solution.  As a result of such a determination it would then
be possible to ascertain the magnitude and source of this non-point source
problem.

Description of the Study Area

     The Mill Creek watershed is located in midwestern lower Michigan.  It
includes Cranberry Lake and watershed.  Mill Creek originates from Cran-
berry Lake at the Ottawa-Kent County line and flows southeasterly through
Kent County, joining the Grand River at Comstock Park.   Three major tribu-
taries enter the creek (Figure 1).   Upstream, the land is rolling with
orchards and grain predominating.  Proceeding downstream the creek goes from
agricultural to urban development.   In general the stream may be described
as a cold water, usually clear creek with a drainage system representative
of a midwestern agricultural and urban creek of moderate size and low relief
gradient.

     Initially, sampling of pesticides, sediments, and nutrients were con-
ducted at nine stations established from Cranberry Lake to the creek's
mouth as it enters the Grand River.  Comprehensive analyses of some 57
pesticide parameters allowed the identification of problem pesticides and
then concentration of efforts on the transport processes responsible for
movement of these problem pesticides within and from the creek.  After the
                                    208

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IV)
o
                                        O  Recording Rain Gage


                                        &  Recording Stream Gage
?
                                                     Kilometers
                                            Scale
                                                                          ^
                                                                           V
                                               Figure 1.  Mill Creek Watershed

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initial survey of the entire watershed, studies were concentrated on the
agricultural portion of the watershed upstream of station 5 at M-37 (Fig-
ure 1).  Downstream of M-37, the watershed becomes urbanized with housing
subdivision, light industry, and a golf course — land uses not indicative
of the problem under investigation.

     Land use in the 3058 ha watershed upstream of station 5 (Figure 1) is
almost completely agricultural with about 90% of the area in cultivation
and the other 10% in woodlots or wetlands.  About 50% of the watershed is
in corn, 30% in fruit orchards predominated by apples but with some cherries
and other furits, and the remaining 10% in pasture or alfalfa.

     Almost 90% of the soils are loams or loamy snads (Table 1) of glacial
origin.  In general, the higher elevation soils are almost exclusively
loam with Nester, Marlette, and Capac being the three predominant soil
types.  In the areas adjacent to the streams, the soils are almost all
loamy sands predominately of the Spinks, Brady, Oshtemo, and Chelsea series
interspersed with pockets of muck, sandy loam, fine sandy loam and other
alluvial lands (Table 1). Slopes are generally in the 2 to 12% range with
some ridges in the 12-18% range.

Table 1. Major Soils of the 3058 ha Mill Creek Watershed

Soil                          Area (ha)                 Percent of Total
Loam
Loamy Sand
Muck
Sandy Loam
Alluvial Land
Fine Sandy Loam
Fine Sand
(Lakes)
2,242
489
153
99
30
6
4
35
73.3
16.0
5.0
3.2
1.0
0.2
0.1
1.1
     Locations of major sampling stations are shown in Figure 1.  There
were three subwatersheds sampled with automatic (ISCO) sequential storm-
water samplers so that loadings of major pesticides, sediments, and nutri-
ents could be calculated.  These three stations include  (1) the 889 ha
North Branch water (station 7, Figure 1), (2) the 1146 ha upper Mill Creek
watershed prior to its confluence with North Branch (station 8, Figure 1),
and (3) the entire 3058 ha agricultural portion of Mill Creek upstream of
the urban area (station 5, Figure 1).  Precipitation on the watershed was
monitored with three recording rain gauges  (Figure 1).

     A review of the data from the stream is given in EPA report EPA-905/
9-78-002.  A short summary is given in the  following tables and graphs.
                                  210

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Table 2. Mass Flow of Pesticides from Mill Creek, Michigan, During Three Storm Events
Storm Mean discharge
date (m3/day)
5/06
5/28
6/30
- 5/07/76
- 5/31/76
- 7/02/76
1764
104
65
Adsorbed pesticide
transported (Kg)
DDT DDE Atrazine
0.008
0.001
0.0004
0.005 a
0.025 a
0.00004 a
Dissolved pesticide
transported (Kg) Suspended solids
DDT DDE Atrazine transported (Kg)
0.011
0.003
0.003
0.0008
None
None
0.022
0.047
0.012
10400
1050
600
     a Data not yet available

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         Table 3. Stream Export  of  Materials  by  the  3058  ha Mill Creek Watershed Above M-37
ro
ro


Nitrate-N
Nitrite-N
Ammonia-N
Total Kjeldahl N
Molybdate Reactive P
Total P
Chloride
Calcium
Sodium
Suspended Solids
Weighted
mean (mg/1)
1.765
0.025
0.078
0.782
0.076
0.153
11.778
49.676
5.482
11.590
1975-76
Total load
(kg/yr)
20573 ±
288 ±
912 ±
9116 ±
882 ±
1782 ±
137303 ±
579095 ±
63901 ±
135114 ±
5546
285
1023
2295
298
1018
23509
111673
8939
137425
Unit area
load (kg/
ha/yr)
6.729
0.094
0.298
2.981
0.288
0.583
44.900
189.371
20.896
44.184
Weighted
1976-77
Total load
mean (mg/1) (kg/yr)
3.656
0.010
0.020
1.117
0.181
0.313
19.808
51.314
5.984
47.985
11786 ±
31.24 ±
62.95 ±
3602 ±
582 ±
1008 ±
63863 ±
165439 ±
19293 ±
154709 ±
3496
3.58
27.72
1090
250
331
8334
56926
3644
146989
Unit area
load (kg/
ha/yr)
3.854
0.010
0.021
1.178
0.190
0.330
20.884
54.100
6.309
50.592

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         Table  4.  Stream Export  of Materials  by the  889  ha North Branch Subwatershed of Mill Creek
ro



\
Nitrate-N
Nitrite-N
Ammonia-N
Total Kjeldahl N
Molybdate Reactive P
Total P
Chloride
Calcium
Sodium
Suspended Solids


Weighted
mean (mg/1)
1.191
0.038
0.073
0.696
0.073
0.171
13.585
53.698
6.687
21.490
1975-76

Total load
(kg/yr)
3529 ± 1433
113 ± 137
215 + 229
2063 ± 938
217 ± 99
506 ± 335
40246 ± 13602
159078 ± 42395
19811 ± 5105
63655 ± 23995

Unit area
load (kg/
ha/yr)
3.970
0.127
0.242
2.321
0.244
0.569
45.271
178.940
22.285
71.614


Weighted
mean (mg/1)
0.885
0.010
0.010
0.465
0.050
0.054
30.527
a
a
a
1976-77

Total load
(kg/yr)
568 ± 66
6.38 ± .11
6.61 ± .34
229 ± 52
32.1 ± 12.5
34.5 ± 14.1
19602 ± 1169
a
a
a

Unit area
load (kg/
ha/yr)
0.639
0.007
0.007
0.336
0.036
0.039
22.049
a
a
a
         a  Insufficient data

-------
Table 5.  Stream Export of Materials by the 1146 ha Mill Creek Watershed Above the Confluence with North Branch
Weighted

Nitrate-N
Nitrite-N
Ammonia-N
Total Kjeldahl N
Molybdate reactive P
Total P
Chloride
Calcium
Sodium
Suspended solids
mean
1.
0.
0.
0.
0.
0.
9.
42.
3.
16.
(mg/D
511
013
100
798
063
139
875
438
781
388
1975-76
Total load
(kg/yr)
5200 ±
44.2 ±
344 ±
2745 ±
216 ±
478 ±
33986 ±
146055 ±
13012 ±
56399 ±
2836
40.5
416
731
105
238
4377
25920
1605
35775
Unit
load
area
(kg/
ha/yr)
4.
0.
0.
2.
0.
0.
29.
127.
11.
49.
358
039
300
395
188
417
656
448
354
214
Weighted
1976-77
Total load
mean (mg/1) (kg/yr)
5.607
0.009
0.013
1.175
0.156
0.248
19.265
44.060
3.807
33.803
4061
6.78
9.26
851
113
179
13954
31913
2757
22484
+
+
+
+
+
+
+
+
+
+
2316
1.74
12.10
301
43
109
2969
15662
1256
73338
Unit area
load (kg/
ha/yr)
3.544
0.006
0.008
0.743
0.099
0.156
12.176
27.847
2.406
21.365

-------
ro
en
          Table  6.  Pesticide Exports from the 3058  ha Mill Creek Water,  1975-76 Water Year0

                         	Event  Flows	
                             Rising
                         hydrograph (kg)
                                        Descending           Non-event
Pesticide      hydrograph (kg)        hydrograph (kg)        flows (kg)
Total Exports
    (kg)
  Unit area
loads (kg/ha)
DDT
.DDE
ODD
Aldrin
Dieldrin
Guthion
Atrazine
Simaz'ine

DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrazine
Simazine
0.500 ±
0.361 ±
0.029 ±
0.043 ±
0.083 ±
0.079 ±
1.933 ±
0.174 ±

4.859 ±
5.214 ±
0.474 ±
0.526 ±
0.696 ±
0.451 ±
13.807 ±
3.307 ±
.0002
.0001
.00001
. 00001
.00003
. 00003
.0006
.0001

.002
.003
.0002
.0002
.0003
.0002
.005
.001
15.427 ±
13.228 ±
1.063 ±
1.159 ±
2.669 ±
0.688 ±
39.247 ±
2.898 ±

281.440 ±
196.550 ±
17.420 ±
1.570 ±
17.107 ±
6.612 ±
283.030 ±
50.644 ±
.013
.012
.001
.001
.004
.002
.124
.005

.09
.13
.017
.002
.024
.018
.85
.172
Dissolved
Filtered
13
12
1
1
3



Pesticides
ND
ND
ND
ND
ND
ND
ND
ND
Pesticides
.859 ±
.573 ±
.500 ±
.786 ±
.429 ±
ND
ND
ND
0.00
0.00
0.00
0.00
0.00



300.160
214.340
19.394
3.882
21.232



± 0.09
± 0.13
± 0.017
± 0.002
± 0.024
—
—
—
0
0
0
0
0



.0982
.0701
.0063
.0013
.0069
—
—

         a There was  3.6  times  more  runoff  in  the  1975-76  Water  Year than in the 1976-77 Water Year
         b ND indicates no  data

-------
        Table  7.  Pesticide Exports from the 3058 ha Mill Creek Watershed, 1976-77 Water Year'
PO
CT>
Pesticide
DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrazine
Simazine
DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrazine
Simazine
•

Rising
hydrograph (kg)
1.852 ±
2.284 ±
0.097 ±
0.113 ±
0.244 ±
0.007 ±
0.791 ±
0.036 ±
24.136 ±
33.261 ±
1.015 ±
0.945 ±
1.912 ±
0.151 ±
7.152 ±
0.706 ±
.001
.002
.0001
.0001
.0001
.000004
.001
.00002
.020
.028
.001
.001
.001
.0001
.005
.001
"


Decending
hydrograph (kg)
3.430
3.411
0.178
0.156
0.279
0.026
1.230
0.052
58.413
55.811
2.888
1.583
4.418
0.697
10.433
0.752
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
+
.036
.074
.006
.005
.014
.00002
.095
.004
0.647
1.261
0.102
0.067
0.235
0.447
0.675
0.061
Non-event
flows (kg)
0.433
0.303
0.026
0.129
0.047
0.031
0.563
0.144
3.001
2.732
0.209
0.182
0.377
0.510
5.537
1.486
± 7 . 104
± 1.245
± 0.000
± 0.553
± 0.276
± 0.032
± 12.865
± 4.140
± 5.201
± 10.424
± 1.674
± 1.239
± 2.841
± 2.600
± 42.580
± 22.590
Total Exports
(kg)
5.715 ±
5.998 ±
0.301 ±
0.398 ±
0.570 ±
0.064 ±
2.584 ±
0.232 ±
85.550 ±
91.804 ±
4.112 ±
2.710 ±
6.707 ±
1.358 ±
23.122 ±
2.944 ±
7.104
1.247
0.006
0.553
0.276
0.232
12.865
4.140
5.241
10.580
1.677
1.241
2.851
2.638
42.585
22.590
Unit area
loads (kg/ha)
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
.00187
.00196
.00010
.00013
.00019
.00002
. 00084
. 00008
.0280
.0300
.0013
.0009
.0022
.0004
.0076
.0010
         a  There  was  3.6 times more runoff in the 1975-76 Water Year than in the 1976-77 Water Year.

-------
Table 8. Flow Weighted Mean Concentrations  (yg/£) of Pesticides  Exported
         from the 3058 ha Mill Creek Watershed
                        Pesticide
             	Event Flows	
               Rising     Descending
             hydrograph   hydrograph
                       Non-Event
                         flows
                                       1975-76 Water Year
                                                         a
Dissolved pesticides
Filtered pesticides
Dissolved pesticides
Filtered pesticides
DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrizine
Simazine

DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrizine
Simazine
DDT
DDE
ODD
Aldrin
Dieldrin
Guthion
Atrizine
Simazine

DDT
DDE
DDD
Aldrin
Dieldrin
Guthion
Atrizine
Simazine
0.531
0.366
0.052
0.094
0.097
0.112
2.245
0.201
5.
5,
  .192
  ,341
 0.799
 0.738
 0.884
 0.535
16.327
 3.828
 4.166
 3.572
 0.287
 0.313
 0.721
 0.186
10.598
 0.782

75.998
53.075
 4.704
 0.424
 4.619
 1.785
76.428
13.676
                                       1976-77 Water Year3
1.201
1.280
0.045
0.093
0.122
0.014
1.198
0.071

1.323
1.232
0.070
0.083
0.113
0.020
0.753
0.027
             13.727
             15.885
              0.640
              0.501
              1.063
              0.351
              6.862
              0.725

             19.831
             18.769
              1.053
              0.585
              1.559
              0.498
              5.624
              0.408
 ND"
 ND
 ND
 ND
 ND
 ND
 ND
 ND

1.940
1.760
0.210
0.250
0.480
 ND
 ND
 ND
             0.170
             0.119
             0.010
             0.050
             0.018
             0.012
             0.221
             0.056

             1.176
             1.071
             0.082
             0.072
             0.148
             0.200
             2.170
             0.582
     a There was 3.6 times more runoff in the 1975-76 Water Year than in
       the 1976-77 Water Year

     b ND indicates no data
                                 217

-------
0)
bO

cfl

U <~s
co T3
•H C
P O

>• $1000-
rH CO
J3 •».
4-J CO
0 H
O 0)
    500-
           J
                   I
           0    N
                      D
                M
                      M
co
CO
O
4-1 /-s
C CO
0) (-
e o
•H H

0) O
W -H
  k
13 4-1
cu m

ci ^^^
cu
&,
CO
     300"
     250 -
     200-
     150-
     100-
      50-
                                                       Suspended sediment  loss
                                                       for  October, 1975 to
                                                       September, 1976
                                                       663  metric tons
                                                    1
            0
                 N
D
J
M
M
A
          Figure 2.  Discharge and Suspended  Sediment Loss  from
                  the Mill  Creek, Michigan, Watershed
                                   218

-------
4J


§
o
o
o
•H
d
3
O
o
•H
       o
       o
       o
       o
       o
       o
       o
       oo
       o
       o
o
CN1
o
o
       o
       OO
       o
       o
      o
      o
      o
      o
           ,:    J   , - ___  J        1         j.  _     p_




        28.00   32.00    36.00    40.00   44.00   48.00




                      Particle Diameter (Microns)
                                                     52.00
56.00   60.00
       10.00   15.00    20.00    25.00   30.00    35.00   40.00



                      Particle Diameter (Microns)
                                                             45.00   50.00
 Figure 3.   Particle size distribution of particles less than 100 microns in

            size transported during low flow periods on October 28, 1976 (flow

            = 110  /sec,  upper figure) and on November 28, 1976 (flow = 189

            /sec, lower figure).   These size distributions were determined with

            a Coulter Counter, Model A.
                                 219

-------
     The work presented in this portion is an effort to characterize the
dynamics and effects of an example compound in the terrestrial environ-
ment, utilizing field and laboratory measurements and the methodology of
systems modeling and simulation.  Data collection, model refinement, and
revised experimental design were done in an iterative fashion, yielding
a model which is parameterizable and data which are relevant to the pro-
blem being attacked.  Reported here is the field experimental program used
to parameterize the model which describes the distribution, attenuation
and movement of the organophosphate insecticide azinphosmethyl, 0,0-di-
methyl-S-(4-oxo-l5 2, 3 benzotriazin-3(4H)-ylmethyl) phosphorodithioate
(Guthion ).  While the laboratory and field work concentrated on the par-
ticular pesticide chosen, the techniques for studying and modeling it are
applicable to a broad range of compounds.  The compound is followed (in
the model and in the field) from its spray application through the orchard
soil/vegetation/litter environment and into aquatic systems.  A further
goal is to identify and model its impacts on non-target organisms in a
terrestrial ecosystem.

     To develop a methodology for modeling the ecosystem effects of
alternative pesticides, a deciduous orchard ecosystem, among the most com-
plex of agroecosystems, was chosen as a challenging example.  In part due
to their perennial nature, orchard ecosystems are more similar to natural
ecosystems than are many other agroecosystems.  Annual and semiannual crops
are more transient in their behavior, a product of periodic radical changes
in their environment due to cultural practices.  In addition, the economic
pressure to produce flawless fruit forces orchard growers to be among the
heaviest users of pesticides in American agriculture.  Ecosystems complex-
tiy, coupled with high pesticide use, makes the orchard ecosystem a good
indicator of possible ecological dangers.  Additional hazards may be seen
in sloping orchards where pesticides may be carried by runoff, as well as
wind, to other terrestrial and aquatic environments, increasing the chances
of potentially harmful pollution.

     The organophosphate insecticide azinphosmethyl was chosen as the
example pesticide to be introduced into the orchard, as it is one of the
most widely used and potentially toxic compounds used in orchards today.

     To develop, parameterize and tesJL a model of the fate and impact of
an alternative pesticide in an orchard ecosystem, four broad classes of
information were desired:

     1.  How is the pesticide initially distributed in the ecosystem;
         what is its availability to the ecosystem population?

     2.  How is the pesticide redistributed; what forces affect this
         distribution?

     3.  How is the pesticide attenuated by its environment (microbial,
         chemical, photochemical degradation, volatilization, organism
         uptake)?

     4.  What is the relationship between the pesticide's attenuation and
         distribution and its effects on organisms?

     It is obvious that the first three questions must be answered before
the last; the model must represent the distribution, movement and attenuation
                                  220

-------
of azinphosmethyl prior to its simulation of organism effects.  The data
base required for such a model is quite extensive.  It amounts to a mass-
balance of azinphosmethyl in the orchard (and leaving the orchard) with
time.  Available data from the literature merely gave initial direction
to the field studies, as a consistent basis for formulating conclusions
that could not be found among the various data reported.

     Residue levels of azinphosmethyl with time on various plant surfaces,
in the soil, and in the aquatic environment, were reported by the Chemagro
Division Research Staff (1974).  Liang and Lichtenstein (1972) examined
the effects of light, temperature, and pH on the degradation of azin-
phosmethyl in water and on glass surfaces.  In a later paper, (1976) they
looked at photbdecomposition of -^C azinphosmethyl in soils and on leaf
surfaces.  Schulz et al. (1970) looked at the persistence and degradation
of azinphosmethyl in soils as affected by formulation and mode of appli-
cation.  Yaron et al. (1974a) followed azinphosmethyl persistence and
movement within the soil profile under irrigated field conditions.  Iwata
et al. (1975) looked at the behavior of azinphosmethyl is dust derived
from several soil types.  Heuer et al. (1974) studied the kinetics of
azinphosmethyl degradation in aqueous solutions and on glass beads as
affected by pH and temperature.  Yaron (1974b) examined azinphosmethyl
kinetics in the soil environment.  Kuhr et al. (1974) examined the dissi-
pation of azinphosmethyl from apple orchard soil when applied as a part of
a routine spray program.  Wieneke and Steffens (1974) compared the degra-
dation of l^C azinphosmethyl on glass paltes to the metabolism on bean
leaves, and later studies (Steffens and Wieneke, 1975, 1976) further
examined plant uptake and metabolism.  Hall et al. (1975) and Hansen et al.
(1978) followed the degradation of dislogeable azinphosmethyl residues on
apple foilage.  McMechan et al. (1972) measured the amount of azinphos-
methyl erosion from apple leaves by rain and overtree irrigation.  Thompson
and Brooks  (1976) looked at dislodgeable residues of azinphosmethyl and 4
other insecticides on citrus leaves and fruit during wet and dry weather
in Florida.  Gunther et al. (1977) discussed the dynamics of both penetrated
and dislodgeable foliar residues on citrus, orchard soil dust residues, and
airborne residues,  fiach of these papers supplies information on the
dynamics of azinphosmethyl in one segment of the environment, be it soil,
water, leaf surfaces, etc.  To understand ecosystem effects, these pro-
cesses must be considered part of the whole ecosystem and azinphosmethyl
dynamics must be considered for every part at any point in time.

     To overcome the gaps and inconsistencies in the literature, an
abandoned apple orchard in the Mill Creek Watershed was converted into an
experimental unit to gather data on the environmental dynamics of azinphos-
methyl under a regime of periodic sprays.  The orchard sampling was based
on this whole-ecosystem principle using the literature as a source of
expected values to determine initial sampling procedures.
                                  221

-------
     The environmental behavior of pesticides was studied to develop a
methodology for modeling ecosystems effects of alternative pesticides.
Studies were carried out in an apple orchard watershed to gather data on
both initial distribution of azinphosmethyl within the orchard and vertical
movement of the pesticide under the influence of rainfall, as well as the
attenuation of the pesticide in various situations.   The orchard was sub-
divided into distinct plots.  Each was further subdivided both vertically
and horizontally in order to adequately represent the variations which
affect the behavior and impact of the pesticide in the orchard ecosystem.
Plots were designed such that each was a distinct watershed, allowing run-
off collection from them individually.  In addition, losses of azinphos-
methyl to the atmosphere were examined, both during application and on
subsequent days.  In 1976 64.9% and in 1977 53.6% of the azinphosmethyl
applied was initially distributed among the various orchard strata.  Exam-
ination of residues reaching each stratum showed the majority of the dis-
lodgeable residues are distributed to the trees and grass.  Litter and soil
residue levels are roughly 10 times lower than tree leaf residues.  Runoff
studies indicate a small contribution to the loss of azinphosmethyl from
the orchard via this route.  Analysis of residue data throughout the season
indicates vertical pesticide movement among strata under both rainfall and
no-rainfall conditions.  Airborne residues collected at the downwind edge
during spraying were roughly uniform to 6 meters and averaged 55.6 ± 6.9
yg/m3.  Levels measured 6 days after application averaged .27 ± .10 yg/m .
The data presented here were used to parameterize a model for pesticide
fate in a orchard ecosystem presented in Goodman et al. (1979).  A model
for organism effects parameterized using data from a companion study, con-
ducted concurrently within the same orchard, is also described in Goodman,
et al. (1979).
                                  222

-------
     The results show that pesticides (chlorinated hydrocarbon pesticides
in particular) are still a significant non-point source of contamination
to Michigan rivers and consequently the bordering Great Lakes.  The con-
centrations found are at the part per billion and trillion level but still
are significant in terms of their effect on aquatic organisms due to bio-
magnification.  The results of Mill Creek are supported by the fact that
pesticides such as DDT and Dieldrin are found in Great Lake fish and are
responsible for the ban on commercial fishing for Coho salmon, etc.

     There does not appear to be any reasonable mechanism for the elimina-
tion of these pesticides from the river and streams short of what has
already been implemented (ban on the use of chlorinated hydrocarbon pesti-
cides) .  Prevention of sheet soil errosion would certainly be a measure
that would reduce the amount of pesticides entering the Great Lakes but
would certainly not stop the introduction of all pesticides due to evapor-
ation, drift and other transport processes.
                                223

-------
               LIVESTOCK INPUTS AND EFFECTS
                            BY
                       FRED MADISON*

LIVESTOCK POLLUTION LOADS GOING INTO THE GREAT LAKES BECAME A
MAJOR CONCERN OF CANADA AND THE UNITED STATES, THUS FROM THE
INTERNATIONAL JOINT COMMISSION THROUGH PLUARG, PROGRAMS
WERE SET UP TO INITIATE STUDIES TO ESTIMATE POLLUTION LOADS
TO THE GREAT LAKES,

THE STUDIES COVERED THREE MAJOR SOURCE AREAS:

      _AND APPLICATION SYSTEMS
      BARNYARD FEEDLOT AREAS
      hlASTE STORAGE AREAS

AN EXTENSIVE LITERATURE SEARCH WAS UNDERTAKEN,  THUS WE
CONCLUDED PHOSPHORUS LOADINGS TO THE GREAT LAKES:

   1, 5% OF THE PHOSPHORUS WAS TREATED ANNUALLY,
   2, 10% SPREAD ON FROZEN GROUND FOR RUNOFF TO STREAMS,
   3, 2% FROM EXCRETED SOURCES OF SOLIDS AND SEMISOLIDS,

DATA SET IN A SIMPLIFIED MODEL AND THESE CONCLUSIONS WERE
DRAWN:

   1, 1 TO 2,5% OF ALL MANURE PHOSPHORUS WAS DELIVERED TO
      THE LAKES,
   2, 75% OF MANURE PHOSPHORUS FROM BARNYARDS WAS DELIVERED
      TQ_STREAMS,
    ,  2
3, 25% WAS FROM MANURE LAND APPLICATION SOURCES,
LOAD ESTIMATES FROM LAND MANAGEMENT PRACTICES APPLIED ON
CROPLAND REVEALED:

   1, 6 TO 15% REDUCTION IN PHO'SPHORUS LOADINGS,
   2, A 10% REDUCTION IN TOTAL PHOSPHORUS IN THE WATERSHED,

ANIMAL WASTE SOURCES ARE REDUCED:
   J
 ,  27 TO 36% REDUCTION IN ANIMAL WASTE PHOSPHORUS,
 ,  TOTAL WATERSHED PHOSPHORUS WAS REDUCED 9-13%,
*DR, FRED MADISON/ DIRECTOR, WASHINGTON COUNTY NONPOINT SOURCE
POLLUTION PROJECT,  UNIVERSITY OF WISCONSIN SPEECH TAKEN FROM
A RECORDING AND INTERPRETED BY CARL D, WlLSON,
                           225

-------
                           2

COSTS FOR CROPLAND TREATMENT:

   1, 30,000 DOLLARS TOTAL COST FOR CROPLAND TREATMENT,

ANIMAL WASTE STORAGE FACILITIES ARE EXPENSIVE:

   1, $15,000 TO $20,000 PER UNIT AND CAN RANGE TO $65,000,

ANIMAL WASTE SYSTEMS:

   1, STORAGE AND APPLY TO LAND GOOD POLLUTION REDUCTION,
   2, WATER QUALITY CONSTRAINTS THAT REQUIRE STORAGE is
      THE EXCEPTION NOT THE RULE IN WISCONSIN,
   3, RURAL LIVESTOCK SYSTEM WITH WATER DIVERSIONS CAN BE
      INSTALLED CHEAP $1500 TO $4000 FOUR YEARS AGO,

QUESTION?

   1, ARE WE LOOKING AT THE WRONG PART OF THE PROBLEM?

OTHER STUDIES WERE SET UP IN WISCONSIN ON six BARNYARD SITES,
THE SIZE OF THESE AREAS RANGED FROM 3 TO 5 ACRES,

   1, DATA REVEALED LIVESTOCK is A SIGNIFICANT SOURCE OF
      NUTRIENTS (POLLUTION LOADINGS),
          ER APPLICATION OF MANURE:
          DEDUCES RUNOFF,
          DEDUCES NUTRIENT LOSSES,
          1FFECT IS SPRING AND ALL THROUGH THE YEAR,

WHITE CLAY LAKE WATERSHED PROJECT SET UP IN WISCONSIN IN 1976,
FIRST UPLAND TREATED WATERSHED PROGRAM,  THE PROJECT WAS
FUNDED BY THE CLEAN LAKES PROGRAM SECTION 314 FROM THE
ENVIRONMENTAL PROTECTION AGENCY,

TWO MODELS DEVELOPED:

   1, ANIMAL WASTE MODEL,
   2, CROPLAND WASTE LOAD MODEL,

CONCLUDED:

   1,  66% OF THE TOTAL PHOSPHORUS GETTING INTO THE LAKE CAME
       FROM CROPLAND,
   2,  34% OF THE TOTAL PHOSPHORUS GETTING INTO THE LAKE CAME
       FROM ANIMAL WASTE,
                             226

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         UPSTREAM POINT SOURCE PHOSPHORUS INPUTS AND EFFECTS

                                  by

                           David B. Baker*
     One of the goals of water quality management is to obtain the great-
est possible improvement in water quality and general environmental
quality per dollar invested in pollution abatement programs.  Although
most water quality management plans include an economic analysis of
alternative solutions to some particular problem, very often the exam-
ination of alternatives operates within a very narrow segment of the
overall interacting set of causes and effects determining water quality.
For example, a facility plan might include the selection of the most cost
effective method of reducing the phosphorus concentrations in an effluent
from 3 mg/1 to 1 mg/1.  If this reduction has no effect on water quality
or if comparable expenditures on nonpoint controls or flow augmentation
would have greater water quality benefits, then the examination of alter-
natives has operated within too narrow a framework of options.  Certainly
the objectives of this symposium and the concepts incorporated into the
Watershed Model reflect the need to broaden the perspectives within which
alternatives can be evaluated.

     Although the concept of integrated point/nonpoint control programs
is clear, the development and implementation of such programs is difficult
because adequate data and necessary understanding is generally not avail-
able.  In planning an integrated control program in the Great Lakes, the
relationships outlined in the model illustrated in Figure 1 should be
understood.  The quality, quantity, timing and variability of inputs from
both point and nonpoint sources into each area of the aquatic system
should be known.  Knowledge of the physical, chemical or biological pro-
cessing of inputs within each area is important.  This processing both
affects and is affected by the water quality in the area.  The processing
also affects the movement of materials into either temporary or permanent
storage within the system and the output of materials to the next area
downstream.  As the number of steps between a particular input and a water
quality effect increases the more tenuous the cause and effect relation-
ships become.  This is certainly the case for the relationships between
point source phosphorus inputs to stream systems and open lake water
quality in Lake Erie.

     Because of the complexities of the interacting systems illustrated
in Figure 1, current efforts at integrated point/nonpoint control programs
involve the use of a number of simplifying assumptions.   Although the use
of such assumptions does allow the development of integrated control pro-
grams, their use may undercut the effectiveness of the programs and pre-
vent the realization of control economies that, given more information and
better understanding, could be achieved.

     The management of phosphorus within the Lake Erie Basin is one area
in which opportunities for integrated point/nonpoint source management
exist.  Some of the major assumptions upon which such programs are based

*Director, Water Quality Laboratory,  Heidelberg College,  Tiffin,  Ohio.
                                 227

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          Stream
         Networks
                    Estuaries
                    Lake Erie
                    Nearshore
                    Lake Erie
                    Open Lake
PS
  \
     inputs
NFS
outputs
outputs
                                       PS
outputs
                                       PS
outputs
         Processing

             I
          Storage

Figure 1.  Areas requiring data and understanding to support the development of effective and economical
           integrated point source/nonpoint source control programs in the Lake Erie Basin.  Abbreviations:
           PS, point sources; NPS, nonpoint sources; W.Q., water quality.
                                                                                                 oo
                                                                                                 OJ
                                                                                                 OJ

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 include:

     1.  Upstream  (indirect) point source phosphorus inputs
         are assumed to have 100% delivery through the river
         to the lake unless large lakes or reservoirs are
         situated on the river system.

     2.  The bioavailability of upstream point source phosphorus
         is assumed to remain constant during transport to the
         lake.

     3.  Reductions in sediment and particulate phosphorus
         yields at river mouths are assumed to be proportional
         to the reduction in gross erosion achieved by the
         application of best management practices in the water-
         shed.

     4.  No systematic differences in the processing of point
         source and nonpoint source-derived phosphorus within
         the estuaries and near shore zones of the lake are
         assumed to occur even though the mode of delivery of
         phosphorus derived from the two sources is very different.

     In this paper some of the assumptions regarding the effects of up-
 stream point source phosphorus inputs will be examined using data avail-
 able in the Sandusky River Basin.  The data indicates that most of the
 phosphorus entering the river from upstream point sources becomes tied
 up within the river bottom sediments.  Its eventual delivery to the lake
 is in the form of particulate rather than soluble phosphorus.  The
 delivery ratio of this phosphorus to the lake is probably less than 100%.
 Evidence of ambient stream water quality problems associated with point
 source phosphorus loading is lacking.  The nonpoint source phosphorus
 loading component is so large and variable that the effects of further
 point source control programs in reducing phosphorus output from the
 basin could not be directly measured.  The transfer of funds from por-
 tions of phosphorus removal programs at upstream municipalities to alternate
 uses such as flow augmentation or nonpoint controls should be examined.

 Upstream Point Source Phosphorus Inputs in the Sandusky Basin

     There are seven municipal sewage treatment plants located in the
 Sandusky River Basin upstream from the Tindall Bridge gaging station
 near Fremont,  Ohio.  These plants are identified in Table 1 and their
 flows,  effluent phosphorus concentrations, loading rates and annual loads
 are listed.  Three of the plants have flows greater than 1 MGD and con-
 sequently are required to meet a 1 mg/1 phosphorus effluent standard.
 Of these three plants, Bucyrus has no phosphorus removal program; Upper
 Sandusky has a partial phosphorus removal program and Tiffin has a
 removal program which meets current requirements.  No phosphorus removal
programs are in effect at the other sewage treatment plants.   The
 locations of these plants are shown in Figure 2 which also includes the
 locations of the nutrient and sediment transport stations in the Sandusky
Basin.

     The combined effluents of these plants load phosphorus into the
 river system at an average rate of 5.3 kg/hr.   The annual loading from
                                  229

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Figure 2.  Location of Municipal Sewage Treatment Plants and Sediment and
           Nutrient Transport Stations in the Sandusky River Basin
        Municipal Sewage
        Treatment Plants

            Over 1 MGD

            0.1 to 1 MGD
        Transport
        Stations
                                       SL.	
                                                    SANDUSKY RIVER BASIN
                                                        Scale in Miles
                                                       i   i  i   i •  *  •
                                                       024   6   8  10
                                    230

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the plants is about 45 metric tons per year.   The mean annual export of
total phosphorus at the Fremont gaging station is 355 metric tons per
year (Baker, 1980).  Assuming that all of the upstream municipally derived
phosphorus is exported from the basin, point sources account for 13 percent
of the total load and nonpoint sources 87 percent.
Table I.  Indirect Municipal Point Source Phosphorus Discharges in the
Location
10
Crestline
Bucyrus
Upper Sandusky
Gary
Attica
Bloomville
Tiffin
Total
Flow
M /day (MGD)
2.1 (.55)
7.7 (1.9)
6.4 (1.7)
2.3 (.6)
.87 (.23)
1.1 (.28)
13. (3.5)
33 (8.8)
Total Phos.
mg/1
6a
8.0
2.5
6a
6a
4a
0.9

Loading
Rate
Kg/hr.
.52
2.6
.67
.57
.22
.18
.49
5.3
Annual Load
M Ton/yr.
4.6
22
5.8
5.0
1.9
1.6
4.3
45
     a Estimated.
       EPA, 1979.
Data from IJC 1979; De Pinto, et al, 1980, and Ohio
Instream Deposition of Phosphorus from Municipal Point Sources

     The extent of deposition of municipally derived phosphorus in the
Sandusky Basin can be studied through an analysis of both flux patterns
and concentration patterns.  Since the transport stations in the Sandusky
Basin have been operated on a continuous basis for periods from 3 to 5
years, extensive data is available on phosphorus transport rates during
both low and high flows.  These data can be arranged in the form of flux
exceedency tables.  A summary of the phosphorus flux exceedency table for
the Fremont gaging station is shown in Table 2.

     The data in Table 2 are based on the analysis of 2,304 samples
collected between December 26, 1973 and November 30, 1979.  These samples
were used to characterize the stream transport for a total period of
32,635 hours  (3.73 years) with individual sample characterizing transport
for periods ranging from 3 to 24 hours.  During this time a total of
2,097 metric tons of total phosphorus and 393 metric tons of soluble
reactive phosphorus were exported past the station.  A computer program
is used to rank all of the samples on the basis of instantaneous flux
from the lowest to the highest value.  The program lists the individual
flux, the percent of the total period of time the fluxes were equal to
or less than the listed value and the percent of the total flux accounted
for by the listed value and all smaller flux rates.  For example, 70%
of the time the flux rate of total phosphorus was 16.5 kg/hr. or less
and during that time 4.0% of the total observed total phosphorus flux
had been exported.

     The weighted average stream flow during the period of observation
was 39 m /sec.  This compares with a long term average discharge at the
                                    231

-------
Fremont station of 27 m /sec.  Thus the data set is biased toward high
flows.
Table 2. Characteristics
Basin,
Time Weighted
Percentile
( instantaneous
Flux)
10
20
30
40
50
60
70
80
90
95
98
100
Tindall
Total

of Phosphorus Export from the Sandusky River
Bridge j_ Fremont, Ohio^ 1974-1979
Phosphorus Soluble Reactive

Flux Rate Cum. % of
Kg/hr.
.74
1.33
2.08
3.06
4.32
7.03
16.5
41.3
137
339
776
2610
Annual Load
.08
.24
.50
.89
1.5
2.3
4.0
8.2
20.
37
61
100

Flux Rate
Kg/hr.
.16
.37
.70
1.13
1.89
3.06
5.44
11.7
33.6
61.2
112
587
Phosphorus

Cum. % of
Annual Load
.07
.27
.70
1.4
2.6
4.6
7.9
14.
32
49
69
100
     From Table 2 it is apparent that the combined export of phosphorus
from all sources is less than the point source inputs for more than 50%
of the time.  Fifty percent of the time the flux rate of total phosphorus
at the Fremont station was less than 4.32 kg/hr.

     It should also be noted that when the flux rate is 4.32 kg/hr. only
about one third of that phosphorus could have come from point source inputs.
Since the flux increases with stream discharge, the median flux should
correspond to the median stream discharge.  At the Fremont stream gage
the median discharge rate is 563 X 103 M /day.  The combined flow of the
upstream municipal sewage treatment plants is 33 X 10  M /day.  Therefore,
530 X 10  M /day or 94% of the median stream flow, is derived from various
components of the basin hydrological cycle.  In Sandusky subbasins lacking
point source phosphorus inputs ((Tymochtee Creek, Broken Sword and Wolf,
East), the average phosphorus concentration at the median flow is 0.13 to
0.14 mg/1.  Assuming that these are the background concentration char-
acteristics of the Sandusky Basin at median stream flows, the background
phosphorus flux at the Fremont gage would be 2.9 kg/hr.  Consequently,
of the 4.3 kg/hr. median flux, only 1.4 kg/hr. could be derived from point
source inputs.  This is about 25% of the point source input rate of
5.3 kg/hr.  These calculations are summarized in Table 3.

     The data presented in Table 2 also show that only 1.5% of the total
observed load had been exported by the cumulative fluxes lower than the
median flux.  Applying this figure to the average annual export of
phosphorus at the Fremont gage, suggests that only 5.3 metric tons of
phosphorus would have been exported during the 50% of the time with the
lowest fluxes.  Since the loading rate from municipal sources is rather
constant, one half of the annual point source inputs of phosphorus
                                232

-------
 (22.5 metric tons) would have entered the river  during this  time.   Thus
during this time the combined point and nonpoint phosphorus  export is
only 24% of the point source phosphorus inputs.  Since much  of the
phosphorus export during this time is derived  from nonpoint  sources,  it
is evident that the bulk of the point source phosphorus inputs is  being
incorporated into the stream sediments.

Table 3.  Components of the Median Phosphorus  Flux at  Tindall  Bridge  in
          Fremont
Median Stream Discharge

Combined STP Discharges

Background Stream Flow

Background Phosphorus Cone.
Background Phosphorus Flux
Median Phosphorus Flux
Point Source Component of Flux
Point Source Input Rate
563 x 103 M3/day

-33 x 103 M3/day

530 x 103 M3/day

0.133 rag/1
2.9   Kg/hr.
4.3   Kg/hr.
1.4   Kg/hr.
5.3   Kg/hr.
     The occurrence of instream deposition of phosphorus  from municipal
point sources is also apparent from studies of  the patterns  of phosphorus
concentration along the river.  During the summer of  1974, from 32  to 52
samples were collected during nonstorm conditions at  each of twenty six
stations along the mainstream of the Sandusky River.   The mean concentrations
of total and soluble reactive phosphorus are shown as a function of mile
point (distance from the river mouth) in Figure 3.  The effects of  inputs
from the Bucyrus, Upper Sandusky and Tiffin sewage treatment plants are
evident.  None of the plants had phosphorus removal programs in operation
at that time.  The decreases in phosphorus concentration  below each town
reflect deposition  of phosphorus rather than dilution effects.   These data
have been presented and discussed in the Proceedings  of the  Sandusky River
Basin Symposium (Baker and Kramer, 1975).

Figure 3.  Profiles of
mean concentrations of
phosphorus along the
river system during
June through September,
1974.  Mileages shown
are the distances from
the mouth of the river.
The three peaks in
phosphorus concentration
are caused by the
effluents of the Bucyrus,
Upper Sandusky and Tiffin
sewage treatment plants.

                             .so
                             I.H .
                             1.00.
        * TOTAL PHOSPHORUS


        • MTHO PHOSPHORUS
                                 120
                                          100
                                                   10       60
                                                       RIVER MILES
                                                                    40
                                                                             20
                                 233

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Export of Upstream Point Source Phosphorus Inputs

     Transmission Coefficients;  Although it is evident from the above
discussion that much of the upstream point source phosphorus input is
incorporated into the river sediments, it is generally assumed that this
phosphorus is resuspended during high flow periods and subsequently trans-
ported as available phosphorus to Lake Erie (Sonzogni, et al, 1980).
Considerable evidence has been accumulated which documents the signifi-
cance of deposition-resuspension phenomena in the transport of both
sediments and phosphorus through river systems (Verhoff, et al, 1978;
U.S. Army Corps of Engineers, 1979).  Although mass balances for in-
dividual storms moving through the Sandusky Basin have been conducted
(Melfi & Verhoff, 1979) the results do not provide information on the
transmission coefficient of point source-derived phosphorus through the
stream system on an annual basis.

     One approach to determining the transmission coefficient from up-
stream point source inputs would be to achieve a known reduction in
phosphorus inputs from these sources and compare this with an accompanying
reduction in total river export of phosphorus.  This approach does not
work well where point source inputs are small relative to nonpoint inputs
and where nonpoint inputs are extremely variable from year to year.  Prom
a study in 1972  (Baker and Kramer, 1973) the mean annual export of total
phosphorus from the Sandusky Basin was estimated to be 445 metric tons.
This estimate was based on a weighted mean concentration from 160 samples
collected during both high and low flows and the mean annual flow for the
period of record.  Since that time, phosphorus removal programs have re-
sulted in a decrease in phosphorus loading from point sources of about 40
metric tons per year.  During the period from 1975 to 1979, the annual
phosphorus export averaged 420 metric tons per year and ranged from 257.5
to 563.4 metric tons  (Table 4).  The average deviation from the mean during
this time was 74 metric tons.  Should Bucyrus and Upper Sandusky meet the
1 mg/1 effluent standard, an additional reduction in phosphorus inputs from
point sources of 23 metric tons per year would be achieved.  The total
reduction program of 63 metric tons per year would still be less than the
average deviation in annual loading observed during the past 5 years.  Thus
determining transmission coefficients of point source phosphorus by com-
paring known reductions of phosphorus inputs with observed reductions in
phosphorus outputs is not feasible within the Sandusky Basin.

     A second approach to determining transmission coefficients is  to
evaluate phosphorus/sediment  ratios  in basins with and without point
sources.  If all of the point source-derived phosphorus is  delivered
through the stream  system, then  subtracting the point  source phosphorus
inputs from the  total phosphorus output  should give nonpoint phosphorus/
sediment ratios  characteristic of  strictly  agricultural watersheds.   This
assumes that all of the observed sediment transport is  derived  from non-
point  sources.   The data in  Table  5  illustrates the application of  this
method.  The mean annual yields, to  which the method has been  applied,
were derived from the  use  of a minimum  of three years  of record at  each
station.  A combination of weighted  mean concentrations and long  term flow
duration tables  were  used to calculate  the  mean  annual  yields  of  sediments
and total phosphorus  (Baker,  1980).

     The phosphorus/sediment ratios  for the Broken  Sword,  Tymochtee and
Wolf East watersheds  reflect the ratios for agricultural watersheds lacking
                                  234

-------
 source  inputs.   In  the  case  of  Bucyrus,  the phosphorus  sediment ratio
 (3.42)  is much  higher than the  adjacent  agricultural watershed  (Broken
 Sword).  Assuming 100%  transmission  of upstream point source  inputs,
 these inputs  are subtracted  from the total phosphorus yield to  give a
 nonpoint phosphorus yield.   The resulting nonpoint  phosphorus/sediment
 ratio  (1.28)  is much lower than the  adjacent  agricultural  watershed.
 It  should be  noted  that agricultural land use dominates all of  these
 watersheds  including those with point source  inputs.  The  low calculated
 ratio suggests  that not all  of  the point source inputs  are resuspended
 and exported  from the stream system.
 Table  4.  Annual variability  in  sediment  and  nutrient  loading from the
          Sandusky  River  near Fremont,  Ohio
Water
Year
1975
1976
1977
1978
1979
Discharge
109M3
1.030
.772
.629
1.391
1.087
Susp.
Solids
M. tons
(mg/1)
302,200
293
124,000
161
98,800
157
193,500
139
285,500
262
Total
Phosphorus
M. tons
(mg/1)
418.9
.406
398.9
.517
257.5
.409
463.4
.333
563.4
.518
Sol . Reac .
Phosphorus
M. tons
(mg/1)
72.42
.070
49.67
.064
65.76
.104
116.90
.084
112.2
.103
Nitrate
Nitrogen
M. tons
(mg/1)
4709.
4.57
2621
3.39
3135
4.98
4958
3.56
5615
5.16
Table 5.  Use of Phosphorus/Sediment Ratios to Analyze Delivery of Upstream
          Point Source Phosphorus Inputs
Location
Bucyrus

Upper Sandusky

Broken Sword
Tymochtee
Wolf, East
Component
Total
Point Source
"Nonpoint Source
Total
Point Source
"Nonpoint Source



Mean Annual
Sediment Yield
M.T./yr .
12,400
II
48,600

18,900
30,800
12,900
Mean Annual
Phosphorus Yield
M.T./yr.
42.5
-26.6
15.9
111.9
-32.5
79.4
31.0
62.8
29.8
TP/SS
g/kg
3.42
1.28
2.30
1.63
1.64
2.04
2.31
                                   235

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     The application of this method at Upper Sandusky gives less clear-
cut results.  The calculated nonpoint phosphorus/sediment ratio of 1.63
is lower than two of the agricultural watersheds but is about the same
as the ratio in the Broken Sword Watershed.  The relatively low ratios
of point to nonpoint source phosphorus in these watersheds makes this
approach to determining point source transmission characteristics
difficult.

     A third approach to evaluating the transmission of upstream point
source phosphorus through the stream system would be to analyze the
delivery of sediment through the system.  One of the probable temporary
sinks of phosphorus in the stream systems is through adsorption to sedi-
ments.  Some fraction of these sediments will be deposited on flood
plains during the large floods which account for much of the sediment
and phosphorus yields.  Point source-derived phosphorus which becomes
adsorded to these sediments could, therefore, be deposited on flood
plains.  The accumulation of materials on flood plains represents per-
manent sinks for sediment and phosphorus relative to the time-frames
of water quality management planning.  According to soil surveys in the
Sandusky Basin, there are a number of flood plains upon which sediments
are accumulating (Steiger, 1975).  Quantification of this accumulation
is lacking and consequently the extent of transmission losses of sedi-
ment and particulate phosphorus through deposition on flood plains cannot
be readily estimated.  Impoundments along streams and rivers could also
provide permanent sinks for point source-derived phosphorus that is
adsorbed on sediment particles.

     Although it is probable that the transmission of point source-derived
phosphorus through the stream system is less than 100%, quantitative
determinations of transmissions coefficient in large agricultural river
basins is very difficult to attain.

     Bioavailability;  The instream deposition of phosphorus from upstream
point sources could involve biological uptake by periphyton or rooted
aquatic plants, adsorption to sediment particles or some type of chemical
precipitation reaction.  Storm routing methods which show resuspension
of total phosphorus do not show release of soluble reactive phosphorus
back into the water column  (Melfi, et al. 1979).  That portion of the
deposited phosphorus that is delivered to Lake Erie apparently arrives
as particulate phosphorus.  It is probable that during its period of
storage in the stream bed, at least some of the point source-derived phos-
phorus is converted to unavailable or slowly available particulate phos-
phorus.  Part of it could be converted into refractory forms by biological
processes while part could undergo chemical transformations.  Once in the
lake particulate phosphorus, whether bioavailable or not, is subject to
removal from the water column through sedimentation.  This particulate
phosphorus is less available than soluble reactive phosphorus derived
from nonpoint sources and delivered to the lake during storms or soluble
reactive phosphorus delivered to the lake by direct point sources.

     By far the highest loading rates of soluble reactive phosphorus to
the lake occur during storm events.  In the Sandusky Basin 50% of the
annual export of soluble reactive phosphorus occurs during the 5% of the
time with the highest fluxes.  At these times, the orthophosphorus loading
                                    236

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rates exceeded 61.2 kg/hr.  These rates dwarf not only the upstream point
source inputs, but also the direct point sources in the basin, including
Fremont at 0.85 kg/hr. and Sandusky at 1.5 kg/hr.(IJC/ 1979).  The higher
flow velocities during these storm events probably result in a high
delivery of this nonpoint-derived soluble reactive phosphorus through
the esturine and nearshore processing zones to the open lake system.
It is possible that during non-storm conditions, soluble reactive phos-
phorus from direct municipal discharges is processed and deposited in the
esturaries and nearshore zones in a fashion similar to the deposition of
upstream point source phosphorus.  Nearshore processing of phosphorus
has been reported by Richards(1979).   If esturine and nearshore processing
of direct point sources to the lake is extensive, then a mass balance of
soluble reactive phosphorus to the open lake water could be dominated by
soluble reactive phosphorus derived from nonpoint sources and delivered
to the lake during storm events.

     Since upstream point source-derived phosphorus is in a particulate
form when it reaches the lake, it will be less available than phosphorus
entering the lake from direct point sources.  Soluble reactive phosphorus
derived from nonpoint sources could be an extremely important component
of the bioavailable phosphorus reaching the open lake system.

Ambient Stream Water Quality Effects

     One effect of upstream point source phosphorus control programs is
to lower the phosphorus concentration in the stream system, especially in
the zones immediately downstream from outfalls.  The effect of point source
loading on stream phosphorus levels is greatest during periods of low
stream flow.  As stream flows increase, the increasing dilution of the
point source effluents decreases the impact of the effluent on stream
concentrations.  Water g_uality problems could be associated with the ele-
valted phosphorus concentrations if they result in increased growth of
rooted aquatic plants, periphyton or phytoplankton.  If these growths reach
nuisance levels and cause excessive diurnal oxygen fluctuations, then
ambient stream water quality problems could be attributed to the point
source phosphorus inputs.

     In the Sandusky Basin rooted aquatic plants are uncommon.  Phyto-
plankton chlorophyll levels along the river were not decreased by the
implementation of phosphorus removal programs along the river  (unpublished
data, Heidelberg Water Quality Laboratory).  Nuisance growth of algae do
develop along the river but these seem to be more related to periods of
low stream flow and stream gradients than to phosphorus levels.  Much of
the time turbidity associated with the transport of fine clay probably
limits growth of plant communities.  It does not appear that the elevated
phosphorus concentrations from point sources, where and when they occur
in the Sandusky Basin, cause significant water quality problems.

     There is a lack of information on the effects of nutrients on plant
growth in stream systems.  Responses probably vary considerably from stream
to stream as well as with position in the stream system  (Cummins,   1975).
The need for additional studies on this topic for streams in southern
Ontario has been recently cited  (Wong, et al. 1979).  In the river quality
assessment program conducted for the Williamette River Basin in Oregon, it
was concluded that flow augmentation was a more effective and economical


                                 237

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procedure for controlling algae than advanced waste treatment.  (Rickert,
et al., 1977).

Discussion

     Although the data available in the Sandusky Basin does not currently
provide quantitative values on the transmission coefficient of upstream
point source phosphorus to Lake Erie or its bioavailability upon reaching
the lake, it is clear that its form and mode of delivery to the lake is
quite different than for direct point sources.  The bulk of the upstream
point source-derived phosphorus that does reach the lake will be delivered
during storm events at which time it is a small part of the total parti-
culate phosphorus load.  The nonpoint component of the particulate phos-
phorus load is so variable that reductions in point source loads cannot be
readily detected.

   Because of in-stream processing of upstream point source phosphorus, the
impacts of this phosphorus on lake water quality are likely to be quite
different than for direct discharges to the lake.  Consequently, different
requirements for phosphorus removal should be considered for upstream point
sources.  This could include careful analyses of the costs for varying
degrees of phosphorus removal at these plants.  Consideration of the water
quality benefits that could be achieved through diverting portions of funds
needed to operate phosphorus removal programs to supporting nonpoint source
implementation programs or flow augmentation programs should be considered.


Table 6.  Summary of Municipal Point Source Phosphorus Loading to the
          Great Lakes, 1978a
Basin
Superior
Michigan
Huron
Erie
Ontario
Total
Detroit
Direct
Kg /day
351
1,353
463
12,165
5,240
19,572 (69%)
7,178
12,394 (59%)
Indirect
Kg /day
291
2,249
693
3,860
1,644
8,737 (31%)
8,737 (41%)
Total
Kg /day
641
3,602
1,156
16,025
6,884
28,308

     a  Source  IJC, July,  1979.
      Within the Great Lakes  System,  indirect point sources account for a
 considerable portion of the  total  point  source phosphorus inputs  (Table 6).
 More information is needed on the  open lake impacts of phosphorus derived
 from upstream point sources  in comparison with the impacts of soluble re-
 active phosphorus delivered  during storm events.  Lacking this information,
 the effectiveness of alternative control programs for the lakes cannot be
 accurately predicted.
                                  238

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                                 REFERENCES
Baker, David B., 1980.  Final Report on EPA Grant No. R805436-01-1 in pre-
   paration.

Baker, David B. & Kramer, Jack W., 1973.  Phosphorus Sources and Transport
   in an Agricultural River Basin of Lake Erie.  Proc. 16th Conf. Great
   Lakes Res., p. 858-871.

Baker, David B. & Kramer, Jack W., 1975.  Distribution of Non-Point Sources
   of Phosphorus and Sediments in the Sandusky River Basin.  Proc. Sandusky
   River Basin Symposium, IJC, p. 61-88.

Cummins, Kenneth W., 1975.  The Ecology of Running Waters, Theory and
   Practice.  Proc. Sandusky River Basin Symposium, IJC, p. 277-294.

IJC, 1979.  Inventory of Major Municipalities and Industrial Point Source
   Dischargers in the Great Lakes Basin.  Great Lakes Water Quality Board.

DePinto, Joseph V., et al., 1980.  Phosphorus Removal in Lower Great Lakes
   Municipal Treatment Plants.  Municipal Env. Res. Lab., U.S. EPA,
   Cincinnati, 147 p.

Melfi, David A., et al., 1979.  "Material Transport in River Systems During
   Storm Events by Water Routing," LEWMS Technical Report.  U.S. Army Corps
   of Engineers, Buffalo, NY, March, 1979.

Ohio EPA, 1979.  Initial Water Quality Management Plan, Sandusky River
   Basin, Prt. I, II, III.

Richards, R. Peter, 1979.  Limnological Surveillance of the Nearshore Zone
   of Lake Erie in Central and Eastern Ohio.  Pt. I: Chemical Limnology.
   Prepared for U.S. EPA, Region V.

Rickert, David A., et al., 1977.  Algal Conditions and the Potential for
   Future Algal Problems in the Williamette River, Oregon.  Geo. Survey
   Circular 715-G.

Sonzogni, William C., et al., 1980.  Watershed: A Management Technique for
   Choosing Among Point and Nonpoint Control Strategies.  U.S. EPA Region V
   Seminar on Water Quality Management Trade-Offs.

Steiger, Joseph R., 1975.  Soil Surveys as a Tool in Studies on Nonpoint
   Sources of Stream Sediment.  Proc. Sandusky River Basin Symposium, IJC,
   p. 89-96.

U.S. Army Corp of Engineers.  1979.  Lake Erie Wastewater Management Study
   Methodology Report.  U.S. Army Corps of Engineers, Buffalo, NY.  146 p.

Verhoff, Frank H., et al., 1978.  Phosphorus Transport in Rivers.  U.S.
   Army Corps of Engineers, Buffalo, NY.

Wong, S. L., et al., 1979.  An examination of the Effects of Nutrients on
   the Water Quality of Shallow Rivers.   Hydrobiologia, vol. 63, 3, p. 231-
   239.
                                 239

-------
  SEDIMENT AND PHOSPHORUS TRANSPORT

                  BY

         STEPHEN M. YAKSICH*

           DAVID A. MELFI*

            JOHN R. ADAMS*
            September 1980
*Lake Erie Wastewater Management Study
    U. S. Army Corps of Engineers
           Buffalo District
                 241

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                     SEDIMENT AND PHOSPHORUS TRANSPORT







INTRODUCTION







    The characteristics of sediment and phosphorus  transport  in  a  particular




river affect how a river should be monitored and the  type  of  information




which can be obtained.  Transport characteristics vary between rivers  and




sections of rivers, as well as hourly, daily, seasonally,  and annually.




Different types of monitoring programs are needed to  measure  ambient water




quality and annual loads.  Changes in annual loads  do not  necessarily  reflect




changes in the watershed conditions brought about by  water quality management




programs.  This paper discusses river transport characteristics  which  are




observed and how they can be used to understand transport  mechanisms.   It




compares sampling programs required to measure annual loads and  examines




variations in annual loads and their effect on success monitoring. It points




out problems with using unit area loads and loading functions to estimate




phosphorus and sediment loads.  Finally, it presents  a monitoring  program  to




make reliable annual load estimates and a program for success monitoring.






OBSERVATIONS OF TRANSPORT







CHEMOGRAPH ,OF A FLOW EVENT







    Figure la shows the changes in total phosphorus,  soluble  orthophosphate,




and suspended sediment with changes in flow for an  event response  river.




Suspended sediment (SS) and total phosphorus (TP) transport in event  response




rivers are dominated by runoff events.  It can be seen from Figure la  that  SS




and TP concentrations increase with increasing flow.  Soluble orthophosphate




(OP) concentrations are seen to decrease during the flow event.  The  major
                                    242

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                                          APRIL  1976         MAY  1976

                                                      TIME IN DAYS



                    (b)  GRAND  RIVER AT EASTMANVILLE


Figure 1 - Variation in Total Phosphorus, Soluble  Orthophosphate, and Suspended

Solids Concentration with Flow for (a) the South Branch of Cattaraugus River near

Cattaraugus,  NY,  and event response river, and (b) the Grand River at Eastmanville,

MI, a stable  response river.  Source: Reference (2).

-------
portion of the phosphorus transport is with the sediment that originates from




the runoff.  The behavior of SS and TP in an event response river is markedly




different than their behavior in a stable response river whose watershed has




soils of coarse texture and high permeability (1).  In these watersheds,




water infiltrates instead of running off, and SS and TP concentrations do not




show large increases with flow as shown in Figure Ib for the Grand River.  In




the Grand River, suspended sediment varies from 50 to 160 milligrams per




liter and total phosphorus varies from 0.08 to 0.22 milligrams per liter as




compared to a range of 120 to 1,100 milligrams per liter for suspended




sediment and 0.16 to 0.78 milligrams per liter for total phosphorus in the




South Branch of the Cattaraugus.  Soluble orthophosphate concentrations are




similar for both rivers.  In the Grand River, approximately one third to one




half the phosphorus transport is in soluble phase.







TOTAL PHOSPHORUS VS. SUSPENDED SEDIMENTS







    As seen in Figure la, the SS and TP concentrations rise and fall together.




Figure 2 shows a plot of the instantaneous TP and SS concentrations.  Lower




SS concentrations have a higher ratio of TP/SS than high SS concentrations.




The reason for this behavior is that the higher SS concentrations are usually




carried by higher flows which also carry larger particles.  Also note that




considerable variation in the TP/SS exists at lower flows.  Table 1 shows the




TP/SS ratios measured for Northwest Ohio rivers for the period 1975 to 1979.




The ratios vary between the rivers and between years for each river.  In




light of the variation seen, caution should be exercised in picking TP/SS for




use as a surrogate in the estimation of phosphorus loadings from suspended




sediment measurements.
                                     244

-------
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                                           SRNDUSKY RIVER  NEflR FREMONT, OHIO
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                                   * *
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500
1000
1500
                                                      SS.  NG/L
                                                                        2000
                                                                                 2500
3000
             Figure 2 -  Relationship of Total Phosphorus to Suspended Solids for the Sandusky River near Fremont, OH.

             Source:  Reference  (4).

-------
       Table 1 - Phosphorus Sediment Ratios for Northwest Ohio Rivers
                 for Water Years 1975-1979 (gm/km)
River
Honey Creek at Melmore
Portage River at Woodville
Sandusky River at Fremont
Tymochtee Creek at
Crawford
1975
-
1.84
1.23
1.39
1.15
1.86
1.64
1976
2.11 CD
1.83 (2)
2.45
1.72
3.22
2.81
1.88
1977
3.18
2.08
2.54
1.69
2.82
2.10
2.65
2.03
1978
3.58
2.40
2.77
1.96
2.39
1.78
3.25
2.27
1979
2.04
1.72
-
1.97
1.58
2.14
1.77
     Total Phosphorus Load X 1,000/Suspended Solids Load
(2)  (Total Phosphorus Load-Orthophosphate Load) X 1,000/Suspended Solids

Source:  Reference 3
HYSTERESIS


     From Figure la, it can be seen that the TP and SS concentrations peak

before the flow.  As a result, the same flow on the rising stage will carry

a higher concentration than the same flow on the falling stage.  This effect

is shown in the hysteresis diagram shown in Figure 3 which plots TP concen-

tration and SS concentration versus flow.  The arrows begin at the start of

the storm and point to increasing time into the storm.  Another way of dis-

playing the concentration differences between the rising and falling stage is

shown in Figure 4 which presents least squares correlations for TP con-

centrations and river flow rate for different days of the storm.  It can be

seen that the steepest slope for this correlation line occurs for the first

day of the storm.  The second and third days have successively lower slopes.

The scatter of the data points about the correlation line should be noted.

It results from difference in stream chemistry among runoff events of similar
                                     246

-------
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              CLINTON  RIVER  AT MORAVIAN  DRIVE

                     MT. CLEMENS,  MICHIGAN
                    MARCH 28  - APRIL I, 1977
                                     TP
                                                                 300
                                                     200 E
                                                         i
                                                                 •100
1000
1500
2000     2500

 FLOW-CFS
3000
3500
     Figure 3 - Hysteresis Diagram for Total Phosphorus and Suspended Solids as a Function of Flow.

-------
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                                     1000
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                                                       FLOW  IN  CFS
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                Figure 4 - Total Phosphorus  Concentration vs. River Flow Rate with Day of  Storm as a Parameter.
                The least squares correlations for each day of the storm is  indicated.  The number in parenthesis
                indicates the day of the storm.  Source:  Reference (5).

-------
size and similarities in stream chemistry among runoff events of different




size.






PATTERNS OF TRANSPORT






    Figure 5 shows the patterns of TP concentration versus log flow for




three river stations.  Tymochtee Creek at Crawford is an example of an agri-




cultural watershed with no significant point sources.  TP concentrations are




low at low stream flow and increase as the flow increases.  The high TP con-




centrations at high stream flow reflect the combined effects of TP carried by




the surface runoff which is producing the high flow and of suspended sediment




carrying phosphorus suspended from the stream bottom by the stream current.






    The Sandusky River at Upper Sandusky is an example of a sampling station




in an agricultural watershed located a considerable distance downstream of




point sources.  The TP concentration shows a slight increase as flow




decreases.  At high flows, the TP concentration increases.






    The Sandusky River at Bucyrus is an agricultural watershed where the




sampling station is located a short distance downstream from a significant




point sources of phosphorus.  The TP concentration and log flow pattern for




this station differs significantly from pure agricultural watersheds.  At




Bucyrus, the sampling station is approximately 1/2 mile downstream from the




outfall of the Bucyrus Wastewater Treatment Plant.  This plant has not yet




initiated a phosphorus removal program although it has a mean daily  flow of




2 million gallons per day.  The TP concentration  increases greatly as  the




streamflow decreases, due to decreasing dilution  of the relatively constant




effluent from the Bucyrus Wastewater Treatment Plant.  The TP concentration
                                    249

-------
19
                  A.TYMOCHTEE   CREEK
                       AT   CRAWFORD
                      Y=0.239(x) - 0.502
  175 2.OO  225   250  275   300  3.25  3.50  3.75  400  4.25  4.50   475  500  525
                            LOG  FLOW  L/SEC
5
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                  B. SANDUSKY  RIVER  AT
                       UPPER  SANDUSKY
                       Y=O.OI7(x) + 0.436
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                        LOG FLOW  L/SEC
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                           BUCYRUS
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 2OO
           250   275
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                           LOG fLOW  L/SEC
4 00   4 25
          450
                4.75  5.0O
 Figure 5 - Least Square Equations for Total Phosphorus and Log Flow:
 (a)  Tymochtee Creek at Crawford, an agricultural river basin.
 (b)  Sandusky River at Upper Sandusky, an agricultural river basin with
 upstream point sources.
 (c)  Sandusky River at Bucyrus, a station immediately below a point  source.
 Source:  Reference  (3).

-------
also increases at high streamflow, but this effect is partially obscured by




the extremely high concentrations under low flow conditions.







TOTAL PHOSPHORUS DEPOSITION






    Figure 6 shows the TP concentrations downstream of the Bucyrus Wastewater




Treatment Plant at Kestetter (0.9 km), Denzer (4.25 km), and Caldwell




(6.53 km).  Samples were collected every 2 hours for this study (7).  The




decrease in TP concentrations downstream is not due to dilution (increase




in flow is insignificant) but deposition and biological processing.  The




diurnal variation in the concentrations at all three stations can be seen.




Also noticeable is the displacement in the peaks as they move downstream.







    In contrast to the well-defined picture of deposition, diurnal variation




and downstream displacement of the concentration peak obtained from the




2-hour samples shown in Figure 6a is the data shown in Figure 6b.  This data




was collected by a grab sampling program at approximately 6-hour intervals.




From this data, downstream deposition between Kestetter and Denzer is not




noticeable.  In fact, concentrations seem to be increasing between the




stations.  The reason for the large variation in concentrations is not




obvious and the concentration peak is not seen to be moving downstream.




Figure 6 is a good example of how a false understanding of a system can be




obtained from an inadequate sampling program.







A TRANSPORT THEORY







DEPOSITION AND RESUSPENSION







    The observations of transport just described can be used with mass and




force balance equations to develop a theory of how phosphorus and suspended
                                     251

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sediment are  transported  in  a  river.   The  important  characteristics used in




developing  the  theory are:   1)   the peak of  the  TP concentration usually




leads the flow  rate peak  of  the  river  at any station;  2)   the  TP con-




centration  declines to  its low flow value  before the flow returns to its




approximate steady flow range  of values; and 3)   the peak TP concentration is




not necessarily higher  at the  downstream stations than at the  upstream sta-




tions (8).






    Figure  7  shows the  results of  calculations for different theories which




explain the three characteristics  described  above.   Figure 7a  shows the




initial conditions, a chemograph with  the  TP concentration peak ahead of




the flow peaks.  The results in Figure  7b  indicate that after  40 miles




downstream  with no water  or  chemical input,  the  peak of total  phosphorus has




moved behind  the peak of  water flow.   This result is in contrast with the




observation that the TP peak is  still  ahead  of the flow peak at downstream




stations.   Figures 7c and 7d compare models  which would explain the fact that




the observed  TP peak does not  lag  behind the flow peak.  Curves TP(1) and




TP(2) assume  local inflow with two different TP  concentrations and  no




resuspension.   Curve TP(1) has the TP  concentration  lagging behind  the flow




peak.  Curve  TP(2), which has  the TP peak  remaining  ahead of the flow peak,




does not have the TP concentration decreasing to  its initial value-  Both of




these results are in disagreement with  the observed  facts.   Only Figure 7d




which assumes resuspension and deposition  proportional  to the  rate  of




change of velocity with time reproduces  the  field observations.   The peak in




TP concentration remained ahead of the  flow  peak  and the  total phosphorus




concentration declined with declining flow.
                                        253

-------
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-------
DISTANCE OF TRAVEL






    From the previous discussion, it has been suggested  that  the  transport




of total phosphorus occurs via a mechanism by which  the  phosphorus  is  picked




up at one point in the stream and deposited at another.   Given  that total




phosphorus is transported from one point in the  stream to another,  the dis-




tance of transport becomes an important issue.   This distance of  travel could




be measured experimentally for any given reach of  stream by employing  tracer




particles.  However, these distance estimates would  be valid  for  only  the




individual stretch and numerous measurements would have  to be made  for




different stream reaches  just to understand one  river basin.  This  same




information can be estimated from the  hydrograph and chemograph measured at a




given point in a stream.  The technique to be described  uses  the  assumption




that the water is moving  as a kinematic wave.  Furthermore, the actual




distances calculated are  derived from  information obtained at one point in




the river and hence the assumption  that the whole stretch of  river  is  similar




to the measurement point  is implied  (9).






    The  calculational  procedure  is  based upon  two data  sets;  the  time




dependency of both flow and total phosphorus  concentration, and the flow




versus area curve for  a rated point  in the  stream.   From this  information,




the average distance traveled by the  total  phosphorus during a  storm event




can be calculated.  Figure  8  shows  the cumulative probability of  travel




distances at various stations in the  Sandusky River  basin for a storm event.




It can be seen from  this  figure  that  50 percent  of the  phosphorus from




Bucyrus  which was resuspended and measured  at  Upper  Sandusky will move at




least 52 miles,  which  is  the  distance to Lake  Erie.   The rest of  this
                                     255

-------
ro
en
en
                                     UPPER
                                    SANDUSKY
                                                      ^-BUCYRU
                                                               ^

                                                               FREMONT
           0
                                          70       90      110       130

                                         DISTANCE OF  TRAVEL-MILES
        Figure 8 - Cumulative Probability that Total Phosphorus will be Deposited In-stream Before Traveling

        the Stated Distance.  Sandusky River Basin, 12 July 1974.  Source:  Reference (9).

-------
material will  be  deposited  before  it  reaches  the  lake.   Flows  at least as




great as the flow event for which  these  calculations  were made occur on the




average of  nine times a year.






INSTREAM PROCESSING






    The steady state deposition  studies  (Figure 6)  show orthophosphate and




total phosphorus  discharged from a sewage  treatment plant are  rapidly




removed from the  water column  (7).  As this material  moves downstream from




the outfall, it is adsorbed to river  sediments by clay  minerals and/or




micro-organisms.   Calculations show that about 75 percent of the total




phosphorus  is  lost after  traveling  16 kilometers  during low flow conditions




which occur 35 percent of the  time  (10).   At  these  periods,  Lake Erie or




stations located  16 or more kilometers downstream do  not experience  increased




phosphorus  concentrations resulting from point sources.






    The phosphorus deposited in  the river  bottom  sediments during steady




state conditions  is resuspended  during high flow  events.   This phenomenon can




be seen in Figure  9 which shows  deposition and resuspension of total phos-




phorus and  orthophosphate between Bucyrus  and Upper Sandusky on the  Sandusky




River.  Deposition and resuspension were calculated utilizing  a dynamic




phosphorus  transport model  (11).  This model routes all  upstream inputs




between Bucyrus and Upper Sandusky  to Upper Sandusky.   If  the  routed sum is




larger than what was actually measured, deposition  is assumed.   If what is




measured is larger than the routed  sum, resuspension  is  assumed.   It can be




seen from Figure 9 that both total phosphorus and orthophosphate are lost




from the water during low flow.  However,  during  high flow, only total




phosphorus is  resuspended.  Orthophosphate is neither deposited  to nor
                                     257

-------
         2.00
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                   8
                                                                                           DEPOSITION

                                                                                       T£ RESUSPENSION
                  9   10   II    12    13   14    15                       789    10    II   12   13   14    15

                         JULY                                                         JULY

Figure 9 - Deposition and  Resuspension of  (a)  Total Phosphorus and (b) Orthophosphate in  the  Sandusky River
near Upper Sandusky - Storm beginning  7 July  1976.   Source:   Reference (11).

-------
released from the sediments during high flow.  It moves right  through  the




system.  This figure very clearly illustrates the instream processing  of




nutrients.  Immediately available orthophosphate is converted  to  potentially




available sediment phosphorus during steady state flow conditions.   The




phosphorus is later transported as potentially available sediment phosphorus




during high flow.  It also should be noted that during high flow, phosphorus




from point sources is transported directly through the river with no instream




processing.







SAMPLING STRATEGIES FOR FLUX ESTIMATION







    It has been shown in the previous sections that SS and TP  transport in




an event response river occurs in a river during high flow events by a




process of resuspension and deposition.  Knowledge of when the material is




moving can help to determine when to sample.







FIXED INTERVAL SAMPLING







    Treuner et al. (12) examined the effect of sampling frequencies  on




determination of annual phosphorus load of small to moderate streams




(Wahnbach River in Germany) with low flows and no relationship between total




phosphorus concentration and flow (stable response river).  They  examined




sampling frequencies of 1 to 29 day intervals between measurements.  They




also examined four different averaging methods to determine annual loads.




They concluded that use of continuous flow measurement by means of a level




recorder leads to annual total phosphorus loads two to four times more




accurate than discontinuous flow measurements with a simple measuring  weir.




In addition, they concluded that sample frequencies of 14 to 21 days (17 to
                                    259

-------
21 samples) and continuous flow measurements with a level recorder are




required to keep deviations within 20 percent of the reference value




(Figure 10).






    In contrast to the above results, Hetling, et al. (13) concluded that a




fixed interval sampling is of little value to obtain annual loads unless




daily or'every other day samples are taken.  With sample frequencies of




14 to 21 days (17 to 21 samples) deviations of 700 percent were obtained




for particulate phosphorus and 1,700 percent for suspended sediment for an




event response river (Figure 11).  They further concluded that a sampling




strategy based on sampling high flow events was necessary to obtain reliable




annual load for an event response river.






HIGH FLOW SAMPLING






    Assuming that high flows must be sampled, the question arises as to




how many samples are required.  Figure 12  shows the  percent deviation  from




the true value for event sampling strategies  for four event response rivers




(Maumee, Portage, Sandusky, and Huron).  The  figure  was  developed by using




only the data collected during  the largest and/or second largest  flow  events




plus a few  low flow samples.  The flow interval method  (14) was used to make




a  flux estimate and from  this,  a  flux calculated from the complete  yearly




record was  subtracted.  The difference was divided  by the flux  calculated




from the total record.






    It can  be  seen from  the figure that  for  all  three parameters  all but




two estimates  are within  a 50 percent  deviation, and most of  the  estimates




are within  20  percent.   In most cases,  the error estimates  overlap  the
                                     260

-------
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             Figure 10  - Wahnbach River, a Stable Response  River  - Deviations of the annual P loads calculated
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-------
                                                                        292
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true value.  The error estimate is calculated assuming a normal distribution




and a 90 percent confidence coefficient.  In contrast to the large variations




obtained from the fixed interval sampling shown in Figure 11, the event




sampling program yields very reliable estimates.






EFFECT OF MISSING HIGH FLOW EVENTS






    Suspended sediment and material transported by sediment  such  as  total




phosphorus increase in concentration with increasing flow.   If water quality




measurements for these parameters are not made during high flow events,-the




annual load can be significantly underestimated.






    Table  2 shows the  total phosphorus  load which was transported by Lake




Erie tributaries during high flow events.  For these event response  rivers,




28 to 47 percent of the total  phosphorus  load was  transported  in  7  to 10 days




during the year.  If  samples collected  during high flow  periods were not




used in the loading calculation, total  phosphorus  loads  can  be  under-




estimated  at 15 to 30  percent.






    There  are a number of  event  response  rivers  which are  heavily impacted




by point sources (i.e., Sandusky River  below Bucyrus).   In these  rivers,




total phosphorus concentrations  first  decrease with  increasing flow (due to




dilution of point  sources) then  increase  with increasing flow during a run-




off  event.  In  these  river,  event  sampling  is not  as  important as in other




event response  rivers. Another  group  of  rivers  in which event sampling is




not  as  important are  stable response  rivers.   They are  primarily fed by




ground water, not  runoff,  and  sediment concentrations  do not vary greatly




with changing  flow conditions  (Figure  Ib).
                                       264

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          Table 2 - Total Phosphorus Transport  During  High Flows*
River
Maumee
Portage
Sandusky
Huron
Vermilion
Chagrin
Cattaraugus
Percent Load
33
46
41
38
28
32
47
Percent Time
2.7
2.6
3.4
1.9
2.5
2.5
1.9
Percent Loss if
in the Loading
23
29
22
19
17
16
29
Not Included
Calculation







*Statistics for flows greater than 40 percent  of  the maximum flow for
 the period June 1974 to May 1975.
HYDROLOGICAL VARIABILITY


    The annual load for any water quality parameter  can  vary  considerably

from year to year and river basin to river basin.  The reason for  this  annual

variation is the type and amount of rainfall which falls  on the  drainage

basin and the condition of the basin when it rains.  Annual changes  in  basin

condition can result from natural or man-made causes.  Basin  soil  moisture,

infiltration capacity, and surface cover can be affected  by climatic factors

such as air temperature, sunshine, and previous rainfall.  An example of  man-

made induced changes which affect basin conditions are changes in  land  use

which can destroy cover over large areas, as during  timbering operations  or

construction activities.  Land use changes can also  reduce the infiltration

capacity when streets and homes are built.  Surface  cover and interception

can be affected by changes in cropping patterns and  tillage methods. Tillage
                                        265

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methods can also change soil structure,  thereby  affecting  the  infiltration


capacity and total porosity of a soil.



    Moderate changes in the total amount  of  rainfall  can have  large changes
                                                                             *,

in the total runoff from a basin.  Not only  does total  runoff  affect pollu-


tant export, but the type of storms and when and how  they  occur  will affect


export.  Two inches of rain falling in 1  hour may erode and  transport much


more sediment than 2 inches of rain over  24  hours.  The same 2 inches per


hour will cause much more erosion when the soil  is  bare and  saturated than


when there is surface cover and low soil  moisture.



TIME VARIABILITY WITHIN A RIVER BASIN



    An example of annual variation is shown  in Figures  13a and b which


show the long-term annual flow and annual suspended sediment record for the


Maumee River at Waterville, Ohio.  These  flow data  were collected with a


recording level gage.  The suspended sediment data  were collected daily with


additional measurements made during high  flows.   It can be seen  from the


figure that the mean annual flow was 4,886 cfs for  the  period  of record.


The minimum annual flow recorded was 1,996 cfs and  the  maximum was 8,587


cfs, a 430 percent variation.  For suspended sediment,  the mean  annual load


was 1,140,000 metric tons per year.  The  minimum load was  260,000 metric tons


per year and the maximum load was 2,106,000  metric  tons per  year, a variation


of 23 to 185 percent of the mean annual  load.



    Annual variations in nutrient transport  are  not as  extreme as those in


sediment transport.  Table 3 shows the annual and sediment flows and nutrient


and sediment flux for the Sandusky River  at  Fremont.  It can be  seen from
                                      266

-------
        « £ 3!   SUSPENDED SEDIMENT (million metric tont/yr.)
                                                                        MEAN  DAILY FLOW (eft)
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this table that although the flow only varied from 64 to 142 percent of the

5-year average, suspended sediment varied from 49 to 150 percent of the

5-year average.  Total phosphorus, which is transported by the suspended

sediment, only varied from 61 to 134 percent of the 5-year average.  Ortho-

phosphate, which is not transported with the suspended sediment, only

varied from 60 to 140 percent of its 5-year average.
               Table 3 - Nutrient and Sediment Transport for the
                         Sandusky River at Fremont
Parameter
Flow (106 cubic
meters)
Total Phosphorus
Soluble Ortho
Phosphorus
Suspended
Sediment
1975
1,030
1.05
419 (1)
1.00 (2)
72
0.86
302,000
1.50
1976
772
0.79
399
0.95
50
0.60
124,000
0.62
1977
629
0.64
258
0.61
66
0.79
98,800
0.49
1978
1,390
1.42
463
1.10
117
1.40
194,000
0.97
1979
1,090
1.11
563
1.34
112
1.34
286,000
1.42
5-Yeai
Average
981
420
83

200,800
(1)  Metric tons/year
(2)  Annual/5-year average

Source:  River Laboratory, Heidelberg College.  Reference (3)
ANNUAL VS. MEAN ANNUAL LOADS


    Calculation of an annual load for a river is a different problem than

calculating a mean load.  Annual loads are necessary for mathematical model

calibrations which relate 1 year's input to a lake from a river to the water

quality measured  in the  lake for that year.
                                        268

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    However, annual loads are not useful  for determining  the  distribution




between point and nonpoint sources of  total phosphorus  inputs to  a lake.   For




example, the nonpoint source load to Lake Erie varied between 40  and  57  per-




cent of the total lake load between 1970  and 1977  (10).   Depending upon  what




year is chosen, opposite conclusions could be reached:  control of diffuse




sources is required to restore the lake or control of diffuse sources is  not




required to restore the lake.  To make a  judgment  on the  need for diffuse




source control, a mean annual load is  needed.







EFFECT OF FLOW VARIATION ON ANNUAL LOAD







    With large variations in annual load, the question  arises, "How can  an




annual load estimate be normalized to  a mean load  estimate?"   One way to




normalize an annual load estimate is to calculate  the annual  weighted mean




concentration (annual load divided by  annual flow) and  multiply it by the




mean annual flow.  This mean annual load  for the Maumee River suspended




sediment data is shown in Figure 13c.  It can be seen from  the figure that




this estimate of mean annual load varies  from 485,000 to  1,668,000 metric




tons per year.  This estimate of annual load is more representative of




export from the basin, but still has a variation of 43  to 146 percent of  the




mean annual load.







    Use of an annual weighted mean concentration to calculate a mean  annual




load removes variations in total annual flow from  the mean  annual load esti-




mate.  However, variations in mean annual loads still exist and result from




differences in flow characteristics such  as the magnitude, duration,




frequency, and seasonal distribution of high flow  events.   Therefore,  if
                                    269

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material  export  from  a  basin is  to  be adequately characterized,  these dif-




ferences  in  annual  flow characteristics  must  be eliminated.







    When  more  than  1  year  of concentration data is  available,  the entire data




set should be  used  to calculate  a flow weight mean  concentration which can be




used with mean annual flow to  calculate  a mean annual  load.







VARIABILITY  BETWEEN RIVER  BASINS







    Sediment,  nutrient,  and  chemical  export from rivers  is  often compared on




a unit area  basis,  i.e., the export measured  at a flow gaging  station is




divided by the area of  the river basin above  the station.   Often,  unit area




loads measured in one river  basin are used to estimate flux  from unmeasured




watersheds.  Table  4  shows the unit area contributions of  total  phosphorus




from nine rivers which  flow  into Lake Erie.   For the 2 years shown,  the




annual unit  area loads  range from 0.75 to 3.57  kilograms per hectare.   This




range of  variation  is typical of the  range of unit  area  loads  which  can be




expected  from  rivers  in  the  same region.   Considerable care  should be  exer-




cised before using  unit  area loads  to calculate fluxes in unmeasured rivers.







    The mean annual loads  shown in Table 4 do not show as much variation as




the annual loads.   They were calculated  from  the flow  and concentration data




collected during 1975 to 1977 and the period  of record flow  duration tables.




The mean  annual total phosphorus loads only vary from  0.79  to  1.65 kilograms




per hectare.   If unit area loads must be used,  mean annual  loads would pro-




vide a better  estimate  than  annual unit  area  loads.







    Also  shown in Table 4  is the,unit area diffuse  source load.   This  load




was calculated by subtracting the upstream point sources from  the  annual
                                    270

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load.  The diffuse source load varies from -0.45 to 1.06 kilograms per

hectare per year.  This range of variability is greater than that shown by

the mean annual load.  The negative loads indicate that all of the point

source phosphorus is not being delivered to the measuring station.   It is

moving into long-term storage in either the streambed or the flood plain.

In summary, unit area loads are not a reliable source of data to make flux

estimates for unmeasured rivers.


           Table 4 - Unit Area Contributions of Total Phosphorus
River
Maumee
Portage
Huron
Sand us ky
Vermilion
Black
Cuyahoga
Chagrin
Cattaraugus
Kilograms as Phosphorus Per Hectare Per Year
(kg/ha/yr)
1975 CD
1.58
1.25
1.20
1.61
1.89
1.89
3.57
1.76
1.31
1977 (!)
1.15
0.99
1.15
0.75
1.03
1.65
1.57
0.98
2.25
Mean Annual (^)
1.12
0.79
0.81
.91
0.71
1.10
1.65
1.00
1.06
Diffuse Source (3)
0.86
-0.16
0.63
0.45
0.48
0.86
-0.45
0.76
1.06
(1)  Water  year,  1 October  to  30 September.
(2)  Calculated with  the  concentration  and  flow data  collected  in 1975
     to  1977  and  the  period of  record flow  duration tables.
(3)  The diffuse  source load was calculated  by  subtracting  the  upstream
     point  source load from the mean annual  load.

Source:  Reference (10).
                                     271

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CONCLUSIONS







    The information described in this paper resulted from an attempt  to




answer the question, "How much phosphorus from tributary point sources




reaches the lake?"  The answer to the question still is, "We don't know."




Despite the answer being the same, our knowledge of sediment and phosphorus




transport in rivers has increased.  Based on the work described in this




paper, the following conclusions can be reached:







    1.  Two types of rivers exist - event response rivers where SS and TP




concentrations increase with increasing flow, and stable response rivers




where suspended sediment and total phosphorus concentrations do not increase




with increasing flow.  The type of river affects how you measure it.







    2.  In event response rivers, the bulk of the phosphorus is transported




by the sediment.  However, the total phosphorus/suspended sediment or




(total-ortho phosphorus)/suspended sediment ratio varies considerably during




an event, between events, annually, and between rivers.







    3.  Considerable variation in the flow concentration relationship for




a river exists.  This variation is caused by differences between the  rising




and falling limbs of individual runoff events, differences in stream




chemistry among runoff events of similar size, and similarities in stream




chemistry among runoff events of different sizes.







    4.  Different patterns of concentration versus flow exist between river




basins with no upstream point sources, point sources immediately upstream,




and point sources considerably upstream.
                                    272

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    5.  Both soluble and partlculate phosphorus which enters a river during




low flow is quickly removed from the water column.  During high flow, the




phosphorus is resuspended and subsequently transported as particulate




phosphorus.  This conversion from immediately available soluble ortho-




phosphate to potentially available particulate phosphorus represents an




instream processing of soluble orthophosphate from point and nonpoint




sources.






    6.  Sediment and phosphorus in suspension travels a finite distance.




The probability it will travel a certain distance can be calculated.  This




probability will change and vary between events and rivers.  However, how




long the material will remain on the bottom before being resuspended cannot




be calculated.






    7.  High flow events must be sampled on event response rivers to obtain




reliable suspended sediment and total phosphorus flux estimates.  If these




events are not sampled, fluxes will be underestimated by 15 to 30 percent.






    8.   Considerable diurnal variation can exist during low flow at river




stations below point sources.  Sample intervals as small as 2 hours may be




required for some studies.






    9.  Annual orthophosphate, total phosphorus, and suspended sediment




fluxes can vary considerably.  A flux measured in any 1 year may not repre-




sent long-term transport for a river basin.  A more representative calcula-




tion is a mean annual load.






    10.  Unit area loads vary between river basins.  Caution should be exer-




cised in using unit area loads measured for other watersheds.
                                     273

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RECOMMENDED SAMPLING PROGRAM







    In order to obtain a reasonable estimate of total loads transported by an




event response river, sampling during high flow events is necessary.




Approximately two to three of the largest events must be sampled for a yearly




estimate, with 15 to 20 grab samples collected over each hydrograph.  An




additional 5 to 10 samples should be collected during steady flow periods.




This program should yield a loading estimate with an error estimate of 10 to




20 percent.







    Fluxes for stable response rivers can be estimated with fixed interval




sampling programs.  The number of samples required will depend upon the




variability of each river and will range from 15 to 45.







    The above program will result in annual estimates for tributaries which




are reliable and estimates which can also be used to detect differences in




annual loads.  However, this program will likely not be sufficient to detect




progress made in control of diffuse sources.  Annual variations in the




frequency and duration of high flow events as well as basin conditions, such




as soil moisture and cover, make any simple evaluation of change in phos-




phorus and sediment loads impossible.  If changes in phosphorus loads are




to be measured, continuous records of rainfall, streamflow, water quality,




soil moisture, and cover will be needed, as well as improved methodologies




for relating this information.  A few watersheds should be selected for




such studies.







    Progress in diffuse source control can best be assessed through moni-




toring the implementation of conservation measures in the agricultural com-




munity and storm water management controls in the urban areas.  Intensive
                                     274

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monitoring programs to accurately measure river loadings could be carried out




on selected rivers as described above.  Implementation of conservation




measures can be used as input to models or tools, such as the Universal




Soil Loss Equation, to estimate progress based on reductions in potential




gross erosion.
                                     275

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                                 REFERENCES
(1)   Sonzogni,  W.  C.,  et al.,  "United States Great Lakes Tributary Loadings,1
      PLUARG Technical  Report,  Ann Arbor,  Michigan, January 1978.

(2)   USEPA Region  V -  STORET  Retrieval.

(3)   Baker, D.  A., Heidelberg  College River Laboratory, Tiffin,  Ohio.

(4)   U.  S. Army Corps  of Engineers,  Buffalo District, Lake Erie  Wastewater
      Management Study, Preliminary Feasibility Report, Buffalo,  New York,
      1975.

(5)   Verhoff,  F. H.,  S. M. Yaksich,  and  D.  A. Melfi, "Phosphorus Transport
      in Rivers," Lake  Erie Wastewater Management Study Technical Report,
      U.  S. Army Corps  of Engineers,  Buffalo, New York, November  1978.

(6)   Baker, D.  A.  and  J. W. Kramer,  "Patterns of Variability in  Stream
      Chemistry Data,"  Lake Erie Wastewater  Management Study Technical
      Report, U. S. Army Corps  of Engineers, Buffalo, New York, March 1979.

(7)   Verhoff,  F. H. and D. A.  Baker, "Moment Analysis for Review Model
      Discrimination and Parameter Estimation with Application to
      Phosphorus,"  accepted for publication  with Water Research.

(8)   Verhoff,  F. H. and D. A.  Melfi, "Total Phosphorus Transport During
      Storm Events," ASCE, Journal of the  Environmental Division, October
      1978.

(9)   Verhoff,  F. H., D. A. Melfi, and S.  M. Yaksich, "Storm Travel Distance
      Calculations  for  Total Phosphorus and  Suspended Materials  in Rivers,"
      Water Resources Research, Vol.  15,  No. 6, December 1979.

(10)  U.  S. Army Corps  of Engineers,  Buffalo District, "Lake Erie Wastewater
      Management Study, Methodology Report," Buffalo, New York, March 1979.

(11)  Melfi, D.  A.  and  F. H. Verhoff, "Material Transport in River Systems
      During Storm  Events by Water Routing," Lake Erie Wastewater Management
      Study Technical  Report,  U. S. Army Corps of Engineers, Buffalo, New
      York, March 1979.

(12)  Treunert,  E., A.  Wilhelms, and  H. Bernhardt, "Effect of the Sampling
      Frequency on  the  Determination of the  Annual Phosphorus Load of Average
      Streams,"  Hydrochem. hyd. geol.  Mitt, Vol. I, pp. 175-198, March
      1974.

(13)  Hetling,  L. J.,  G. A. Carlson,  and J.  A. Bloomfield, "Estimation of
      the Optimal Sampling Interval in Assessing Water Quality of Streams,"
      Environmental Modeling and Simulation, EPA 600/9-76-016, pp. 579-582,
      July 1976.
                                    276

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(14)   Verhoff,  F.  H.,  S.  M.  Yaksich,  and D.  A.  Melfi,  "River Nutrient and
      Chemical  Transport  Estimation,"  ASCE,  Journal  of the Environmental
      Engineering  Division,  June 1980.
                                   277

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                             BIOAVAILABILITY OF PHOSPHORUS
                                   SOURCES TO LAKES
                                           by

                                   Terry J. Logan*
* Associate Professor,  Agronomy Department,  The  Ohio  State University, Columbus, Ohio
                                       279

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     The role of phosphorus in accelerated eutrophication of Lake Erie
and other areas in the Great Lakes drainage basin has been recognized
and documented in recent years.  Studies by LEWMS and PLUARG have shown
that a major part of the total phosphorus load entering the lakes from
tributary drainage is in the form of particulate P,  and lake shoreline
erosion also contributes large amounts of P.  While  it is readily accepted
that soluble inorganic P in drainage water is available to algae and other
aquatic vegetation, the bioavailability of sediment-bound phosphate is
largely unknown.  As a result, one is faced with two extreme scenarios:
a) only the soluble inorganic P is bioavailable or b) all sources of P
including sediment P are available.  The first scenario is supported by the
findings in New York where soluble inorganic P was shown to be the dominant
form of stream-transported phosphate in stimulating growth of algae (Porter,
1975).  On the other hand, Golterman (1977) found that sediment P in shallow
polder lakes in Holland would maintain highly eutrophic conditions even if
all external P sources were removed.  Recent work by Allan and Williams (.1978)
demonstrated the importance of biologically available sediment P in fairly
shallow Canadian prairie lakes.

     The importance of sediment as a source of P for algae is governed by
a number of factors.  Streams which carry a low sediment load, and/or  sedi-
ment of coarse-texture and stream-bank origin will have much of their bio-
logically available P as soluble inorganic P as a consequence of the lower
P content of coarse sediment  (Williams et al, 1976 a).  Consideration must
also be given  to physical  lake dynamics.  Stream sediments which settle
rapidly into deep  lakes will  only be positionally available to algae in the
photic zone for short periods  as in the central and eastern basins of Lake
Erie, thereby  minimizing the  significance of sediment P as a source of
biologically available phosphorus.  In contrast, we have the situation
where streams  carry a high load of fine-grained sediment into shallow  lakes,
a situation similar to that in the western basin of Lake Erie.  In this in-
stance, factors which serve to increase the importance of sediment P are:
the high percentage of the total phosphorus load as sediment P, the higher
content of P in clay-sized sediment, and  the longer period  that this suspended
sediment load  is positionally available to  algae in  the photic zone.

      Procedures to estimate bioavailability of sediment P from tributary
sources must take  into account the conditions under which algae obtain P
from  sediment.  Algae can  derive  some P from sediment  in the photic zone
for short periods  and under aerobic conditions.  In addition, available P is
derived from bottom sediments during anoxic regeneration and subsequent lake
inversion,  a markedly different chemical  environment  than exists in the
photic  zone.   While much of the P regeneration is from decomposed algal
biomass, sediment  P is also released under  anoxic conditions.  As a result
of  this dichotomy, bioavailable sediment  P  will be viewed here in two  ways:
a)  positionally available,  to represent short-term release  of P to algae  in
surface waters, and b) total  potentially  available,  to represent  maximum
P which can be released over  time by all  mechanisms.   Procedures to estimate
sediment P  bioavailability will be discussed in the  context of this concept.

      In this paper, I will discuss the bioassay procedures  used to measure
available P,  the  studies which correlated biological  availability with
chemical extraction,  estimates of bioavailability of  Great  Lakes sediments
and waters,  and  interpretations of these  findings for  point and nonpoint
source  P management.
                                     280

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                     BIOASSAY MEASUREMENT OF AVAILABLE P

     Recent bioassays of the availability of sediment P for uptake by
aquatic plants have simply involved culturing algae in a suspension of
river or lake sediments, in which the sediment P is the only possible
phosphorus source and other necessary nutrients are in excess supply.
Following an incubation period either the algal phosphorus content or the
algal biomass (employing a P/biomass conversion factor) is used to esti-
mate the amount of phosphorus that had become available.

     Cowen and Lee (1976a) employed the test alga Selenastrum capricornutum
to measure the available P in the particulate P portion of urban runoff
samples collected in Madison, Wisconsin.  After 19-22 day incubation of
the Selenastrum in assay flasks containing AAP medium minus P
and runoff particulate P, they compared the cell counts obtained to a
standard curve of 18 day cell counts versus initial orthophosphate con-
centration.  In this way they converted cell counts to available P.  This
availability was most closely approximated by the NaOH-extractable frac-
tion, while exchangeable P (anion exchange resin extractable) slightly
underestimated the algal available fraction.

     Cowen and Lee (1976a, b) applied the same procedure described above
to the assessment of available P in sediment carried by tributaries to
Lake Ontario (Niagara, Genesee, Oswego, and Black Rivers).  They found
that 6 percent or less of the particulate P was available based on growth
of Selenastrum. In this case the algal available P was not consistent with
NaOH-extractable P (mean, 17-25% of inorganic particulate P; range, 11-28%) or
resin-extractable P  (mean. 17-25%; range 6-31%).  The relatively low availa-
bility was, however,  consistent with the findings of Logan et al (1979)
on four New York streams and Porter (1975) in Fall Creek, a small New
York watershed emptying into Cayauga Lake.

     Sagher et al (1975) determined NaOH-extractable P in Wisconsin lake
sediments before and after algal incubation and found that 0.1 N NaOH
extractablePat wide extraction to sediment ratios (>500:1) was highly
correlated with the P utilized by algae.  This agreed with the findings
of Cowen and Lee (1976a, b)  who also had a good correlation between NaOH
extractable P and P bioavailability.

     Dorich and Nelson  (1978) measured availabiltiy of sediment-bound P
in Black Creek by culturing algae for two weeks in synthetic medium with
gamma radiation sterilized sediments as the only P source, and determining
the quantity and chemical extractability of particulate P in the flask
before and after incubation.   By performing the same procedure for sedi-
ment-free algae culture (containing 0.2 mg/>   as soluble orthophosphate),
the extractability of the algal P was analyzed and the results were used
to correct the values obtained from the sediment-algal system extractions.
From the chemical extraction data,  they surmised that most of the algal
available P was from the Al- and Fe-bound inorganic fractions.   They used
NH4F followed by NaOH extraction, but I believe that the sum of these two
extractions are approximately equal to a single NaOH extraction and
therefore, their data support the availability of NaOH extractable P found
by Sagher e^ al (1975) and Cowen and Lee (1976a, b).

     In a recent study Verhof f  et^ _al  (1978)  attempted to determine the
rate at which an indigenous  phytoplankton population could utilize
phosphorus from Lake  Erie tributary waters.  The procedure involved incubation


                                   281

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of the algae with  the river sediments and periodic harvest of the bio-
logical solids.  A mass balance performed on total phosphorus and total
inorganic solids allowed the calculation of the rate of conversion to
available P.  In contrast to studies on lake suspended material and lake
bottom muds, the rate of algal immobilization of available P from the
river sediments was quite low.  The conclusion was that a linear avail-
ability rate of between 0.2 - 0.4%P/day could be expected.  This slow
rate of release over long time periods suggests that the rate of P release
is more important than the ultimate availability.
              CHEMICAL EXTRACTION OF SEDIMENT PHOSPHORUS


     The only true measure of algal available phosphorus is a biological
assay which determines the amount of phosphorus that an algal community
can withdraw from the sample.  Since bioassays are often tedious and more
variable than chemical methods, however, it would be quite advantageous
to relate the biologically determined available P to some fraction of the
sediment P as measured by chemical extraction.

     There is a growing body of research on chemical extraction procedures
to estimate bioavailable sediment P.  Much of the early work was done on
soils, with more recent studies on lake and stream sediments.  Differences
in these studies can be attributed, in part, to differences in the bio-
ogical and physicochemical characteristics of soils and sediments.   A major
treatment of the subject is not intended here.  However, several major
differences between soils and sediments are apparent.  First, because
of their fluvial transport, sediments are unstructured and generally more
fine-grained than the soils from which they were derived.  They tend to
be enriched in organic matter, and this together with their fine-grained
nature results in an enrichment of sediments with phosphate, hydrous
oxides of iron and some aluminum and, in some sediments, with carbonates.
Suspended stream sediments behave  much like their  soil precursors except
for their P enrichment (Green et_ aL,  1978).  Bottom sediments, on the
other hand, in both lakes and streams may be subjected to long periods
of anoxia with subsequent reduction and solubilization of iron (Patrick
and Mahapatra, 1968).  Phosphate release from suspended sediments is much
more similar to that from soil than from bottom sediment.s.  Discussion
of chemical extraction of sediment P must consider these significant
differences.

     Workers at Wisconsin (Chang and Jackson, 1957) began to look at
sequential chemical extraction to characterize soil P.  Their original
theory was that phosphorus in soil occurred as discrete chemical forms
which could be selectively removed by sequential chemical extraction.  This
theory of .discrete P forms in soil has been questioned by Bache (1963,
1964), Bauwin and Tyner (1957) and others.  A more prevalent view today
is that much of the inorganic P in soil is chemisorbed to a number of
reactive surfaces including iron and aluminum oxides and hydrous oxides,
amorphous alumino-silicates and carbonates, or occluded in the matrices
of a number of soil mineral forms.

     Major developments in the basic scheme proposed by Chang and Jackson


                                   282

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 (1957) have been accomplished by Williams and Walker  (1969 a and b);
Williams et al  (1971 a, b); Allan and Williams  (1978) for soils and lake
sediments.

     In recent years, Williams  (Williams et^ a\^, 1976  a, b; Allan and
Williams, 1978) has      simplified the scheme  for lake sediments even
further.  He proposed two  inorganic sediment-P  fractions:  non-apatite in-
organic phosphorus (NAIF)  extracted by citrate-dithionite-bicarbonate  (CDB),
and apatite-P extracted by HC1  or H2SO,.  Allan and Williams (1978) have
proposed that the NAIP fraction be considered bioavailable, based on
correlation of CDB extraction with the NTA extraction of Golterman  (1976)
which was found to estimate sediment P availability of Scenedesmus.  Arm-
strong et al (1979) have recently used NaOH with dilute sediment suspensions
to extract NAIP.  These procedures and others are summarized in Table 1.

     In order to obtain a  true  assessment of algal availability the method
must make use of the algae themselves as an indicator of the quantity and P
should be defined as that  quantity actually taken up  by the algae, rather
than the growth response under  test conditions.  It is therefore recommended
that an assessment methodology  actually measure the amount of P incor-
porated into the biomass of the test organism.

     On the other hand, a  chemical assessment technique is desirable from
the standpoint of relative ease and quickness of obtaining results.  These
are very important attributes if one is attempting to evaluate all the
tributary sources to one of the Great Lakes, for example.  It is therefore
necessary for future research to place equal emphasis on both chemical and
biological approaches to assessing P availability.  Even more important is the
need for future work to attempt to correlate the quantity and the rate of
production of biologically measured available P with  the chemical tests.  In
other words, every attempt should be made to find an operationally defined
chemical extraction which best estimates algal available phosphorus.

     The previous discussion indicates that there are two independent approaches
to measurement of sediment bioavailability:

     1.  Incubation with algae and correlation of algal uptake with chemical
or resin extraction (Golterman, 1976; Sagher ejt al_, 1975; Cowen and Lee,
1976 a, b; Dorich and Nelson, 1978)  which showed that NaOH was a good measure
of algal available sediment P.

     2.  Chemical extraction (fractionation) of soil and sediment phosphorus
with the underlying assumption that some "forms" of particulate P are more
available to algae than others  (Williams e^ _al, 1976b).   These assumptions
were based on studies which showed a low availability of apatite phosphate
(Golterman et al, 1969)  on the one hand, and others which indicated that,
terrestrial plants (crops)  at least,  got their "available" P from inorganic
forms associated with iron and aluminum minerals (Robertson et al, 1966).

     The concepts developed by these two approaches have been combined or
used singly to determine algal bioavailability of particulate P.   They
all assume that non-apatite inorganic P (NAIP) is available over time
and several methods are  given for NAIP measurement (Table 1).  Cowen and
Lee (1976 b)  considered resin extractable P to be short-term available
                                 283

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                       Table 1.   Summary of phosphorus  forms,  their biological  availability  and  methods  for  their  analysis.
                   Phosphorus Fractions and Forms
                                  Bioavailability
                                    Methods of Analysis
                                     References
ro
oo
                     Dissolved reactive P (DRP):
                     H2P04- and HP04=

                     Dissolved condensed P(DCP):
                     P-O-P bonds
                     Dissolved organic P (OOP):
                     bonds
Inorganic P
  Non-Apatite Inorganic P
  (NAIP):   P adsorbed on
  metal  hvdrous oxides (Fe, Al)
  Fe-and Al-P minerals,
  Ca-P (non-apatite)
                       Apatite
                     Organic P
                       Nucleic acids,
                       phospholipids,  inositol
                       phosphates,  others
                     Condensed P
                                                  Dissolved  Phosphorus

                                 Directly  available               Orthophosphate  in  filtrate*
                                 Converted  to  DRP  through
                                 fairly  rapid  hydrolysis
                                 Converted  to  DRP through
                                 biological mineralization;
                                 usually  slow  except  for
                                 "fresh"  plant tissue extracts
                                 and  huiran  and animal wastes
                                 Orthophosphate analysis
                                 following acid hydrolysis
                                 of filtrate*

                                 Difference between total
                                 dissolved P and sum of DRP
                                 and DCP in filtrate*
                                                                  Standard Methods (1975)
                                 Standard Methods (1975)
                                 Standard Methods (1975)
                                                                      Particulate  Phosphorus
Available through dissolution
or desorption of phosphate
when DRP concentration is low
due to dilution, biological
uptake or chemical
immobilization
                                 Essentially unavailable
                                 because  of slow dissolution
                                 of apatites

                                 Converted to DRP through
                                 biological mineralization;
                                 may be rapid for substantial
                                 fraction of fresh plant
                                 tissue or human and animal
                                 wastes;  slow for soil and
                                 sediment organic P

                                 Released from plant tissues
                                 at senescence and hydrolyzed
                                 to DRP.  Small fraction
                                 compared to organic P
NAIP has been extracted from
particulate material with: NaOH
(dilute sediment suspensions)
citrate-dithronite-bicarbonate
(CDB)
CDB/NaOH (sequential)
NaOH/CDB (sequential)
Anion resin
Aluminum Resin

HC1 extraction following
NAIP extraction
                                 Difference between total
                                 particulate P and inorganic
                                 particulate P
                                 Usually included as organic
                                 P unless hydrolysis is rapid
                                 and would then be extracted
                                 as NAIP
Williams et al_ (1980)

Williams et al (1976a)

Williams et al (1976b)
Logan et aJ_TT980)
Cowen and Lee (1976)
Huettl et al 0979)

Williams et al (1976a)
                                 Sommers et al (1972)
                      *Dissolved phosphate is defined as that P which is  not retained by a  0.45y dia.  filter (Standard Methods,  1975).

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with NaOH-P available over a long period of time (unspecified).   Logan
et a.1 (1979) assumed that NaOH-P (at an extractant/sediment ratio of
50~:T~rather than the wider ratios used by others) represented P that-
could be extracted by algae in the photic zone of lakes under aerobic con-
ditions, while the subsequent CDB extraction reflected P that might become
available under the reducing conditions found in the anoxic hypolimnion of
stratified  lakes.  These views should be considered when reviewing the bio-
availability data in the next section.


                BIOAVAILABILITY OF SEDIMENT PHOSPHORUS

     A large part of the research on sediment bioavailability has been
done on Great Lakes Basin soils and sediments and are, therefore, very
pertinent to this discussion.

     Sagher et al (1975) used bioassay and NaOH extraction to measure
bioavailability of Wisconsin lake sediments and found that 60 to 95%
of the sediment inorganic P (Pi) of noncalcareous and 60 to 85% of the
Pi of calcareous sediments were available.

     Cowen  and Lee (1976 a, b) used bioassay with resin and NaOH extrac-
tion to estimate bioavailability of urban storm runoff and tributary
sediments.  Resin and NaOH extraction of Madison, Wisconsin urban run-
off sediments gave mean values of 22-27% of total particulate phosphorus
(TPP) and 13-17% TPP, respectively.  Similar samples from Genesee River,
N.Y. urban  runoff gave mean values of 18-30% of TPP and 11-25% TPP for
NaOH and resin extraction.  Cowen and Lee (1976 b) also sampled tribu-
taries to Lake Ontario and found NaOH and resin extractable values of
13-18% TPP  and 6-17% TPP for samples taken at the mouth of the Genesee
River.  NaOH and resin extraction percentages of TPP were similar for
urban and rural sediments and were somewhat higher for Wisconsin than
New York sediments.  Lee et al (1980) have recently proposed that a value
of  20% of TPP  is a  reasonable  estimate  of bioavailability  of Great Lakes
tributary sediments.

     Logan  et al (1979) used sequential extraction with NaOH and CDB  to
estimate bioavailability of 66 suspended sediment samples from 36 tribu-
taries in the Lake Erie drainage basin.  A summary of their data expressed
as percentage of Pi is given in Table 2.  Their data showed that New York
tributaries had lower bioavailability than those from Michigan and Ohio,
a finding similar to that of Cowen and Lee (1976 b).  They attributed
this difference to greater stream-bank erosion and coarser-grain nature
of the New  York samples.

     Armstrong et al (1979) used resin and NaOH extraction to estimate
the availability of stream sediments in five tributaries to the Great
Lakes; they also studied recessional shoreline soils.  Resin P ranged
from 7-19%  of TPP for the tributary samples and NaOH-P was 14-37% of TPP.
Recessional soil samples were 2-10% of TPP and 1-10% of TPP for resin and
NaOH extractions, respectively.  Armstrong et al (1979) also extracted
individual  particle size fractions and found that there-were slightly
higher values for resin-P and NaOH-P in the clay fraction expressed as percent of TI

     Dorich and Nelson  (1978) used algal bioassay and NH^F and NaOH sequential


                                  285

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Table 2.  Percent Unavailability of Sediment-P* as Estimated by Sequential
Chemical Extraction with NaOH and CDB (Logan et al , 1979).
                        NaOH-P     CDB-P    (NaOH + CDB)-P
Michigan
Western Ohio
Eastern Ohio
New York
30.0
41.9
32.8
14.0
45.0
35.9
55.8
28.5
75.0
77.8
88.6
42.5
     * Expressed as percent of total sediment inorganic phosphorus.

extraction to analyze stream sediments from Black Creek in northeastern
Indiana, an agricultural watershed.  They found that about 20% of the TPP
was available with somewhat higher values for the Maumee River at the junc-
tion with Black Creek.

     Finally, Thomas (unpublished) reported that samples from Canadian
tributaries to the Great Lakes contained about 20-40% of TPP as NAIP,
which Williams et al (1976 b) consider to be available in the long term.

     Considering these data collectively, it would appear that the value
of 20% of TPP proposed by Lee _et^ _§JL(1980) is not unreasonable for Great
Lakes sediments, with a range of 10-50%.  Sediments from tributaries
draining into the eastern basin of Lake Erie (Logan et al, 1979) and Lake
Ontario (Cowen and Lee, 1976 b) appear to have lower availabilities than
those from the Corn Belt region.
                  AVAILABILITY OF OTHER PHOSPHORUS SOURCES

Precipitation Phosphorus

     Lee e^t a.1 (1980) reviewed the literature on P in precipitation. There
was only one study (Cowen and Lee, 1976 b) which used bioassay to study
availability of precipitation P, and it showed that ^10% of the total P
in Madison, Wisconsin snow samples were bioavailable.  The great majority
of precipitation studies showed that ~50% of the total P is soluble
inorganic P although the values can range from 7-100%.  Assuming that
soluble inorganic P is 100% available (an assumption that may not be true,
as discussed in the next section) then about 50% of precipitation phosphate
is available.

Soluble Phosphorus

     Several investigators (Rigler 1966, 1968; Lean 1963 a, b; Dorich and
Nelson 1978) have found that soluble inorganic P (SIP)  is not 100% available,
while Walton and Lee (1972) found that SIP was essentially all available
using standard bioassay procedures.  The problem lies in the analytical
method used to measure SIP.  This is usually done by filtering the sample
through 0.45 u pore diameter membrane filters and analyzing the filtrate
as reduced phosphomolybdate.  As Lee et al (1980) have pointed out, the
acid molybdate may react with arsenic or colloidal material containing P
and overestimate the true SIP.  This is especially of concern with the low

                                  286

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SIP concentrations normally found in lakes, but the error is much lower
for the concentrations found in tributaries or wastewater discharges and
these values can probably be considered to be 100% available.
               THE IMPACT OF BIOAVAILABILITY OF P SOURCES
              ON A MANAGEMENT STRATEGY FOR THE GREAT LAKES

     The Lake Erie Management Study in their Phase II Methodology Report
(1979) estimated through Universal Soil Loss Equation (USLE)  analysis that
a maximum adoption of conservation tillage practices by basin farmers on
suitable soils could reduce soil loss in the basin by ^ 70%.   A recent review
of conservation tillage research studies by Logan (1980) has  shown that
conservation tillage is only 90% as effective in reducing total particulate
phosphorus (TPP) loads as in reducing soil loss.  That is, if soil loss is
reduced 70% by conservation tillage, TPP will be reduced by 63%.  Logan
(1980) also showed that conservation tillage increased or had little effect
on soluble P loads.  The Lake Erie Management Study (1979) showed that, if
point source phosphorus discharges to Lake Erie are reduced by achieving a
1.0 mgP/1 effluent standard, this maximum adoption of conservation tillage
would almost achieve the target annual load of 11,000 metric  tons of P con-
sidered necessary to eliminate anoxia in the Central Basin of the lake.
Table 3 gives the various sources of P entering the lake before and after
adopting conservation tillage in terms of total P and available P.  The point
source loads remaining after reduction to the 1.0 mgP/1 effluent standard
is separated into those loads which are discharged directly into the lake
(e.g. Toledo, Cleveland, etc.) and those which discharge into Lake Erie
Basin tributaries (e.g. Fort Wayne, Defiance, etc.).  The direct discharge
effluent P is assumed to be 75% available based on the bioassay work of
DePinto et al (1980), while the tributary point sources are assumed to be
so mixed with the tributary water and sediment that they have the same
availability as rural diffuse loads (Table 3).  The rural diffuse load is
assumed to be 80% particulate and 20% soluble as shown by tributary monitoring,
and the soluble load is assumed to be 100% available.   The particulate rural
diffuse load is assumed to be 20 and 40% available, a range found by Logan
et al (1979) for Lake Erie tributary suspended sediments.  The urban diffuse
loads, the upper lakes loads and the tributary point source loads are all
assumed to be 80% particulate and 20% soluble, with the soluble load 100%
available and the particulate P 30% available (mean of the 20 and 40% values
for rural diffuse particulate P.)

     Table 3 shows that conservation tillage would reduce the total P load
to 11,404 metric tons, close to the target load of 11,000 tons, a 26.5%
reduction.  In terms of available P, however, the reduction is only 9.7 to
16.6%, depending on the percent availability assumed for particulate P.
The data (Table 3) also show that the residual direct point source load and
the soluble rural diffuse load contribute a major portion of  the available P
load before or after adoption of conservation tillage.

     Present lake models (Bierman, 1980) do not adequately account for
varying availability of P sources, and therefore, there is no way to deter-
mine an available P target load for Lake Erie or other Great  Lakes.  However,
it is obvious that response of algae to soluble P must be different than to
                                   287

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        Table 3.  Total and available phosphorus loads (metric tons) to Lake Erie before and after adoption of
                  conservation tillage practices.
Rural Diffuse





Before
After

Point f
Upper
Lakes3 K Atmospheric c Particulate*"
Direct Tributary3 20% 40%
Total P
1080 2455 617 1119 6610 6610
1080 2455 617 1119 2496 2496

Total Load
Urban*
Soluble Diffuse
20% 40%

1530 1570 15518 15518
1530 1570 11404 (26. 5%) d 11404 (26. 5%)d
Objective = 11,000
ro
Before

After
475

475
1841

1841
272

272
        Available P

560      1132     2264     1530       691

560       499      998     1530       691

                           Objective = ?
                                                                                                    6501
7633
                                                                                                    5868 (9.7%)d  6367 (16.6%)d
        a   Assumption:  80% of the total load is particulate and 30% of the particulate load is available; 100% of the
                         soluble load is assumed to be available.

        b   Assumption:  direct discharge of sewage effluent to the lake is 75% available (DePinto et al, 1980).

        c   Assumption:  short term availability of rural diffuse sediment P is 20% and long term availability is
                         40% (Logan et al, 1979).

        d   Percent reduction with conservation tillage.

        e   Atmospheric P sources are assumed to be 50% available.

        f   Residual point sources after reduction to 1 mgP/1.

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particulate P sources which may settle out of the photic zone before they
can be completely utilized.  Phosphorus control strategies for deep lakes
with little sediment resuspension or lake overturn must emphasize soluble
P sources more than for shallower lakes where sediments are continuously
resuspended and lake overturn can bring to the surface P released from
bottom sediments.  If the emphasis is to be placed equally on sediment as
well as soluble P sources (e.g. for Western and Central Lake Erie) then
erosion control by conservation tillage merits equal consideration with
point source reduction.  If, however, soluble P loads are the most important,
then control of direct point sources should receive the most attention.  In
addition, agricultural practices which control soluble P losses would need
to be emphasized.  These would include fertilizer management (Oloya and
Logan, 1980) and livestock waste management (Porter, 1975).

     Excluded from the phosphorus input list in Table 3 is phosphorus
contributed from shoreline erosion.  The total P load from shoreline erosion
is more than half of the entire P load to Lake Erie from all other sources
(Thomas e_t al, 1980), but shoreline sediments have an availability < 5%.
While even a low availability of 5% still gives a large available P load, its
impact is likely to be in the near-shore zone and not in the mid-lake area
for which the target loads were developed.
                            CONCLUSIONS

     Phosphorus exists in soluble and particulate forms, and research has
shown that these forms vary in availability to algae from a low of 5% or
less for subsoil materials (detached and transported during streambank
erosion and lake shoreline erosion) to essentially 100% available for soluble
(dissolved) inorganic P.

     Phosphate availability has been determined by algae biassay as well as
chemical extraction techniques, and depending on the method used, may reflect
total availability or short-term availability.  While these methods all measure
the capacity of sediment to release P to algae, few studies have investigated
the rate at which sediment-P is made available.  A knowledge of P release
kinetics is important in determining the positional availability of P from
sediments which enter lakes and are subjected to varying rates of settling
and resuspension.

     Phosphorus management strategies must consider the bioavailability of
the various P sources as well as the positional availability of particulate
P as determined by the sedimentation and resuspension characteristics of the
receiving lake.  Deep lakes will respond more to control of soluble P sources
than to sediment-P control, while in shallow lakes, algae may obtain a large
percentage of bioavailable P from sediments, and control of sediment loads by
controlling erosion on basin soils might be more effective.
                                  289

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                                   REFERENCES


 1.  Allan, R.J. and J..D.H. Williams.  1978.  Trophic status related to sediment
     chemistry of Canadian Prairie Lakes.  J. Environ. Qual. 7:  99-106.

 2.  Armstrong, D.E., J.R. Perry, and D. Flatness.  1979.  Availability of pollutants
     associated with suspended or settled river sediments, which gain access to
     the Great Lakes.  Final Report.  Wisconsin Water Resources Center, Madison.

 3.  Bache.  B. W.  1963.  Aluminum and iron phosphate studies relating to soils:
     1. Soil Sci. 14:113-123.

 4.  Bache, B.W.  1964.  Aluminum and iron phosphate studies relating to soils:
     2. Soil Sci. 15:110-116.

 5.  Bauwin, G.R. and E.H. Tyner.  1957. The nature of reductant soluble phosphorus
     in soils and soil concretions.  Soil Sci. Soc. Amer. Proc. 21:250-257.

 6.  Bierman, V.J.  1980.  A comparison of models developed for phosphorus manage-
     ment in the Great Lakes.  In Phosphorus Management strategies for Lakes.
     R. C. Loehr, C. S. Martin, W. Rast, Eds. Ann Arbor ^cience.


 7.  Chang, S.C. and M.L. Jackson.  1957.  Fractionation of soil phosphorus.
     Soil Sci.  84:133-134.

 8.  Corps of Engineers, Buffalo District.   1979.  Lake Erie Management Study
     Methodology Report.  Buffalo, N.Y.  146 pages.

 9.  Cowen, W.F. and G.F. Lee.  1976a.  Algal nutrient availability and limitation
     in Lake Ontario tributary waters.   Ecological Research Series.  EPA-600/3-76-094a.

10.  Cowen, W.F. and G.F. Lee.  1976b.   Phosphorus availability in particulate
     materials transported by urban runoff.   J.  WPCF.  48:580-591.

12.  Dorich, R.A. and D.W. Nelson.  1978.  Algal availability of soluble and sediment
     phosphorus in drainage water of the Black Creek watershed.  Unpublished report.
     Purdue Agric. Exp. Sta.

13.  Golterman, H.L.  1976.  Sediments  as a source of phosphorus for algae growth.
     Jin H. L. Golterman (Ed.) Interactions between sediments and freshwater.  Proc.
     51L-UNESCO Conf. Junk and Pudoc, The Hague, Netherlands.

14.  Golterman, H.L.  1977.  Forms and  sediment associations of nutrients, pesticides
     and metals.  Nutrients-P.  In Proc. Workshop on Fluvial Transport of Sediment-
     associated Nutrients and Contaminants.   H.  Shear, Ed.  IJC-PLUARG, Windsor,
     Ontario.

15.  Golterman, H.L., C.C. Bakels and J. Jakobs-Mogelin.   1969.  Availability
     of mud phosophates for growth of algae.  Verh. Int.  Verein. Limnol.  17:467-479.

16.  Green, D.B., T.J.  Logan and N.E. Smeck.  1978.  Phosphate adsorption-
     desorption characteristics of suspended sediments in the Maumee River
     Basin of Ohio.   J. Environ. Qual.  7:208-212.


                                      290

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17.   Huettl, P.J.,  R.C.  Wendt and R.B.  Corey.   1979.   Prediction of algal-available
     phosphorus in runoff suspensions.   J.  Environ. Qual.  8:130-132.

18.   Lean,  D.R.S.  1973a. Phosphorus dynamics  in lake water.   Science 179:  678-679.

19.   Lean,  D.R.S.  1973b.  Movements of phosphorus between its biologically impor-
     tant forms in freshwater.  J. Fish Res.  Board Can.  30:1525-1536.

20.   Lee, G.F., R.A.  Jones and W. Rast.  1980.   Availability of phosphorus  to
     phytoplankton and its implications for phosphorus management strategies.
     In Phosphorus Mangement Strategies for Lakes. R. C.  Loehr, C.S.  Martin,
     W. Rast.  Eds.  Ann Arbor Science.

21.   Logan, T.J.  1978.   Available phosphorus  levels in Lake Erie Basin soils.
     LEWMS Final Technical Report.  Corps of Engineers,  Buffalo District, Buffalo,
     N.Y.

22.   Logan, T.  J.  1980.  The effects of conservation tillage on phosphate  trans-
     port from agricultural land.  Lake Erie Management Study.  Technical Report
     Series.  Corps of Engineers, Buffalo District, Buffalo,  N.Y.

23.   Logan, T.J., T.O. Oloya and S.M. Yaksich.   1979.  Phosphate characteristics
     and bioavailability of suspended sediments from streams draining into  Lake
     Erie.   J.  Great Lakes Res. 5:112-123.

24.   Oloya, T.  0. and T. J. Logan.  1980.  Phosphate desorption from soils  and
     sediments with varying levels of extractable phosphate.   J. Environ. Qual.
     9:526-531.

25.   Patrick, W.H. and I.C. Mahapatra.   1978.   Transformation and availability
     of nitrogen and phosphorus in waterlogged soils.  Advan. Agron.  20:323-359.

26.   Porter, K.S.  1975.  Nitrogen and phosphorus, food production, waste and
     the environment.  Ann Arbor Science, Ann Arbor,  Mich. 372 pages.

27.   Rigler, F.H.  1966.  Radiobiological analysis of inorganic phosphorus  in
     lake water.  Tech.  Internat. Verein. Limnol.  16:456-470.

28.   Rigler, F.H.  1968.  Further observations inconsistent with the hypothesis
     that the molybdenum blue method measures  orthophosphate in late waters .  Limnol
     Oceanogr.   13:7-13.

29.   Robertson, W.K., L.G. Thompson, Jr. and C.E. Button.   1966.  Availability  and
     fractionation of residual P in soils high in aluminum and iron.   Soil  Sci.
     Soc. Amer. Proc. 30:446-451.

30.   Sagher, A., R.F. Harris, and D.E.  Armstrong.  1975.   Availability of sediment
     phosphorus to microorganisms.  Univ. of Wisconsin Water Res. Cent. Tech.
     Report WIG WRC 75-01.  Wisconsin.

31.   Sommers, L.E., R.F. Harris, J.D.L. Williams, D.E. Armstrong and J.K. Syers.
     1970.   Determination of total organic phosphorus in lake sediments.  Limnol.
     Oceanog.  15:301-304.

32.   Standard methods for the examination of water and wastewater.  13th Ed. 1975.
     American Public Health Assoc. Washington,  D.C.
                                      291

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34.  Verhoff, F.H.,  M.  Heffner and W.A.  Sack.   1978.   Measurement  of  availability
     rate for total  phosphorus from river waters.   Final Report.   LEWMS,  Corps of
     Engineers,  Buffalo,  N.Y.

35.  Walton,  C.P.  and  G.F.  Lee.   1972.   A biological evaluation of the molybdenum
     blue method for orthophosphate analysis.   Tech.  Internat.  Verein.  Limnol.
     18:676-684.

36.  Williams, J.D.H.  J.K.  Syers, and T.W. Walker.  1967.   Fractionation of
     soil inorganic  phosphate  by a modification of Chang and Jackson's  procedure.
     Soil Sci. Amer. Proc.  31:736-739.

37.  Williams, J.D.H.,  J.M.  Jaquet and R.L. Thomas.  1976a.   Forms of phosphorus
     in surficial sediments  of Lake Erie.  J.  Fish. Res. Board  Can. 33:413-429.

38.  Williams, J.D.H.,  T.P.  Murphy and T. Mayer.  1976b.  Rates of accumulation
     of phosphorus forms  in  Lake Erie sediments.  J.  Fish.  Res. Board Can.  33:430-439.

39.  Williams, J.D.H.,  J.K.  Syers, R.F.  Harris, and D.E. Armstrong. 1971a.   Frac-
     tionation of inorganic  phosphate in calcareous lake sediments.  Soil Sci. Soc.
     Amer. Proc. 35:250-255.

40.  Williams   J.D.H., J.K. Syers, D.E. Armstrong, and R.F. Harris.  1971b.  Charac-
     terization of inorganic phosphate in noncalcareous lake sediment.   Soil Sci.
     Soc. Amer.  Proc. 35:556-561.

41.  Williams, J.D.H. nad T.W. Walker.  1969a.  Fractionation of phosphate in a
     maturity sequence of New Zealand basaltic soil profiles:   1.   Soil Sci.
     107:22-30.

42.  Williams, J.D.H. and T.W. Walker.  1969b.  Fractionation of phosphate
     in a maturity sequence of New Zealand basaltic soil profiles;  2.  Soil
     Sci. 107:213-219.
                                       292

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               WATER MONITORING PROGRAM - PLANNING FOR 1981
                           WILLIAM H. SANDERS III
                       DIRECTOR S&A DIVISION REGION V
Regardless of the control program we are attempting to implement, the
underlying question is to what extent does a remedial program—be it AWT/
AST treatment facilitis, best management practices for NPDS control, etc.-
the question remains: to what extent does the program correct the problem
by resulting in improved water quality.  That is a basic question to ask,
yet a most complex and difficult one to answer.   All of the programs you
have heard about and discussed at this seminar are focused upon that
ultimate objective of improving water quality.  Yet we have found that
our tools for assessing changes in water quality, particularly in being
able to definitively associate those changes with remedial programs, have
been lacking.  It is in order to fill that informational void that the
agency is redefining and refining, our water monitoring programs.

Develoment of the Region V Monitoring Planning for 1981 is based on
recognition of the re-newed emphasis on the human health aspects of water
pollution control.  The driving force behind this concern for protection
of health is the awareness of the scope and potential hazard of the
toxic wastes entering the nations's waters through industrial processess,
materials handling and waste disposal.  Because  of the large number of
sources of all description concentrated in Region V, the problem of
identifying and quantifying the impact of toxic  and hazardous wastes is
of particular concern.  We have recently begun an assessment of the
adequacy of the existing monitoring networks and programs to provide a
data base for use in identifying problem areas throughout the Region.
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While the importance of the control of toxic and hazardous wastes cannot
be overemphasized, it is also intended to maintain the capability to
assess water quality for the more traditional pollutants.  For this reason,
the assessment of existing monitoring against current needs is best made
with repect to the basic program as described in the "Basic Water Monitoring
Program", U.S. EPA Standing Work Group on Water Monitoring, (EPA 440/9-76-025,
1977).

Given the adequacy of the basic program and the availability of resources,
a re-definition of the Federal and State activities may be necessary
to monitor water quality, particularly to ensure that the Region waters
are free of the more harmful health related pollutants.

2.   HIGHLIGHTS FROM THE REVIEW

From the assessments of the state programs, it is obvious that the strategy
envisioned in the Basic Water Monitoring Program has not had complete
acceptance.  As a result, the program has had only marginal success in
developing a data base useful for managers in carrying out pollution
control programs.  An important element integral to the strategy in the
basic program is the need to enter monitoring data into STORET.  The
usefulness of the data is dependent on its availability to users at all
levels.  However, the only parameter in STORET in sufficent quantities
for comparative analysis was dissolved oxygen.  An even more glaring
omission is the paucity of information related to toxics xvhich is available
for use.

Based on state acceptance in their own programs, most parts of the basic
program are considered viable and should be retained.  However, several
parts of the program have had little or no state support.
                                 294

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Portions of the ambient monitoring program have received wide acceptance,
primarily because the National Ambient Monitoring Stations are a subset
of existing state ambient networks.  These are fixed stations intended to
provide trend information.  However each state has a much larger ambient
network designed to gather trend data that is not covered by the basic
network and to provide a measure of the effectiveness of pollution abatement
programs.  The latter may not be the best use of fixed station monitoring.

Intensive surveys should be used for multiple purposes rather than to
support a single program.  They should be used in identifying or quantifying
problems related to toxics and NPDES permitting, waste load allocation
and stream model development and verification.  However, resources are not
available to routinely carry out all of these surveys.  This is particularly
true for toxics.  Efforts spent on fixed station monitoring competes for
resources'which may be better spent on intensive surveys.  The ambient program
will be reviewed jointly with the state agencies, with the intent to
free-up more resources for intensive survey purposes.

The toxic monitoring needs which are surfacing at the present time far
outstrip the toxic portion of the basic program.  Recognizing that the
basic program was introduced in 1977,  and reflects the known need for
toxics data at that time.  That need is minimal when compared to current
needs.  Since most of the states have  been unable to meet the basic
requirements, the program requires significant restructuring accompanied
by a large shift in resources and initial capital investment, particularly
to develop laboratory capabilities.

By including toxic monitoring in the ambient program as described in the
basic document,  trend data will be developed over time.   Of more immediate
                               295

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need, toxic monitoring should be made part of intensive surveys conducted
near known or suspectd dischargers in support of the permitting program.
As in the ambient monitoring, fish will be used as the sample medium.
The use of fish is chosen as the best indicator of stream quality since
they are an excellent bio-accumulator of toxic pollutants.  The analysis
of fish tissue shall be broad scan and include the parameters listed in
the basic document.

Having discussed several of the issues we found in assessing existing
state monitoring programs, I now move to brief highlights of a strategy
under active consideration for the next five years that will accommondate
non-point sources as well as point sources of pollution.

3.   WATER MONITORING STRATEGY

It is the intent in Region V to oversee a water monitoring program which
will provide program managers with a valid data base which is responsive
to their needs.  For the next five years, the most pressing concern  is
the protection of the public  health through control of toxic and hazardous
sources of pollution.  This strategy is intended to enhance the data base
for use in the important decisions on identificaiton and  control of  this
type of pollution.  It is also intended that the more  traditional
pollutants, those which have potenital adverse impact  on  public health,
are not to be  ignored.  As a result, the Basic Water Monitoring Program
provides the basis of this strategy.  The components of the water monitoring
program are:   ambient monitoring  (including  toxic monitoring), effluent
monitoring, intensive surveys, biological monitoring,  quality assurance
and  STORET.
                                  296

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AMBIENT WATER MONITORING

The States should fully implement the basic water monitoring network,
including sampling for fish tissue, sediment and water once yearly at
all "core" stations.  Where toxics are found in the fish tissue, bottom
sediments should then be analyzed.  If toxics are found in the sediment
samples, water column samples should be analyzed for the toxic parameters.
The States should make a thorough evaluation of their own ambient water
monitoring stations to eliminate any duplication or any stations that are
not vital to establishing trend data.  All stations in excess of those
needed for trend purposes should be discontinued.  The intent of this re-
evaluation is to reduce resource needs in this activity to devote more
time to intensive surveys and toxic monitoring.

All States in Region V must develop full field and laboratory capabilities
for toxic monitoring at all trend stations using fish as the sample medium.
Fish tissue analysis shall be broad scan and include the priority pollut-
ants.  This capability will also be used to support the effluent monitoring
(permitting program and intensive survey program).

EFFLUENT MONITORING

The States should concentrate their compliance monitoring efforts on the
re-issuance of permits with special emphasis on the control of toxicants.
Consistent with the basic monitoring program, all major dischargers shall
be inspected annually to determine compliance status.  Known toxic sources
shall be first priority for compliance sampling; however, this in no way
relieves the states of their responsibility to evaluate all majors.
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INTENSIVE SURVEYS

The States should revise their monitoring strategy to reflect higher
priority for the use of intensive surveys in such areas as toxic pollu-
tants, water-quality limited streams and to detertninne treatment levels
to meet water quality standards.   To assure that the objectives of the
Section 106 and the basic water monitoring programs are met, more re-
sources and emphasis should be devoted to intensive surveys as a means
of verifying the usefulness of pollution control strategies.

BIOLOGICAL MONITORING

The proposed Biological Monitoring Program as described in the basic
document shall be revised so that each state shall be required to imple-
ment biological studies as part of intensive surveys, where such surveys
are conducted near known or suspected toxic sources.

QUALITY ASSURANCE

To assure the validity of the data generated through this water quality
program, the quality assurance policy as established in Region V will be
followed.  The first priority in the Region V quality assurance policy
is to establish and implement a plan to define and quantitate the end
product-data quality.  This includes all data generated by the Federal
and State/local agencies.  To ensure that this policy is carried out,
all State/local agency quality assurance programs must be approved by
the Region V, Quality Assurance Office.  To facilitate this documenta-
tion, peer reviews of state plans shall be completed in the other
Region V states.  This review shall be coordinated by the Region V
Quality Assurance Office.
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STORE!
The states should enter all ambient quality assured data into STORET
within 90 days after sample collection and analysis.  Additionally, the
states should assess the ambient water quality data in the STORET system
in order to determine ambient water quality conditions and trends.  This
assessment should be forwarded to EPA/State program managers in order to
impact toxic source identification, Section 208 planning, wasteload
allocations/intensive surveys and state EPA agreements.  To improve STORET
in Region V, use of data management and interpretation tools such as
summaries and trends on a quarterly basis should be made Region policy.
Routine use of these tools will result in an improved data file.

Finally, the intent of this effort will be to provide decision makers
data of known precision and accuracy that will allow for an evaluation
of program effectiveness.  That is a tall order, but is key to our ability
to making those critical decisions on which programs to focus upon in
the future.
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   CONSERVATION TILLAGE PRACTICES TO CONTROL AGRICULTURAL POLLUTION

                                  by

                    J.  P. Crumrine and D.  U. Wurm*

     When shopping around for point and non-point source control mea-
sures, you soon find yourself asking questions as if you were shopping
at a local supermarket.  Which product or control measure does the
best job, and what is the cost of each?  In other words, how do I get
the most for my money?

     While the Honey Creek Watershed Project was not designed specifi-
cally to answer these questions, as a nonpoint source control demon-
stration program, it does provide valuable information regarding the
effectiveness and implementation costs of control practices for a
96000 acre (38000 hectare) agricultural watershed in the Lake Erie
Basin of north central  Ohio.

     The Honey Creek Proj ect, now in its second year of a 3-year ef-
fort, is managed by local Soil and Water Conservation Districts, but
funded by the U. S. Army Corps of Engineers as part of their Lake Erie
Wastewater Management Study (1).  Purpose of the Project is to see how
farmers and local agricultural agency personnel respond to the need
for improved water quality and to demonstrate "best management prac-
tices," that would contribute to improved Lake Erie water quality,
particularly conservation tillage.  It is through the implementation
of conservation tillage practices (2), coupled with data from previous
Army Corps studies (3)  that we may gain insight as to how well the
practices reduce erosion or phosphorus transport and practice costs.


                          CONSERVATION TILLAGE

     First, what is conservation tillage?  Soil Conservation Service
in Ohio defines conservation tillage as a "method of working the land
leaving crop residues on the surface to protect the soil from the
erosive forces of wind and rain." (4)  For the Honey Creek Project
conservation tillage has been defined as any tillage system that
leaves a minimum of 1000 pounds (454 kilograms) of previous crop res-
idue on the soil surface at planting.  The ultimate conservation til-
lage system is "no-till" where virtually all previous crop residue
remains on the surface at planting, normally 4000 to 6000 pounds
(1800 to 2700 kilograms) expressed as corn residue equivalent.  Til-
lage systems incorporating a portion of previous crop residue but
having more than 1000 pounds (454 kilograms) on the surface at plant-
ing time are described as "reduced" tillage systems.  Table 1 gives a
comparison of tillage systems based on the amount of previous crop
residue left on the soil surface at planting, showing tillage opera-
tions that might typically occur in each.

*Project Manager and Project Conservationist, Honey Creek Watershed
Project, Crawford, Huron, and Seneca Counties, Tiffin, Ohio
                                  301

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Table 1.  Comparison of Tillage Systems by Amounts of Previous Crop
          Residue on Soil Surface at Planting and by Mechanical Op-
          erations That Might Typically Occur in Each.
                                        Conservation Tillage
 Conventional Tillage       Reduced Tillage           No-till

 Spring fertilize           Spring fertilize          Spring fertilize
 Plow                       Chisel plow               Plant
 Disk - 1                   Disk                      Spray - 1
 Disk - 2                   Plow                      Spray - 2
 Level                      Spray                     Combine
 Plant                      Combine
 Spray
 Cultivate - 1
 Cultivate - 2
 Combine
 0 to 1000 pounds                       1000 pounds plus
 (454 kg) residue                       (454 kg)  residue
 at planting                            at planting
                     EROSION,  PHOSPHORUS REDUCTIONS

     With an idea now of what conservation tillage is, how well do the
various practices work?  Do they reduce erosion and phosphorus loss and
if so by how much?  For 10-15 acre (4-6 hectare) demonstration plots in
the Honey Creek watershed, on those soils having yield responses to no-
till equal to or greater than conventional tillage either naturally or
with artificial drainage, soil loss estimates using the Universal Soil
Loss Equation showed that reduced tillage systems on the average in
1979 decreased erosion rates from 7.1 to 4.5 T/Ac/Yr (16 to 10 MT/Ha/
Yr) or 40 percent over the conventional fall plow system.  On the same
soils, but different fields, no-till decreased erosion rates from 6.9
to 1.4 T/Ac/Yr (16 to 3 MT/Ha/Yr) or 76 percent.

     With respect to phosphorus yield reductions, the Lake Erie Waste-
water Study Methodology report (3) assumes that application of conser-
vation tillage practices will be from 60 to 90 percent effective in re-
ducing phosphorus transport relative to reduction of erosion.  These
ranges of possible reductions are based on the fact that most phosphor-
us moves attached to the clay fraction of river sediment loads (5) (6) ,
and that while reduced tillage practices may increase the proportion of
clay sized particles in runoff, significant reductions in phosphorus
transport can still occur (7) (8) (9).

     For a relative effectiveness then of 75 percent, reduced tillage
systems in the Honey Creek watershed would potentially decrease phos-
phorus transport from a present watershed condition rate of 0.84 Kg/
Ha/Yr to 0.59 Kg/Ha/Yr or by 30 percent.  No-till would decrease phos-
phorus transport from 0.84 to 0.36 Kg/Ha/Yr or by 57 percent.
                                  302

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 Table  2.  Average Effectiveness of Conservation Tillage  Systems  in Re-
          ducing Erosion Over Conventional Fall Plow System, T/Ac/Yr
          (MT/Ha/Yr), and Phosphorus Transport, Kg/Ha/Yr, for Demon-
          stration Plots Within the Honey Creek Watershed.

                          EROSION REDUCTION
   Conventional   	Conservation Tillage	
   Fall Plow         Reduced Tillage3	No-till	
  T/Ac/Tr  (MI/Ha) T/Ac/Yr (MT/Ha) % reduced  T/Ac/Yr (MT/Ha) % reduced
   7.1    (16)     4.3    (10)      40
   6.9    (16)                                1.4    (3)       76
                        PHOSPHORUS REDUCTION6
          Kg/Ha/Yr  Kg/Ha/Yr  % reduced  Kg/Ha/Yr  % reduced

            0.84      0.59        30       0.36        57
      a.  Chisel plow, disk field cultivate, etc.
      b.  At relative effectiveness of 75%.
 COSTS OF IMPLEMENTING CONSERVATION TILLAGE IN A DEMONSTRATION PROJECT

     Now that we know what the various tillage "products" will do, how
much do they cost?  Actually costs of implementing practices can vary
considerably, from practically nothing to more than $100 per acre ($250
per hectare) depending on current state of the economy, abundance of
farm fuel supplies, past emphasis on tillage programs within a water-
shed, cultural factors and the rate at which adoption is desired.
Costs to encourage implementation can be grouped by increasing costs to
the general public as follows:

     1.  Information-education programs,
     2.  Information-education plus technical assistance, and
     3.  Information-education, technical assistance plus monetary
              incentives.

     In the Honey Creek watershed the highest cost incentive approach
was used at approximately the following annual costs:

     Information-education:                                $25,000
     Technical assistance:                                 $35,000
     Landowner payments for tillage demonstration plots:   $25,000
          and
     Special Agricultural Conservation Program cost share
          payments:                                        $12,000

     In Table 3 calculations relating only landowner payments, either
demonstration or cost share, to acre accomplishment show that applica-
tion rates ranged from a high of $125 per acre ($312 per hectare) for
no-till in 1979 to a low of $24 per acre ($60 per hectare)  for reduced
                                  303

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tillage in 1980.  Note, however, that when acre accomplishments done
without benefit of monetary assistance are included in the calcula-
tions, acre costs are lowered considerably, especially during the sec-
ond year of the Project, 1980, where no-till cost $15 per acre ($37
per hectare) and reduced tillage, $5 per acre ($13 per hectare).   In
Honey Creek, benefits like these were due almost entirely to high
quality on-the-farm technical assistance.

Table 3.  Payments Made to Landowners for Implementing Conservation
          Tillage and Acres (Hectares) Treated by Practice During the
          First Two Years of the Honey Creek Watershed Project.

          Demonstration $/Ac Special ACP $/Ac Est. Other Summary  $/Ac
             Project  ($/Ha)   Project ($/Ha) Acres (Ha)  Effort($/Ha)
                                 1979
 No-till $    17500     125      7117     28      -       24617   35
  Ac(Ha)     140(56)   (312)   253(101)  (70)  300(120)  693(277)(89)
Reduced
Tillage $
Ac (Ha)

10000
116(46)

86
(217)

2170
74(30)

29
(72)
 No-till $
  Ac (Ha)

 Reduced
 Tillage $
  Ac(Ha)
 17300
216(86)
  2200
 28(11)
  80
(200)
  80
(200)
  1980
 11589
460(184)
  1478
 65(25)
                                               300(120)
 25
(63)  1300(520)
                                             12170   25
                                            490(196)(62)
 28889   15
1976(790X37)
 24      -        3678    5
(59)   600(240)   690(276)(13)
     Application costs per acre don't really tell the whole story,
though, unless, of course, you are an expert at comparing apples with
oranges.   You might be able to compare such fruits in a supermarket,
but not when shopping for point or non-point control practices.   You
really need to know how much it costs to keep a ton of soil or kilo-
gram of phosphorus in a field rather than in a lake or stream.  Prac-
tice effectiveness data from Table 2 plus incentive payment data from
Table 3 provide one way of determining cost effectiveness of conserva-
tion tillage systems in reducing erosion (dollars/ton) and phosphorus
yield (dollars/kilogram).
                          COSTS PER TON OF SOIL

     In Table 4, calculations using this approach show that costs for
keeping a ton of soil in place ranged from a high of $31 per ton ($34
per metric ton) for reduced tillage demonstration systems^in 1979 to a
low of $5 per ton ($6 per metric ton) for no-till done with ACP cost
share funds in 1979 and 1980.  When acre accomplishments done without
benefit of monetary assistance are included in the calculations, costs
are in the $2 to $9 per ton ($2 to $10 per metric ton) range, quite
                                  304

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reasonable considering the nutrient value alone of a ton of soil is in
the neighborhood of $8.

Table 4.  Cost Effectiveness of Conservation Tillage Systems in Reduc-
          ing Erosion, $/T/'(MT), and in Reducing Phosphorus Yield,
          $/Hg, During the First Two Years of the Honey Creek Water-
          shed Project.  Note:  1979 Erosion, Phosphorus Reduction Data
          of Table 2 Applied to Both 1979 and 1980 Cost Acreage Data of
          Table 3.
           Demonstration    Special ACP        Other         Summary
             Project          Project          Acres          Effort
          $/T($/MT) $/KgP $/T($/MT) $/KgP $/T($/MT)  $/KgP $/T($/MT)  KgP
 No-till
 Reduced
 Tillage
                        1979
23  (25)   650   5   (6)    148

31  (34)   833  10  (11)    289

                        1980
No cost

No cost
6  (7)  185

9 (10)  248
No-till
Reduced
Tillage
15

28
(16)

(31)
422

800
5

9
(6)

(10)
132

237
No

No
cost

cost
3

2
(3) 7

(2) 5
                   COSTS PER KILOGRAM OF PHOSPHORUS

     Calculations for phosphorus show that costs for keeping phosphorus
in place ranged from a high of $833 per kilogram for reduced tillage
demonstration systems in 1979 to a low of $132 per kilogram for no-till
done with ACP cost share funds in 1980.  Again, when other acre accom-
plishments are included, costs range from $53 to $248 per kilogram,
substantially less than the initial start up or demonstration costs.

     With regard to both soil and phosphorus, respective unit costs
were in each case less during the second year, 1980.  Projections over
a 20-year period, assuming acres with conservation tillage to remain
constant though that time, would show significant decreases in unit
costs:  $.10 to $.30 per ton of soil and about $3 to $12 per kilogram
of phosphorus based on the summary effort data of Table 4.  Annual
costs of about $60,000 for information-education and technical assis-
tance would be reduced similarly.
                  FARM ECONOMICS OF CONSERVATION TILLAGE

     In final analysis, the purchase of any product, be it a box of
soap or a tillage practice, must provide you something in return.  In
the case of conservation tillage systems, it must provide the farmer a
means of existence.  Economic data for one year only from tillage dem-
onstration work in Honey Creek suggests that conservation tillage
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farming can keep an operator in business.   Compared to an average net
return of $85 per acre ($212 per hectare)  for conventional systems,
reduced tillage systems returned $107 per  acre ($268 per hectare) while
no-till returned $73 ($182 per hectare).   Data gathered in years 2 and
3 of the Project will provide a better understanding of costs and re-
turns to the farmer.

Table 5.  Average Per Acre (Hectare)  Production Costs, Crop Values and
          Net Returns to Farmers from Conventional and Conservation
          Tillage Systems, 1979 Honey Creek Demonstration Plot Data.
1979
Number plots
Average costs
Range
$/Ac($/Ha)
Average value
Range
$/Ac($/Ha)
Average return
Range
$/Ac($/Ha)
Conventional
3
192 (480)
127 to 228
(318 to 570)
227 (692)
252 to 307
(630 to 768)
85 (212)
42 to 125
(105 to 312)
Reduced Tillage
12
180 (450)
124 to 228
(310 to 570)
287 (718)
155 to 381
(388 to 952)
107 (268)
-13 to 179
(-32 to 448)
No-till
18
198 (495)
124 to 245
(310 to 612)
271 (678)
166 to 325
(415 to 812)
73 (182)
-36 to 181
(-90 to 452)
                                 SUMMARY

     This report attempts to describe what happened during the first
two years of the Honey Creek Watershed Project, a 3-year demonstration
Project within an agricultural portion of the Lake Erie Basin in north-
central Ohio.  While the data are by no means definitive, they provide
insight as to the effectiveness and implementation costs of agricultur-
al non-point source controls, particularly when planned as part of a
start up or demonstration program.  For such programs the data suggest
that while practice application costs may initially be great, costs
will decrease with time and as spinoff benefits occur.

     In turn, implementation cost effectiveness of conservation tillage
systems will increase.  In Honey Creek costs decreased as a result of
information-education and technical assistance efforts complementing
incentive payments to landowners.  Most effective of these was high
quality on-the-farm technical assistance.

     Now when you are shopping around for point or nonpoint source con-
trol practices, attempting to decide how much of which to implement
where, you will have a rough idea of how to get the most from your mon-
ey, at least with respect to conservation tillage practices.  But when
you shop, buy only what you need to do the job.  Anything else would
discredit the phrase, "best management practices."
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                               REFERENCES

1.  Cahill, J. H. and R. W. Pierson.   1979.   Honey  Creek Watershed
    Report.  Buffalo District,  U.  S.  Army Corps  of  Engineers,  Buffalo,
    N. Y.  79 pg.

2.  Wurm, D. U. and J. P. Crumrine.   1980.   Honey Creek Watershed
    Project:  Tillage Demonstration  Results, 1979.  Honey  Creek Joint
    Board of Supervisors, Tiffin,  Ohio.   61  pg.

3.  Yaksich,  S. M.  1979.  Lake Erie Wastewater Management  Study
    Methodology Report.  Buffalo District, U.  S.  Army  Corps of En-
    gineers, Buffalo, N. Y.  146 pg.

4.  Quilliam, R.  1979.  Modern Farming  with Conservation  Tillage.
    USDA-SCS, Columbus, Ohio.   12  pg.

5.  Logan, T. J.  1978.  Summary Pilot Watershed Report Maumee Basin,
    Ohio.  International Joint  Commission Task Group  C, Windsor,
    Ontario.

6.  Spires, A. and M. H. Miller.   1978.   Contribution of Phosphorus
    from Agricultural Land to Streams  by Runoff.  International Joint
    Commission Task Group C, Windsor,  Ontario.

7.  Schwab, G. A., E. 0. McLean, A.  C. Waldron,  R.  K. White, and
    D. W. Michener.  1971.  Quality  of Drainage  Water from a Heavy
    Textured Soil.  Transactions of  the  ASAE,  Vol.  16,  No. 6,  St.
    Joseph, Michigan.

8.  Romkens, M. J. M., D. W. Nelson,  and J.  V. Mannering.  1973.
    Nitrogen and Phosphorus Composition  of Surface  Runoff  as Affected
    by Tillage Method.  Jr. Environmental Quality,  Vol.  2, No. 2.

9.  Mannering, J., C. B. Johnson,  and  D.  Nelson.  1977.  Simulated
    Rainfall Study Results in Environmental  Impact  of Land Use on
    Water Quality.  Final Report on  the  Black Creek Project-Tech-
    nical Report, Allen County  Soil  and  Water  Conservation District.
    U. S. Environmental Protection Agency, Chicago, Illinois.
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                    NONPOINT  SOURCE POLLUTION IN URBAN AREAS

                                       by

                  James Baumann, Andrea Domanik and John Konrad
     The  passage of the Amendments to the Federal Water Pollution
 Control Act  in  1972, P.L. 92-500, set the stage for a major new initiative
 in  our nation's water quality management program.  This law provided
 for a comprehensive examination of the two sources of water pollution,
 point and nonpoint, and the development of a control strategy to deal
 with them.

     Prior to that time, almost all water pollution control work was
 undertaken piecemeal with the great bulk of the effort being devoted
 to  point  sources of pollution.  Nonpoint source (NPS) pollution is
 associated with pollutants contained in stormwater runoff and groundwater
 seepage.  This diffuse pollution enters water bodies at an almost
 limitless number of places.  Because of the difficulty of trying to
 deal with sources of this type and an inadequate understanding of the
 magnitude of NPS pollution, little effort had been directly devoted to
 its control.  Indirectly, soil conservation efforts undertaken by
 rural agricultural interests have served to reduce the level of water
 pollution control associated with farmland erosion, but in urban areas
 the effort has been almost nonexistent.

     Section 208 of P.L. 92-500 recognized the need to:  examine
 nonpoint  source pollution; measure the impacts in relation to those
 resulting from point sources; and develop a comprehensive control
 strategy  which included best management practices to reduce pollution
 from both sources.  In rural areas, the soil conservation experience
 has provided a basic implementation structure to build upon having
 identified control practices most likely to be effective.  In urban
 areas no  such focus has been available; instead, regional and state
 agencies  were designated under Section 208 to generate the needed
 water quality studies and identify the practices and agencies needed
 to  carry  out the NPS water quality control program within urban areas.

     The  designated planning agencies in Wisconsin have undertaken in
 cooperation with state and university staff,  a number of urban runoff
 investigations to determine the nature and extent of pollution resulting
 from urban runoff.  The most significant work has been done in the
 Milwaukee and Madison Metropolitan areas.   Four major studies have
 been undertaken in this southeastern corner of the Metropolitan areas.
 Four major studies have been undertaken in this southeastern corner of
 the state.  They are:   1)   The Menomonee River Pilot Watershed Study,
 sponsored by the International Joint Commission in the Milwaukee area,
 2) The Washington County Project funded by the Environmental Protection
 Agency;  3) The Regional "208" studies undertaken by the Southeast
Wisconsin Regional Planning Commission (SEWRPC) and 4)  The Dane
 County Regional Planning Commission study for the Madison area.   The
 first three studies mentioned are interrelated in that they all are
 focused on the greater Milwaukee Metropolitan area.   Two agencies,
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SEWRPC and the Wisconsin Department of Natural Resources (DNR),  played
a role in each of the investigations.   Information gathered in one
study was often used in another.

     This paper will synthesize the results of these and other studies
with an aim to determine the type and  effect of urban nonpoint sources
of pollution in Wisconsin, their  characteristics, and the overall
strategy for dealing with these sources of pollution in the context of
a comprehensive water pollution control program for urban and rural,
point and nonpoint sources.
               TYPES AND EFFECT OF URBAN NONPOINT SOURCE POLLUTION

     Studies clearly indicate that urban nonpoint sources of pollution
can cause serious localized water quality impacts on receiving waters
and may have wider regional impacts.  The two major types of NFS
pollutants generated from urban land uses are Q.) nutrients and sediments
and (2) toxic materials.  In addition, some concern has been expressed
about bio-chemical oxygen demand (BOD)5  fecal coliform bacteria, and
chlorides.

     It is important to recognize that both point and nonpoint sources
contribute to water pollution problems.   For example, SEWRPC had
estimated in 1975 that only 19% of the perrenial streams (1,118 miles)
and major lakes (100 lakes over 50 acres surface area), in Southeastern
Wisconsin met the national goal of "fishable and swimmable waters".
If only point sources were treated, by the year 2000, only 30% of the
total stream miles and 18% of the major lakes could be expected to
meet the national goal.  The reasons why national goals would not be
achieved are related to the contribution from nonpoint sources.
Conversely, if only NFS controls were implemented, by the year 2000,
61% of the stream miles and 90% of the major lakes could be expected
to meet national weather water quality goals.  These figures illustrate
the significance of nonpoint sources of pollution in this region of
Wisconsin.

     Perhaps the most immediately recognizable impact of NPS pollution
in Wisconsin is the cultural eutrophication of lakes and streams
resulting from the runoff of sediments and associated nutrients,
especially phosphorus.  This influx of excessive amounts of nutrients
tends to accelerate the production of aquatic vegetation.  The luxuriant
growth of algae and rooted aquatic species impairs the recreational
potential of these lakes and streams, alters the basic aquatic community
and accelerates the filling of shallow lakes or impoundments.  Phosphorus
has probably received more attention that any other  single pollutant
in Wisconsin's NPS pollution control program.  This  is almost entirely
due to its central role in the eutrophication process.  Nitrogen is
not identified as the controlling or limiting nutrient for most of  the
waters in Wisconsin and therefore has not been studied with same
intensity.

     In the Menomonee River Watershed, much of which flows through  the
City of Milwaukee, two-thirds of the  total phosphorus load is from
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nonpoint sources.  The other one-third is from point source discharges,
most of it in soluble form discharged during nonstorm periods providing
a very significant source of available phosphorus.1  This emphasizes
the need to account for point sources of phosphorus, as well as nonpoint
sources in order to have an effective control program.

     Rural nonpoint sources of phosphorus also contribute very significantly
to the water quality problems of Wisconsin, because of the large
amount of farm land in the state.  However, a recent study conducted
in Dane County suggests that the average amount of P in the runoff
from an acre of rural land is likely to be only one-half that carried
in the runoff from an acre of urban land.

     Sediment is a pollutant of considerable importance not just
because of the nutrients, BOD, and toxics associated with it, but also
because by itself it can cover and destroy and aquatic biological
community, create conditions unsuitable for sensitive aquatic life
such as trout, and may accelerate the filling up of lakes and impoundments.
As will be discussed later, such problems with sediment may be especially
severe near developing urban construction areas if adequate control
measures are not adopted.

     One characteristic of sediment as a pollutant which is important
to understand in selecting control measures is sediment size.  The
relative surface area of a sediment particle is inversely related to
the particle size.  Therefore, the amount of surface area increases
very rapidly as particle size decreases.  Surface area also determines
the quantity of pollutants which can be absorbed to these particles.
This effect can be clearly seen in the concentrations of lead in the
clay-sized particles found in suspended and bottom sediments in the
Menomonee River, one of the rivers flowing through Milwaukee.  Between
70% and 90% of the total phosphorus and lead is found in the fine,
clay-sized fractions.  These small sized particles, easily picked up
and transported by a storm event, are also the most difficult to
capture and control with most management strategies.

     Toxics associated with heavy metals, other inorganic elements, or
organic compounds constitute a public health hazard as well as a
threat to the biolgoical communities of both lakes and streams.  The
toxics which have received the most attention in the studies have been
lead, mercury, cadmium, chromium, copper, nickel, zinc, and PCB's.
Aside from lead, the loadings of the toxics listed above appeared to
be very low and their concentrations in surface waters are low as
well.  However, even though the concentration and loadings are low
many of these pollutants persist in the environment, they attach
themselves to sediment and accumulate in the bottom materials of the
lakes and streams.  Average concentrations of these substances in
bottom sediments range from about 1,000 to 20,000 times the concentrations
measured in flowing water in the Kinnickinnic River in Milwaukee.
These toxics can have an adverse impact on bottom feeders and rooted
aquatics, and during wet weather conditions some of these substances
may be resuspended in association with the sediments.  As with all of
the pollutant parameters discussed these toxic substances are not
derived solely from urban runoff, although such runoff is frequently
the major source of these contaminants.
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     The fecal coliform standard in Wisconsin has been shown to be
violated during periods of wet weather in the urban watersheds.  This
may or may not indicate the existence of a public health hazard.
Fecal coliform is only an indicator of the possible presence of pathogenic
or disease-carrying pollution.  Since much of the fecal matter found
in urban runoff is from nonhuman sources it is not thought to pose as
serious a problem as that associated with domestic sewage.

     Chlorides and BOD associated with runoff have not been demonstrated
to present serious water quality problems in Wisconsin.  This may be
due to the dilution of these constituents in the large amounts of
stormswater present during runoff periods.  Chloride resulting from
winter road salting activity has been shown in Madison's Lake Wingra
to elevate concentrations, but the effect on water quality has not
been determined.

     BOD and associated dissolved oxygen problems have been tied
indirectly to the phosphorus contained in urban and rural runoff.  As
pointed out previously, this phosphorus fuels the growth of algae and
rooted aquatics; when the organic matter dies and decays it can exert
a significant oxygen demand.

     Overall there are significant water quality problems arising from
pollutants contained in urban runoff in Southeastern Wisconsin.  The
most prominent of these are those associated with phosphorus.  However,
sediments and toxics can present serious problems as well.  As developed
areas expand and the required controls on the point sources are implemented,
the overall amount and relative significance or urban nonpoint sources
of pollution can be expected to increase.
                    CHARACTERISTICS OF URBAN NONPOINT SOURCES

     When analyzing the extent and nature of urban nonpoint sources of
pollution it is useful to differentiate between various types of urban
land uses, because of the significant differences in pollutant loadings
from these land uses.  Two land-use related factors have been identified
as having a significant affect on the amount of NFS pollution.  The
first is the hydraulic factor which measures the amount and duration
of storm related runoff.  Many types of urban development increase the
amount of impervious surface and often alter natural drainage patterns.
The general result of this type of development is to increase the
amount of runoff and decrease the runoff period, thus increasing the
intensity and velocity of the runoff event.  This results in an increase
in the scouring and transporting capability of the runoff water.

     Another important hydraulic consideration affecting water quality
is the impact of the increase in impervious surface (increased runoff)
on the groundwater regime.  The decrease in infiltration results in a
lessening of the amount of groundwater derived baseflow available
during low flow periods.  These low flow periods are frequently the
most critical periods from a water quality standpoint because the
amount of water available for dilution is at a minimum.
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     The second factor ±s the differing types of pollutants generated
by different land uses.  Areas undergoing urban development are generally
associated with disturbed vegetative cover and exposed soils.  Such
areas provide a very significant potential source of sediment.  Industrial,
commercial, and high density residential developments are generally
associated with heavy transportation traffic and air pollution.  The
pollutants generated by cars and trucks, and fallout from air pollution
caused by industrial production are usually deposited in the immediate
vicinity of the source.  An accumulation of these and other pollutants
will occur because this type of development also has large amounts (a
high percentage) of impervious surface.

     The contaminants are then readily washed by storms into surrounding
(available for transport tol surface waters.  Especially important in
this regard are lead and other toxic substances which are associated
with transportation and industrial activity.  Table 1 illustrates the
variation in the approximate pollution generation potential for various
urban land uses in the Menomonee River watershed.

Table 1.  Pollution Generation Potential for Urban Land Use Categories
          In Menomonee River Watershed


Land
1.
2.
3.
4.
5.
6.
7.


use category
Industrial
Commercial
High density residential
Medium density residential
Low density residential
Land under development
Parks and recreation
Suspended
solids
kg/ha/yr
5,10Q
3,450
3,650
3,100
650
43,700
460
Total
phosphorus
kg/ha/yr
4.46
1.51
2.77
2.46
1.05
78.7
.81

Lead
kg/ha/yr
6.9
13.2
5.6
4.2
0.48
0.10
0.00
     Source:  Menomonee River Pilot Watershed Study, Summary Report,
by J.G. Konrad, G. Chesters, and K.W. Bauer,  May 4, 1978, p.o. 34.

     Another indication of the relative seriousness of urban runoff
from heavily built-up impervious urban areas  can be seen in the General
Mitchell Field Nonpoint Source Study undertaken in 1976 and 1977 by
the Wisconsin DNR.  General Mitchell Field is the primary commerical
airport serving the Milwaukee Metropolitan area.  It is located in a
heavily built-up area on the south side of Milwaukee.  This study
found that storm water runoff from the airport area is a significant
source of pollution to nearby streams.  At times the concentrations of
nutrients, suspended solids, and BOD approximate the levels found in
raw domestic sewage.

     Areas with storm sewers also tend to experience greater pollutional
problems that those which lack such urban amenities.  This may be
easily explained by the above discussion concerning hydraulic factors
and the types of urban land uses which would  be associated with the
presence of storm sewers.  Storm sewers decrease the opportunity for
infiltration and creates a very efficient runoff system.  Storm sewers
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are generally associated with medium and high density residential,
commercial, and industrial land uses.  Table 1 demonstrates the potential
reduction in pollutants which can be expected in nonsewered areas such
as low density residential neighborhoods.  It should be understood
that the absence of storm sewers need not automatically be associated
with a reduction in pollution problems, but rather if the hydraulic
and land use characteristics associated with such a sewer are accounted
for in the development of nonpoint controls then a reduction might be
expected.

     The intensity and duration of storm events is considered to have
an important impact on urban pollutant loadings.  Early thinking on
this subject speculated that most pollution would be associated with
the initial runoff resulting from a storm event; reduced loadings
would occur as the storm continued since most of the pollution would
be washed off in the "first flush".

     The studies in Wisconsin indicate instead that with one exception,
the total mass of pollutants washed from urban land surface, is directly
proportional to the volume of precipitation associated with the
event; pollutant concentration is relatively insensitive to the volume
and duration of the storm event.  This may be caused by the more
intensive scour and transport capacities of larger volumes of water
and the large reservoir of pollutants available for transport in the
areas studied.

     Snowmelt runoff during thaws in the winter and early spring
provides an exception to these findings.  The Mitchell Field study
determined that the greatest seasonal pollutant yield did not occur
during the season generating the largest runoff volume, summer, but
rather during the season with the least runoff volume, winter, for all
constituents, except suspended solids.  This can be explained by the
accumulation rates, differences in storm event characteristics and the
presence of frozen pervious surfaces.  Investigations of winter and
spring snow melt events are very sparse, and a great deal of work
remains to be done in this area.

     In summary, not all urban areas contribute equally to the pollution
problem.  Developing urban areas are by far the most significant
sources of sediments and associated phosphorus.  The amount of impervious
surface contributes both to the increases in the volume, scouring, and
transport capability of storm water and contributes to the build-up
and availability of pollutants.  The amount of impervious surface and
industrial land uses which are associated with this type of impervious
surface are found to be the most significant sources of toxic pollutants
and may also contribute important amounts of sediment and phosphorus.
                          MANAGEMENT STRATEGY

     In the development of a management strategy to control urban
nonpoint sources of pollution it is essential that clear-cut water
quality objectives or standards be formulated and that point sources
and rural nonpoint sources of pollution are considered in a comprehensive
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and integrated fashion.  The lack of clearly established and agreed
upon water quality objectives for NFS pollution has been an obstacle
in developing an overall water quality management strategy.

     Three aspects of this urban problem are the most difficult to
assess.  They are:  (1) The absence of an established standard for
phosphorus in either lakes or streams, (2) The lack of guidance in
dealing with acceptable levels of toxics in bottom sediments, and (3)
The inadequacy of the present water quality standards to deal with
high flow periods.

     The SEWRPC areawide water quality management planners have taken
major initiatives toward dealing with these problems.  They have
employed a complex water quality model (HYDROCOMP) to simulate the
inter-relationships between the various sources of pollution, anticipated
storm events, hydraulic characteristics of the area and water quality
conditions.  This model, within various levels of confidence, is then
able to predict the water quality expected when employing alternative
point and nonpoint source control strategies.  They have applied a
total phosphorus standard of Q.10 mg/1 for flowing streams and a 0.02
mg/1 concentration in lakes during the spring turnover period.  These
are not standards which have been officially adopted by the Wisconsin
DNR, and they have been subject to widespread scrutiny and criticism.
However, it must be pointed out that these are the concentrations
provided in EPA's Water Quality Criteria - 1976, the so-called "red
book", and no one has suggested more appropriate concentration limits.

     The water quality model also allows SEWRPC to take a new approach
to the application of water quality standards.  This approach considers
the assessment of the proportion of the total time under various
anticipated flow conditions can be expected to exceed specified
concentrations, such as that listed above for phosphorus which do not
directly affect aquatic organisms, but are primarily related to
recreational use.  This statistical approach was not employed for
concentrations of toxic materials under the presumption that these
materials should never be present in toxic concentrations in the water
body.  SEWRPC did not directly address the control of toxic levels in
the bottom sediments.

     In developing a specific control strategy for urban nonpoint sources
it is necessary to consider the character of this type of pollution.
There are four key considerations in this control strategy.   (1)
Control of the sediments, especially the clay-sized particles to which
phosphorus and toxic compounds are adsorbed.  (2) Concentrate first on
those land uses which provide the most significant sources of pollution,
specifically developing areas and those parts of the city where residential
and industrial urban land uses are densely concentrated.   (3) Develop
measures which increase the amount of infiltration and reduce and
attenuate the amount of overland flow.  (4) Prevent the pollutants
from being generated in the first place.

     Since virtually all significant types and amounts of urban nonpoint
sources of pollution are associated with sediments, the. control of
sediments is an important consideration.  In effect, almost all cost-
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effective control strategies are aimed at either keeping these sediments
in place, removing them from impervious surfaces, or causing them to
be placed in areas where they will not be eroded and carried into
surface waters.

     An exception to this general rule of concentrating on sediment
control are actions which prevent .associated pollutants from being
generated at all.  This can be seen in the ban on leaded gasoline,
control on industrial air emissions, and limitations on various types
of fertilizer and pesticide use.  It is anticipated that the control
on the use of leaded gasoline will take care of most of the problems
currently experienced with lead pollution.
                   RESIDENTIAL HOUSING CONSTRUCTION

     The most promising area for overall control is in developing or
redeveloping urban areas.  In the Menomonee River watershed developing
urban areas represented only 2.6% of the total area of the watershed,
but contributed 37% and 48% respectively of the suspended solids and
total phosphorus at the river mouth.  Data from the Washington County
Project showed that subdivisions constructed without preventative
measures to reduce soil disturbance contributed significantly to water
quality nonpoint source problems (Washington County Final Report,
November, 1979).  In the Washington County Project, sources of sediment
and methods of controlling sedimentation were studied for three phases
of the residential construction process:  1) site selection and plat
planning, 2) plat development of streets and services, and 3) lot by
lot house construction.  Housing construction was emphasized because
this phase of development has not been critically evaluated as contributing
to the sediment control problem.  Legal mechanisms for regulating
subdivision construction activities at the local level were also
examined.

Site Selection

     One of the best methods for minimizing erosion and sedimentation
may be proper environmental planning prior to development.  A high
degree of quality may be achieved without increasing development cost;
this is accomplished through proper selection of sites suitable for
development and sensitive plat planning and development.  When investigating
potential development sites, physical and natural conditions should be
critically evaluated.  Areas with unsuitable soil types, lowlands,
steep slopes and high water tables  (to name a few limitations) would
be expensive to develop, requiring extensive filling or grading,
difficult to minimize erosion, and troublesome to maintain.  Preparation
of the plat plan should take into account such factors as natural
drainage patterns, existing vegetation and the amount of land disturbance
necessary to develop the plat.  An effort should be made by developers
to minimize the degree to which the landscape will be altered particularly
with respect to drainage.  When necessary, erosion and sedimentation
controls should be incorporated into the plat plan.
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Plat Development

     Plat development can be viewed as the construction of streets and
services.  Numerous publications have been written offering suggestions
for reducing sediment loss during this stage.  One common development
practice has been to strip topsoil and vegetation from the entire plat
then proceed with construction.  Often the topsoil is stockpiled for
several years while streets and services are being built.  A more
environmentally source practice would be to only disturb the area
where construction is currently concentrated or to protect large areas
of exposed soil.  If topsoil must be removed, temporary measures to
protect the exposed soil should be taken.  Seeding, mulching or other
protective covers would achieve adequate control.

     Other innovative measures can be implemented to minimize stormwater
runoff; porous pavement and protective buffers or berms increase
stormwater infiltration.  It is critical that all control measures be
incorporated into the plat plan, thus insuring enforcement and
implementation.

Housing Construction

     Construction of residential dwellings within a subdivision can
cause large amounts of sediment to be transported through storm sewers
to surface water.  The problem is magnified by the simultaneous construction
of several dwellings.  Table 1 illustrates monitored sediment yield
during uncontrolled housing and construction (Washington County Project).
Three subdivisions being rapidly developed were monitored during 1977.
No treatments for erosion and sediment controls had been used.  The
amount of sediment, measured as suspended solids, leaving the subdivision
through its storm sewer, has been estimated in kilograms per hectare
per year.  Differences in site conditions may account for variations
in annual yield.  No comparable values are currently available for
treated residential construction activity.

Table 1.  Annual Suspended Solid Yield (kg/ha) From Untreated Residential
          Construction in 1977
Station
G2
G3
G5
Yield
27,215 kg/ha
17,365 kg/ha
13,148 kg/ha
     Building practices common during construction, that were examined
in the Old Farm Annex, might be mitigated without interfering with
construction.  The following list, by no means complete, attempts to
highlight damaging activities and conditions:

          Exposed and unprotected soil throughout the subdivision
(highly erodible).

          Excavated soil, in large mounds, placed near and often in
the streets (rapid erosion and delivery of sediment to storm sewers).
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          Unlimited access to lots by vehicles and heavy equipment
(tracking soil adhered to tires into streets; gullies formed by tire
tracks that channelizes flow).

          Pumped water from flooded basements (dewatering) onto exposed
areas (generates and transports sediment to storm sewers).

     -    Drained rooftop runoff onto unprotected areas (forms gullies,
erodes and transports sediment to storm sewer system).

     Many of these activities occur during work performed by subcontractors
who are onsite for a very short time.  Cooperation and communication
between builders and subcontractors are essential if mitigating
measures are to be effective.

On-Site Controls

     The following list of practices are divided into two categories,
those that do not require additional funds to implement but are suggestions
for timing activities to reduce impact.  Other practices do have a
minimal cost but are usually incurred at some point during construction.
It is recommended that many of these measures be implemented early in
the building process so that their benefit will be incurred throughout
the housing construction period (which takes from four to six months).

     No Cost Practices:  1.   Retain existing trees and shrubs wherever
possible, since vegetation filters, retards and absorbs overland
runoff.

     2.   Locate excavated basement soil a reasonable distance behind
the curb, such as in the backyard or sideyard area.  This will increase
the distance eroded soil must travel to reach the storm sewer system.

     3.   Remove excess soil from the sites as soon as possible and
rough grade the lot.  This will eliminate large soil mounds which are
highly erodible and prepares the lot for temporary cover.

     4.   If a lot has a soil bank higher than the curb, a trench or
berm should be installed moving the bank several feet behind the curb.
This will reduce the occurrence of gully and rill erosion while
providing some storage and settling area for sediment-laden storm
water.

     5.   Roughen the soil surface by rototilling areas that are to be
stripped for too short a length of time to allow establishment of
temporary vegetative cover.  Roughening will increase the infiltration
of storm water and reduce erosion.

     6.   Direct flowing water away from steep slopes and other highly
erodible areas by constructing diversion structures such as terraces,
benches, dikes and ditches.
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     Other Practices:  7.     Provide for periodical street sweeping
or vacuuming to remove sediment during construction.

     8.   Stabilize the lot by seeding and mulching or sodding as soon
as possible after exterior construction is completed.  This will
minimize erosion as well as make the area more visually pleasant.

     9.   When not feasible to stabilize the entire lot with vegetation,
cover an area approximately 20-30 feet behind the curb with a protective
material such as filter fabric or mulch and netting.  This covering
may be installed before backfilling, provided excavated soil is placed
in the backyard area and the lot has been rough graded.  Lateral lines
may be installed by removing the protective covering and then replacing
the cover after filling.  This measure will reduce raindrop intensity
while protecting the soil.

     10.  Apply 1-inch gravel to the driveway area and restrict truck
traffic to this one route.  Driveway paving can be installed directly
over the gravel.  This measure will eliminate soil from adhering to
tires and being tracked into the street.

     11.  Install roof downspout extenders and sump pump drainage
tubing to disperse water or to divert it directly to the curb and
stormsewer.  Keeping clearwater from running across exposed soil will
prevent gully and rill erosion from these sources.

     12.  Install straw bales, sand bags, tarps or filter fences along
curbs to reduce the amount of eroded soil reaching the curb gutter or
stormsewer.

Legal Controls Case Study

     Many states, counties and incorporated areas have enacted some
type of ordinance that attempts to control subdivision developments.
In Washington County, developers are required to submit preliminary
plat plans to the County Soil and Water Conservation District for
proposed developments within unincorporated areas.  This subdivision
ordinance is fairly modest requiring a land suitability test where
lands with greater than 12 percent slope are presumed unsuitable for
development unless developers can provide adequate erosion and sediment
controls.  The ordinance also requires stormwater management facilities
be designed to handle the maximum flow potential from a 10-year 24-
hour storm.  If development requires substantial land disturbing
activity, practices to minimize erosion and sedimentation are required.
Several towns within the county have adopted the county ordinance.
Washington County's subdivision ordinance does not, however,,address
the lot construction phase of development.  It also does not apply to
unplated housing construction (less than five lots).  There are limited
provisions for enforcement and penalties.  Authorities are not defined
stating who is responsible for monitoring compliance with this ordinance
and insuring implementation of required erosion and sediment control
measures.
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     The Village of Germantown has drafted a land division ordinance
requiring plat review by the Village Engineer and County Soil and
Water Conservation District.  Maps of the natural and physical conditions
within the proposed development are required in order to determine
suitability.  Soil and water conservation practices are also required
where land disturbing activities are proposed.   Developers are required
to minimize the amount of area exposed and must stabilize by revegetating
as soon as practical.  In an attempt to control lot construction, the
Village has also developed an ordinance that requires builders to post
a $100 cash bond when applying for a building permit.  The bond will
be used to pay for services, if any, incurred by the Village because
of construction activity; any remaining money will be returned to the
builder upon issuance of an occupancy permit.  The ordinance also
levies a $200 per day fine on any person,  firm or corporation found
guilty of violating the ordinance.

     In order to provide for the control of erosive construction
practices, subdivision and building ordinances should be strengthened
to include:

     -    tracking provisions requiring vehicle traffic to clean
sediment in the street as a result of their tire tracking;

          handling requirements for excavated soil so that soil is
placed behind a set back line or tied to an egress line, from the
house front to the curb line;

     -    placing limits on the amount of  time soil can be exposed and
require temporary protection;

     -    providing for the periodic cleaning of sediment from streets
and gutters during construction;

     -    limiting alterations in natural  drainage patters or provide
for retention of stormwater resulting from channelized drainage ways;
and

          requiring that rooftop runoff be diffused onto vegetative
areas and provide for the proper handling  of pumped water (from dewatering
or sump pump activity).

     By including these provisions into ordinances that control land
disturbing activities, environmental and aesthetic qualities will be
greatly improved.

     Experience on the Washington County project has demonstrated that
a three pronged approach is needed to effectively implement a program
for control in these developing and redeveloping areas:

     They are:

     1.   An informational and educational program to explain the need
for erosion and sediment control during construction.
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     2.   Standards and design specifications for erosion control
practices written in understandable language.

     3.   Cooperation between local officials and developers, builders
and subcontractors in setting reasonable and effective regulations.
                         DEVELOPED URBAN AREAS

     The outlook in developed areas is less optimistic.  Most of the
available controls are relatively expensive and questionably effective.
Surprisingly, the most effective control measures may be instituted in
parts of the city now served by combined sewers.

     Dry weather street flushing can be employed prior to comprehensive
actions to control the combined sewer overflow problems.  Such flushing
can transport street contaminants to municipal treatment plants and
dislodge deposits in the sewer.  Eventually, in the elimination of
combined sewer overflows some form of storage and treatment can deal
with both point and NFS pollution problems, if properly designed.
SEWRPC is recommending such a method to deal with pollution problems
in the combined sewer areas of Milwaukee.

     In the other developed urban areas only very carefully selected
management practices should be recommended for implementation.  The
most commonly discussed, street sweeping, does not appear cost-effective
under most conditions, but may be useful if employed for spring clean-
up and during autumn leaf drop periods.  Certain housekeeping activities
such as catch basin cleaning and redirecting roof drains to areas
where infiltration will occur may also be useful.  The most effective
actions may be those mentioned previously which prevent the generation
of the pollutants.  Regulations on the generation of leaded gasoline
and on materials handling as well as air pollution controls are examples
of such action.

                              CONCLUSIONS

     Urban runoff is a major contributor to the water quality problems
being experienced in and near our major cities.  The eutrophication of
our valuable lakes, as well as the degradation of the streams can be
traced to urban nonpoint sources of pollution in these areas.  As our
metropolitan areas expand and point sources of pollution are brought
under control, the relative importance of urban nonpoint sources will
increase even more.  Any water quality management strategy for our
metropolitan areas which ignores or downplays this source of pollution
is destined to be ineffective in the attainment of the national goal
of fishing and swimming water quality.

     Stormwater runoff from urban and developing areas have unique
hydrological characteristics which requires special consideration in
order to control nonpoint sources of water pollution.  As impervious
ground cover increases the area's hydrology changes so that stormwater
does not infiltrate,  but rather the volume of water running off increases.
Therefore, more water is available to transport pollutants through
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storm sewers and roadside ditches to surface waters.   Degradation of
surface waters accelerates as more polluted water enters,  ultimately
affecting their recreational and natural amenities.   Control strategies
that increase infiltration or retention time within  urhan  areas should
be investigated.

     The urban runoff program will,  in all probability not be as
effective or cost-efficient as it should be until comprehensive programs
are developed which examine all sources of pollution and their relationships,
Standards must be developed which deal with high flow periods.  The
control of sediments from developing urban areas, special  consideration
for nonpoint source pollution in dealing with combined sewer overflows,
and the elimination of pollutants at the sources in  other  developed
areas seem to provide the most promising means of dealing  with pollution
contained in urban runoff.

     Stormwater runoff from residential subdivisions that  are undergoing
development can generate and transport large amounts of sediment and
associated pollutants (nutrients, metals) to surface waters.  Low cost
practices are available to reduce sedimentation during the lot construction
phase of development.  Subdivision and building ordinances should be
strengthened to include erosion control practices.
     Authors are all members of the Bureau of Water Quality in the
Wisconsin Department of Natural Resources, Madison, Wisconsin.
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                                NURP

                                 by

                             Doug Ehorn
              Chief, Michigan Water Quality Management


The purpose of this speech is to present you with an up-to-date summary of

progress made under the National Urban Runoff Program.  While there are many

attendees in this room who are familiar with the NURP program there are

several new faces and therefore I'll first present a brief historical  state-

ment.


HISTORY

Over the past several decades, several studies conducted  across our nation

indicated that storm runoff was a major pathway through which pollutants  were

carried to receiving waters.  Under the Federal Water Pollution Control Act

(PL 92-500) there was an initial way to fund storm water  projects  in conjunction

with the construction grants program.  However, storm control was  not  regarded

as a critical element which initiated grant action, but oncillary  and  should  be

studied to provide cost-effective solutions to pollution  control.  And even

then the major of funds were to be spent combined sewer overflow controls or

Abatement.  With the later amendments to the Act, there was  less emphasis put

on storm water control for a variety of factors; the main factor being that

there was an insufficient data base to support the program.


During the last three years, studies conducted with Section  208 planning  funds

have supported the concept that urban runoff appears to be a major pathway  of

pollution.  Studies were conducted at numerous locations  on  a nationwide

basis.  Even with this expanded data base, Congress did not  provide  sufficient

funds to expand the program to any great extent.  They did provide funds  for
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                                 2
problem assessment and planning, but held back on implementation  funds  because
the current state of technical knowledge was insufficient to justify  large-
scale actions.
The National Urban Runoff Program was initiated to respond to  several of  the
prominent deficiencies such as:  areal accumulation patterns,  washoff,  transport,
instream behavior of pollutants and effectiveness of control measures.  The EPA
hopes that the current studies will provide knowledge concerning  the  practical
implications of urban runoff pollutants on water quality and aquatic  ecosystems.
Several of the goals envisioned when the NURP program was initiated in  1978 was
to gather knowledge that would provide a holoistic approach to the problem and
the state of the art for control technologies that would provide  EPA, the States
and local decisionmakers with a rational basis for problem assessment,  postula-
tion of controls, and development of local stategies to implement controls that
would show benefits to the receiving waters.  To date NURP 30  projects  at a cost
of $20,658,000 have been funded with the intent of providing a report to  Congress
in 1983 to support further planning and implementation activities.  The report
will have to deal with the nature, and extent of runoff problems, cause of the
problem, severity of the problem (based on beneficial uses and W2 standards of
receiving stream) and the opportunities for controlling the problems.

Where are we today?

The EPA has substantially completed the initial phases of the  NURP Program at
the present time.  A nationwide program was developed and current status  of
problems was assessed, projects were selected to provide a "Prototype"  base.
Program management and coordination is continuing with headquarters providing
technical assistance to the projects.  I might add that even though liaison
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functions were rough during the initial year of NURP, both Headquarters  and the



the Regions have been able to develop a "report" that provide excellent  service



to the grantees.





As data from the prototype projects is gathered, reduced  to  usable  form  and



provided to the EPA, the process of Program assessment  and evaluation will



begin in earnest.  The culmination of all these activities is the already men-



tioned report to Congress in 1983.  While EPA will not  fund  any more NURP type



projects during the planning process, we are anxious to supply all  relevant



data and control strategies to local planning and implementing agencies  at  the




earliest possible date.





By the way the report I have with me entitled "Quarterly  Progress Report,



National Urban Runoff Program" provides initial data on management  aspects  of



the NURP program.  It does not provide data on control  mechanisms,  BMPs, pollu-



tant sources or other technology aspects of the program due  to early stage  of



NURP development.





Of the 30 projects that were targetted for NURP, 10 projects are underway and



yielding data, most of these projects have their planned  BMPs  in operation.



Ten projects are just beginning.  Their work plans are  approved and consultant



contracts have been signed.  Nine projects do not have  fully approved work  plans



and one project is in an early stage of planning.  I should  note that projects



which started late had the most difficulty achieving approval because of the



keen interest and insight provided by EPA's technology  consultants  who required



ever increasing high standards of performance.
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The General characteristics of these prototype projects are summarized as

follows:

A.  Receiving water type (by major emphasis)

    8  projects study small streams
    5  projects study lakes
    6  projects study rivers
    1  project studies oceans
    2  projects study groundwater

B.  Impacts

    9  projects study actual impairment of beneficial use
    8  projects study standards violations
    4  projects study public concern

    Impacted beneficial uses fall into 5 major categories:  water  supply,
    contact recreation, non-contact recreation, fish and wildlife,  aesthetics

C.  Suspected Problem Pollutants

    1 project studies  BOD, COD, DO
    8 projects study   nutrients
    1 project studies  sediments
    7 projects study   heavy metals
    1 project studies  other toxics
    7 projects study   coliform bacteria

D.  Major Best Management Practices

    4 projects study   street sweeping
    4 projects study   Detention basins
    1 project studies  Catch basin cleaning
    2 project study    wet land treatment


There are other practices being studied at localized site  including:   swirl

concentrators (which offer great promise), runoff  ordinances,  sewer alternatives

and filters.


Technological status

The EPA is concerned about the potential  threat of urban runoff to the Great

Lakes ecosystem.   Currently projects have not progressed far  enough to provide

sufficient details that would warrent  a generalized status statement.  From the
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early data, this Agency  is aware that  toxic  pollutants in urban runoff may not



have received sufficient attention at  this time.   One report from the Seattle



study indicated that toxics could be a localized  problem, however the data




base was not as good as  it might have  been.  New  analytical  methods are being



devised to overcome problems.  At another location high concentration of



Salmmella were found and in the Final  Report for  the Castor  Valley project



measurable asbestos levels were indicated.






As you can tell the data base  is slim  at this  time.   Several projects are being



realigned to provide answers to questions arising from earlier  projects or to



take advantage of developing technologies.





My best advise to you is..., Use your  head make logical decisions,  well thought




out, not under pressure.  For  instance street  sweeping projects may not work




because you don't pick up fine materials that  carry pollutants.  Then proper



disposal methods timing of sweeping.   For Detention basins - longer detention




time to get fines settled out.  These  are just a  few of the  logical things that



must be done.  I believe that  small, well organized projects will probably give



us more pertinent data than the large  megabuck projects.





The Future of NUPP



We are just beginning to crawl in certain aspects of urban runoff and its



technology.  We are certain that pollutants  are reaching  receiving  waters in



our urban areas.  Further quantitative work  must  be accomplished in the areas



of sources and control of sources.  The EPA  does  have sufficient knowledge



concerning wastewater treatment plans  and our  data base is growing  on combined



sewer overflow control and sludge.  However  in the area of separate storm water



discharges there is a paucify of data.
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NURP's future is uncertain at this point.  Very preliminary data indicates that



there is no real problem in some areas.  Urban runoff may  not  be a National



problem.  In that case, controls and strategies would have to  become concentrated



in localized areas.





The pollutant of most concern that has emerged from  the early  studies is bacteria.



So what?  What does that mean in terms of beneficial uses  or standards.   From a



public health aspect we have found certain discharges to be laced with Salmonella



and animal coliform.  These results will have to be  followed up on.





There was some early data to indicate that all nonpoint sources were significantly



contributing to degradation of water.  These studies are reconfirming that fact on



a localized basis.  It appears to me that the upshot of all this is—Nationally we



are going to have to re-look at out water quality standards after sufficient non-



point source data is available from programs similar to the NURP program.





Let me encourage everyone who is interested in pollution control to do their



utmost to make available good data that can contribute to  our  knowledge  of causes,



effects, and solutions to pollution of our National  waters.
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 LFW/ib
 WIBLE-F
                    HIGH FLOW WATER QUALITY STANDARDS

                                  By

                            Lyman F. Wible
                             INTRODUCTION

     This  paper  discusses  high  flow  water  quality  standards  as  they
have  been addressed  in  the  areawide  water quality  management  planning
program   of   the   Southeastern   Wisconsin  Regional  Planning  Commission
(SEWRPC).   This  discussion will  include  the  need  for  standards,  the
analyses  and resulting  approach taken by  SEWRPC,  and  the more  recent
actions  taken by  SEWRPC,  and  the  Wisconsin  Department  of Natural  Re-
sources  (DNR)  and the  U.S.  Environmental  Protection Agency   (EPA)  to
further address the question.

     The  Southeastern Wisconsin  Region  includes  the  seven counties  in
and  around  the  Kenosha,  Milwaukee,  and  Racine  metropolitan areas.   As
the  designated  areawide  water  quality  management  planning agency  for
the  Region,  SEWRPC addressed three  generalized questions  in preparation
of  its  Section 208 plan.   Here are  the questions:   first,  what are  the
historic  trends  in water quality and in the attainment of  the  state  and
federal  water quality standards?  Second,  what are  the  existing sources
of  water  pollution   which  affect  water  quality?   Third,  what  are  the
future  actions  which  will  be necessary in order to  achieve and  maintain
the  water quality standards  in  the  1,180 miles of  continuous  stream  and
in  the  100  major  lakes  in  southeastern Wisconsin through the year 2000?

     In  this process,  the  development of meaningful  quantitative plans
required  the use of  analytic  tools.   Such  tools  can  be  applied only in
the  framework  of  explicit  quantitative  planning  standards.    Planning
standards  provide  the  basis  for  comparison  of  current  conditions,  the
current  trends,  and   the  alternative  plans  for water  quality management.
The  Southeastern  Wisconsin  Regional   Planning   Commission  has  always
developed  planning standards of this  sort in  order  to  serve  specific
use  objectives.   The  Section   208   planning  process  addressed  program
objectives for  supporting  sound land use,  supporting  the  intended water
uses, protecting  the  natural resource  base, developing  a cost-effective
plan,  and  establishing  effective   and locally  acceptable  implementing
mechanisms.   For  each of these  program objectives,  a series of quanti-
tative planning standards was  developed.

     At  this juncture,  a definition  must be clarified.   Since  1967,  the
Wisconsin  Department  of  Natural  Resources has  referred  to  the  intended
use  of  a  stream  as  a  "use  designation"  or  "use  classification".   The
Regional  Planning  Commission--in the  framework  of  definitions  developed
in  comprehensive  planning  since  196l--refers  to  these  as  "water  use
 Chief  Environmental  Planner,  Southeastern  Wisconsin Regional  Planning
 Commission, Waukesha, Wisconsin.
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objectives,"  objectives  to be  achieved by  action in various  programs.
The  objectives  include, in  various combinations,  the  maintenance of  a
trout  fishery and  related aquatic  life,  the  maintenance  of  a  salmon
fishery and  related aquatic  life,  the maintenance of a  warmwater fish-
ery  and  related  aquatic life,  the  maintenance of a  limited  fishery  and
related aquatic  life,  recreational use,  limited recreational use,  and
the  maintenance  of  minimum  water  quality  conditions for the  avoidance
of nuisance or aesthetic offense.

     The attainment  of these objectives  may be  measured against speci-
fic  standards,   as   discussed  above.   Among  these  standards  are  what
SEWRPC  calls  the  "water  quality  standards," which  are  referred  to  by
the  Wisconsin DNR  as "water quality  criteria".   In  this  paper  I  will
utilize the  Regional Planning Commission's  definitions,  which  recognize
water  use  objectives  and  supporting  water  quality  standards as being
among  the  set  of multiple  objectives  and  supporting  standards to  be
addressed  and evaluated in  the  development of a meaningful,  comprehen-
sive  plan  for  water pollution  control.  I  will address standards  for
flowing streams,  since  the issue of water quality standards  definitions
for  lakes  includes   a  substantial  body of literature  and technical work
which could not be addressed properly in these brief comments.

     Clearly,  the  basic  water  use  objective which was  sought to  be
achieved in  the  development  of  the Section 208  plan was the  attainment
of  water   suitable  for the  maintenance of  fish  and  other aquatic  life
and  for  the  support of  human recreation in and  on the water:   in other
words,  "fishable and  swimmable" water quality  conditions.   Only  upon
the  basis  of  (1)  specific  findings regarding  limitations  due  to  natural
conditions, or  due  to  (2) irrevocable human modification of  the water-
shed  and  drainage  system  were  the   nationally  identified  water  use
objectives compromised in the development of the Section 208 plan.

     It should also  be noted that  this  approach  differs  from the use of
water  quality standards  by  state  and  federal  agencies.  The U.S.  EPA
and  the  Wisconsin DNR, being regulatory agencies,  utilize  water  quality
standards  as  the  basis  for enforcement actions and for  compliance moni-
toring for current  conditions.   This requires that the  standards have a
rigid basis  in  research findings and in field  experience.   By contrast,
the  Regional  Planning  Commission  must anticipate  regulations  and tech-
nologies  into the  future, documenting  the  assumptions   used  to  analyze
conditions  and problems  which may not yet exist.   As a  result,  more
recent—and  sometimes  more  controversial — study  findings must sometimes
be  applied.   This   results   from   the  Commission's  need to  use  water
quality  standards  as  a  criterion to  measure   the  relative merits  of
alternative future conditions.

     A  classic  example  of the need  for appropriate  quantitative plan-
ning standards,   as  a  basis for  plan  alternative  comparisons,   may  be
found  in   the  determination  of  point  source and  nonpoint  source trade-
offs  in the  Section 208  planning  process.   Intuitively, the most cost-
effective  solution  to  water quality   problems  in any given  area would
appear  to  include  combinations of point  and nonpoint  source  pollution
controls.   However,  if  as a basis  for comparison of alternative plans,
a  low-flow-based  water quality  standard   (for  example,  the  seven-day-
average,  one-in-ten-year-recurrence interval,  low-flow  condition)  were
used exclusively,  then  the stream  response to point  source   controls
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would appear  exaggerated.   If  the  average annual  pollutant loads  to  a
surface water  system were  used exclusively,  this  measure  of effective-
ness may  indicate an  exaggerated  response to  nonpoint  source  controls.
However,  a  fair  comparison  of  the  two  types  of  sources requires  a
planning standard or  a combination  of planning standards expected  to be
responsive to both types, in those cases where both are important.

     Historically, water  quality management  efforts  at all  levels have
been oriented  toward  the  dry  weather,  low  flow  problem.   Water pollu-
tion  problems  have   generally  been  considered most  apparent  when  the
stream  flows  decline  significantly  during dry  weather.    By  contrast,
the point  sources of  pollution normally discharge sewage  effluent at a
relatively constant  rate  or at a uniform frequency,  and  of a relatively
uniform quality;  and  are relatively less affected  by  changes in weather
conditions than is  the associated stream flow  response.  These concerns
have also  led  to  consideration of dissolved  oxygen as the  most critical
water quality  indicator.   Thus, water quality management  programs have
been  designed  to attempt  to  control  point  sources of  pollution  by
specifying  appropriate  sewage  treatment  plant  effluent   limitations.
The  effluent  limitations   are  chosen  with  the  intent  to  ensure  that
in-stream  water  quality  standards  are  met  during   all   but  the  very
lowest  of  stream  flow  conditions.   At  higher  flows,   the  dissolved
oxygen  standard  was  considered to  have been  attained,  because  of the
dilutional effects of the receiving stream.

     Recent  water quality monitoring programs  have indicated that water
pollution  is  not exclusively  a dry weather,  point source-related prob-
lem.   As   evidenced  by the water  quality monitoring  results documented
in  the  SEWRPC  continuing water quality monitoring program  since  1964,
numerous violations  of water  quality standards have been known to occur
under  conditions  other  than  dry weather low-flow  conditions,  and  as  a
result  of  sources other  than  point  sources  of pollution.   Accordingly,
it  was  determined in the Section 208  program for southeastern Wisconsin
that the  recommended  plan  must address  the  surface  water  quality prob-
lems attendant  to high flow-as well as  low flow-conditions.

     To  formulate  the  applicable  water  quality  standard  which  would
support  the  intended  water  use  objectives,  an  analysis  was  made of
water  quality  monitoring  data  from  those  streams in  the  Region that
have  relatively  clean water  and  healthy  fisheries,  and  for  which the
water  use  objectives  are  considered  to be  met  at  the  present  time.
Review  of  these  data  indicated  that  even  in   such relatively  clean
streams,  the specified  water  quality standards  are  not met  all of the
time.   Standards  violations were  found on occasion,  but were generally
of  such  short  duration  and  low intensity that these  violations  would
not be  expected to  adversely affect fish and aquatic life  and the human
use  of  the  surface  waters.  Therefore,  it was  concluded  that it would
be  impractical  to   interpret   water  quality  standards  on  an absolute
basis — that  is,  as  being  required to  be met  100  percent   of  the  time.
Accordingly,  it  was  determined  to  assess  water   quality  conditions
against  the  pertinent  water  chemistry  criteria  on  a  probabilistic
basis,  specifying in  effect the  percent of  total time that  the  water
quality  conditions  were  to  be  in  compliance  with  the  water  quality
criteria.   This  approach  was   subject  to  the  requirement that  point
source  pollution abatement measures  would continue  to be  designed to
meet these standards during the seven-day average one-in-ten-year
                                     331

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recurrence  interval  low-flow  condition  in   receiving  streams.   Thus,
the  interpretation  would  provide  for  standards   to  be  violated  for
extremely  low flow  conditions  and  for a  specified proportion of  time
under  relatively  high flow conditions.   This constitutes a  risk assess-
ment  procedure,   and  is  reinforced  by the  recognition that  a  finite
probability  exists—typically  in  southeastern  Wisconsin,  on  the  order
of  one-tenth of  one percent—that the  seven-day, one-in-ten-year  recur-
rence interval design would be  inadequate as well.

     Further  analyses  were  made  to determine the percent of  time  that a
given  standard  should be  allowed  to be violated.   A 95  percent compli-
ance  level  was  selected  as a  practical criterion for meeting the  water
quality  standards  for those indicators  which directly  affect desirable
forms  of aquatic  life.   These  included dissolved  oxygen,  temperature,
un-ionized  ammonia  nitrogen,  and  pH.  A 90 percent  compliance level was
selected  as  the  criterion for  those indicators which  do not directly
affect  desirable  forms  of  aquatic  life.   These  include phosphorus  and
fecal  coliform  organisms.   The Commission analyses  indicated that  if
these  compliance  levels  were met  during periods other  than  extreme low
flow  conditions,   the duration  of  violation would  be  expected  to  be
relatively  short   and the  intensity  would  be  relatively  low.   Thus,
desirable forms of  aquatic  life  should not be adversely  affected.   This
probabilistic approach to  the  interpretation  and  application  of  water
quality  standards  formed a very  important basis for  the evaluation  of
alternative  plans and the selection of a recommended plan,  by consider-
ing  the effects  of  nonpoint  sources  of  pollution.   It was  therefore
recommended  that  this probabilistic approach to water  quality standards
and  interpretation  be considered  by the state  for  use  as  a  supplement
to  the  current  exemption  in  State standards  for  low  flow  conditions,
flows below  the  seven day Q10>

     This approach  has been recommended to the Wisconsin Department  of
Natural  Resources  for  all of  the  standards  supporting the   water  use
objectives  used in  the preparation of the  Section 208 plan.   The recom-
mendation  renders  it  more complex  to  interpret  a field-sampled  water
quality  violation:   is  the  observed condition a member  of  an acceptable
and  infrequent  set  of  occurrences,  or  is  it representative  of a  "pol-
luted"  condition  having  an unacceptable  frequency  of  violation.   This
procedure  will  require  the Department  of  Natural  Resources  to develop
new  field techniques,  or interpretive methods for the analysis of  field
survey  data as  presently  gathered;  or  to  develop  a  set  of assumptions
regarding the probabilities of standards violation  associated with what
had  been historically recognized  as  "background"  or  "natural"  condi-
tions,  which interfered with  achievement  of water  quality  standards  by
point  source control.   It is  now apparent that  the  effects  of  uncon-
trolled  nonpoint  sources  must  be  differentiated  from  the  effects  of
"natural" limitations of the surface water systems.

     The  results  of the  Regional  Planning  Commission's approach  were
checked  for reasonableness against  other study  findings.   Such compari-
sons  considered  the SEWRPC adopted Regional  Sanitary  Sewerage  System
Plan  completed in 1972,  and within  the  framework of point  source pollu-
tion  control; the Department of Natural Resources'  wasteload  allocation
studies  and  resulting effluent limits;  the "common  sense"   recommenda-
tions  of long-standing soil and water  conservation  agencies;  the recom-
mendations  of the  Menomonee River  Pilot  Watershed Study  conducted  by
                                     332

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the  International Joint  Commission;   and  the  findings  of  Washington
County Sediment  and  Erosion Control Study conducted under  Section  108
of PL. 92-500.   The SEWRPC results were found to be consistent with  the
results of these other studies.

     The Regional Planning  Commission  believes  that the  work which  was
conducted as part of its Section  208  program can serve  as  a  point of
departure for  analysis  and further development  of solutions to this
relatively new problem  regarding  water quality standards for high flow
conditions.   The technique utilized by the Commission was practical  for
its work programs, since the hydrologic-hydraulic water quality simula-
tion  model  (Hydrocomp)  which was  applied,  gives  results  in  a  proba-
bility distribution  of  the  water  quality indicators studied.  However,
the Commission staff believes  that the probabilistic interpretation of
standards and of in-stream water quality samples may be capable of more
simplified application,  by  use of nomographs,  charts,  or  figures, if
these tools  are properly and rigorously developed.  The extension of an
approach to  high flow water quality standards is one of the major goals
of  the "Phosphorus  and High-flow Assessment  Study for  Water Quality
Standards."   This project is  currently being conducted  by  the Depart-
ment  of Natural  Resources in  cooperation with the EPA and SEWRPC.   The
project is being undertaken in part as a result of the DNR inclusion of
this matter  as  a "highlighted  issue" in the  Wisconsin-EPA Agreement  for
fiscal year  1980.   The  project  has initiated  studies of  the related
aspects  of  biological  field  monitoring  of  aquatic  flora  and  fauna,
biomass  estimates,  pollutant-mass load  analyses, and bioassays.   The
project is  also  evaluating the  potential for  inclusion of biological
parameters into analytic and simulation models.

     The SEWRPC  staff believes  that with thoughtful consideration,  the
effects  of  nonpoint  sources  of  water pollution can be properly  ad-
dressed in the  water quality standards and in the related water quality
monitoring and  enforcement programs.
                                 333

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         THE USE OF COMMUNITY PARAMETERS DERIVED

        FROM ELECTROFISHING CATCHES OP RIVER FISH

          AS INDICATORS OF ENVIRONMENTAL QUALITY

                             by

                       J .  R.  Gammon
Professor of Zoology, Department of Zoology, DePauw University,
Greencastle, Indiana 46135
                             335

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Acknowledgements

     The analysis  presented in this paper  is based upon re-
search supported  by Public Service  Indiana,  Dayton Power and
Light, Eli Lilly  Company, and the Office of  Water Resources
Research.  Field  collections involved  many students includ-
ing Terry Teppen,  Chris Yoder , Doug Meikle,  Brandon Kulik,
Jim Thayer, Michael Stroup, Doug Bauer, Robert Gammon, Rick
Wright, and Ernest Roggelin.  The system of  data storage and
computer analysis  was developed by  Dr.  Carl  Singer, Marcile
Dudley, Ann Kohlstaedt, Ron Van Seventer,  Art Buis, David Dee,
and Clifford  Gammon.   Mrs. Betty McKee was extremely helpful
in preparing  this  report.
                                336

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               The Use of Community Parameters

            Derived from Electrofishing Catches  of

          River Fish as Indicators of Water Quality


                        J .  R. Gammon
Introduction

     There  is  a  pronounced need for methods of measuring  the
effect of various  human activities on the aquatic  communi-
ties of running  water ecosystems.  Major impacts which  lead
to an elimination  of  entire species may be interpreted  with
little difficulty,  but it is unacceptable today to  await  the
disappearance  of entire species from an ecosystem  in  order
to assess detrimental environmental effects.  Nevertheless,
biological  investigations too often generate a list of  spe-
cies collected which  is supposed to reflect the health  of the
biological  community  in itself.  Such a list is of  value, but
its length  is  strongly dependent upon the effort devoted  to
its construction and  basing a judgement of environmental  ef-
fects on a  comparison of two or more species lists  alone  is
highly inadvisable.

     Other  methods  of gauging environmental effects on  biota
generally include  some quantitative measure of the  size of
the population,  either that of a single group of related  or-
ganisms or  of  a  single species of special ecological  or com-
mercial importance.   For example, Larimore and Smith  (1963)
found the effects  of  organic pollution on fish populations  to
be first a  reduction  in the number of species present,  then a
reduction in the total weight or biomass, and finally a re-
duction in  the number of individuals.  For those working  with
fish populations in rivers it has become almost automatic to
structure studies  which use some measure of numeric density
as the data base.

     Some measure  of  diversity often is used to characterize
the structure  of benthic communities (Wilhm and Dorris  1966,
1968), but  is  not  usually employed in work with fish.   In a
study of fish  communities in small streams in Pennsylvania,
Denoncourt  and Stambaugh (1974)  found relatively high species
diversities at several sites receiving moderate to  heavy  pol-
lution and  recommended against using diversity indices  with
fish populations.   However, Richards (1976)  found diversity
indices of  value in interpreting faunal changes in  the  Au
Sable River over a  50 year period.

     Bechtel and Copeland (1970)  found diversity indices  based
on otter trawl tows to be useful indicators of pollution  in
Galveston Bay, Texas.   McErlean and Mihursky (1969) examined
the application  of diversity measures to a variety  of fish  col-
lection data and subsequently applied them to collections in
                              337

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estuaries  to  demonstrate seasonal changes  and annual trends
(McErlean,  et.  al.  1973).

     Several  years  of site-intensive  studies in the immediate
vicinity of two  electrical generating  stations located on  the
middle Wabash  River determined that fish moved around predict-
ably in response to varying thermal conditions and were rarely
killed directly  (Gammon 1971, 1973).   However, it was not  pos-
sible to determine  whether the positive and negative behav-
ioral responses  reflected long-term changes in the populations
or if the  fish communities in the immediate vicinity of the
electrical  generating stations differed significantly from
fish communities uninfluenced by thermal inputs.  We also
needed to  determine how much of the river  was being influenced
by the EGSs .   Consequently, a study program was initiated
which continued  to  monitor the fish communities near the two
electrical  generating stations, but also included studies  of
flanking reaches of the river.

     During 1973 and 1974 the fish  communities over 100 miles
of the middle  Wabash River were examined by repeatedly elec-
trofishing  at  24 similar sites, including  4 comparable sites
at each EGS  (Teppen and Gammon 1976) .  A majority of species
were non-randomly  distributed through  the  100 miles of river,
some more  abundant  in the lower river, e.g. shortnose gar  and
bowfin near reproductive bayous, and  others more abundant  in
the upper  river, e.g. redhorse which  were  particularly sensi-
tive to increased  temperatures caused  by the two EGSs.  Other
species populations were found to be  either more or less com-
mon near the  EGSs  than in flanking  regions of the river.   The
species composition, therefore, shifted considerably in dif-
ferent parts  of  the river, sometimes  in response to natural
factors and sometimes because of man-induced changes in water
guali ty.

     We also  examined five quantitative measures of community
structure  including  (1) relative density  (no/km),  (2) relative
biomass  (wt/km), (3) number of species per station,  (4) Shan-
non index  of  diversity based on numbers,  and  (5) Shannon index
of diversity  based on weights.  The  two  Shannon indices were
calculated as  follows:

           H =   - T(ni  Ln
                   ^~- 1
                      \N

     Where nj_ = the  numbers or weight of  individual species
                 in the sample

           N = the total number or weight  of fish in the
               sample

All of  these  community parameters  exhibited a common general
pattern  over  the 100 miles of river,  but  with some interest-
ing anomalies here and there which  made  interpretation diffi-
cult.
                               338

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     In 1975  an  additional 100 miles of  the  upper Wabash
River was included  in the sampling program and  all of the
data collected during 1973-75 was analyzed for  evenness in-
dices associated with the two Shannon diversity indices and
a composite index in addition to the previously mentioned
measures of community structure  (Gammon  1976) .   The compos-
ite index of  well-being (Iwb) was calculated according to
the formula:

     3-wb =  0.5 Ln N + 0.5 Ln W + Shannon (no.)  + Shannon /wt \

where N = the number captured per km
      W = the weight captured per km
      Shannon/no^)  = Shannon index based on  numbers
      Shannon(wt^)  = Shannon index based on  weights

     This composite index combines two widely  used indices of
diversity and two widely used indices of abundance in approxi-
mately equal  quantities to form a single composite value re-
flecting both the diversity and abundance of fish in the col-
lections.   It appears to reflect the general "health" of the
fish community and, hence, the water quality somewhat more
satisfactorily than any single community index  or indicator
species.

     In 1976  a thirty mile segment of the Great Miami River
was investigated by this general method  as part of a larger
effort which  attempted to measure the relative  impact of two
electrical  generating stations within a  great  number of po-
tential impacts  (Gammon 1977).  In 1977,  130 miles of the
Wabash River  were again studied and demonstrated some inter-
esting contrasts to the 1973-75 study.   It is  the intent of
this paper  to examine and evaluate the findings of this com-
munity structure approach as applied to  the  Wabash and Great
Miami Rivers.
                               339

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The Rivers and Methods
                   The  Great  Miami River
     The Miami River  Valley  from Dayton to the Ohio River  is
thickly settled  and heavily  industrialized.  The river  at
Dayton, Ohio drains 6,508  km2 (2,513 mi 2)  of land and has  a
flow which averages 2,206  cfs.  (Todd 1970).  Weston  (1967)
has detailed the uses and  polluted state of the river.

     Seventeen collecting  stations were established on  the
river and two each on the  lower  portions of the Mad and  Still-
water Rivers  (Figure  1).   Each  station was located on the  out-
side of gradual  bends in  the  river and were about 0.33  km  long
as measured with a Lietz  optical rangefinder.  A series  of dams
created lentic-like habitats  and also blocked upstream  move-
ments of fish, including  the  Steele Dam (River Mile 81.3), Tait
Dam (RM 76.6), Hutchings  Dam  (RM 63.5), and Chautauqua  Dam
(RM 61.6).

     Each month  from  June  through September, 1976 fish  were
collected from each station  using a battery-powered 600  VDC
electrofishing unit.   When depth and discharge permitted each
station was electrofished  from  upstream to downstream by wad-
ing, otherwise a 12'  boat  containing the electrofishing  unit
and two personnel was moved  slowly near shore over the  measured
di stanc e.
                              340

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              Dayton STP
    Hutchings
Electrical
Generating
    Plant
                                    Tait Electrical
                                    Generating Plant
                                    Moraine STP

                                   CARROLLTON
                               •W. Carrollton STP
                           MIAMIBURG

                             Miamiburg STP
                       FRANKLIN
                        Franklin STP
                MIDDLETOWN
 Figure 1;  Location of sampling stations in relation  to
            sewage treatment effluents and electric
            generating stations.
                        341

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                    The Wabash  River
     The Wabash River at Terre  Haute  drains 31,598 km2
(12,200 mi2) and has an average discharge of 10,200 cfs.
(Todd 1970).  Although several  large  flood control reservoirs
have been constructed on tributaries,  the Wabash River itself
flows freely in response to  changing  weather conditions.  Tur-
bidity is generally high because of  silt during high discharge
and because of high densities of diatoms during summer.  Water
quality is  influenced importantly by  extensive agriculture
throughout  the basin, by coal strip mines in the southern part
of the drainage basin, and by discharges from municipalities
and industries  (Figure 2).

     In 1977 a total of 47 collecting  stations were established
throughout  145 miles of river,  including 8 stations at the Cay-
uga Electrical Generating Station (EGS)  and 6 at the Wabash EGS
(Figure 2).  Each sampling station consisted of a 0.5 km sec-
tion of outside bend as measured with  a  Lietz rangefinder.
Many stations were in the same  locations used in 1973, 1974,
and 1975.

     The collecting apparatus consisted  of a Smith-Root Type VI
electrofisher powered by a 3000 watt  generator.  Pulse configu-
ration consisted of a triangular wave  interrupted into 60 pps
and producing 400-600 VDC at approximately 5 amps.  The pulsed
DC current was fed into an electrode  system consisting of two
circlets of short stainless-steel anodes extended by booms ap-
proximately 8 feet off the bow  of a 16 foot John boat and two
gangs of long woven copper cathodes weighed at the ends and sus-
pended from port and starboard  gunwales  near the bow.

     The basic procedure for collecting  was to begin at the up-
stream boundary and slowly electrofish downstream as close to
shore and cover as possible  to  the end of the station.  Sta-
tions were  electrofished sequentially  from up-river to down-
river until all had been visited,  usually within a 4-6 day period

     Following each collecting  run fish  were identified to spe-
cies, weighed, and measured  and then  returned unharmed to the
river.  All data was recorded on magnetic tape and disc and then
analyzed.
                              342

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                      WHITE
                    I	
                       TIPPECANOE
WARREN JL/278
                       MONTGOMERY
        VIGO ,   Figure 2: River  mile location
                          of  electrofishing

                          sampling stations.
SULLIVAN
               343

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Results - The Great Miami River

     A total of 2,545 individuals  belonging  to  40  species of
fish were collected in 1976 by electrofishing  over a total
distance of 27.24 km.  The most  common  species  were longear
sunfish, green sunfish, carp, stoneroller,  smallmouth bass,
gizzard shad, rock bass, goldfish, golden  redhorse, and hog
sucker, which together comprised 76.4%  of  the  numeric catch
(Table 1) .

     However, the nature of the  fish  community  changed mark-
edly as the river passes through Dayton, Ohio.   The largest
and most diversified fish community was  found  in the Still-
water River  (Figure 3).  This community  was  dominated by hog
suckers, golden redhorse, spotted  sucker,  smallmouth bass,
rock bass,  and longear sunfish.

     The upper three stations of the  Great Miami River were
also supportive of a large, relatively  diverse  fish commun-
ity although rock bass were scarce and  green sunfish much
more abundant.

     The fish community in the lower  part  of the Mad River
was of a different character than  anywhere else and was dom-
inated by stonerollers with a scattering of  other  species.
Industrial effluents above and in  this  reach may affect the
biotic composition, as noted previously  by Conn (1972) .

     The fish communities in the Dayton  Pool of the Great
Miami River between the Steele and Tait  Dams (RM 81.3 and RM
76.6) were somewhat less diverse and  numerous  than upriver
stations.  This section appeared to be  severely stressed
prior to the June sampling period  and then improved through-
out the  summer despite falling water  levels.  The  community
immediately below the Steele Dam was  always  more diverse and
numerous than stations further downstream.  Gizzard shad,
golden 'Shiner, and largemouth bass were  far  more common in
this pool than anywhere else.  Species  which were  reduced in
abundance compared to further upstream  sections included
smallmouth bass, rock bass, green  sunfish, bluegill, golden
redhorse, and spotted sucker.  White  sucker, carp, and gold-
fish - all of which are pollution  tolerant species - increased
in abundance compared to upstream  stations.

     The pool between Tait and Hutchings Dams  (RM  76.6 and
RM 63.5) contained fish communities  very similar qualitatively
to those just upstream although  much  lower in density.  How-
ever, in the section  of river downstream from the Dayton STP
the  fish community consisted primarily  of  carp, goldfish,
carp/goldfish hybrids, and,  in certain  areas, white suckers.
Not  only was the catch reduced  to  only  about 40 individuals/km
(compared to 150/km  in the upper stations, for example) , but
the  individuals captured were  often  small, young fish.  At
times  it appeared that no  fish whatever inhibited  some parts
of this  pool.
                              344

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        Table 1: Number  of  fish captured by electrofishing in 1976 in  several sections of  the
                 Great Miami  River and its main  tributaries.
CO
-P»
01

Species
Gizzard shad
Grass pickerel
Hog sUcker
White sucker
Golden redhorse
Black redhorse
Silver redhorse
Shorthead redhorse
Spotted sucker
Quillback
Carp
Goldfish
Carp/Goldfish hybrids
Golden shiner
Striped shiner
Spotfin shiner
Silver shiner
Mimic shiner
Emerald shiner
Creek chub
Stoneroller
Bluntnose minnows
Fathead minnow
Suckermouth minnow
Channel catfish
Yellow bullhead
S tonecat

Mad
River
10
-
11
9
1
-
-
-
4
-
10
-
-
1
4
4
7
-
-
-
127
6
-
-
-
-
1

Still-
water
River
4
-
52
2 '
42
x -
2 \
2
19
-
9
-
-
10
2
3
2
-
-
2
6
5
-
-
-
-
1

Above
Dayton
16
-
4
12
29
1
-
1
12
-
9
-
-
33
2
23
1
1
-
-
2
30
5
-
-
1
-
Gree
In
Dayton C
110
-
28
22
29
4
-
4
5
3
24
28
2
47
1
9
8
-
2
2
28
32
2
3
1
-
-
it Miami River
Dayton STP
to
^hautauqua Dam
2
-
3
28
-
-
-
-
-
-
125
69
4
4
-
5
1
-
-
7
6
6
-
-
-
1
-
~~~— •"-":=•-- ~- — =: — — — -~
Chautauque Dam
to
Middletown
1
1
3
2
1
-
-
-
-
-
53
32
2
1
4
24
1
-
-
-
-
-
-
-
-
-
-

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          Table  1:  continued
01



Species
Smallmouth bass
Largemouth bass
Rock bass
Warmouth
Longear sunfisji
Orangespot sunfish
Green sunfish
Pumpkinseed
Bluegil 1
Black crappie
White crappie
Log perch
Greenside darter
Banded darter
No . collecting
stations
Total distance
electrof i shed -Km
Total no . fish
Mean No . /Km .
No . of species


Mad
River
13
-
9
-
6
-
16
-
-
-
-
-
2
~

2

2.28
241
105.7
18

Still-
water
River
48
3
79
3
154
1
54
-
15
-
-
4
2
•~

2

2 .48
526
212 .1
26


Above
Dayton
54
2
14
-
169
3
118
-
33
2
-
5
-
*~~

3

3 .84
582
151 . 6
26
G:

In
Dayton
41
10
21
3
106
10
63
2
15
-
7
2
4
1

5

7 .08
688
97 .2
35
:eat Miami River
Dayton STP
to
Chautauqua Dam
5
2
3
-
19
1
18
-
5
-
-
-
-
"

6

7.92
314
39 .6
20

Chautauque Dam
to
Middletown
3
-
3
1
28
1
27
-
6
-
—
—
-


3

3.64
194
53.3
19

-------
                              W. Carrollton
                          Miamisburg
                        Goldfish
                        & Carp
                      Franklin
                                        Other
                                         Cyprinidae
Other
 species

 suckers  &
  redhor s e
                                       \longear,green,
                                        & orangespot
                                           sunfish
               Middletown
Figure 3s? Composition of the fish  communities of the
          Great  Miami -River system.   The area of each
          circle is proportional to  the relative den-
          sity  (no/km) .
                        347

-------
     The fish  community in the pool between  Hutchings Dam
(RM 63.5) and  Chautaugua Dam (RM 61.7) was  similar to those
above the former,  consisting principally  of  carp and gold-
fish with a  small  scattering of other  species.

     Carp and  goldfish continued to dominate the community be-
tween Chautauqua Dam (RM 61.7)  and Middletown Dam (RM 55.8),
but longear  sunfish, green sunfish and spotfin  shiner also be-
come common  elements in the catch.  In the  last collecting
stations in  this pool (RM 58.0) there  appeared  to be a numer-
ous and diverse community which probably  indicated a recovery
from the stresses  further upstream.

     The major  sources of pollution appeared to be the waste
treatment effluents  from Dayton, Miamisburg, West Carrollton,
and Moraine, the organic particles of  which  settled out in
pools causing  a steady production of bubbles throughout the
summer and early fall.  The dissolved  oxygen concentrations
fell to lows of 2.0  mg/1 and less each month of the study as
measured by  the Miamisburg A water quality monitor of the
Miami Conservancy  District at RM 65.75.   Numerous other efflu-
ents bearing a  variety of industrial wastes  to  the Great Miami
River and two  small  electrical generating stations are also
present, but the major problem is of an organic nature.

     Such a  stressed system where the  impacts are large and
clearcut provides  a  good opportunity to examine the community
structure approach as a tool of evaluation.   As would be ex-
pected, the  trends exhibited by all of the  community indices
reflected the  altered fish communities with  relatively high
numbers, biomass,  and diversities characterizing the communi-
ties upstream  from Dayton and lo-w values  for the communities
below Dayton (Figures 4,5, and 6).  A similar  pattern is ex-
hibited by the  mean  weight of fish (excluding carp and gold-
fish) with means of  60-120 g in upstream  stations and 10-30 g
in environmentally degraded sections.  The  combined local in-
fluence of the  Tait  EGS and dam causes a  brief  decrease in bio-
mass and'an  increase in the two Shannon diversities.

     The composite index of well-being brings together these
elements to  regularize the basic pattern  which  shows, in ad-
dition to the  community extremes, a zone  of  intermediate char-
acter within Dayton  (RM 75 to RM 80) and  a  zone of recovery
below Chautauqua Dam (RM 57 to RM 62)  (Figure 7 ).  The stan-
dard errors  were much smaller both in  the upstream zones and
in the recovery area indicating a comparative stability of the
environment  in  these segments compared to the more unstable,
impacted areas.
                               348

-------
CO
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to
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                          CD P n>
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S C^O
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d. cr n
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                                               Mean  number of Species
                                                collected per trip
                          H-

                          CD
  Hi CD
  o n

  <-i CD

  rt

  H- CD
                                                    Total  number of
                                                    different  species
                                                    taken  in  4 trips
                                      CD
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                                      CD
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-------
CO
in
o
              V)  rX





              I  1
10
rt
E
o
•H
PQ
                   250


                   200
50


 0

25


20


15


10


 5


 0
                        55
                     60
65
                                   River Mile


                                   70         75
         80
                              t
                          Franklin
                             STP
                         o Mad R.


                         X Stillwater  R.
                                     t
                                   V,' . C a r r o 1 1 1 o n
                              iamisburg   STP
                                  STP
                           Hatchings Dam

                                  Dam
                    t t
                        I
                     I
     Tait
       Dam
Day ton
   STP
                                                         t
85
                                                           S te ele  Dam
                                     Chautauqua
             Figure  5;  Relative density and biomass profile of the fish community  of  the
                       Great Miami R. and tributaries.  Based on four collections  June  -
                       September, 1976 (mean ± 1 S.E.)
90
                                                    250


                                                    200


                                                    150


                                                    100


                                                     50


                                                     0

                                                     25


                                                     20


                                                     15


                                                     10


                                                     5


                                                     0

-------
                                                      River Mile
                       55
                      60
65
                                           70
75
80
85
90
GO
cn
    c/1

 X    ,0
 •H  £
 C/l  ^
 fn  2;
 0

 •H
 Q
CD

CD
•H
^
l

O


cd   4-1

co   e»o
    •H
    CD
      2.0

      1.5

      1.0


      0.5

        0


      2.0


      1.5

      1.0

      0.5
                                                                           o Mad R.
                                                                           x Stillwater R
                             t
                         t ^   i * t *
      r
                                                      I
                                                      I    Tait Dam
                                                      Dayton STP
    r
                                                                   S teele Dam
                                   W.  Carrollton
             Franklin                     STP
                STP            Miamisburg STP
                              Hutchings Dam
                        Chautauqua Dam

Figure 6: Shannon-Wiener  indices  of diversity (numbers and weights)  for fish
          collections of  the  Great Miami R.  and tributaries.  Based  on four
          collections June  -  September,  1976. (mean ± I S.E.)
                                                    2.0

                                                    1.5

                                                    1.0


                                                    0.5

                                                    0



                                                    2.0

                                                    1.5

                                                    1.0


                                                    0.5

                                                    0

-------
                                                     River Mile
                        55
             60
65
70
75
80
85
90
GO
cn
ro
                CxO
                0)
                o

                X
7


6


5


4


3
                                                   o Mad  R.

                                                   X Stillwater R.
                         Franklin
                              STP
                                         11 /.
                        W. CarrolIton
                                STP

                      Miamisburg STP
                                          Hutchings Dam
                                    Chautauaua  Dam
                                                        t
                       Tait Dam

                     Dayton STP
                                                                              Steele Dam
                                                    7


                                                    6


                                                    5


                                                    4


                                                    3


                                                    2


                                                    1


                                                    0
                     Figure 7;  Composite  Index profile of fish community of the Great Miami R.
                               and tributaries.   Based on four collections June - September,
                               1976.  (mean  ±  1 S.E.),

-------
Results - The Wabash River

     The analyses of the  fish  communities  in the Wabash River
are based upon 7,120 individuals  of  57  species captured dur-
ing the period 1973-75 and  3,795  individuals of 51 species
captured in 1977  (Table 2) .

     The character of the  fish communities in the Wabash River
also changes fxom place to  place.  As  illustrated by the 1975
data (Figure  8) upriver  from  Lafayette the community is dom-
inated by redhorse, hog sucker, carpsucker, and carp.  The
various species of sportfish,  although  more common here than
elsewhere, make up a relatively small part of the catch.  Down-
stream from Lafayette gizzard  shad and  carp dominate the catch
while carpsuckers and redhorse diminish in importance.  Flat-
head catfish, which have  been  shown  to  be  stimulated by the
thermal inputs, become common  downstream from Cayuga EGS .

     The various community  parameters generated from electro-
fishing data exhibited patterns which declined from upstream
to downstream, but with a  good deal  more "noise" than with the
Great Miami River data.   Only  the composite index is included
here (Figure  9 ), but all  of the  community parameters exhibited
the same basic pattern  (Gammon 1976).   Some annual variations
occurred primarily in relation to summer discharge, but gener-
ally regional variations  were  greater  than temporal variations.

     The range of IWJD values is less extreme, but of the same
magnitude as those obtained in the Great Miami River study.
High values from 7.0 to 8.0 were  found  upstream from Lafayette
(RM 310).  A general, erratic  decline occurred from Lafayette
to Cayuga (RM 250 to RM 310),  then a low plateau from Cayuga
to Wabash EGS  (RM 215 to  RM 250).  A brief recovery is indi-
cated in the immediate vicinity of Terre Haute and then another
decline occurred downstream from  Terre  Haute (RM 185 to RM 200)

     Between 1975 and 1977  there  appeared  to be a rather sig-
nificant improvement downstream from Lafayette.  The reach of
river between the two EGSs  was found to have the poorest fish
communities during the 1973-75 period with Iwk values around
5.0 - 5.5.  In 1977 the Iwj-> values declined even further to
4.0 - 5.0.  This decline  in the composite  index was indicative
of worsened environmental  conditions.   Immediately following
the last series of collections in mid July 1977 this section of
river developed severe problems with low dissolved oxygen con-
centration (Gammon and Riedy,  1980).  Thus, the fish community
showed by its abundance and diversity that unfavorable environ-
mental conditions were present in this  segment long before any
stress was detected by chemical means.
                              353

-------
Table 2: Aggregate  electrofishing catch of  fish  in 145
         miles  of  the  Wabash River during 1977.
NAME
Silvery Lamprey
Shlnse. Sturgeon
Paddlef ish
Bowf in
Longnose Gar
Shortnose Gar
Gizzard shad
Skipjack Herring
Goldeye
Mooneye
Yellow Bullhead
Channel Catfish
Flathead Catfish
American Eel
White Perch
White Bass
Freshwater Drum
+Carp
Goldf ish+Carp Hy
Qback Carpsucker
White Sucker
Nrthrn. Hogsucker
Bigmouth Buffalo
Spotted Sucker
Silver Redhorse
Black Redhorse
Golden Redhorse
Shorthd. Redhorse
River Redhorse
N. Riv. Carpsucker
Hifin Carpsucker
Blue Sucker
Smallmth. Buffalo
Black Buffalo
Emerald shiner
Spotfin Shiner
Creek Chub
Silvery Minnow
River Chub
Rockbass
Bluegill
Longear Sunfish
Smallmouth Bass
Largemouth Bass
White Crappie
Black Crappie
Spotted Bass
Redear Sunfish
Greenside Darter
Logperch
Sauger
# CT.
17
9
1
13
52
60
1704
13
37
26
1
39
135
9
2
60
57
586
1
6
2
60
9
1
58
4
118
184
10
205
6
17
20
3
11
19
8
6
1
5
3
105
15
1
12
1
21
1
1
2
50
: = = = = = := = = :
% CT.
0.44
0 .23
0 .02
0 .34
1.37
1.58
44 .90
0 .34
0 .97
0.68
0.02
0 .02
3. 55
0 .23
0 .05
1 .58
1 . 50
15 .44
0 .02
0.15
0 .05
1.58
0 .23
0.02
1.52
0.10
3 . 10
4 .84
0.47
5.40
0 .15
0.44
0 .52
0 .07
0 .29
0 .50
• 0.21
0.15
0 .02
0 .13
0.07
2.76
0 .39
0.02
0.31
0 .02
0. 55
0.02
0 .02
0 .05
1.31
WT . (KG)
0.19
11.57
1.70
16.89
26.30
31 .64
325 .72
1.75
16.59
7 .71
0 .37
23 .73
59.59
4.64
0 .31
10.90
37 .67
1115.24
1 .00
2.16
1.18
17.62
24.27
0.59
56 .47
2.38
89 .09
122.63
22.56
142.52
3.15
35^47
52 .32
8.29
0 .16
0 .15
0 .15
0.11
0.00
0 .84
0.23
4.60
5.46
0 .21
1.70
0 .17'
3 .49
0 .02
0.00
0 .05
35.95
% WT.
0 .00
0 .49
0 .07
0.72
1.13
1.35
13 .99
0 .07
0 .71
0.33
0 .01
1.01
2 . 56
0.19
0.01
0.46
1 .61
47.91
0 .04
0.09
0 .05
0 .75
1 .04
0.02
2.42
0 .10
3 . 82
5 .26
0 .96
6.12
0 .13
1 .52
2. 24
0.35
0 .00
0.00
0 . 00
0.00
0. 00
0.03
0 .01
0.19
0.23
0.00
0.07
0.00
0.15
0.00
0 .00
0 .00
1 .54
                               354

-------
                          Andrews
                            to
                         Lafayette
       Lafayette
          to
     Big Pine Crk
Cayuga.
K • G • S •
Wabash
E.G.S.
       Terre  Haute
           to
        Darwin
 Figure
GS=gizzard shad
 A=carp
 R=redhorse and
   hog sucker
 C=carpsuckers
 F=flathead catfish
 S=w.bass,blk.bass,
   sauger,walleye,&
   centrarchids other
   than longear sunfish
 O=other species	
   Composition of the electrofishing catch during 1975
   in  designated segments of the Wabash River. The area of
   the circle is proportional tc the mean No/Km. (Gammon, 1976
                             355

-------
Pi scussion

     The fish communities of  the  Wabash  River and the Great
Miami River are formed from the same  species  with some excep-
tions.  These communities respond to  various  environmental
stresses by reorganizations in  species composition.   Where
stress is large, as in the Great  Miami River  below Dayton,
Ohio, the community composition shifts toward obviously pol-
lution tolerant species of fish.   However,  where stress is
small and/or diffuse, as in most  of the  Wabash River and in
the Great Miami River at Dayton,  the  shift  in species compo-
sition, if present at all, is too subtle to detect with assur-
ance.  It appears that different  indices of community struc-
ture may provide a means of detecting subtle  shifts in stressed
communities and that a blend  of different indices, as for ex-
ample the composite index, may  serve  to  magnify and clarify the
community response to subtle  perturbations.

     A composite index may also act as a normalizer, permitting
comparisons of different rivers as well  as  different sections
of river .  In the Great Miami River good sections of stream
yielded catches whose community parameters  were 150/km, 20
kg/km, and Shannon indices of 1.5 to  2.0, while poor sections
yielded catches less than 50/km,  5 kg/km, and shannon indices
of 0.8 to 1.2.  Fewer, but larger, fish  were  taken in the
Wabash River, but Shannon diversities tended  to be similar to
those from the Great Miami River  communities.  Table 3 summa-
rizes the community parameters  from good and  poor sections of
both rivers and an intermediate value for each parameter.

     Of special interest is the fact  that,  although there are
differences in relative density and relative  biomass, the com-
posite indices are very similar for good, intermediate, and
poor communities in the two rivers, approximately 7.5 for good
communities, 6.25 for intermediate communities, and 5.0 for
poor communities.  Using these  values to delineate environmen-
tal conditions of these rivers, values  exceeding 7.5 appear to
reflect a good environment, a fair environment is indicated
when values are 6.25 to 7.5,  a  poor  environment from 5.0 to
6.25, and a degraded environment  when values fall below 5.0.

     Applying this criteria to  the composite index profiles
for the two rivers helps clarify  and  interpret the results of
studies of this kind.  The deteriorating environmental condi-
tions in the Wabash River between Cayuga and Wabash EGSs is
indicated by a decline in Iwb values  from the poor interval in
1973-75 to the degraded interval  in  1977 (Figure 10 ).  Using
this criterion for the Great  Miami River profile the 15 mile
segment from the Dayton STP to  Franklin, Ohio is clearly de-
graded, the lower Mad River and the  short portion of main river
in downtown Dayton is poor, and the  upper section of river as
well as the Stillwater River  would be classified as good
 (Figure 11 ).

     It may be that  this kind of  approach may be of value for
other rivers of this kind.  Would that there were clean rivers
                              356

-------
in the midwest which could be used as a comparison for the
majority.  In the absence of such desirable waters and taking
the optimistic view that some rivers may become less polluted
and environmentally upgraded, this community structure ap-
proach may be useful in gauging progress toward the desired
goal .
                             357 ,

-------
Table 3: Community values delineating  good,  intermediate,
         and poor fish communities  in  the  Wabash and Great
         Miami Rivers.

Parameter
No/km
Kg/km
Shannon-no .
Shannon-wt .
zwb
Great
Good
150
20
2 .0
1.5
7.5
Miami Rive
Intermed .
100
10
1.6
1.1
6.15
r
Poor
50
5
1.2
0.8
4.76

Good
60
50
1 .8
1.8
7 .60
Wabash Rive
Intermed .
45
35
1.4
1.4
6.48
jr
Poor
30
20
1 .0
1.0
5. 20
                              358

-------
                     ese
MEAN  COMPOSITE  INDEX -  I
                          WB
01    cn
                          00
40 320 300 280 260 240 220" 200 180
RIVER MILE
Figure 9: The composite index as it reflects environmental conditions
of the Wabash River in 1973-75 and 1977.
\\
\v—
—» e
i
0 , 	 '
Vv^
""«!
M
0 •
<5 CD
->l -vl
OJ ^
-J
Ol
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u JL
0^
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4
c.
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^®
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<
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— 	 —
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1
oj
\
V
\
\
o
1
s° ]
J "
cn
o
o
&
i
^-Delphi
^"'Tippecanoe R.
W. Lafayette STP
v-Lafayette STP
Eli Lilly
<- Black Rock
<— Big Pine Crk.
^-Attica STP
<— Olin Corp:
<— Covington STP
^~Big Vermilion R.
^-Cayuga EGS
"^^Inland Container
«— Sugar Crk.
<— Montezuma STP
<~~"Big Raccoon Crk.
<-EII Lilly
<— Clinton STP
^-Wabash EGS
<- Terre Haute STP
*— Honey Crk.
33
rn
o
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OJ
4^
01
cn
•>!
00
CO
O
—
^ i-fi (Ti ^l QO

-------
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                                                                  C
                                                                  O
                                                                  O
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coo
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CJ
CJ
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                                                                      td
                                                                      p;
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                                                         1977


                    340
                                                               240         220         200
                                              River Mile

    Figure 10: **«»£ «P««nt.tion of  the magnitude and  direction  of changes
                                                                                                                 180

-------
                                                 River Mile
CO

O-l
            pq
           c
           •H
           CD
           PQ
            i >.
              W.Carrollton
                      STP

            Miamisburg STP
                                     Hutchings  Dam
                               Chautauqua  Dam
                                                            t
t         t
Tait Dam   Steele Dam
                                                             Dayton STP
                Figure  ll;The composite index as it  reflects  environmental conditions
                          of the Great Miami River in  1976.

-------
References
Bechtel, T. J. and  B.  J.  Copeland.   1970.  Fish
     sity indices as  indicators of  pollution in
     Texas. Cont. Mar.  Sci.,  15:103-132.
                                     species diver-
                                     Galveston Bay,
Conn, C. C.  1972.   Biological  survey of the Mad River
     Cons. Dist. Report.   21  pp.  mimeo.
                                              Miami
Denoncourt, R. F.  and  J.  W.  Stambaugh, Jr.  1974.  An ichthyo-
     faunal survey  and discussion of fish species diversity  as
     an indicator  of water  quality,  Codorus Creek drainage,
     York County,  Pennsylvania.   Proc. Pa. Acad. Sci. 48:71-78.

Gammon, J. R.  1971.   The response of fish populations  in  the
     Wabash River  to heated  effluents.  Proc. Third Nat. Symp.
     Radioecology,  Vol.  1:513-523.

Gammon, J. R.  1973.   The effect of  thermal inputs on the  popu-
     lations of fish macroinvertebrates in the Wabash River.
     Water Res. Res. Center,  Purdue  U., Tech. Report No.
     32:105 pp.

Gammon, J. R.  1977.   The fish community of the Great Miami
     River near Dayton,  Ohio.   Report to Dayton Power and  Light
     Co., Dayton,  Ohio.   52  pp.  mimeo.

Gammon, J. R. and  J. M.  Reidy.  1980.  The role of tributaries
     during an episode of low dissolved oxygen in the Wabash
     River.  Warmwater Streams Symposium.  In press

McErlean, A. J.,  S. G. O'Connor, J.  A. Mihursky, and C.  I.
     Gibson.  1973.  Abundance,  diversity and seasonal  patterns
     of estuarine  fish populations.   Est. & Coastal Mar. Sci.  I

McErlean, A. J. and J. A. Mihursky.   1969.  Species diversity-
     species abundance of fish populations: an examination of
     various methods.   Proc.  22nd Ann. Conf. So. Coast  Assoc.
     Game & Fish  Comm. : 367-372.
Richards, J
     the Au
     Trans.
 S.  1976.  Changes  in  fish species composition in
Sable River, Michigan from the 1920's to 1972.
Am. Fish. Soc .   1Q 5 (.1) : 3 2-40 .
Teppen, T. C. and  J.  R.  Gammon.   1976.  Distribution and  abun-
     dance of fish populations in the middle Wabash River.
     Thermal Ecology  II  (ERDA Symp. Series) CONF - 75-425:
     272-283.
Todd, D. K.  1970.   The  water encyclopedia.
     Port Washington,  N.Y.  559 pp.
                                  Water Inf. Center,
Wilhm, J. L. and  T.  C.  Dorris.   1966.  Species diversity  of
     benthic macroinvertebrates in a stream receiving  domestic
     and oil refinery  effluents.  Am Midi. Nat. 76:427-449.
                              362

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Wilhm, J. L. and  T.  C.  Dorris.  1968.  Biological parameters
     for water  quality  criteria.  Bioscience  18:477-481.
                              363

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BIOTIC IMPACT OF ORGANIC AND INORGANIC SEDIMENTS
                                          J.K. BLAND
                                          Project Officer
                                          Water Quality Management Branc
                                          United States Environmental
                                            Protection Agency
                        365

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Introduction

     For the past two years I have functioned as a 208 program project
officer in the Ohio Water Quality Management Section of United States
Environmental Protection Agency (USEPA).  Prior to that time  I was  an
environmental educator at the Field Museum of Natural History and
was involved in several years of stream related work.  During this
period I have the followed the development of 208 water quality
management initiatives in several cities and states and have  had a
continual concern about the infusion of biological objectives into
those programs.  From my perspective we seem to be inordinately
concerned about water quality from a chemical standpoint  to the
detriment of clearly articulated biological goals and monitoring.
Most resource managers wouldn't think of grading the "quality" of
a prairie by its soil chemistries yet streams are continually "graded"
and managed largely on the basis of in-stream chemistries and waste
load allocations.  We don't deny the need for such chemical measurements
but feel that we have been spending a great deal of time  gauging
the "baby's bathwater" without looking at how the baby itself is doing.
Furthermore, in-stream chemical standards have too frequently been
developed on a state wide basis without recognition of the biogeo-
graphical distinctions necessary to give resolution to the standard
setting process.  In Region V I know of only one State, Illinois
(James Park, Illinois Environmental Proteciton Agency personal
communication), which is developing a biologically based  hierarchy
with which to generate stream use-classifications.

Gauging Biological Responses

     Institution of a set of management practices is based on the
assumption that the causal events of the system under study are
known, that the major determinants of the system are susceptible
to management, and that the effects of management will not be obscured
by contingencies.  If a set of "best management practices"is  to
be determined, it is necessary to have specific goals for the response
of the system/watershed being managed.  This is difficult because various
schools of biolog'ists have different concepts of what represents biological
integrity in a stream.  The stated goal of the Clean Water Act of
fishable, swimable, waters is too broadly stated to be meaningful
in actually judging the performance of a set of best management practices
within a watershed.  Several recent monographs published  by USEPA
have dealt with the problem of establishing a conceptual  framework
for setting management goals for watersheds (cf. "Toward  a Classification
for Watershed Management and Stream Protection" C. Warren, 1979,
U.S.E.P.A.-600-79-059; and "Impacts of Sediment and Nutrients on Biota
in Surface Waters of the United States."  Farnsworth, et.al,
EPA-600/3-79-105).  Currently, such goal setting has de facto reverted
to the states and areawide agencies.  What exists, as a consequence,
is a patchwork quilt of management perspectives and a variety of approaches
to the problem of watershed management.  In a situation where a scientific
consensus doesn't exist it is perhaps useful that a variety of approaches
does exist.  However, without a conceptual framework with which to
judge the effectiveness of these approaches there is no way to assess
their comparitive merits.  Restoring the chemcial, physical,  and biological
integrity of the nation's waters requires knowledge of the structural
and functional characteristics of natural aquatic ecosystems  and the
adoption of a systematic set of biologically based goals.
                                    366

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Organic Sediments

     Two broad classes  of sediments  can be distinguished,  organic
and  inorganic.   For  the purposes  of  characterizing in-stream impacts
of organic  sediments we will  outline the work of Ken Cummins (1975),
and  James Karr (1977a,  1977b).

     Cummins  (1974,  1975)  proposed a process-oriented,  functional
framework for for  analyzing running  water environments.   The framework
describes stream systems as a continuum beginning with  first, second and
third order streams  typical of  headwater environments through mainstem
streams segments.  As part of our slide presentation we will follow
a typical midwestern stream system (Hickory Creek) from a first order
stream reach  through its confluence  with the Des Plaines River at
which point it represents a fifth order stream.   Cummins distinguishes
the  various physical, chemical, and  biological differences characteristic
of the transition  in stream order.   A summary of these  differences
is given in table  No. 1 and diagramed in Fig. No. 1.

     Headwaters  portions of streams  (first, second, and third order reaches)
are  dominated by inputs from  stream-side vegetation.  Energy input
into the system  derives from  leaf fall, twigs, etc.  Levels of sunlight,
especially  during  the late spring and summer, are greatly reduced by
the  overhanging  vegetative cover  and as a consequence comparitively
little "primary  production" in  the form of algal communities originates
in this portion  of the  stream.  For  the same reason temperature
fluctuations  in  these reaches are more moderate.  Coarse Particulate
Organic Matter (CPOM) which is  deposited is processed by a community
of bacteria,  fungi and  macroinvertebrates adapted to this  type of
organic base.  Macroinvertebrate  communities are dominated by "shredders"
capable of dissecting and  processing leaves and  twigs (CPOM).  The
ratio of photosynthesis to respiration is less than one in these
headwater reaches, indicating that the system has a heterotrophic energy
economy dominated  by the import of organic matter from  the contiguous
terrestrial communities.   As  a consequence of the processing of
macroinvertebrate  communities CPOM is broken down and fragmented into
finer particles  or Fine Particulate  Organic Matter (FPOM)  which is
subsequently transported downstream.   Coarse sediments  in  the form
of rubble and gravel dominate the bottom surface of the  stream.  Fish
communities are  characterized by  headwaters species which  are largely
insectivorous.   Cummins (1975) has estimated that the biota processes
about 80 percent of  the Particulate  Organic Matter (POM) and 50 percent
of the Dissolved Organic Matter (DOM)  in first through  third order
streams.

     In mid-reaches of  the stream continuum (fourth through sixth order
streams) the basic energy  economy of the system  shifts.  Stream width
increases, overhanging  vegetation no longer  provides dense shading, and
available light  and  substrate increase to the degree that  substantial
primary production can  now take place.   The ratio of photosynthesis
to respiration shifts to a value  greater  that one indicating that the
system is no longer predominately heterotrophic.   Upstream import of
both CPOM and FPOM is still taking place  with FPOM the dominant variety
of import material.  As  a  consequence  a varied assemblage  of macro-
invertebrates inhabit these reaches.  Grazers,  which feed off algal
forms originating  in these reaches,  are  an  addition to the invertebrate
fauna, and a variety of  "collectors"  or  filter feeders  is  common.
Fish populations include insectivores  and piscivores (fish eaters).


                                   367

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             STREAM  ORDER
STREAM  ORDER
STREAM ORDER

GO
•
00

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     Figure -i   A theoretical diagrammatic representation  of certain changes in
                structure function in running water  ecosystems from headwater
                to the mouth (stream order shown at  the  left).  The organisms
                pictured are merely possible representatives of the functional
                groups shown (A).  The decreasing direct influence of the adjacent
                terrestrial component of the watershed and increasing importance
                of upstream import from the headwaters  (B, orders 1-3) to the
                mouth is a basic feature of the system.  Coupled with this is a
                decrease in shredders and an increased dominance of collectors.
                The mid-region of the river system is seen as the major region
                of primarily production (growth of green plants) and associated
                grazer populations  (C, orders 4-6).   The lower reaches become
                more turbid with increased importance of plankton  (D, orders 7-12).
                The fishes are dominated by invertivores in the headwaters, and
                piscivores in the larger sections with planktivores important in
                the highest order.
Torn K.Cummins,1975;"The  Ecology of  Runnin.j  WaLors;Theory and Practice",
              ±-£iLJ:J!£-^^^
                                               369

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       Table 1.  General characteristics of running uaters clustered into three stream order groupings.

Stream
Orders



1-3




4-6








7-12







Size
Small, head-
vater
springs
and streams.



Medium sized
rivers.







Large
rivers.







Ueteroirophy
Autoirophy '
He tero trophic
(P/R<1,
see Table 2).




Autotrophic
(P/R >1,
(see Table 2).







He tero trophic
(P/R <1,
(see Table 2).





Organic Matter
Inputs of
Terrestrial Origin
Of major
importance.
Coarse
particulate
organic matter
(CPOM)
dominant.
Of moderate
importance.
CPOM less
significant,
fine
particulate
organic matter
(FFOM) from
upstream of
greater
importance
Of minor
importance.
F?OM frora
upstream
dominant




'•'rim.iry
Production
Of minor
importance;
some algae
and mosses.



Of major
importance;
algae and
vascular
hydrophytes






Of moderate -to
minor
importance;
primarily
planktonic.




Light
Regime
Heavily
shaded.





Little
shading,
good
light
penetra-
tion.





Little
shading,
poor
light
penetra-
tion due
to
turbidity.

Temperature
Regirce
Lesser daily
tei.iperaturc
fluctuation
(shading and
groundwater
effect).

Greater daily
temperature
fluctuation
(open, less
groundwater
effect) .





Lesser daily
temperature
fluctuation
(moderation
by large
volume)



Document
Sediments
Coarse






Coarse and
fine.







Fine







                                                                                                       o
                                                                                                       f~~
                                                                                                       oo
From K.Cummins,1975;"The Ecology of  Running Waters;Theory and  Practice",

in Procoodinqa   ftho  Sandur.k

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     Further downstream  (seventh to twelveth order)  the  stream energy
economy again shifts and becomes heterotrophic.  The stream has become
deeper, it has collected more upstream sediments,  it has a higher
nutrient load, and attached algal forms are no longer as common as
they were in the mid-reaches.  The increased turbidity reduces light
penetration, the potential for photosynthesis is reduced,  and  substrate
availability is reduced  for bottom attachment of periphyton.   Primary
production and photosynthesis take place through free floating algal
forms and a greater diversity of planktonic forms  develop.   The
macroinvertebrate community is dominated by "collector"  organisms.
Fish populations of the  large rivers will  include  a  large variety
of planktivores along with other varieties of fish eating and  insect
eating species.  It will be apparent that  regional and seasonal variations
must be superimposed on  Cummins archtype.

     Potential implications of such a functional-process oriented
framework for stream management become apparent if we consider the
decision to locate a sewage treatment plant outfall  pipe.   A sewage
treatment plant discharges DOM and FPOM from its outfall pipe.  The
impact of such materials for the in-stream energy  economy and  the
fisheries and macroinvertebrate communities would  require not  only
a consideration of concentrations of chemical parameters but an estimation
of overall organic loads, a consideration  of the position of the outfall
pipe along the stream continuum, and a gauging of  the significance of the
sewage treatment plant organic discharge against "normal"  or "typical"
in-stream organic loads.

     Karr and Dudley (1977a) adopted the major elements  of Cummins framework
to analyze point and non-point source impacts to Black Creek,  an agricultural
watershed in Northeastern Indiana, which had been  targeted as  a demonstration
basin for the application of agricultural  best management practices.
Their analysis indicated that Black Creek  had shifted to an autotrophic
system through considerable portion of its length  instead of maintaining
the "normal" heterotrophic energy economy.  Ecological factors which
they felt were tied to resource degradation included the following
(modified from Karr and  Dudley, 1977a):

     1.  Large comparitive contributions of FPOM from sewage treatment
plants

     2.  Large comparitive contributions of simple nutrients from  both
point and non-point sources.

     3.  Loss of stream  side vegetation with subsequent  increases  in
in-stream solar energy,  and a reduction in input of  CPOM.   Algal
populations increase in  response to this and item  #2.

     4.  Exageration of  temperature and dissolved  oxygen values as a
consequence of the loss  of stream-side vegetation.
                                    371

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     5.  Ditching, channelization, and drainage manipulations resulting
in the loss of in-stream habitats and substrates.

     6.  Removal of natural vegetation and the construction of drainage
networks resulting in the alteration of seasonal drainage patterns.

     Karr and Dudley (1977a) reemphasized in their study that the
biological integrity of a watershed can only be gauged by a functional/
structural framework which looks at the three major classes of variables
impacting stream systems.  These variables include a characterization
of:  1) the energy relationships of the system 2) the water quality of
the system and 3) the character of the habitat.  An approach which
looks at only one of these areas will be doomed to failure since the
other factors have the ability to impact the biological integrity
of the system being considered.

Impacts of Inorganic Sediments

     Several comprehensive literature reviews on the effects of sediment  on
biota have recently been published by the USEPA (cf. "Impacts of Sediment
and Nutrients on Biota in Surface Waters of the United States", Farnsworth
et. al, 1979; and "Effects of Suspended Solids and Sediment on Reproduction
and Early Life of Warmwater Fishes", 1979, Muncy et.al).  Sediment per se
has long been recognized as a potential pollutant.  Smith (1971) estimated
that "silt" (largely of agricultural origin) was the principal factor  involved
in the destruction of Illinois native fisheries.  He judged that 2 species
of fish had been decimated and 14 species had undergone range reductions
as a consequence of the impacts of silt.  Milton Trautman (1957), the
chronicler of Ohio fisheries history, similarly states, "Studies made  since
1925 have proved that since then, if not before, soil suspended in water
has been the most universal pollutant in Ohio, and the one which has most
drastically affected the fish fauna."

     Inorganic sediments are generally assigned on the basis of size and
physical method of transport to:

     1.  Suspended load:  particles maintained in the water column by
         turbulence and carried with the flow of water; and

     2.  Bed load:  particles resting on the stream bed and pushed or
         rolled along by the flow of water.

     Suspended loads typically are compromised of silts and clays supplied
by the watershed.  Bed load is composed of larger particles including
sand and gravel which are not typically a part of the water column.
Biotic impacts of bed load movement are generally attributable  to
abrasion, scour, and burial.  Suspended load increases turbidity, and
may interfere with photosynthesis and/or respiration.  Impacts of sediment
on biota as described in Farnsworth, et.al, 1979 and Muncy et.  al,
are summarized in Table No. 2.  Farnsworth, et.al (1977),  indicate  that
a number of factors interact with sediments to determine the ultimate
impact on a particular ecosystem.  Such factors include discharge,
temperature, bottom type, light, nutrients, pesticides, metals, and
dissolved gases.  These  factors interact confdunding an explicit  reading
of the impact of sediments on the biota.
                                     372

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TABLE NO. 2 BIOTIC IMPACTS of SEDIMENT as ADAPTED from FARNSW3RTH
	et.al. (1979) and MUNCY, et. al. (1979)	
TROPHIC LEVEL
                             IMPACT
PRIMARY PRODUCERS

(Attached algal forms
planktonic algal forms,
and macrophytes)
                              Increase in turbidity of water column
                              with subsequent reduction in photosynthetic
                               activity	
                              Increase in associated nutrient levels
                              with subsequent increase in algal growth	

                              Siltation of microhabitats and substrates
                              resulting in a reduction in attached algal
                              forms.	

                              Scouring and abrasion of microhabitats
                              resulting in a reduction of attached algal
                              forms	

                              Impacts on primary producers as a consequence
                              of associated heavy metals and or toxics
MACROINVERTEBRATES
                              Avoidance of adverse conditions by migration,
                              and drift

                              Increased mortality from sedimentation due
                              to physiological effects, burials, and physical
                              destruction.	

                              Reduced rates of reproduction resulting from
                              physiological effects, changes in suitable
                              substrates, and loss of early life stages	

                              Modified rates of growth and reproduction
                              caused by habitat modification and changes
                              in type and availability of. food.
                              Modification of natural movements, habitat
                              exploitation, and migration patterns.	

                              Increased mortality of adults and juveniles
                              resulting from abrasion an smothering
                              of gill tissue by fine sediment.  This may also
                              act indirectly in the form of decreased
                              resistance to stress.	

                              Suppressed development of fish eggs and larvae

                              Reduced abundance and availability types of food
                              with subsequent chnages in species composition
                              and biomass.
FISHERIES
                                    373

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     Muncy, et.al. (1979) extensively reviewed the literature on  the
impacts of sediment on fisheries.  Early field studies equated extremely
high suspended sediment concentrations with direct mortality.  More
recent studies have indicated that different species and year classes
of fishes are not equally susceptible to various types and levels
of suspended sediments.  The authors conclude that the large volume
of studies done to date describe "indirect evidence" of the impacts
of sediment.  They propose that substantial controlled laboratory studies
are needed to elaborate and corroborate suspected fisheries impacts.

     As with organic sediments the resource manager is faced with problem
of determining what is a "normal" or "allowable" sediment load and
what is an "acceptable" biological response.  Existing allowable  sediment
yields have been defined by the Soil Conservation Service for various
types of soils, agricultural practices, and topography.  Farnsworth, et.al.
(1979) suggest the formulation of regional goals based on biogeographic
or ecological regions.  We wish to reiterate the need for adoption of  a
systematic set of goals based in a review of functional/structural
biological perspectives.
                                    374

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REFERENCES
Cummins, K.W. 1974.  "Structure and Function of Stream Ecosystems,"
  Bioscience. 24:631-641

Cummins, K., 1975, "The Ecology of Running Waters, Theory and Practice"
  in Proceedings of Sandusky River Basin Synposium, Ed. D. Baker et. al.,
  Pub. of Int. Joint. Commission p. 277-293

Farnsworth, E. et.al., 1979, Impacts of Sediment and Nutrients on Biota
  In Surface Waters of the United States, USEPA pub. EPA-600/3-79-105

Karr, J. and Dudley, D. 1977(a), "Biological Integrity of a Headwater Stream:
  Evidence of Degradation, Prospects of Recovery," in Environmental
  Impact of Land Use on Water Quality; A Final Report on the Black Creek
  Project, Ed. J. Morrison, USEPA pub., EPA-905/9-77-007

Karr, J. and Schlosser, I, 1977(b), Impact of Nearstream Vegetation and
  Stream Morphology on Water Quality and Stream Biota, USEPA pub., EPA-
  600/3-77-097

Muncy, R. et.al, 1979, Effects of Suspended Solids and Sediment on Reproduction
  and Early Life of Warmwater Fishes;  A Review, USEPA pub. EPA-600/3-79-042

Smith, P. 1971, Illinois Streams;  A Classification Based on Their Fishes
  and on Analysis of Factors Responsible for Disappearance of Native Species,
  Bio. Notes no. 76, pub. 111. Nat. History Survey, 14p.

Trautman, M. 1957, Fishes of Ohio, Ohio State Univ. Press., Columbus Ohio,
  68 3p.

Warren, C., 1979, Ttoward Classification and Rationale for Watershed
  Management and Stream Protection, USEPA pub. EPA-600/3-79-059
                                    375

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                           CONFERENCE SUMMARY

                          Clifford Risley, Jr.
                         Senior Science Advisor
                    Surveillance & Analysis Division
                            US EPA, Region V
                           Chicago, IL  60605

My closing remarks are to be a summary of the highlights of this seminar.
1 want to apologize to all of the speakers whom we had to cut short.  We
knew this would happen.  We took a deliberate risk when we planned this
seminar.  We knew, when we put it together and when we invited these
speakers; the kinds of work they have been doing; the importance of their
work; and we knew that it was impossible for them to cover their experience
in such a short time.  We wanted, though, to expose you to this particular
variety of people so that you would be aware of what they have been working
on and what their experiences have been.

We are going to put out a seminar publication.   The complete text of the
seminar papers will be in this publication so that any of the papers which
have struck you as being of particular interest to you will be readily
available to you.  This is one way in which you can go a little further
into the work that has been undertaken.

Another way open to you, now that you have been introduced to these people,
will be for you to personally follow up with them concerning those areas
which are benefical to you.  This can benefit the work in two ways.  You
can go to them for their knowledge and their help and also you can go to
them with your experiences and your inputs to their work.
                                   377

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The same opportunity exists to contact those of us who work in the
management areas in EPA and in the state and local regulatory agencies.  We
can all benefit from this exchange of ideas.  We feel that the greatest
outcome of this seminar is to stimulate such an exchange and find out
who is doing what.

Until recently, the non point source work has been taking a back seat in
EPA.  In going back far enough into the fifties and sixties, before the
kind of legislation we have today, those of us who go that far back were
involved in looking at stream water quality; looking at water quality
criteria, ways to improve quality and the costs of cleanup; the very things
we were talking about here today.  However, there is no doubt in my mind,
for those of us who had that experience, that we were then greatly con-
cerned about point source pollution.  Where we had uncontrolled point
source pollution, our streams were being seriously affected.

The legislation of 1972, the Water Quality Acts, properly, I think, put
the focus on the point source pollution and said: "we have to eliminate
point sources."  Congress said, in effect:  "we have to require everyone to
go to secondary treatment.  We have to eliminate the industrial discharges."
And they set up the mechanism of enforcement powers and grants in order
to do this.

I think the decade of the 70's was, then, the decade of enforcement.   In
the seventies we said:  "Let us go out and put a stop to all these
discharges."  We are pretty well  into that process.  Now, we are far enough
along that we have discovered that we have other inputs.  I don't think we
realized how much of a contribution we got from non point inputs back  in
                                   378

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the sixties.  We learned this during the seventies while many of us were
still working on these problems.  At the same time we felt frustrated that
we couldn't do anything about it.

The agency is now taking the view that:  "We have done all this point source
pollution work and we still have degraded water quality!  Why?  The agency
realizes that non point source pollution is there and some controls have
to be made.

We are still moving forward and I am looking forward to the decade of the
eighties, when we look again at water quality with renewed knowledge.  We
know, now, many of the things that we have to do to achieve better water
quality.  We are going to go back to more monitoring despite the views of
one of the speakers who said "monitoring is not working and what we need
to do is modeling."  I think monitoring is important and we are going to
go back to doing more monitoring.

That is not to say that modeling is not important.  The fact of the matter
is, that since the publication of PL 92-500, the EPA has not had an adequate
management model to serve as a guideline to the states to evaluate non point
source pollution.  We feel that a process is urgently needed to evaluate
non point pollution abatement costs and compare them to conventional point
source abatement costs.  You have heard this before.  This is what I started
off the Seminar by saying.  This is why we had this seminar: to stimulte
the development of another model, if you will, only this model is to be a
desk top model that we could all use to get a handle on the trade offs—the
management trade offs.
                                  379

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The emphasis on this seminar has been to this end.  We have heard many
good inputs describing what some of these trade offs are.  I was pleased
to find that many of the speakers are aware of this and they are
suggesting various trade offs in their area of specialization.  I think
the message is there, across the board, in all of our areas of expertise.

Following are some additional points made during the seminar that I feel
are worthy of repeating, for emphasis.  Basically what did the seminar say?
Well, it says:  "What are we going to emphasize in each basin?  In one
basin controlling waste water treatment plants might be the major impact
and maybe that's all we need to control.  In another basin, control of point
sources may not be of any great consequence at all, and we have to go back
and look at the impacts of "the cornfield," if you will, and determine the
erosion loss in a certain sector.  We have learned that in some of these basins,
you don't have to clean up an entire basin.  All you-have to do is find
the critical areas and put your best management practices to work in those
few critical areas.  All of this says that we have to integrate point
source and non point source in all kinds of management.  It all has to be
integrated.  We must all get the big picture and start looking at all
phases of it before we enter into the final decision making.

Don Urban once said to me, that we have been spending 45 years trying to
get the land owners to implement best management practices.  We were doing
it on the basis of saving their own land.  We didn't get very far with that.
Now we want them to implement best management practices to protect our vital
water resource, and we're not going toLget any place with them again, on
the same basis we have tried to for the last 45 years. That is, to expect
them to do this strictly on a voluntary basis.
                                   380
                                      r

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So, I think we have to do things like they did in Black Creek.  To find
what it is that makes good sense to the landowners and what the incentives
are to get the landowners involved in this process.  It means we have to
obtain some monetary support for them.  We must provide a lot of guidance;
a lot of loving and tender care, which was best said by Dan McCain when he
explained the process he went through working with the landowners.  He said
that he had to get out there and marry them.  He had to live with them every
day and help guide this process.  I think that in order to make the whole
process work, when it comes to best management practices, this is what you
are going to find.  If you have somebody at the local level who understands
the problem and who is willing to get in there and work like this, then
something can happen.  If you have nobody like this at the local level,
I don't think somebody sitting in Chicago, behind the desk, saying this is
a good plan and this is the best model, is going to have any effect at all.
An even less effect will be accomplished from Washington deciding that if
we spend a million dollars on three or four projects, it is going to solve
our problem.  No way.  We have to get to the local level to get the kind
of program that will work there.  This is not to say that we don"t need
the planners and the modelers and the professors.  We do.  We have to have
this kind of thinking behind it to guide the way.

One of the things that came out in the Seminar is the fact that we have
been tripping over each other models.  Everybody comes up with their model
and thinks this is the way to go and the only way to go and I think that it
came very clear to me that there are several models that are very valuable
and they are valuable for different purposes.  We should make use of these.

We shouldn't get so involved in one particular approach that we think
we've got the only answer.  We can modify what we are doing.  If we are
working on a large scale basis, we need one kind of model and if we are
working on a smaller scale basis we need another kind of model.  We need
to use the small scale model to get better inputs to use on our larger
model.
                                     381

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With all these approaches come criticism of what someone did in the past,
or what they are doing now, or what they didn't do.  I know, and you know,
that we all do as much as we can within the resources that we have.  I
don't think we should criticize somebody for not having done something more
than they did.  I think they have all done the best they could from their own
geographic area, their own particular background and training.  All of these
inputs—and I think we heard a great many of them from different sources
today—all of them are valuable to us.  I think we should embrace the exper-
tise and the outputs of these experts and make use of them in solving our
own particular problems.

I want to thank all of you who have stayed through to the end.  I applaud
you for this.

I want to applaud all the speakers and the moderators for their presentations.
I think they were excellent.

I hope that we have provided you with an update on the need for integrated
planning and consideration of integration and trade offs in your decision
making.  We tried to introduce you to some of the Who's Who in the forefront
of Water Quality Management and what they have been doing, and as I said
before, I hope you will follow up on this seminar by contacting these people
and letting them know what you think of what they are doing, and let them
know what you are doing.

Let's work together to try to achieve the goal of clean water tht we have
all been working toward.  Thank you all again.  This officially closes the
seminar.
                                 382

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                      Attendees for September 16-17 Seminar
                         Pick Congress Hotel, Chicago, IL
John B. Adams
Director, Environment and Food Regulatory
  Affairs
National Milk Producers Federation
30 F. Street, N.W.
Washington, D.C.  20001

John R. Adams
U.S. Army Engineer District
Buffalo, NY 14127
Mark Alderson
U.S.EPA-5WWQ
230 S. Dearborn
Chicago, IL  60604
David Beasley
Ag. Eng. Dept.
Purdue University
W. Lafayette, IN  47907
Howard Allen
Project Hydrologists
U.S. Geological Survey
Post Office Box 427
DeKalb, IL  60115

Joan G. Anderson
PCB
309 W. Washington
Chicago, IL  60606
David Baker
Professor
Heidelberg College
Tiffin, Ohio
Joan Balogh
1815 University Avenue
Madison, WI
Dr. Michael J. Barcelona
Head Aquatic Chemistry Section
IINR-State Water Survey Division
Box 232
Urbana, IL  61801

Jim Baumann
Wisconsin Department of Natural
  Resources
Post Office Box 7921
Madison, WI  53711

John Becker
Environmental Planner
NOCA
1501 Euclid Avenue
Cleveland, OH  44115

Bob Bellandi
Asst. Proj. Director
Central NY Regional Plan, and Dev. Bd.
700 E. Water Street
Syracuse,  NY  13210

William Benjey
USEPA-Region V
Chief, Ohio Water Quality Mgmt. Sectior
230 S. Dearborn
Chicago, IL  60604

James Bland
USEPA-Region V
Ohio Water Quality Mgmt. Section
230 S. Dearborn
Chicago, IL  60604
                                       383

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Lee Cunningham
Administrator Assistant
Illinois Pollution Control Board
309 W. Washington Street
Chicago, IL  60606

Tom Davenport
Environmental Protection Agency
2200 Churchill Road
Springfield, IL  62706
Jon V. DeGroot
Assistant State Conservationist
USDA Soil Conservation Service
316 N. Robert Street, Room 200
St. Paul, MN  55101

Basin Dihu
S&A-CDO, IL/IN Field Inv. Section
536 South Clark Street
Chicago, IL  60605
Roderick A. Oorich
Grad Research Assistant
Purdue University, Agry Dept.
West Lafayette, IN  47907
Ron Drynan
Senior Engineer
Great Lakes Regional Office, IJC
Windsor Ontario, Canada
Jacob D. Dumelle
Chairman, IL Pollution Control Bd.
309 W. Washington Street
Chicago, IL  60606

Doug Ehorn
USEPA-5WQM
Chief, Michigan Water Quality Mgmt. Sec,
230 S. Dearborn
Chicago, IL  60604
Mr. Richard Cahill
Associate Chemist
Illinois State Geological Survey
322 Nat. Res. Bldg.
Urbana, IL  61801

Randolph 0. Cano
Project Officer
USEPA-Region V-5WWQM
230 S. Dearborn Street
Chicago, IL  60604

Howard Essig
Illinois EPA
1701 First Avenue
Maywood, IL
Ronald C. Flemal
Professor of Geology
Northern Illinois University
Dept. of Geology
DeKalb, IL  60115

Christopher R. Freeman
Environmental Planner
MACOG
1120 County-City Bldg.
South Bend, IN  46601

Jeffery Gagler
Water Quality Modeler
USEPA-Water Quality Policy Section
230 S. Dearborn
Chicago, IL  60604

Robert Gallucci
Monroe County Pure Waters
65 Broad Street, Room 100
Rochester, NY  14614

James R. Gammon
Professor of Zoology
DePauw University
Greencastle, IN  46135
                                        384

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Albert A. Almy
Department of Public Affairs
Michigan Farm Bureau
Post Office Box 20960
Lansing, MI  48909

Ralph G. Christensen
Ecologist
Great Lakes National Program Office
USEPA-Region V
536 South Clark Street
Chicago, IL  60605

Roy Christenson
WDNR
26 Breese
Madison, WI
Mary Cock!an
P.O. Box 68
Maple Park, IL
60151
 Evelyn Cooper
 Surveillance and Analysis Division
 USEPA-Region V
 230 S. Dearborn
 Chicago,  IL  60604

 Terry E.  Cox
 IL Pollution Control Board
 309 W. Washington,  Rm. 300
 Chicago,  IL  60606

 John Crumerine
 Manager,  Honey Creek Watershed  Project
 Tiffin, OH
 Elizabeth  Cunningham
 Environmental  Engineer
 CT  208  Program
 Post Office  Box  1088
 Middletown,  CT  06457
                                  Jeffery B.  Bode
                                  WDNR
                                  Milwaukee S.E., WI   53213
                                  Susan Boldt
                                  USEPA-5WWQM
                                  230 S. Dearborn
                                  Chicago, IL  60604
                                  Dan Bondy
                                  Great Lakes Regional Office, IJC
                                  Windsor Ontario, Canada
James Bosch
Mgr. Env. Engineering
Land 0 Lakes, Inc.
614 McKinley Place
Minneapolis, MN  55413

Donald E. Brand, P.E.
Project Officer
Balto. Co. Dept. of Health
401 Bosley Ave. - 4th Floor
Townson, MD  21204

Charles Brasher
USEPA-5WWQM
230 S. Dearborn
Chicago, IL  60604

James Brentlinger
Fieldman
State Soil & Water Conservation  Commit,
Room #7, AGAD Bldg. Purdue Univ.
West Lafayette, IN  47907

Marcia (Marcy) Brooks
Environmental Programs  Coordinator
South Central MI  Planning Council
70  E. Michigan
Galesburg, MI  49053
                                          385

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Bill  El man
FUWQPA
Neenah,  WI
Wayne El son
USEPA-5WWQM
230 S. Dearborn
Chicago,  IL  60604
Gary Erickson
Regional  Fishery Biologist
Illinois  Department of Conservation
110 James Road
Spring Grove, IL  60081

Wayne Gorski
USEPA-5WWQM
230 S. Dearborn
Chicago,  IL  60604

Jon T. Grand
WDNR
4049 Cherokee
Madison,  WI
John R. Gray
Project Hydrologists
U.S. Geological Survey
Post Office Box 427
DeKalb, IL  60115

Dr. David Gross
Associate Geology
Illinois State Geological Survey
264 Nat. Res. Bldg.
Urbana, IL  61801

Edwin Hammett
Director of Regional Planning
TMACOG
123 Michigan St.
Toledo, OH  43624

Albert Horner
Eng. Qua!. Manager
S.  Carolina  Dept.  Env.  Control
2600 Bull Street
Columbia, SC  29210
Linda A. Gawthrop
USEPA-Region V
230 S. Dearborn
Chicago, IL  60604

Raymond Giese
Project Officer
USEPA
230 S. Dearborn Street
Chicago, IL  60604

Irvin G. Goodman
Illinois Pollution Control Board
309 W. Washington, Room 300
Chicago, IL  60606
Thomas M. Heidtke
GLBC
Ann Arbor, MI
Bob Hennigan
Project Director
Central NY Regional Plan. & Dev. Bd,
700 E. Water Street
Syracuse, NY 13210

Henry J. Hess
Chem. Engineer
CDO, S&A Div. USEPA
536 South Clark St. Room  1008
Chicago, IL  60605

Marian Hirt
USEPA-Region V
230 S. Dearborn
Chicago, IL  60604
J.S. Horn
717 Birch Road
Lake Bluff,  IL  60044
James Hanlon
USEPA-5WEEB
230  S.  Dearborn
Chicago,  IL   60604
                                         386

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William J. Horvath
Regional Representative
Nat. Assoc. of Conservation Districts
1052 Main Street
Stevens Point, WI  54481

George Horzepa
Acting Program Manager
NJ Dept. Envir. Prot. Water Resources
P.O. Box CN-029
Trenton, NJ  08625

Larry F. Muggins
Professor
Purdue University
W. Lafayette,  IN
Garth Jackson
University of Michigan
Ann Arbor, MI
Eileen L. Johnston
Environmental Educator
505 Maple Avenue
Wiltnette, IL  60091
Robert S. Jonas
39 Rockhill Road
Rochester, NY 14618
Don Jos if
WQMP-USEPA-Region V
230 S. Dearborn
Chicago, IL  60604

Chun-Wei Kao
Research Associate
Michigan State University
Crop and Soil Science Dept.
East Lansing, MI  48824

John A. Kill am
R. 1
Jacksonville, IL  62650
Peggy Harris
USEPA-5GLNP
536 South Clark Street
Chicago, IL  60605
Jonathan Harsch
The Christian Science Monitor
100 N. LaSalle St. #600
Chicago, IL  60602
Joe B. Hays
RC&D Coordinator
Hoosier Heartland RC&D
54 Boone Woods
Zionsville, IN  46077

Al Krause
Environmental Scientist
USEPA-5WEEB
230 S. Dearborn
Chicago, IL  60604

Joe Kruz
Aquatic Biologist
Wisconsin Department Natural Resources
P.O. Box 13248
Milwaukee, WI  53213

Madeline Lewis
USEPA-5WQMB
230 S. Dearborn
Chicago, IL  60604

Terry Logan
Professor
Ohio State University
Columbus, Ohio

John Lowrey
Soil Conservationist
USDA-SCS
P.O. Box 475
Lisle, IL  60532

Darrell McAllister
IDEQ
Des Moines,  Iowa
                                         387

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 Dale  Luecht
 USEPA-WD
 230 S. Dearborn
 Chicago,  IL 60604

 Richard W. Lutz
 Head  Impact Analysis Section
 Div.  of Planning, IL Dept. Conservat,
 601 Stratton Bldg.
 Springfield, IL  62706

 Noel  W. Kohl
 Chief, IL/IN Wqm. Section
 USEPA-Region V, Water Division
 230 S. Dearborn
 Chicago,  IL  60604

 Ron Kolzow
 USEPA-Region V
 Chicago,  IL  60604
Madonna F. McGrath
Director, Great Lakes National Program
  Office
USEPA-5GLNP
536 S. Clark Street
Chicago, IL  60605

Donald M. McLeod
VA State Water Control Board
Roanoke, VA 24019
Steven E. Mace
Wisconsin DNR
P.O. Box 13248
Milwaukee, WI 53226
Michael MacMullen
Chief, Water Quality Policy Section
USEPA-Region V
230 S. Dearborn
Chicago, IL 60604
 Bob  Kirschner
 NIPC
 400  W.  Madison
 Chicago,  IL  60606

 David  Klinedinst
 111  Dept.  Cons
 Springfield, IL
 LeLand J. McCabe
 Director, Epidemiology  Div.
 USEPA-HERL
 Cincinnati, Ohio
Dan McCain
District Conservationist
USDA-SCS
Fort Wayne,  IN

Edward G. Maranda
Twin Cities Metropolitan Council
300 Metro Square Bldg.
St. Paul, MN 55101
Russell J. Martin
USEPA-Region V
230 S. Dearborn
Chicago, IL  60604

Bob Martini
Water Quality Analyst
Wisconsin DNR
Box 818
Rhinelander, WI 54501

Gertrude Matuschkovitz
Environmental Protection Specialist
USEPA
230 S. Dearborn Street
Chicago, IL  60604
                                      388

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Orville Macomber
Environmental Engineer
USEPA-CERI
11280 Foremark Drive
Cincinnati, OH  45241

Peter G. Meier
Associate Professor
The University of Michigan
2516 SPH 1, 109 Observatory
Ann Arbor, MI  48109

Tom Mitchell
Water Resources Planner
USEPA
230 S. Dearborn Street
Chicago, IL  60604

E.J. Monke
Ag. Eng. Dept.
Purdue University
W. Lafayette, IN 47907

Tim Montieth
Water Resource Engineer
GLBC
Ann Arbor, MI
 Ron Mustard
 Director, Office of Environmental
  Review
 USEPA-Region V
 230 S. Dearborn
 Chicago,  IL  60604

 Michael T. Phillips
 Senior Env. Planner, Water Div.
 USEPA
 230 S. Dearborn Street
 Chicago,  IL 60604

 John Piccininni
 USEPA-Region V
 230 S. Dearborn Street
 Chicago,  IL  60604
Fred Madison
Project Director
Washington Co. Project
U. of Wisconsin
Madison, Wisconsin

Larry I. Madsen
Wheatland, ND
Joe Magner
Soil Scientist
MN Pollution Control Agency
1935 W. County Road B-2
Roseville, MN  55113

James L. Magruder
Ground Water Age
Elmhurst, IL
Thomas F. Maher
Environmental Engineer
USEPA-Region  II
26 Federal Plaza
New York, NY  10278

John S. Nagy
Project Officer
USEPA Region  V
230 S. Dearborn St.  5WWQ
Chicago,  IL   60604
 Vladimir  Novotny
 Associate Professor
 Marquette University
 1515  W, Wisconsin
 Milwaukee,  WI   53233
 Jeffery  Nedelman
 Administrative  Assistant
   Senator  Gaylord  Nelson
 Wisconsin
to
                                         389

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Nancy Prehler
USEPA-5GLNP
536 S. Clark Street
Chicago, IL  60605
Barry O'Flanagen
WDNR
Box 7921
Madison, WI 53207

Bernie Orenstein
USEPA-Region V
230 S. Dearborn Street
Chicago, IL  60604
Jame Pendowski
EPA
2200 Churchill Road
Springfield, IL  62706

Mary Ann Rodewald
USEPA-Region V
230 S. Dearborn
Chicago, IL  60604
Richard Rising
Senior Planner
Monroe County Dept.
39 W. Main Street
Rochester, NY 14614
of Planning
Clifford Risley
Senior Science Advisor
USEPA-Region V
536 S. Clark Street
Chicago, IL 60605

J. H. Rolfes
One Wheaton Center, Suite 1901
Wheaton, IL  60187
Angela H. Preston
Water Quality Coordinator
Indiana Heartland Coording Com.
7212 N. Shadeland Ave., #120
Indianapolis, IN  46250

Hoody Price
Seminole County Planning
Courthouse
Sanford, FL  32771

J. Steve Reel
Assistant to Director
South Florida Water Management Dist,
P.O. Box V
West Palm Beach, FL  33402

Don Roberts
USEPA-Region V
230 S. Dearborn
Chicago, IL  60604

Phillip D. Peters
Assistant Director
Plans and Programs
Northeastern IL Planning Commission
400 W. Madison Street
Chicago, IL  60606

John Pfender
Water Quality Planner
Madison, WI
                             Richard Parkin
                             USEPA-WD WQMB
                             230 S. Dearborn Street
                             Chicago, IL  60604
                             Rob Striegl
                             Project Hydro!ogist
                             U.S. Geological  Survey
                             P.O. Box 427
                             DeKalb, IL  60115
                                         390

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William H. Sanders III
Director, S&A
USEPA-Region V
536 South Clark Street
Chicago, IL  60605

Wesley D. Seitz
Prof, of Univ. of IL
305 Mumford Street
Urbana, IL 61801

Herb Selbrede
National Milk Producers
Rt. 1
Sparta, WI
Pat Sharkey
IL Federal Liason
IL Pollution Control Board
309 W. Washington
Chicago, IL 60606

Gerald Sipple
RR 3, Box 187
Menomonee, WI
William Sonzogni
Water Resources Scientist
Great Lakes Basin Commission
Ann Arbor, MI

Gary Stewart
Govt. Affairs Coordinator
Michigan Manufacturers Assn.
124 E. Kalamazoo Street
Lansing, MI  48933

Randall Wade
WDNR
1220 Rut!edge Street
Madison, WI
A.T. Wallace
CE Dept.
Univ. of Idaho
Moscow, Idaho
David Stringham
Regional Program Coordinator
USEPA-Region V
230 S. Dearborn Street
Chicago, IL 60604

Rose Ann Sullivan
GLBC
Ann Arbor, MI
Jeffrey A. Taylor
Water Resources Engineer
VA State Water Control Board
2111 N. Hamilton Street
Richmond, VA 23230

Mike Terstriep
Engineer, IL Water Survey
Box 232
Urbana, IL 61801
Nelson Thomas
USEPA
9311 Groh Road
Grosse He, MI

Lowell Thompson
Metro Council
300 Metro Square Bldg.
St. Paul, MN 55101

Don Urban
Nonpoint Coordinator
EPA-Region V
230 S. Dearborn Street
Chicago, IL  60172

Thomas Windau
Environmental Engineer
FC WQPA
1919 American Ct.
Neenah, WI 54956

Peter Wise
Director, Water Quality Planning Div.
USEPA
401 M. Street
Washington, D.C.
                                         391

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                                      10
Thomas Warn
Environmental Protection Specialist
USEPA
230 S. Dearborn Street
Chicago, IL  60604

William Wawrzn
State of Wisconsin
Dept. Natural Resources
P.O. Box 13248
Milwaukee, WI 53226

David Wurm
Honey Creek Project
155 E. Perry Street
Tiffen, Ohio
Keith K. Young
Soil Scientist, Soil Technology
Soil Conservation Service
P.O. Box 2890
Washington, D.C. 20013

Bruce Yurdin
Environmental Protection Specialist
IEPA
2200 Churchill Road
Springfield, IL  62706

Mathew Zabik
Professor Pesticides Institute
Michigan State University
Lansing, MI
Greg Zelinka
Madison Metro Sewerage District
Lab Supervisor
104 North 1st Street
Madison, WI  53704
William Withrow
IPCB
309 W. Washington
Chicago,  IL
Larry Vend!
Project Hydrologist
U.S. Geological Survey
P.O. Box 427
DeKalb, IL 60115

Terry L. Wells
Senior Planner
Ohio Dept. Nat'l. Resources of Water
Fountain Square, Bldg. E
Columbus, Ohio 43224~

Douglas G. Whitaker
Assistant  General Manager
The Miami Conservancy District
38 E. Monument Avenue
Dayton, OH 45402

Lyman Wible
Chief Environmental Planner
S.E. Wisconsin Regional Planning
  Commission
Waukesha, WI

Carl D. Wilson
Coordinator Nonpoint Source
USEPA-5GLNP
536 S. Clark Street
-Chicago, IL  60605
                                         392

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                                  TECHNICAL REPORT DATA
                           (Please read Instructions on the reverse before completing)
1. REPORT NO.
   EPA-905/9-80-009
                                                           I. RECIPIENT'S ACCESSION-NO.
4. TITLE AND SUBTITLE
                                                           I. RPPORT DATE
   "Seminar on Water  Quality Management Trade-Offs"
   (Point Source vs Diffuse Source Pollution)
                                                 September 1980
                                              6. PERFORMING ORGANIZATION CODE
7. AUTHOR(S)
   Compiled
                                                           8. PERFORMING ORGANIZATION REPORT NO.
by:
Ralph G.
Cli fford
Christensen and
Risley, Jr.
9. PERFORMING ORGANIZATION NAME AND ADDRESS
   U. S. Environmental  Protection Agency
   Great Lakes  National  Program Office
   536 South Clark  Street, Room 932
   Chicago, Illinois  60605
                                              10. PROGRAM ELEMENT NO.

                                                 A42B2A
                                               11. CONTRACT/GRANT NO.
12. SPONSORING AGENCY NAME AND ADDRESS
   U. S. Environmental  Protection Agency
   Great Lakes  National  Program Office
   536 South Clark  Street, Room 932
   Chicago, Illinois  60605
                                               13. TYPE OF REPORT AND PERIOD COVERED
                                                Conference Report
                                               14. SPONSORING AGENCY CODE
                                                 U.S. EPA-GLNP
15. SUPPLEMENTARY NOTES
   Conference Committee-Ralph G. Christensen,  U. S. EPA; Carl  D.  Wilson, U. S. EPA;
   Clifford Risley, U.  S. EPA; Orville  Macomber, U. S. EPA;  Donald  Urban, U. S. DA-SCS
16. ABSTRACT
   This report  is  a  collection of technical  papers presented at  the  "Seminar on
   Water Quality Management Trade-Offs"  Point Source vs Diffuse  Source Pollution
   held in Chicago,  Illinois September 16-17, 1980 at the Pick Congress Hotel.
   Seminar speakers  were selected for their  expertise in the different areas
   of point and diffuse source pollution.  Many were principal investigators
   of Section 108(a) and Great Lakes Program demonstration project  grants.  The
   seminar pointed out the need for nonpoint source control implementation to
   meet 1983 water quality goals.
17.
                                KEY WORDS AND DOCUMENT ANALYSIS
                  DESCRIPTORS
                                              b.IDENTIFIERS/OPEN ENDED TERMS
                                                            c.  COS AT I Field/Group
   Water Quality
   Sediment
   Erosion
   Land Use
   Land Treatment
   Wastewater Treatment
   Nutrients
            Phosphorus
              availability
            Pollutant Loadings
            Treatment costs
            Institutional
13. DISTRIBUTION STATEMENT
 Document is available  to the public through
 the National Technical  Information Service
 Sorinafield. Mirainia  22151  	
                                  19. SECURITY CLASS (This Report)

                                  	NA	
                                                                         21.
                                                                                 PAGES
                                  20. SECURITY CLASS (This page)
                                         NA
                                                            22. PRICE
EPA Form 2220-1 (9-73)
                                                             U. S. Government Printing Office. 1981 750-799
                                              393

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