UPPER POTOMAC ESTUARY
EUTROPHICATION CONTROL REQUIREMENTS
Technical Report 53
Annapolis Field Office
Environmental Protection Agency
Region III
April 1972

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Prepared for presentation at the 44th Annual Conference of the Water
Pollution Control Federation which was held October 3-8, 1971,
San Francisco, California.
U.S. EPA Region III
Regional Center for Environmental
Information
1850 Arch Street (3PM52)
Philadelphia, PA 19103 ^g^ggpj
UPPER POTOMAC ESTUARY
EUTROP HI CAT ION CONTROL REQUIREMENTS
By
i
Norbert A. Jaworski
2
Leo J. Clark
Kenneth D. Feigner
Technical Report 53
April 1972
:F — sj
%•	r<-~
PRO^
Regional Ccnicr for Environmental Information
US FJ'A Region III
16*50 Arch Si
Philadelphia, PA 19103

Jaworski, Dr. Norbert A., Chief, Grosse lie Field Site, EPA, Office
of Research and Monitoring, 9311 Groh Road, Grosse lie, Michigan 48138
Clark, Leo J., Chief, Engineering Section, Annapolis Field Office, EPA,
Annapolis Science Center, Annapolis, Maryland 21401
Feigner, Kenneth D. , Sanitary Engineer, EPA, Office of Water Programs,
Systems Analysis and Economics Branch, Washington, D. C. 20242

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TABLE OF CONTENTS
Title	Page
Introduction 		1
Brief Description of the Study Area		2
Water Quality Problems 		4
Nutrient Concentrations and Sources 		9
Eutrophication Control Requirements 		14
Nutrient Criteria 		16
Wastewater Management Zones 		18
Water Quality Simulation Models 		19
Maximum Constituent Loadings Per Zone 		22
Seasonal Waste Treatment Requirements 		23
1.	Ultimate Oxygen Demand 		23
2.	Phosphorus and Nitrogen		25
Selection of Unit Processes to Achieve Water
Quality Objectives 		28
Estimated Costs	- .	31
Management Planning 		32
Summary		34
References		41
i i i

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LIST OF TABLES
Number	Titie	Page
1	Water Quality Problems, Upper Potomac Estuary . . 6
2	Average Range of Concentration, Summer Conditions,
Upper Potomac Estuary	 10
3	Summary of Major Nutrient Sources, Upper and
Middle Reaches of the Potomac Estuary 	 11
4	Subjective Analysis of Algal Control Requirements . 15
5	Maximum UOD, Phosphorus, and Nitrogen Wastewater
Loadings for Low-flow Summer Conditions .... 24
i v

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LIST OF FIGURES
Number
A map of the Potomac Estuary showing wastewater
discharges and loading zones 		1
A map of the Upper Potomac Estuary indicating
major water quality problems 		2
A chronological history of nutrients entering
the Upper Potomac Estuary from wastewater
discharges and resulting biological
communities 		3
Observed and simulated NH3, NO2 + NO3, and
chlorophyll profiles for the Upper Potomac
Estuary 		4
Observed and simulated annual phosphorus profiles
for the Potomac Estuary at Indian Head		5
Simulated annual nitrogen profiles for the Potomac
Estuary at Indian Head		6
v

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1
INTRODUCTION
Based on studies by the U. S. Public Health Service beginning in
1965, the conferees of the Potomac River-Washington Metropolitan Area
Enforcement Conference agreed on May 8, 1969, to limit the amount of
biochemical oxygen demand, phosphorus, and nitrogen which could be
discharged into the Upper Potomac Estuary from wastewater treatment
facilities. The conferees recognized a need, not only for high degrees
of wastewater treatment for the reduction of carbonaceous and nitrogenous
oxygen demanding material, but also a need, for the control of eutro-
phi cation.
Additional detailed studies by the Chesapeake Technical Support
Laboratory (CTSL)* of the Federal Water Quality Administration** to
further define the interrelationships among wastewater inflow, freshwater
inflow, and water quality in the Potomac Estuary were undertaken in
November 1969. These studies had two purposes: (1) to refine the
allowable oxygen demanding and nutrient loadings previously established
and (2) to determine the feasibility of using the estuary as a municipal
water supply source.
Presented herein is a summary of numerous reports published by CTSL
with major emphasis on the eutrophication control aspects developed in
the recent studies.
* Now the Annapolis Field Office
** Now the Environmental Protection Agency

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2
BRIEF DESCRIPTION OF THE STUDY AREA
The Potomac River Basin, with a drainage area of approximately
38,000 square kilometers (km2), is the second largest watershed in the
Middle Atlantic States. From its headwaters on the eastern slope of
the Appalachian Mountains, the Potomac flows first northeasterly and
then generally southeasterly some 644 km, flowing past the Nation's
capital. The Potomac is tidal from Washington, D. C., to its confluence
with the Chesapeake Bay, a distance of 183 km (Figure 1).
The study area includes the tidal portion, which is about 60 meters
(m) in width at its uppermost reach near Washington and broadens to
nearly 10 km at its mouth. Except for a 7.5 m shipping channel and a
few reaches where depths up to 30 m can be found, the tidal portion is
relatively shallow with an average depth of approximately 5.5 m.
Of the 3.3 million people living in the entire basin, approximately
2.8 million reside in the upper portion of the Potomac Estuary within
the 7,300 km2 which comprises the Washington Metropolitan Area. The
lower area of the tidal portion, which drains 8,300 km2, is sparsely
populated.
The upper reach above Indian Head, although tidal, is essentially
fresh water. The middle reach is normally the transition zone from
fresh to brackish water. The lower reach is mesohaline with chloride
concentrations near the Chesapeake Bay ranging from approximately 7,000
to 11 ,000 mg/1.

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The average freshwater flow of the Potomac River near Washington
before diversions for municipal water supply, is 305 cubic meters per
second (cms) with a median flow of 185 cms. The flow of the Potomac
virtually unregulated and is thus characterized by extremely high and
flashy flows often approaching 2,500 cms during flood conditions and
30 cms during droughts.

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4
WATER QUALITY PROBLEMS
Early historical observations of the water quality conditions
include reports that in the late 17901s President Adams swam in the
Potomac Estuary near Washington, D. C. By the 18601 s when Abraham Lincoln
was president, the canals leading into the Potomac Estuary, as well as the
Potomac Estuary itself, often emitted objectionable sewage odors forcing
Mr. Lincoln to leave the White House at night. From the year 1870, when
the first sewers and culverts were constructed, to the year 1938, when the
first primary treatment plant was built, almost all of the sewage from the
Washington Metropolitan Area was discharged untreated into the Potomac
Estuary.
The burgeoning population growth in the Washington Metropolitan Area
has compounded the water quality management problem. The accelerated
population growth has completely outstripped attempts to provide adequate
facilities for wastewater treatment. In addition, much of the growth has
been uncontrolled in nature and location, and it is now difficult to pro-
vide adequate wastewater collection and treatment within the limited
space available for such facilities in the area. Changes in composition
of the wastewater, mainly in the phosphorus content, have also had a pro-
nounced effect on water quality.
Since the first sanitary survey was made by the U. S. Public Health
Service in 1913 [1], the water quality with respect to bacterial den-
sities and dissolved oxygen levels in the Washington Metropolitan Area has
been degraded as a result of the discharge of either untreated or
inadequately treated municipal sewage.

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5
The upper estuary has been divided into four reaches according to
type and source of pollution as itemized in Table 1 and shown in Figure
2. There are about 90 kilometers of the upper estuary degraded with
the effects of eutrophication being pronounced in approximately 50
kilometers. In addition, the Upper Potomac Estuary, including the
Anacostia Tidal River, is subjected to periods of high concentrations of
sediment.

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Table 1
WATER QUALITY PROBLEMS
Upper Potomac Estuary
Reach
Ki lometers
of River
Affected
Major Type
of
Pol 1ution
Major Source
of
Pol 1ution
Chain Bridge to
Hains Point
11
Frequently high
bacterial counts
Overloaded sanitary
sewers and combined
sewer overflows
Hains Point to
Piscataway Creek
Low-di ssolved
16 oxygen concen-
trati ons
Effluents from
wastewater treatment
faci1ities
Piscataway Creek
to Maryland Point
Anacostia Tidal
Ri ver
Nuisance algal
50 growths
Frequently high
13 bacterial counts
and low-dissolved
oxygen concen-
trations
Nutrients in waste-
water discharges
Combined and sanitary
sewer overflows

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7
During initial studies of the estuary, major emphasis was placed on
the high bacterial and low-dissolved oxygen problems [2] [3]. More
recently, the nuisance algal problem has also been included.
The time frame of algal problem development has been developed from
several studies as summarized by Jaworski et al. [4], As shown in Figure
3, there have been historical invasions of nuisance growths in the Upper
Potomac Estuary.
From a review of data in Figure 3, it would appear that nuisance
conditions did not develop linearly with an increase in nutrients.
Instead, the increase in nutrients appeared to favor the growth and
eventually the domination by a given species. As nutrients increased
further, the species in turn was rapidly replaced by another dominant form.
For example, water chestnut was replaced by water milfoil which in turn
was replaced by blue-green algae, mainly Anacystis.
The massive blue-green algal blooms, which have occurred every summer
since I960, appear to be associated with large increases in phosphorus and
nitrogen loadings in the upper reaches of the Potomac River tidal system
(Figure 3). The blooms have persisted since the early 1960 's although
during this period the amount of organic carbon from wastewater was
reduced by almost 50 percent when compared to that discharged prior to
1960.
Under warm temperature and low-flow conditions, large standing crops
of this alga develop forming green mats of cells. Chlorophyll ^concen-
trations range from approximately 50 to over 200 ug/1 in these areas of

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8
dense growth which at times extends over approximately 80 km of the upper
and middle reaches of the estuary. These high chlorophyll levels are
5 to 10 times those reportedly observed in other eutrophic waters by
Brezanik et al. [5] and by Welch [6]. During a dense bloom, the dry
weight of cells ranges from 10 to 25 mg/1 which is almost twice those
reported for the lakes in Madison, Wisconsin.
In the mesohaline portion of the lower reach of the Potomac Estuary,
the algal populations are not as dense as in the freshwater portion.
Nevertheless, at times large populations of marine phytoplankton
(primarily the dinoglagel1ates Gymnodinium sp. and Amphidinium sp.)
occur producing what are known as "red tides."

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9
NUTRIENT CONCENTRATIONS AND SOURCES
The concentration of nutrients along the estuary varies as a function
of wastewater loading, temperature, freshwater inflow from the upper
basin, biological activity, and salinity. The annual distribution of the
various nutrient concentrations has been reported by Jaworski et al. [4],
and the summer levels are summarized in Table 2 for five key stations
along the estuary.
In the vicinity of the Woodrow Wilson Bridge, there is an increase in
alkalinity, total phosphorus, N02 + NO3 nitrogen, and ammonia nitrogen
with a corresponding decrease in pH, all of which can be attributed to the
1230 million liters per day of wastewater discharged in the Washington
Metropolitan Area. The rapid disappearance of the ammonia nitrogen bet-
ween Woodrow Wilson Bridge and Indian Head is caused by the oxidation of
NH3 to NO2 + NO3 by the nitrifying bacteria. The sharp drop in NO2 + NO3
nitrogen between Indian Head and Maryland Point is attributable to the large
uptake by the pronounced algal growths in this area.
A complete analysis of the nutrient sources in the Upper Potomac
Estuary has been made by Jaworski et al. [4]. A summary of the major
sources is presented in Table 3 for low, median, and high Potomac River
flows.

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Table 2
AVERAGE RANGE OF CONCENTRATION
SUMMER CONDITIONS
Upper Potomac Estuary
Station and	Total	NO2 + NO3 NH3
Kilometers from	pH Alkalinity Phosphorus	Nitrogen Nitrogen
Chain Bridge	(units)	(mq/1) 	(mg/1)	(mg/1)	(mg/1)
Chain Bridge	7.5 - 8.0 80 - 100 0.08 - 0.20	0.3 - 1.0 0.10 - 0.50
(0.0)
W. Wilson Bridge	7.0 - 7.5 90 - 110 0.30 - 1.20	0.8 - 1.2 1.00 - 3.00
(19.5)
Indian Head	7.2 - 8.0 70 - 90 0.20 - 0.40	0.5 - 1.5 0.10 - 0.50
(49.3)
Maryland Point	7.5 - 8.2 60 - 85 0.10 - 0.25	0.1 - 0.3 0.05 - 0.30
(84.3)
301 Bridge	7.5 - 8.0 65 - 85 0.05 - 0.20	0.1 - 0.2 0.05 - 0.20
(104.7)

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Table 3
SUMMARY OF MAJOR NUTRIENT SOURCES
Upper and Middle Reaches of the Potomac Estuary
Low-flow Conditions
(95 % of time exceeded)
(Potomac River Discharge at Washington, D. C. = 40 cubic meters/sec)

Upper
Basi n
Runoff*
Percent
of
Total
Estuari ne
Wastewater
Discharges
Percent
of
Total
Total

(kg/day)

(kg/day)

(kg/day)
Carbon
77,100
52
72,600
48
148,700
Nitrogen
3,000
10
27,200
90
30,200
Phosphorus
450
4
10,900
96
11 ,350


Median-flow Conditions
(50 % of time exceeded)


(Potomac
River Discharge
at Washington, D. C. = 185 cubic meters/sec)
Carbon
159,000
68
72,600
32
231 ,600
Ni trogen
18,100
40
27,200
60
45,300
Phosphorus
2,400
18
10,900
82
13,300


High-flow Conditions
(5 % of time exceeded)


(Potomac
River Discharge
at Washington,
, D. C. = 1150
cubic meters/sec)
Carbon
680,000
90
72,600
10
752,600
Ni trogen
185,000
87
27,200
13
212,200
Phosphorus
10,000
47
10,900
53
20,900
* Upper basin runoff includes
basin.
both land runoff and wastewater discharges
in upper

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12
When considering only upper basin runoff and wastewater discharges
to the estuary as summarized in Table 3, it can be concluded that the
order of percentage of nutrients controllable by wastewater treatment is
(1) phosphorus, (2) nitrogen, and (3) carbon.
While the controllable phosphorus and nitrogen percentages decrease
at higher flows, these conditions usually occur during the months of
February, March, and April, when temperatures and algal crops are lowest.
Since nuisance algal conditions occur primarily in the upper or the fresh-
water portion of the estuary, the higher flow effects are reduced consider-
ably by the time the blooms are most prolific during the months of July,
August, and September.
Under low- and median-flow conditions, both nitrogen and phosphorus
are largely controllable. If allowances are made for atmospheric contri-
butions of nitrogen, only an approximate 2200 kg/day of nitrogen could be
added to the upper estuary, which is less than 10 percent of the nitrogen
in the wastewater discharges. Thus, during summer months, algal control
by management of nitrogen instead of phosphorus appears to be a feasible
alternative.
Using only 0.1 percent of the transfer rate, the amount of carbon (CO2)
potentially available from the atmosphere was estimated to be approximately
431,000 kg/day [4], Moreover, with the upper reach of the estuary well
mixed due to tidal action, recruitment of carbon from benthic decomposition
appears to be a significant source of inorganic carbon as well. When all

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13
potential sources are considered, it appears that management of carbon
for algal control is not a feasible alternative at the present time.

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14
EUTROPHICATION CONTROL REQUIREMENTS
For water quality management purposes, the Upper Potomac Estuary
may be considered hypereutrophic when nuisance plant organisms become
predominant as is now occurring with the blue-green algae. Four major
water use interferences have been offered by Jaworski et al. [4]
including the desired reduction in the algal standing crop for each of
the conditions as shown in Table 4.
The first two are related to the oxygen budget. Studies have demon-
strated that during the summer months more ultimate oxygen demand is
added to the upper estuary as a result of these algal growths than from
the present wastewater discharges, though this demand may not be fully
exerted.
The aesthetic and recreational potential of the upper estuary are
impaired by the extensive mats of algae which cause objectionable odors,
clog marinas, and cover beaches and shorelines. The potential use of the
estuary as a water supply source could also be impaired because of possible
toxin problems associated with the blue-green algae.
Of the four interferences, the highest reduction percentages are for
control of algal growths to prevent nuisance conditions. From the data in
Table 4, a 75 to 90 percent reduction in chlorophyll ^concentrations will
be required to limit chlorophyll levels to approximately 25 yg/1 , the
concentration selected as the desired upper limit for eutrophication control
in the Upper Potomac Estuary.

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Table 4
Water Quality or
Water Use Interference
DO Depression Caused by
Algal Respiration
Increase of Total Oxygen
Demanding Load
Recreational & Aesthetic
Nuisance Conditions
Toxi ns
Indications of
Interference
SUBJECTIVE ANALYSIS OF ALGAL CONTROL REQUIREMENTS
Desired Limit
mg/1 of DO Below
Saturation
mg/1 of Increase
in Ultimate BOD
Chlorophyll a^
Concentrati on
Undefined
Magnitude of
Current Interference*
1.5 to 3.0 mg/1
15 to 30 mg/1
100 to > 250 yg/1
Unknown
0.5 mg/1
5.0 mg/1
25 ug/1**
Unknown
Required Percentage Reduction
of Current Standing Crop	
65-85
65-80
75-90
Unknown
* Under nuisance-bloom conditions, chlorophyll a_ concentrations range from 100 to >250 pg/1
** Average over entire water column

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16
NUTRIENT CRITERIA
The desired nutrient criteria were developed using data from:
(1) algal composition analysis, (2) annual nutrient cycles and longi-
tudinal profiles, (3) bioassay studies, (4) review of historical data,
(5) comparison with a noneutrophic estuary, and (6) algal modeling.
Each method was used independently in the development of a nutrient
phytoplankton relationship in the Potomac Estuary.
When investigating the role of nitrogen and phosphorus in eutrophication
of the Potomac Estuary, a detailed study of the movement of these nutri-
ents was made using both a real-time dynamic water quality estuary model
[8] and an average tidal mathematical model [9]. The dynamic model was
expanded to predict the concentration of chlorophyll a^ based on the
utilization of inorganic nitrogen. In Figure 4, predicted NO2 + NO3,
NH3, and chlorophyll a_ profiles are presented. The predicted maximum
concentrations conform closely to observed data in both distribution and
magnitude.
From field data, bioassay studies, and mathematical model runs, it
was concluded that the standing crop of blue-green algae can be pre-
dicted using the nitrogen cycle. This further supports the premise that
the nitrogen availability appears to control the standing crop. Similar
methods also indicated that if total phosphorus were in the range of 0.03
to 0.1 mg/1, the desired 25 ug/1 level of chlorophyll could be realized.

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17
Based upon the six independent methods of analysis and the 25 yg/1
level of chlorophyll a_, the following nutrient criteria were developed
for reversing the eutrophication process occurring in the freshwater
portion of the Potomac Estuary:
Parameter	Concentration Range
Inorganic Nitrogen	0.30 - 0.5 mg/1
Total Phosphorus	0.03 - 0.1 mg/1
Since there are over 5.0 mg/1 of inorganic carbon in the estuary, even
under maximum bloom conditions, no criterion for carbon could be established
at the present time.
The lower values in these ranges are to be applied to the freshwater
portion of the middle reach and to the embayment portions of the estuary
in which the environmental conditions are more favorable toward algal
growth. The higher values are more applicable to the upper reach of the
Potomac Estuary which has a light-limited euphotic zone of usually less
than 0.60 meters.
Since the growth of massive blue-green algal mats are apparently
restricted to the freshwater portions and dinoflagellates are often
encountered in the mesohaline environment, no specific nutrient criteria
have been established for the mesohaline portion of the Potomac Estuary.
It appears that if the aforementioned nutrient criteria are achieved in the
upper estuary, adequate control of the eutrophication process in the lower
reach of the estuary should also be realized.

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18
WASTEWATER MANAGEMENT ZONES
To facilitate the determination of wastewater management require-
ments, the upper and middle reaches of the estuary were initially
divided into three 15-mile (24 km) zones with similar physical character-
istics, beginning at Chain Bridge (see Figure 1). This zoning concept,
patterned after the Delaware Estuary, allows for greater flexibility in
developing control needs and was adopted by the Conferees at the Potomac
Enforcement Progress Meeting on May 8, 1969.
More recent studies in 1970 have suggested that Zone I be divided
into three subzones described as follows:
Subzone	Descri pti on
I-a	Potomac Estuary from Chain Bridge to Hains Point, a
distance of 12.1 kilometers.
I-b	Anacostia tidal river from Bladensburg, Maryland, to the
confluence with the Potomac, a distance of 14.4 kilometers.
I-c	Potomac Estuary from Hains Point to Broad Creek, a distance
of 12 kilometers.
Discharges into tidal embayments were investigated on an individual basis.
Using the zonal concept, total maximum loadings for each pollutant
were developed for each zone. Allocation of pound loadings for each dis-
charge can be obtained by prorating the zonal poundage using various
bases such as population, drainage areas, geographical subdivisions, and
others.

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19
WATER QUALITY SIMULATION MODELS
Water quality simulations and wastewater treatment investigations
were made using the FWQA Dynamic Estuary Model (DEM) and the DECS III,
a general purpose estuarine model. The DEM [8] is a real-time system
utilizing a two-dimensional network of interconnecting junctions and
channels which permits direct inclusion of tidal embayments in the flow
representation. The model is comprised of a hydraulic component that
describes tidal movement and a quality component. The DEM includes the
basic transport mechanisms of advection and dispersion as well as the
pertinent sources and sinks for each constituent. This model was used to
simulate water quality conditions on an hourly basis and to determine
zonal loadings under low-flow conditions.
DECS III is based on a time-dependent tidal average solution of the
basic mass balance equations [9]. This model was used to investigate
seasonal variations in the nitrogen and phosphorus distributions in the
Upper Potomac Estuary.
The interrelationship between ultimate oxygen demand* (UOD) loadings
and dissolved oxygen (DO) in the Potomac Estuary was determined assuming
the following conditions:
* The ultimate oxygen demand represents the sum of unoxidized carbon and
Parameter
Val ue
Water Temperature
Freshwater inflow from upper
Potomac River Basin
DO standard (average)
DO saturation at 29°C
Background DO deficit
Allowable DO Deficit
29.0°C
10.0 CMS
5.0	mg/1
7.7 mg/1
0.7	mg/1
2.0 mg/1
nitrogen

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20
In the DO model, the oxidation of carbonaceous and nitrogenous
fractions, including the reaction kinetics, were formulated separately.
Simulation of phosphorus discharges into the Potomac Estuary was
made using second-order reaction kinetics with a deposition rate of
0.05 mg/day at a temperature of 29°C. The allowable phosphorus
loadings were determined based on maintaining an average of 0.1 mg/1 of
phosphorus (P) within Zone I, 0.067 mg/1 (P) within Zone II, and 0.03
mg/1 (P) within Zone III.
For investigating the role of nitrogen in water quality management,
a feedback system of the nitrogen cycle was incorporated into the
dynamic estuary mathematical model similar to that proposed by Thomann
et al. [10]. The model consists of six possible reactions: (1) chemical
and biological decomposition of organic nitrogen to ammonia, (2) bacterial
nitrification of ammonia to nitrite and nitrate, (3) phytoplankton utili-
zation of ammonia, (4) phytoplankton utilization of nitrite and nitrate,
(5) deposition of organic nitrogen, and (6) decay of phytoplankton. With
the area near Woodrow Wilson Bridge being light limiting with respect to
algal growth, the utilization of ammonia by phytoplankton appears to be
insignificant and thus the model was simplified as given below:
Organic Nitrogen
expressed as
Wastewater NH3 Kni NO2 + NO3 Kn2	Chlorophyll a^
i \
	~-
Kn4
	
t
\
Kn3
1
»
To the sediments

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21
For summer temperatures of 26°C to 29°C, first-order kinetic
reaction rates have been established for the various processes as
given below:
Nitrification by bacteria (Kn-|)	0.30 to 0.40
Nitrogen utilization by phytoplankton (Kn2)	0.07 to 0.09
Deposition of algal cells (Kn3)	0.005 to 0.05
Remineralization (IO14)	(less than 0.05)
The reaction rates of the first two processes (nitrification and
nitrogen utilization) have been well established as demonstrated in the
profile shown in Figure 3. The latter two, Kn3 and Kn4, although not
as well defined, do not appear to be as significant. The nitrogen
criteria used for Zones I, II, and III were 0.5, 0.4, and 0.3 mg/1,
respectively.

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22
MAXIMUM CONSTITUENT LOADINGS PER ZONE
Using the models and coefficients as described in the previous
sections, zonal loadings were determined for UOD, nitrogen, and phos-
phorus (see Table 5). The loadings presented are maximum allowable
loadings for each zone, assuming that adjacent zones are loaded to
their maximums.
The increase in loadings for the lower zones mainly reflect the
increase in the estuary's volume and tidal transport. Since nitrogen
and phosphorus criteria for the lower zones are more stringent, the
increase in nutrient loadings in this area is not as pronounced as for
UOD.
For the projected 1980 wastewater loading conditions, the antici-
pated percent removal rates for Zone I-c would be approximately 93 per-
cent UOD, 96 percent phosphorus and 93 percent nitrogen. Since Zones II
and III do not currently receive as much wastewater, the removal percent-
ages will not be as high.

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23
SEASONAL WASTE TREATMENT REQUIREMENTS
1. Ultimate Oxygen Demand
The maximum allowable UOD loadings, as presented in Table 5 for the
three upper zones of the Potomac Estuary, were developed for low-flow
and summer temperature conditions. During high temperature periods, the
effects of nitrogenous oxygen demanding substances on the dissolved
oxygen budget were determined to be quite significant.
Studies have shown that during very warm periods, when nitrification
rates are high, the nitrogenous component of UOD exerts 250,000 lbs/day
of oxygen demand as compared to approximately 200,000 lbs/day from the
carbonaceous demand. During low temperature periods, when the ambient
water temperature is less than 15°C, the effects of nitrification on the
dissolved oxygen budget have been shown to be negligible.
Based on these findings, it was recommended that (1) UOD loadings
presented in Table 5 be applied only under summer conditions, (2) the
removal or oxidation of ammonia in wastewater discharges be provided
whenever the water temperature is above 15°C, and (3) a high degree of
removal of suspended solids (a maximum of 15 mg/1 in the effluent) and
carbonaceous oxygen demanding material (a minimum of 90 percent) be pro-
vided on a year-round basis to prevent the accumulation of sludge deposits
in the vicinity of sewage treatment plant outfalls during cooler weather
and to maintain high DO levels under ice cover.

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Table 5
MAXIMUM UOD, PHOSPHORUS, AND NITROGEN
WASTEWATER LOADINGS
FOR LOW-FLOW SUMMER CONDITIONS
(kg/day)
Zone	Allowable	UOD Phosphorus	Nitrogen
I-a	1,800	90	450
I-b	1,400	40	140
I-c	33,800	400	1,580
II	85,500	680	2,600
III	171,000	900	4,100

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25
2. Phosphorus and Nitrogen
The loadings, as presented in Table 5, were established for low-
flow conditions. During these periods, the nutrient contribution
from the upper basin is insignificant when compared to that contained
in the wastewater discharges.
To determine whether the nitrogen and phosphorus criteria could be
met under varying Potomac River inflows and varying nutrient contri-
butions from the upper basin, an annual simulation was made of conditions
from February 1969 to September 1970. This period was critical because
a drought condition occurred during June and July of 1969, and August
flows were over four times above the average discharge. Thus, both low
and high summer flows were simulated.
Mathematical model analysis of the annual distribution of phosphorus
in the critical algal growing area showed close agreement between the
observed and predicted phosphorus profiles (see Figure 5). Also shown in
Figure 5 are the predicted annual phosphorus profiles resulting from year-
round wastewater phosphorus removal in the upper estuary, assuming:
(1) no control and (2) 50 percent control of the phosphorus loading
originating in the Upper Potomac River Basin. From the data presented in
Figure 5, it was concluded that both (1) the adherence to maximum
allowable phosphorus loadings from wastewater effluents being discharged
directly into the estuary (see Table 5) and (2) a 50 percent reduction of
the total incoming phosphorus load from the upper basin, will be required

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26
if the recommended maximum phosphorus criteria are to be realized.
In order to achieve a 50 percent reduction in the present phosphorus
load from the Upper Potomac River Basin, the current overall waste-
water contribution of 2700 kgs/day must be reduced to less than 320
kgs/day.
Because of the more stringent criteria, particularly in the lower
zones including longer transport time, the possibility of recycling
previously deposited phosphorus from bottom muds and the unpredictability
of phosphorus in various forms being transported from the upper basin,
year-round phosphorus removal at all wastewater treatment facilities in
the Potomac River Basin was recommended.
As presented earlier, the necessity for unoxidized nitrogen control
in wastewater discharges to maintain a high dissolved oxygen content in
the Potomac Estuary was restricted to that time of year when water tempera-
tures exceed 15°C. When evaluating the need for annual nitrogen control
to prevent excessive algal blooms, controllability, duration of nuisance
blooms, and temperature become significant factors.
While spring blooms of diatom algal cells have been observed, the
major nuisance blue-green algal blooms of algae usually occur during the
months of July, August, and September. During these months, the controlla-
bility of nitrogen by wastewater treatment is usually greatest and the
water temperature highest.
Mathematical model predictions of inorganic nitrogen concentrations in
critical algal growing areas based on (1) no estuary wastewater nitrogen

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27
removal, (2) nitrogen removal during periods with temperatures above
15°C (Apri1-November), and (3) year-round nitrogen removal are presented
in Figure 6. For the nitrogen loading as given in Table 5, the inorganic
nitrogen concentration of less than 0.3 mq/1 can be achieved for drought
conditions such as in June and July. The abnormally high August Potomac
River flow condition and resulting high upper basin loading caused the
nitrogen level to increase to approximately 0.5 mg/1.
While it may be desirable to maintain nitrogen concentrations at or
below the selected criteria at all times, the high flows from the upper
basin during the winter and spring months contribute high nitrogen
loadings which increase the nitrogen concentrations above acceptable
levels regardless of wastewater treatment practices. In considering (1)
that nuisance algal growths occur mainly during the months of July, August,
and September, (2) that seasonal nitrogen removal is generally adequate
for maintaining the desired nitrogen concentration during this time, and
(3) that unoxidized nitrogen control is required only for warm temperature
periods, it was recommended that nitrogen removal for algal control, as in
the case of nitrogenous demand for oxygen enhancement, be limited to
periods when water temperatures in the estuary exceed 15°C.
In developing the seasonal requirements, emphasis was placed on main-
taining a balanced ecological community structure in the upper or freshwater
portion of the estuary. More research efforts in both transport mechanisms
and nutrient algal relationships are needed to determine management require-
ments for the lower or saline portion of the estuary.

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28
SELECTION OF UNIT PROCESSES TO ACHIEVE WATER QUALITY OBJECTIVES
The decision, as developed throughout this report as to which
nutrient or nutrients in a natural system should be controlled by
removal from point sources, may depend upon many factors, including
the four listed below:
1.	Desired level of nuisance algal reduction,
2.	Minimum algal nutrient requirements,
3.	Controllability and mobility of a given nutrient, and
4.	The overall water quality management needs.
In establishing an overall wastewater management program for the
Potomac Estuary, a need for a high degree of removal of wastewater
carbonaceous and nitrogenous ultimate oxygen demand was established for
maintaining the desired oxygen standards along with a need for a 75-90
percent reduction in algal standing crop. To provide for algal control,
maximum concentration limits for both nitrogen and phosphorus were
adopted. Concentration limits for both were incorporated for the
following reasons:
1. Since the flow of the Potomac River is unregulated and subject
to periods of high runoff, neither phosphorus nor nitrogen can be con-
trolled by wastewater removal alone at all times. The advantage of
controlling phosphorus or nitrogen depends on the flow conditions.
To reduce eutrophication in the entire estuary for years with average
or above average flow conditions, phosphorus control appears to be more
feasible. In the middle and upper estuary, nitrogen control is four times

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29
as effective during low-flow years in that the nitrogen criterion for
restriction of algal growth is 10 times that for phosphorus (0.30
versus 0.03 mg/1) while the nitrogen loading from wastewater treat-
ment facilities is 2.4 times that of phosphorus (27,200 versus 10,900
kg/day). Since phosphorus control is more advantageous during high flows
and nitrogen control more advantageous at low flows, removal of both
would be needed to control the nuisance growths effectively.
2.	Various investigators have reported that increases in nitrogen
and/or phosphorus can increase heterotrophic activity which in turn
stimulates algal growth, and
3.	There is a compatibility between the wastewater treatment methods
to increase dissolved oxygen levels and the methods used to control
eutrophication.
Compatibility in treatment requirements is probably one of the most
important considerations influencing the selection of wastewater treat-
ment unit processes. For example, in order to achieve and maintain the
dissolved oxygen standard in the upper estuary under summer conditions,
a high degree of carbonaceous and nitrogenous oxygen demand removal is
required, whereas the control of algal standing crops is predicated on
phosphorus and nitrogen removal. To obtain a high degree of carbonaceous
oxygen demand removal, an additional unit process is usually required
beyond secondary treatment. If the proper unit process is selected, it
will also remove a high percentage of phosphorus.

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30
The removal of the nitrogenous oxygen demand can be satisfied by
one of two methods: (1) by converting the unoxidized nitrogen to
nitrates (commonly called nitrification) or (2) by complete removal of
nitrogen. If a unit process such as ion exchange or biological
nitrification-denitrification is employed, both DO and algal reguire-
ments for nitrogen can be met.
Recent chemical analyses of the sediments of the Potomac Estuary
indicate high concentrations of heavy metals near the wastewater dis-
charges. Since there are no major industrial waste discharges in the
Washington area, the buildup of heavy metals from the municipal discharges
could become a future control need in that the lower portion of the
estuary is a prime shellfish producing area.
With proper selection of wastewater treatment unit processes, it is
feasible to enhance the DO by removing the carbonaceous and nitrogenous
UOD. In addition, it is feasible also to reduce nuisance algal growth
by removing these nutrients and to reduce the potential hazard of
heavy metals.

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31
ESTIMATED COSTS
The present worth cost of providing for additional wastewater
flows and treatment requirements from the year 1970 to 2020,
including operation, maintenance, and amortization cost, has been
estimated to be $1.34 billion, with a total average annual cost of
$64.8 million. The unit treatment processes assumed include activated
sludge, biological nitrification-denitrification, lime clarification,
filtration, effluent aeration, and chlorination.
The tabulation below is a reduction of the initial capital and
operation and maintenance costs to a per capita basis:
Item	1970-1980 1980-2000	2000-2020
Average Population	3,350,000 5,350,000	8,000,000
Initial Capital
Cost/Time Period	$570,000,000 $528,000,000 $1,173,000,000
Capital Cost/Person/Year	S17.0	$4.9	$7.3
0 & M Cost/Year	$25,100,000 $46,200,000 $72,400,000
0 & M Cost/Person/Year	$7.5	$8.6	$9.1
Total Cost/Person/Year	$24.5	$13.5	$16.4
The above summary, which does include replacement cost, indicates that
the cost of wastewater treatment in the Upper Potomac Estuary is about
$13 to $24/per person/per year. This expenditure, which includes the
cost of the activated carbon process, will renovate the water to the
chemical and bacteriological levels to meet drinking water quality
standards.

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32
MANAGEMENT PLANNING
The current program to control water pollution in the National
Capital Region, developed by the 1969 Enforcement Conference, includes
a schedule for completion of the needed treatment facility construction.
For the major waste discharge in the area, the District of Columbia
treatment facility at Blue Plains, progress has been slow.
In the fall of 1970, the parties involved in the Blue Plains problem
developed a "Memorandum of Understanding on the Washington Metropolitan
Regional Water Pollution Control Plan." This memorandum of understanding
was the first formally adopted planning approach to wastewater management
in the Washington Metropolitan Area. It recognized that the maximum
capacity of the waste treatment facility at Blue Plains should be limited
in size and established the basis for financing and cost sharing in the
proposed expansion and upgrading of the facility. It also recognized the
need for the development of a second regional wastewater treatment facility
and a schedule for the development of plans for this facility.
The primary problem to be overcome in achieving the wastewater treat-
ment requirements, as stipulated by the Potomac Enforcement Conference,
is financial. The total capital cost of these improvements, if storm and
combined sewer control and intercept costs are included, is estimated to
be approximately $857,000,000 for the program through 1980.
The capital cost of nutrient control has been estimated to be about
$250,000,000 or about 28 percent of total wastewater collection and treat-
ment cost. Considering wastewater treatment cost only, the capital cost is

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33
approximately 44 percent with approximately 85 percent of the operating
cost for nutrient control.
To aid in managing the water supply and waste treatment problems of
the National Capital Region, EPA has proposed the creation of a regional
authority [11]. Public hearings are currently being held to give the
public, state, and local officials an opportunity to offer their views
on the management plan.

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34
SUMMARY
In summary, the needs, costs, and mechanisms for controlling eutro-
phication in the Potomac Estuary have been identified and a start has
been made in implementing the program. With a capital cost for nutrient
removal of over $250,000,000, a need exists for continuous efforts to
improve eutrophication control, treatment methods, cost estimates, and
institutional arrangements. A need also exists to maintain a free-flowing
continuous exchange of information among the various agencies conducting
the removal requirement studies, designing the facilities, and planning
the overall management needs. These interactions are the keystones to
successful management planning.

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Figure I

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Periodically
High Bacterial
Densities
Periodically High
Bacterial Densities
and Low Dissolved
Oxygen Levels
Periodically Moderate
Bacterial Densities,
Low Dissolved
Oxygen Levels and
Beginning of
Algal Blooms
Pronounce
Nuisance Algal
Growths
Brackish
Waters
Figure 2

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10,000-
-100,000
- 80,000
- 60,000
- 40,000
U
10
O
o _
CD >\
cc o
<
O
C7>
2
<
O
cr
o
r 20,000
1910
1920
1930
1940
1950
I960
1970

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I25H
100-
> _ 75
x cr
r> 01
O s
a: cr
O 50
_j
u
25
0
1.4-
1.2-
1.0-
w ~ 0.8-
o -r
o
PREDICTED-
/
/

v

/>
~7
\
/
/
/
¦OBSERVED
TEMP.= 27.5 C
FLOW = 79.29 cms
cr
cn
I-
0.6-
0.4-
0.2-
0.0
¦NH3 (PREDICTED)
N02+N03 (OBSERVED)
N02 + N03 (PREDICTED)
SALINITY INTRUSION
1—
10
-I—
20
—r~
60
~T~
70
30
40
i
50
KILOMETERS BELOW CHAIN BRIDGE

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0.9-
0.8-
0.7-
0.6-
0.5-
0.4-
g1 0.3 H
^ 0.2 H
oc
X 0.1 H
CL
O0
0	o.O H
1
CL
ANNUAL PHOSPHORUS PROFILES
POTOMAC ESTUARY AT INDIAN HEAD
PREDICTED
OBSERVED
CONTINUOUS (YEAR AROUND) PHOSPHORUS
REMOVAL
0.3 H
0.2-
0.1 -
0.0-1
-NO PHOSPHORUS CONTROL IN UPPER POTOMAC BASIN
¦ASSUMING 50% OF PHOSPHORUS LOAD FROM UPPER
BASIN IS CONTROLLED
FEB. ' MAR. ' APR. ' MAY ' JUNE ' JULY 1 AUG. ' SEPT. ' OCT. ' NOV. ' DEC. ' JAN. ' FEB.
00
L
1969
1970

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SIMULATED ANNUAL NITROGEN PROFILES
POTOMAC ESTUARY AT INDIAN HEAD
	NO NITROGEN REMOVAL
OQ
C
«	1969	1970
O*

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41
REFERENCES
1.	U. S. Public Health Service, "Investigation of the Pollution and
Sanitary Conditions of the Potomac Watershed," Hygienic Laboratory
Bulletin No. 104, Treasury Department, February 1915.
2.	U. S. Army Corps of Engineers, "Potomac River Basin Report,"
Vol. 1 - Vol. VIII, North Atlantic Division, Baltimore District,
February 1963.
3.	Davis, Robert K., "The Range of Choice in Water Management, A Study
of Dissolved Oxygen in the Potomac Estuary," Johns Hopkins Press,
Baltimore, Maryland, 1968.
4.	Jaworski , N. A., Donald W. Lear, Jr., Orterio Villa, Jr., "Nutrient
Management in the Potomac Estuary," Presented at the American Sociel
of Limnology Symposium on Nutrients and Eutrophication, Michigan
State University, East Lansing, Michigan, February 1971.
5.	Brezanik, W. H., W. H. Morgan, E. E. Shannon, and H. D. Putnam,
"Eutrophication Factors in North Central Florida Lakes," Florida
Engineering and Industrial Experiment Station, Bulletin Series
No. 134, Gainesville, Florida, August 1969.
6.	Welch, E. B., "Phytoplankton and Related Water Quality Conditions it
an Enriched Estuary," Journal Water Pollution Control Federation,
Vol. 40, pp 1711-1727, October 1968.
7.	Lawton, G. W., "The Madison Lakes Before and After Diversion,"
Trans. 1960 Seminar on Algae and Metropolitan Wastes, pp 108-117,
Robert A. Taft Sanitary Engineering Center, Technical Report W61-3,
1961.
8.	Feigner, Kenneth and Howard S. Harris ^'Documentation Report, FWQA
Dynamic Estuary Model ,"FWQA, U. S. Department of the Interior,
July 1970.
9.	Thomann, Robert V., "Mathematical Model for Dissolved Oxygen,"
Journal of the Sanitary Engineering Division, ASCE, Vol. 89,
No. SA5, October 1963.
10.	Thomann, R. V., Donald J. O'Connor, and Dominic M. DiTorro,
"Modeling of the Nitrogen and Algal Cycles in Estuaries," presented
at the Fifth International Water Pollution Research Conference,
San Francisco, California, July 1970.
11.	Environmental Protection Agency, "National Capital Region Water and
Waste Management Report," Washington, D. C., April 1971.

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