EPA-R2 73 085
FEBRUARY 1973            Environmental Protection Technology Series
                  The  Influence  of
                    Log Handling
                 on  Water  Quality
                                    Office of Research and Monitoring

                                    U.S. Environmental Protection Agency
                                    Washington, D.C. 20460

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            RESEARCH REPORTING SERIES
Research reports of the  Office  of  Research  and
Monitoring*  Environmental Protection Agency, have
been grouped into five series.  These  five  broad
categories  were established to facilitate further
development  and  application   of   environmental
technology.   Elimination  of traditional grouping
was  consciously  planned  to  foster   technology
transfer   and  a  maximum  interface  in  related
fields.  The five series are:

   1.  Environmental Health Effects Research
   2.  Environmental Protection Technology
   3.  Ecological Research
   »*.  Environmental Monitoring
   5.  Socioeconomic Environmental Studies

This report has been assigned to the ENVIRONMENTAL
PROTECTION   TECHNOLOGY   series.    This   series
describes   research   performed  to  develop  and
demonstrate   instrumentation,    equipment    and
methodology  to  repair  or  prevent environmental
degradation from point and  non-point  sources  of
pollution.  This work provides the new or improved
technology  required for the control and treatment
of pollution sources to meet environmental quality
standards.

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                                        EPA-R2-73-085
                                        February  1973
     THE  INFLUENCE OF LOG HANDLING

           ON WATER QUALITY
                  By

          Frank D. Schaumburg


           Project 12100 EBG


            Project Officer

          Dr. H. Kirk Willard
National Environmental Research Center
    Environmental Protection Agency
        Corvallis, Oregon 97330
             Prepared for

   OFFICE OF RESEARCH AND MONITORING
 U.S.  ENVIRONMENTAL PROTECTION AGENCY
        WASHINGTON, D.C.  20460

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               EPA Review Notice
This report has been reviewed by the EPA and approved
for publication.  Approval does not signify that the
contents necessarily reflect the views and policies
of the Environmental Protection Agency, nor does
mention of trade names or commercial products con-
stitute endorsement or recommendation for use.
                      11

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                             ABSTRACT
The water storage of logs is widely practiced in the Pacific Northwest.
An investigation has been made to determine the effect of this practice
on water quality.

Soluble organic matter and some inorganics leach from logs floating in
water and from logs held in sprinkled land decks.  The character and
quantity of leachate from Douglas fir, ponderosa pine and hemlock logs
have been examined.  Measurements including BOD, COD, FBI, solids and
toxicity have shown that in most situations the contribution of soluble
leachates to holding water is not a significant water pollution problem.

The most significant problem associated with water storage appears to be
the loss of bark from logs during dumping, raft transport and raft stor-
age.  Dislodged bark can float until it becomes water logged and sinks
forming benthic deposits.  Floating bark is aesthetically displeasing
and could interfere with other beneficial uses of a lake, stream or
estuary.  Benthic deposits exert a small, but measurable oxygen demand
and may influence the biology of the benthic zone.  Implementation of
corrective measures by the timber industry to reduce bark losses could
make the water storage of logs a practice which is compatible with a
high quality environment.
                                 111

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                                CONTENTS


                                                                Page
Conclusions                                                       1
Recommendations                                                   3
Introduction                                                      5
Experimental Apparatus and Procedures                             9
Experimental Findings
  Part I:   Leachates                                             27
  Part II: Bark Debris                                           51
  Part III: Comprehensive Field Studies                          71
  Part IV: Magnitude of the Problem                              79
Discussion                                                       81
Acknowledgements                                                 85
Bibliography                                                     87
Publications                                                     89
Appendix A - Development of Masking Procedures                   91
Appendix B - Leachate Preservation With The Mercuric  Ion         95
Appendix C - Quantity of Bark  Dislodged During  Log Handling      97
Appendix D - Method for Extrapolation  of  Laboratory Test         101
             Data  for Field Application with  Example  Cal-
             culation

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                                  FIGURES

1
2
3
4
5
6
7
8
9
10
11
12

Log Storage Tanks for Leaching Studies
Schematic of Leaching Apparatus
Custom-made Tripod on Floating Log Raft
Details of Tripod Leg Joints
Reverse Image Slide Viewer with Slide Projector
Schematic Representation of Sunken Bark Removal
from Laboratory Test Barrels
Benthic Sampling Apparatus
Details of Benthic Sampling Apparatus
Freezing Chamber for Benthic Core Samples
Frozen Core Sample from Benthic Deposit
In Situ Benthic Respirometer
FBI Results for Douglas Fir and Ponderosa Pine
Page
10
12
14
15
16
17
18
19
20
21
22
28
       Logs in Fresh Water

13     COD Results for Douglas Fir and Ponderosa Pine            30
       Logs in Fresh Water

14     Total Organic Carbon (TOG) Results for Douglas Fir        31
       and Ponderosa Pine Logs in Fresh Water

15     Total Solids Results for Douglas Fir and Ponderosa        32
       Pine Logs in Fresh Water

16     Total Volatile Solids Results for Douglas Fir and         33
       Ponderosa Pine Logs in Fresh Water

17     COD and PBI Results for Unaltered Douglas Fir Logs        34
       in Fresh and Saline Water

18     COD Results for Unaltered Douglas Fir Logs in Fresh       37
       Water and Water Which Was Polluted by a Submerged Log

19     PBI Results for Unaltered Douglas Fir Log in Fresh        38
       Water

20     Leachate COD from Dynamic Storage Tests with Ponderosa    42
       Pine Logs
                                       VI

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                                                               Page
21     Leachate COD from Dynamic Storage Tests with             44
       Douglas Fir Logs

22     Sinkage for Composite Grab Samples of Bark               55

23     Percentage of Bark Sunk for a Graded Sample of           55
       Douglas Fir Bark

24     Percent of Bark Sunk for a Graded Sample of              57
       Ponderosa Pine Bark

25     Sampling Areas for Bark Distribution Study of            59
       Yaquina Estuary

26     Sampling Areas for Bark Distribution Study of            60
       Klamath Falls

27     Bark Distribution at a Typical Log Storage Area          62
       in Yaquina Estuary

28     Volatile Solids of Benthic Deposits at Selected          64
       Sites in Yaquina Estuary

29     Volatile Solids of Benthic Deposits at Selected          65
       Sites in the Klamath River

30     In Situ Benthic Oxygen Demand Results for Two Respiro-   67
       meter Runs at the Same Test Site on the Little
       Deschutes River near Gilchrist, Oregon

31     Benthic Oxygen Demand as a Function of Volatile Solids.  70
       (all values corrected for corresponding control area
       values)

32     Little Deschutes River Flow Curve Upstream from          74
       Gilchrist Pond.

33     Results of Dye Tracer Study at Gilchrist Pond.           74
                                     vn

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                                 TABLES
                                                                 Pages^

 1      BOD,  COD,  FBI  and  Toxicity  Associated  with  Leachate          39
       from  Logs  Held in  Static  Water  Storage for  Seven  Days

 2      Pollutants Contributed  by Douglas  Fir  and Ponderosa          41
       Pine  Logs  Two  Feet in Diameter  and Thirty Feet  Long
       Floating One-half  Submerged

 3      Total Kjeldahl Nitrogen and COD in Leachates  from           43
       Douglas fir Logs During Dynamic Leaching Studies

 4      Physical Characteristics  of Selected Log Ponds  in           46
       Oregon

 5      Chemical Characteristics  of Log Ponds  Studied               48

 6      Ponderosa  Pine Cold Deck Data                               49

 7      Incremental Percentages of  Bark Dislodged  During            53
       Logging, Unloading, and Raft Transport

 8      Bark  Losses from Douglas Fir Logs  During Unloading          53
       by Two Different Methods

 9      Size  Distribution  of Samples of Bark Collected Ran-          58
       domly from Log Dumping  Areas

10      Average Unit Weights, Percentage of Volatile Solids          61
       and Volatile Solids per Cubic Foot for Core Samples
       from Area D (Figure 25)

11      Total and  Volatile Solids for Benthic Core Samples          63
       as a Function of Depth Below the Water-Soil Interface

12      In Situ Benthic Oxygen Uptake as a Function of Volatile     69
       Solids Content in the Top Two Inch Layer of Bark Deposits

13     Percentage of Log Submergence in Water  (Based on            72
       Diameter)

14     Statistical Data for Raft Volume-Area Parameters            72

15     Measured Concentration of COD, BOD, PBI and TQC  at the      75
       Inlet and Outlet  of the Gilchrist  Log Storage Site

16     BOD, COD, PBI and TOC  in Inflow and Outflow from           75
       Gilchrist Log Storage  Reservoir
                                      Vlll

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17     BOD,  COD, FBI and TOC in Inflow and Outflow from the
       Log Storage Area on the Deschutes River

18     Predicted Increases in BOD, COD, FBI and TOC from the       78
       Log Storage Area on the North Fork Coos River

19     Predicted Increases in BOD, COD, FBI and TOC from the       78
       Log Storage Area on the South Fork Coos River

20     Total Organic Carbon (TOC) in Leachate from Plexiglas       92
       Blocks and Wood Blocks Coated with Different Masking
       Substances
                                      IX

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                           CONCLUSIONS
The following conclusions are based upon the results of a three year
research investigation outlined in this report.

     1.  Water storage of logs is widely practiced in Oregon,
         Washington and Alaska.

     2.  Leachates from logs held in water storage contribute
         organic substances which exert a BOD and COD.   In most
         situations the quantity of these substances which enter
         the holding water do not represent a significant water
         quality problem.

     3.  Log leachates  exert  some  acute toxicity  to  fish.
     4.  Color-producing substances measured by the FBI are
         found in log leachates, and are derived primarily from
         bark.

     5.  Bark is dislodged from logs in significant quantities
         during dumping and raft transport activities.  Consid-
         erably more bark is dislodged from Douglas fir logs
         than from ponderosa pine logs.

     6.  Log dumping methods significantly influence the amount
         of bark which is dislodged from logs.

     7.  Dislodged bark sinks at a rate dependent upon particle
         size and species of tree.

     8.  Bark deposits exert a small, but measurable, demand
         for oxygen from overlying waters.

     9.  Should the loss of bark to holding water be minimized
         by improved handling practices by the  timber industry,
         the water storage of logs would not constitute a major
         water quality problem.

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                         RECOMMENDATIONS
I.    Further study should be undertaken to determine the effect of bark
     deposits on the biology of the benthic zone and to evaluate the
     effect on water quality created by the dredging of bark deposits.

2.    The timber industry should strive to improve methods of depositing
     logs into water storage areas.  Methods for consideration might
     include:  (a) debarking logs on land before dumping, (b) installation
     of a sling hoist or fork lift to convey logs from trucks to holding
     water or  (c) utilization of a man-made dumping channel or pond
     adjacent to storage areas which would retain floating and sunken
     bark.

3.    The water storage of logs, with provisions for minimizing bark
     losses, should not be discouraged unless a suitable alternate
     storage method is  available which results  in  less  input to the
     environment.

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                           INTRODUCTION
Purpose

This research was intended to evaluate the water pollution potential of
log storage practices in the Pacific Northwest.  Specific aims of the
research were the determination of:

     - the quantity, character and pollution potential of substances
       "leached" from logs while floating in water,

     - the degree to which leached substances are toxic to biological
       life as measured by bioassays,

     - the extent and rate at which leached substances are degraded
       biologically,

     - the distribution of debris under and in the vicinity of log
       rafting and storage areas,

     - the rate and extent of aerobic biodegradation of benthic bark
       deposits, and

     - the extent of log raft storage in the Pacific Northwest.
This research included both laboratory and field studies dealing with
pollution problems from soluble leachates and bark debris from several
species of timber in the Pacific Northwest.  The three year project was
conducted in a region extending from California to Alaska, however, the
major  study area was central and western Oregon.
 Background

 Timber  is a bountiful  resource in the Pacific Northwest and is an impor-
 tant  factor in  the  economic stability of the region.  The timber industry,
 which includes  the  production of pulp and paper,  lumber, plywood, and a
 multitude of  other  forest products, ranks as the  region's leading indus-
 try  (19).

 The numerous  sawmills  and pulp and paper mills which dot the Pacific
 Northwest find  it necessary to retain large inventories of logs to pro-
 vide  a  continuous timber supply throughout the year.  Logs which are
 simply  piled  upon the  land, soon dry out at the ends and deep cracks
 develop longitudinally.  This phenomenon, referred to as "end checking",
 greatly enhances product wastage.  End checking can be minimized by
 sprinkling land-decked logs or, more commonly, by floating the logs in

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water.  Rafted logs are commonly found in lakes, rivers, estuaries,
sloughs and man-made ponds.  Oregon alone has over 12,000 acres of log
ponds and 2,000 acres of sloughs and canals used for log storage (18).

Prior to this research investigation little effort had been put forth to
determine the magnitude of the pollution problem associated with log
handling practices.  McHugh, Miller and Olsen (18) surveyed over 80 log
ponds in Oregon in an attempt to find a chemical means to measure the
degree of pollution of a pond.  Generally, they found the log pond waters
to be high in chemical oxygen demand (200 ppm to 700 ppm) and total solids
(200 ppm to 800 ppm).  Average concentrations of 0.48 ppm for phosphates,
0.56 ppm for nitrates, and 5 ppm for soluble carbohydrates were reported.
Very low concentrations of nitrites, sulfates, and dissolved oxygen were
found for most of the ponds.  The researchers concluded that ponds con-
taining logs without bark  (peelers) were just as polluted as those con-
taining an equivalent volume of bark-covered logs per unit volume of
water.

Ellwood and Ecklund  (8) reported the following values for a log pond
storing ponderosa pine:  suspended solids, 38 ppm; dissolved oxygen,
0 ppm; and pH 6.8.  The authors attributed the strong, sour smell of log
ponds to the production of organic acids as a result of carbohydrate
breakdown by microorganisms present in the ponds.

Henriksen and Samdal (11) agitated bark with distilled water and measured
the chemical oxygen demand  (COD) at different intervals.  After 65 hours
they found that a total of 43,200 mg COD/kg bark had been extracted.

Wood bark pollutants from both softwood and hardwood trees were evaluated
by Sproul and Sharpe (24).  They measured the quantity of COD, color,
lignin^like extracts and other "pollution parameters" which enter natural
water from benthic bark deposits and from drainage from bark piled on land.

Wood is customarily differentiated into major cell wall components and
extraneous components.  The major cell wall components consist of cellu-
lose, hemicelluloses and lignin.  Cellulose makes up 40 to 50% of wood
by weight.  Hemicelluloses  are polysaccharides which are closely related
chemically to cellulose.   Lignin forms the boundary between adjacent
cells and acts as a  cementing material which bonds the cells together (6).
With the exception of a small part of the lignin these components are
insoluble in organic solvents and in water  (27).

The extraneous components  are soluble in many solvents, including water,
and are frequently termed  extractives for that reason.  The character of
the extractives depends upon  the species of wood but generally include
tannins, resins, essential  oils, fats, terpenes, flavanoids, quinones,
carbohydrates, glycosides,  and alkaloids  (27).

Douglas fir and ponderosa  pine are the two predominant timber species
in the Pacific Northwest;  therefore, their extractives are of particular
interest.  Considerable research has been conducted on the extractives
from the bark of the above two species.  Since the vast majority of ponded
logs still have their bark intact, the bark extractives could well be the
major components of  the pond  water.

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Kurth and Hubbard (16) have reported that the principal water soluble
extractive of Douglas fir and ponerosa pine bark is tannin.  They found
the tannin content of Douglas fir bark to vary from 7.5 to 18% (based
on oven-dry bark weight) and that of ponderosa pine bark from 5.6 to
11.4%.  Although the above percentages are based on hot-water extractions,
Kurth (14) has found that the tannin content of bark taken from ponded
logs is considerably lower, indicating that tannin is also soluble in
cold-water.

In addition, Kurth, Hubbard and Humphrey (17) have found ponderosa pine
bark to have a water soluble reducing sugar content of 3 to 6% (based
on oven-dry weight of bark) whereas Douglas fir bark contained only one-
tenth of this amount.
Organization of Research

Initial phases of this research involved the development and application
of techniques and methodology for evaluating the rate of leaching of
soluble organics from logs immersed in water; the quantity of bark dis-
lodged from logs during unloading and transport operations; the rate of
bark deposition; the distribution of bark debris in benthic deposits;
and the rate of oxygen uptake by benthic deposits containing bark debris.
Results of these determinations provided a basis for predicting the
magnitude of pollution from the water storage of logs.  These studies
were conducted both in controlled laboratory experiments and in field
situations.

Extensive field investigations at three different locations in Oregon
were undertaken after the developmental work in an attempt to determine
the impact of log handling activities on water quality.  Results of
direct water quality measurements in selected log storage areas were
compared with predicted values.

An unproductive attempt was made to ascertain the magnitude of pollution
problem in the Northwest resulting from the log handling activities.
Limited quantitative data was obtained.

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                EXPERIMENTAL APPARATUS AND PROCEDURES


Introduction

A search of the technical literature revealed that very little research
activity had been undertaken regarding pollution problems associated with
log handling and storage.  Furthermore, very few standard methods or pro-
cedures have been reported for studying problems of this type.  As a
consequence a considerable portion of this research effort was devoted to
the development of apparatus and procedures which could provide meaningful
information on this somewhat unique problem.  The following sections of
this phase of the report describes in considerable detail the apparatus
and procedures developed to study leachate and bark problems associated
with the water storage of logs.


Leachate Studies

General.  Floating logs present  two different types of surface for con-
tact with the water, the cross-cut end sections and the cylindrical
surface.  Since logs in floating rafts are generally 20-40 feet in length,
the cylindrical surface area contributes the majority of the surface
area exposed.  Laboratory facilities at Oregon State University were not
adequate to handle full-length logs, consequently sections 14-20 inches
long were used.  These sections  had a much higher ratio of end area to
cylindrical area.  Since the leaching mechanism was not clear at the
beginning of the research, the relative effect of the end area versus
cylindrical area had to first be determined.  This was accomplished by
application of a masking material to the cross-cut ends.  A discussion
of the procedure developed for masking log ends is presented in Appendix A.

Static tests.  The three species of timber selected for this study were
Douglas fir, ponderosa pine and  hemlock.  These are the most prevalent
species in Oregon and the Pacific Northwest.  Log sections were cut from
freshly felled trees in central  and western Oregon.  Some of the sections
were debarked by hand and others were left with bark intact to determine
the effect of bark on the leaching rate of soluble substances from logs.
The cross-cut ends of selected log sections were sealed with paraffin
whereas others were left unsealed.

The prepared log sections were immersed in six custom-built,150-liter
plexiglas tanks.  All tanks were fabricated from one quarter-inch clear
plexiglas sheet stock to allow visual observation of the logs during the
leaching period.  Figure 1 shows the construction details of the holding
tanks.  Water-tight joints were  developed by cementing the sections to-
gether with, dichloromethane solvent.  The tank dimensions were chosen
to maximize the size of samples  within the storage space available.  Two
shelves were constructed in a temperature-controlled room to support the
test tanks.  There was no outflow from the test tanks in the static
leaching tests.  However, some mixing was provided in each tank to reduce
the development of concentration gradients near the log surfaces.  Teflon

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rn_^— - hold-down
1..I t _Jt j li J
^_^— 1/2° 1/2" plexiglass bracing
in corners
1
=o
CM



T
O
CM


       PLAN
28 1/2
28"

^^-— 1/4" plexiglass sheet

^ — drain


~o
CM


O
CM

                                                          20'
                              ELEVATION
FIGURE  I.Log  Storage   Tanks  for  Leaching   Studies.

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coated stirring bars were placed in each tank and were rotated by
magnetic stirrers mounted flush with the shelf surface as shown in Figure 2.

Log samples were held at 20°C +^0.5 throughout the test period to provide
a consistent basis for comparison of the experimental data.  This temper-
ature was selected because it approximated the mean summer water temper-
atures surrounding existing log rafts in the inland and coastal waters of
Oregon.

Mercuric chloride was added to each tank to provide a mercuric ion (Hg++)
concentration of 2 to 25 mg/1.  This metabolic poison was added to retard
biological degradation of the organic material leached from the logs.
Other methods of inhibiting biological growth were considered including
pH extremes, heat sterilization and organic biocides.  These were rejected
due to the uncertainty of an effect on leaching rate and measured indices
of pollution.  For instance organic biocides would add COD, total organic
carbon and volatile solids to the storage water.

Samples of leachate were withdrawn from the six test tanks at specified
intervals during 7 to 40 day log storage periods and analyzed for the
following indices of pollution:  chemical oxygen demand (COD), Pearl-
Benson Index (PBI), total solids, total volatile solids, total organic
carbon, wood sugar, biochemical oxygen demand (BOD) and acute toxicity.
BOD and toxicity determination were performed on samples which were pre-
treated by selective chelation to remove the mercuric ion added as a
preservative.  A discussion of the mercury removal technique is given
in Appendix B.   A more detailed description of the apparatus and proce-
dures used in the leaching studies is given by Graham (10) and Atkinson
(3).

Dynamic leaching tests.  The second type of log leaching study involved
a flow-through system.  The plexiglas holding tanks used for the static
leaching study were adapted for flow-through experiments.  An overflow
port was positioned at the end opposite the inflow to minimize short
circuiting.  Tap water was metered at different flow rates into different
test tanks holding Douglas fir and ponderosa pine logs.  Evaporation
losses were controlled by covering the tanks with plastic sheets.  Mer-
curic chloride was added to the inflow water to maintain a concentration
of about 50 mg/1  (as Hg++).  The poison was to retard biological break-
down of leached organic substances.  Since constant flow was exceedingly
difficult to maintain at the required low rates, overflow was collected
in a carboy and measured every 2 to 3 days with a graduated cylinder.
Overflow samples were collected for COD analysis only.


Bark Studies

The following experimental methods were developed to study the quantity
of bark dislodged from logs, the rate of bark deposition, the distribution
of bark in the benthic zone and the oxygen demand resulting from bark
deposits.
                                 11

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                          water  level
                                  log  section
                                                            hook
                                        teflon-coated stirring  bar
                                                                                      plexiglass  tank
_ring
                                                                         x  1/2" x 2"
                                                                   plexiglass  block
                                                            3/4"  plywood  shelf
                             _LJ	ii  ,   r
                   / magnetic  stirrer
FIGURE  2.Schematic  of    Leaching   Apparatus.

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Dislodged bark.  In order to accurately determine the percentage of bark
missing from logs in rafts, a photographic measurement technique was
developed.  A slide camera was mounted on a custom-made 20-foot tripod
as shown in Figures 3 and 4.  The legs were made from 2-inch aluminum
tubing in two ten-foot sections and one 8-foot section.  The tripod could
be readily assembled and disassembled on the log rafts.  The camera was
a Hasselblad model 1000F.  Ektachrome-X 120 film was used at a shutter
speed of l/250th of a second.  The camera shutter was controlled by a
long shutter release cable held by the operator on a log raft or boat
adjacent to the log raft being photographed.  Photographic slides were
also taken of Inaded log trucks to provide information on bark losses
during the unloading operation.  The camera was held by hand at a distanc
of approximately 20 feet.  Tabulated photographic measurements  are  given
 in Appendix  C.
The photographic slides of log rafts were projected upon a reverse-image
slide viewer.  The viewer consisted of a mirror set at an angle to pro-
ject an image on a horizontal viewing surface.  The viewing surface was
a 2-foot square frosted plexiglas sheet.  Figure 5 is a schematic repre-
sentation of the slide viewer.  Planar areas of logs with and without
bark were measured with a polar planimeter from the image projected on
the plexiglas sheet.

Bark sinking studies.  The rate at which dislodged bark sinks in water
was evaluated with grab samples and graded samples of Douglas fir and
ponderosa pine bark.

In the first experiment, grab samples of bark were deposited in 55-gallon
drums which were filled with water.  The drums were kept uncovered out-of-
doors.  At specified intervals during the experimental run the bark re-
maining on the surface was removed by a screening device.  Sunken bark
was retrieved by passing the water in the drum through a fine sieve.
Floating bark was returned to the drum and the drum was refilled.  The
sunken bark, which was collected on the sieve, was dried and analyzed
for total and volatile solids.  A schematic representation of this test
procedure is shown in Figure 6.

In a parallel experiment, randomly collected samples of Douglas fir and
ponderosa pine bark were screened through custom-fabricated sieves which
had square openings of 1/2,  1, 2, 3 and 4 inches on a side.  The graded
bark pieces  were then placed in open 55-gallon drums filled with tap
water.  Duplicate tanks were set up for all samples.  Sunken bark was
collected, dried and analyzed by the procedures described above.

Benthic deposits.  A core  sampling procedure was developed to study the
distribution of bark debris  in benthic deposits.  Sample tubes were made
from 2-inch  diameter, thin-walled aluminum tubing, 18 to 36 inches long.
One end of the tubing was reinforced and threaded for connection with
the benthic  sampler.

The benthic  sampler, shown in Figures 7 and 8, consisted of three separate
sections.  The top section was made of four pieces of 1/2-inch galvanized
                                  13

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    FIGURE  3.  Custom  Made  Tripod  on   Floating   Log  Raft.
steel pipe each four feet long.  These pipes were threaded on both ends
and one end had a 1/2-inch coupling permanently attached to it.  The
pieces of pipe could be added or removed to allow for the variable depth
of water encountered while sampling.

The middle section consisted of a 1/2-inch check valve and connecting pipe
fittings.  The check valve held the sample in the sample tube by maintain-
ing a vacuum seal in the sample tube as the tube was withdrawn from the
benthic deposits.  The water displaced from the sample tube during sam-
pling discharged externally through the check valve.

The bottom section was made of a 2-inch pipe coupling welded to a 1/4-inch
by 3 1/2-inch square steel plate.  The plate had a 1/2-inch diameter hole
drilled through its center point to allow for the discharge of the water
from the sample tube.  The sample tubes were easily screwed into and out
of the 2-inch coupling.

Samples withdrawn from the deposits were immediately frozen inside the
sample tube to preserve the vertical distribution of solids.  The sample
freezing unit, shown in Figure 9, was a 6-inch diameter insulated aluminum
tube.  The tube acted as the freezing chamber when dry ice and acetone
were added.  A center well inside the tube was made of window screen and
held in position with four evenly spaced vertical wood slats.   The sample
tubes were inserted into the center well and the dry ice chips were added
between the center well and the aluminum tubing.  The aluminum tube was
wrapped in 1 1/2-inch thick fiberglas insulation and enclosed in a 1/2-
inch plywood carrying case.
                                -

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                             v   3/16
  2" I.D. * 1/8"  walled  aluminum  pipe
2" 0-D. x I/IB"  walled
aluminum   tubing
                                             MIDDLE   JOINT
                         2" O.D. x  i/ie"  walled
                         aluminum   tubing
              2" l.D. x i/e"  walled
              aluminum   pipe
                                                            IS
                                              END    JOINT
    FIGURE 4. Details   of   Tripod   Leg   Joints.
                               15

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  projector
                                    PLAN   VIEW
                                                                                         CM
                                                                            24'
                                                   frosted   plexiglass
                                         1/4   plate  glass  mirror

                               ELEVATION   VIEW
FIGURE  5. Reverse  Image  Slide  Viewer  with   Slide  Projector.

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                    screening   device
         r-r •AOfc* fV\ <"•%
                        bark  debris
                               sunken  bark
                                                                    water
                                                    //a
                                10.20 mesh  screen
FIGURE 6. Schematic  Representation  of   Sunken   Bark   Removal   from
           Laboratory   Test   Barrels.
                                  17

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                                            Mil 'ta'TIg  ml
              FIGURE  7. Benthic  Sampling  Apparatus.
Sampling was done from boats or, when possible, from the log rafts.  A
minimum of two persons were required for sampling, one to physically obtain
the samples and the second to freeze and store the samples and to record
the location of the samples.  Maps were drawn to record the specific
location of each sample taken.

Samples were taken in the sampling tubes mounted on the benthic sampler.
The sampling tube was gently forced into the benthic deposit until a solid
bottom was reached, and was then removed.  In some cases a solid bottom
was not reached because of a very deep, soft deposit.   In this case the
sample tube would fill until the frictional skin resistance of the sample
in the tube exceeded the frictional resistance of the entire sampler
moving through the bottom deposit.  This condition was not frequently
encountered in the sites selected for this study.   The check valve kept
the semi-fluid sample from dislodging from the sample tube while the
sample was brought to the water surface.  At the water surface a rubber
stopper was placed in the open end of the sample tube to prevent dislodg-
ment and loss of the sample during the freezing process.  The sample
and sample tube were then taken to the boat while  still connected to the
benthic sampler.

The sample tube, containing the sample, was removed from the benthic
sampler and immersed into the dry ice-acetone mixture with the rubber
                             L8

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00
CM
                    0.5"   pipe
                    0.5"  check  valve

                    0.5"  nipple

                    0.5"  pipe coupling

                    	Q/l   3/16
         2.25'
          3.5"
                               3/16
                                      0.25   steel  plate
                            2   10  pipe  coupling
                    in
                    ro
   Benthic  Sampler
2  OD  aluminum  pipe
                                    3/16  K
                                2  ID  aluminum  tubing •
                                                              2.25'
CJ
                                                                        (0
                                                                        10
                                                         Sample  Tube
  FIGURE 8. Details  of  Benthic  Sampling  Apparatus.
                                  19

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       :
    FIGURE 9.  Freezing   Chamber  for  Benthic   Core   Samples.
 stoppered  end  down.   The  sample  tube  remained  in  the freezing unit  until
 :he sample was completely frozen.  About  three to five  minutes were needed
    freeze  a 24-inch  long  sample.   Frozen  samples  from the  freezing  unit
      :ied  to.the boat  by  a cord  and placed  in  the river or bay.  The warm
       in the river or  bay melted a thin layer  of  the  sample next to the
               This procedure required about three minutes.  The sample
    • was then  removed  from the water  and  shaken vertically to release
     :rozen sample from the tube, completely intact.   Figure 10 shows a
 rrozen sample  as removed  from the  sample  tube.  The  samples were then
wrapped in plastic paper,  held in  place with a strip  of masking tape at
            the  sample.  Packaged samples  were  labeled to correspond with
the map location from  where the samples were taken.  The samples were
           a portable ice  chest and covered with chipped dry ice to keep
      :rozen during transport to the laboratory.  At the laboratory the
       i were removed from  the portable ice chests and placed  in a chest
type freezer until removed for analysis.

A portable power circular saw fitted with a 7 1/4-inch abrasive blade was
            the frozen cores into 2-inch thick wafers starting from the
      soil  interface.  In order to decrease the ignition time of samples
:he wafers were then cut exactly in half.   These pieces  were then dried
in a drying oven at  103°C for 24 hours.
                              20

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        FIGURE  10.  Frozen   Sample  from  Benthic  Deposit.
The dried samples were placed in a tarred evaporating dishes which had been
previously fired at 600°C for 15 minutes and cooled in a dessicator.   The
samples were ground with a mortar and pestle before placing in the evapor-
ating dish if a large amount of cohesion existed in the samples.   Loose
samples were finely ground in the evaporating dish with a small scoop.
The dish plus sample was then weighed on a Mettler 46 analytical  balance.

Samples were preignited with a bunsen burner for 60 minutes to burn the
large pieces of bark debris.  Next,the samples were placed in the muffle
furnace at 600°C for another 60 minutes to ignite all of the volatile
material.  After this final ignition, the dish and sample were allowed
to cool in the open air for a few minutes and then were placed in a
dessicator until they had reached room temperature.  The sample and dish
were th'en weighed on the Mettler balance and the percentage of volatile
solids calculated.

A more detailed description of the apparatus and technique used in the
bark study is provided by Williamson (26).
Benthic respirometer.  A
to provide in situ oxygen
apparatus shown in Figure
housing, 79 cm long with
enclosed at both ends and
covered a planar area of
metal skirt was attached
deposits and restrict the
special respirometer was designed and fabricated
 uptake measurements on benthic deposits.   The
 11 was made from a plexiglas half-cylinder
an inside radius of 24 cm.   This chamber,  when
 bottom, contained a volume of 65 liters and
0.24 square meters.  A 4.5  inch galvanized
to the bottom of the chamber to penetrate  the
 zone of measurement.
                                21

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Is)
M
(|)
(3)
0
(5)
©
(?)
(5)
(9)
(To)
               MAIN CIRCULATION PUMP
               AQUARIUM PUMP
               REGULATING  VALVE
               UNION JOINT
               SENSOR  PORT
               DIFFUSING  SCREENS
               8ALVANIZED  SKIRT
                AIR  BLEEDING  PORT
                SAMPLING PORT
                PLEXIGLASS  SHELL
                   FIGURE  II.   IN  SITU   Benthic   Respirometer.

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A 40 gpm (at 10 ft head) centrifugal submersible pump and connecting
piping were mounted on the housing for circulation of water through the
chamber.  The recycled water passed through a series of nylon window
screens positioned at the inlet and outlet ends of the chamber.   The
screens served as baffles to provide a nearly uniform vertical flow pro-
file.

Once designed and fabricated, the respirometer was tested in a large lab-
oratory tank which had side wall windows.  A brightly colored dye was
injected into the intake end of the respirometer and was followed visual-
ly and photographically as it passed through the chamber.  The inlet and
outlet baffles were found to be effective in minimizing short circuiting.
The frontal edge of the dye tracer moved relatively uniformly through the
chamber.  Valve settings on the recirculation pump were calibrated with
the dye tracer test results.

A YSI (Yellow Springs Instrument Company) dissolved oxygen sensor was
mounted in the chamber as shown in Figure 11.  The sensor lead was con-
nected above the water surface to a YSI oxygen meter.  A small aquarium-
type pump and connecting tubing were mounted on the housing and recycled
liquid in the chamber past the oxygen sensor at a rate sufficient to
prevent stagnation.  A 1.0 mv potentiometric recorder was connected to
the oxygen meter to obtain a continuous readout of dissolved oxygen.

Electrical power was supplied to the oxygen meter, submersible pumps and
recorder by a 1500-watt gasoline-powered generator.

A trained scuba diver placed the respirometer in the appropriate location
for benthic oxygen uptake measurements.  The following procedure was
followed by the diver and assisting personnel:

      1.  Open union joint, air bleeding valve and sample port.

      2.  Remove inlet hose from the aquarium pump.

      3.  Submerge the respirometer in the water.  Start the pump,
          then rotate and shake to remove entrained air bubbles in
          the pump and piping.  Turn off pump,

      4.  Force the respirometer into the deposit.  A knife or trenching
          tool may be needed in hard deposits.

      5.  Start pump to flush the respirometer.

      6.  Calibrate oxygen meter and sensor and insert sensor into
          the port on the respirometer.

      7.  Close union joint, air bleeding valve and sample port.

      8.  Attach aquarium pump inlet hose.

      9.  Take grab samples from sample port for dissolved oxygen anal-
          ysis by a chemical method and for other desired analyses.
                                23

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     10.  Check seal around skirt and check for proper valve settings.

     11.  Start recorder and take oxygen uptake readings.

     12.  Operate system until a uniform uptake rate is established,
          usually 2 to 4 hours.

     13.  Take grab samples from the sample port for subsequent analyses.

     14.  Turn off the power, remove the sensor and remove the respiro-
          meter.

     15.  Take core samples at the respirometer site, to determine total
          and volatile solids.


Analytical Methods

Pearl-Benson Index (FBI).   The concentration of tannin, lignin and other
phenolic compounds leached from log segments while in water storage was
determined by the standardized Pearl-Benson, or Nitroso method (7).  FBI
is a colorimetric determination of the quantity of lignin and other phe-
nolic compounds present in a sample.  The FBI test is used to evaluate
spent sulfite liquor (SSL) concentration in waste streams from pulp mills.
A DU spectrophotometer was used to measure the color developed in the test.
A standard SSL in a range of known concentrations was used to standardize
test results.  The standard was calcium SSL, (Orzan+)> made from a ten
percent concentration of SSL.

Chemical^ oxygen demand  (COD).  COD analyses were made using the Jeris
"rapid" COD technique (13).  The standard COD method (1) was applied to
one series of samples to obtain a correlation between the rapid and stand-
ard procedures.  Results with the Jeris method were within 4 percent of
those obtained by the standard method.

Biochemical oxygen demand (BOD).  Five day BOD analyses were made using
300 milliliter BOD bottles and applying the dilution technique described
in Standard Methods (1).  Seed for the BOD tests was obtained from a
bench scale activated sludge unit containing microorganisms acclimated
to effluent from a fibreboard plant.  The unit was batch fed daily to
accomplish the acclimation of seed.

BOD reaction rate (k-rate) .  Oxygen uptake data used in k-rate determi^-
nation was obtained using the Hach manometric BOD apparatus.  Interval
oxygen uptake readings correspond to the BOD exerted.  The determination
of k-rate was accomplished by matching curves obtained from experimental
data to standard curves obtained using a mechanical plotter in connection
with the Oregon State University computer.  To obtain a standard curve
for matching with an experimental curve, 5-day BOD values from experimen-
tal data and an assumed series of k-rates were supplied as input to the
computer program.  A series of mechanically plotted curves was obtained.
The closest fit between standard and experimental plots determined k-rate.
                               24

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Reducing sugar content.  Reducing sugar content was determined using
techniques described by Somogyi  (23) and the procedure presented by Hodge
and Hofreiter (12).  The titrimetric method applying the 1945 alkaline
copper reducing agent was used.

Bioassay for toxicity determination.  Bioassays were conducted at the
Oregon State University Oak Creek Laboratory by a standardized procedure
(1).   The test tanks were located in a constant temperature room held
at 14°C.  Test fish were acclimated to Oak Creek water.

Each bioassay test unit consisted of a 2-gallon circular cardboard con-
tainer fitted with a plastic liner.  Six liters of water were placed in
the container and a stream of air was bubbled slowly through the water
for 24 hours before the test fish were introduced.  A total of 10 fish
were used in every unit and the number of dead fish counted visually at
24 hour intervals for a period of 96 hours.  The water was not mechanically
stirred and the fish were not fed during the 96 hour test period.  No
fish was used more than once and surviving fish were kept separated from
the remaining unexposed test fish.  Oak Creek water was also used for
log storage to eliminate differences in quality between bioassay and
storage water.

Two types of fish were acquired for use as test organisms in toxicity
determination.  Chinook salmon, Oncorhynchus tshawytscha  (Walbaum),
approximately three months of age, were used until the supply was ex-
hausted.  The salmon were obtained in May, 1969 from the Department of
Fisheries and Wildlife Hatchery, Netarts, Oregon.  Kamioops rainbow
trout, Salmo gairdneri (Richardson), also three months of age, were
purchased from Trout Lodge Springs Hatchery, Soap Lake, Washington.  The
trout were obtained in June, 1969 and were used during the remainder
of the study.
                               25

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                       EXPERIMENTAL FINDINGS

                        Part I:   Leachates
Introduction

Soluble organic matter and color-producing, lignin-like substances which
are extracted from logs floating in water can lead to a gradual deterio-
ration of holding water quality.  The organics, measured in this study
as BOD, COD, TOG and volatile solids, can create a dissolved oxygen
demand on the holding water during biodegradation and could lead to foam-
ing problems.  Color-producing substances measured by the FBI test affect
the aesthetic quality of water and, thereby reduce its value for recrea-
tional use and as a water supply source.  Furthermore, some of the water
soluble extractives may be deleterious to fish and other forms of aquatic
life.

The quantity and character of substances leached from logs in water
storage were determined by both static and dynamic leaching tests con-
ducted under carefully controlled laboratory conditions.  A description
of the apparatus and procedures used in these tests is presented in an
earlier section of this report.
Static Leaching Tests

Set-up.  In initial experiments, Douglas fir and ponderosa pine log sec-
tions were submerged in tap water and in saline water poisoned with mercu-
ric chloride.  Some of the sections had ends sealed with paraffin; others
had all bark removed and ends sealed; whereas others remained unaltered,
i.e., bark intact and ends open.  Chemical analyses were performed on
samples of water withdrawn at specified intervals during 30-40 day holding
periods to measure the rate of leaching of soluble,color-producing sub-
stances and organic matter.  Several duplicate runs were made to deter-
mine the reproducibility of experimental findings.  Close agreement was
consistently observed for the duplicate samples.

Color-producing substances.  Soluble tannins and lignin-like substances
impart a yellow to brown color to natural waters.  The addition of these
substances to log holding water was measured by the FBI test with results
expressed as grams of equivalent spent sulfite liquor  (10% solids basis)
per square foot of cylindrical log surface area submerged.

The experimental results plotted in Figure 12 clearly illustrate that
nearly all of the color, as represented by FBI, is contributed by the
log bark.  This was not unexpected since bark is known to contain a
considerable quantity of water extractable tannins and lignins.  The
peeled logs  (w/o bark) of both species yielded very low FBI values after
40 days of soaking.  Furthermore, the rate of--FBI loss to the holding
water was found to be significantly higher for the unaltered log with
                               27

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    30
    20
a
DL
     :
On i
a 	 &
D 	 D



^<
fe^ff-i
InnlforAH
Ends Sealed,
Ends Sealed ,
_x
~^

— D
i — zs 	

tf/0 Bark
W Bark
'O
Douglas

r


D

fir

	 &
i i
                    :
  20           30


TIME   (days)
40
t.  20
CD
a.
                -O  Unaltered

                -^  Ends  Sealed, W/0 Bark
       _D	D  Ends Sealed,  W Bark
                   10
  20           30


TIME   (days)
      FIGURE 12. FBI  Results  for  Douglas  Fir and   Ponderosa


                 Pine  Logs  in  Fresh  Water.
                           .

-------
unsealed ends.  This demonstrates that the ratio of end area to cylindrical
surface area is significant and must be considered in field application
of laboratory results.

Soluble organics.   The loss of soluble organic matter from floating logs
was measured initially by COD, TOG, total solids and total volatile
solids tests.  BOD determinations were made in a later study.  Experi-
mental results obtained during a 37-40 day test are graphically presented
in Figures 13, 14, 15 and 16.  Each graph shows that ponderosa pine logs
yielded significantly greater quantities of organic matter per square
foot submerged than Douglas fir logs.  This observation is consistent
with the findings  of Kurth, et.al. (17).  They found that the extractable
tannins from pine  bark contain nearly 10 times more soluble sugar than
do the tannin extracts from the bark of Douglas fir.

The rate of leaching of soluble organics during the first 3 to 4 days of
soaking was apparently influenced by the presence of intact bark.  This
is illustrated in  Figures 13 and 14.  The logs with ends sealed and bark
removed, lost COD  and TOC at a higher initial rate; however, the rate de-
creased as the soaking period lengthened.

The open ends of floating logs are responsible for a substantial portion
of the soluble organics lost to the holding water.  This is readily
apparent in Figures 13 and 14 when comparing the COD and TOC contributed
by unaltered logs  with that from logs having sealed ends but bark in
place.  This observation is not surprising since the physiological flow
pattern of water and nutrients proceed longitudinally through a living
tree.  By using the calculation method outlined in Appendix D it can
be estimated that  12 percent of the COD lost from a 30-foot long Douglas
fir log 2 feet in  diameter is derived from the end section.

A high percentage  of the total solids leached from the experimental logs
were found to be volatile.  Figures 15 and 16 show that over 80 percent
of the solids leached from the Douglas fir log in 40 days were volatile,
and nearly 62 percent of the solids from the pine logs were volatile.

Saline water.  A vast quantity of Douglas fir logs are rafted and held
in storage for extended periods of time in the saline estuaries and bays
along the Pacific  coast.  A laboratory experiment was undertaken to deter-
mine whether the leaching rate of substances from logs held in saline
water is measurably different from the rate for logs held in fresh water.
A saline water solution was artifically prepared by mixing equal quantities
(by volume) of fresh tap water and synthetic sea water.  Nearly identical
unaltered Douglas  fir logs were submerged in both the saline preparation
and in an equivalent quantity of fresh tap water.  Figure 17(a) shows
COD exerting substances were extracted from the logs at nearly the same
rate regardless of the character of the holding water.  There was less
than 10 percent difference in total loss of COD after 38 days of soaking.

The FBI results shown in Figure 17(b) indicate that considerably more
lignin-like material was present in the fresh water after 38 to 40 days
of soaking than in the saline water.  The apparent lower FBI yield in
                               29

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              -O Unaltered
              -A Ends  Sealed, W/0 Bark
         	rj Ends  Sealed, W  Bark
TL  6
    5
a
8  4
V— — u I
A 	 a 1
a 	 D i




jnunvrra
inds Sealed, \
Ends Sealed,


^
O/^
/^ n^-
¥/0 Bark
IW Bark

^
>^
___„, — *""

^±
^^

• — •
                                  ponderosa  pine
                  10
30
                              20
                           TIME  (days)
FIGURE I3.COD  Results  for  Douglas  Fir and  Ponderosa  Pine
           Logs  in  Fresh  Water.
                              30

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c
c
         O——O Unaltered

         A	a Ends  Sealed, W/0 Bark

         D	D Ends  Sealed, W Bark
                   1C
  20          30


TIME   (days)
 c
 c
                 O  Unaltered

                    Ends Sealed, W/0 Bark
         O	D  Ends SeaJed, W Bark
                    10
   20           30


TIME  (days)
                                                         40
    FIGURE 14. Total Organic  Carbon  (TOG)  Results  for Douglas  Fir

               and  Ponderosa  Pine  Logs  in Fresh  Water.
                              31

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        O	O  Unaltered     I

        &	&  Ends  Sealed, W/0 Bark

        D	D  Ends  Sealed, W Bark

                      a
                      A
CO
Q



O
V)
       -O	O  Unaltered
                    Ends  Sealed, W/0 Bark


       -D	D  Ends  Sealed, W Bark

                                I
en
o


o
CO
                                                          40
    FIGURE 15. Total  Solids  Results  for  Douglas  Fir  and  Ponderosa


               Pine Logs in  Fresh  Water.
                               32

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CO
G   3
3
LJ
             —O  Unaltered
             —6  Ends  Sealed,W/0 Bark
        D	D  Ends  Seated ,W  Bark
                   10           20           30

                          TIME  (days)
                             40
r  5
               -Q  Unaltered
               -A  Ends Sealed, W/0  Bark
        D	D  Ends  Sealed, W  Bark
                   10
   20           30

TIME  (days)
40
   FIGURE 16. Total  Volatile  Solids  Results  for  Douglas Fir  and
              Ponderosa  Pine  Logs in  Fresh  Water.


-------
  25
  20
   15
oo
Q-  |0
             -O  Fresh Water
       D	D  Saline  Water
                10
   20

TIME (days)
  (B)
30
40
a
O
O
•J— — v-»
3 	 D

WUIt
Saline Water
Q^"3"




a^--

                                                   .-a
                 10
   20
30
40
                        TIME  (days)
                          (A)
FIGURE 17. COD  and  FBI  Results  for  Unaltered  Douglas  Fir

           Logs  in  Fresh  and  Saline   Water, (note. (A)  COD

           and  (B)   PBI.)
                          34

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salt water may be due to the precipitation of lignin-like substances  by
divalent cations present in high concentrations in the water.   This pre-
cipitation phenomen was observed by Andrews (2) in a study of kraft pulp
mill discharges into saline waters.

Effect of holding water quality.  Two different conditions occur in  actual
log rafting and storage operations which were not represented by the
laboratory experiments outlined above.

First, log rafts in flowing natural waters such as rivers and estuaries
are subjected to a continual interchange of water over the log surfaces.
Consequently there is little tendency for the formation of a concentration
gradient of leached substances which might retard the rate of diffusion.
This condition was approximated in the laboratory by placing a presoaked
Douglas fir log, which had been submerged for 40 days into a tank of
fresh water and measuring the release of COD and FBI. The results of this
experiment plotted in Figures 18 and 19 show that the amount of COD
leached from the log in each 40-day period was very nearly the same,
indicating that a continuous rate of leaching is likely if a concentration
gradient is not allowed to develop.  This observation is significant since
logs are frequently held in water storage for 80 days or longer.  Further
information regarding the rate of leachate over extended storage periods
is presented in the section of this report entitled "Dynamic Leaching
Experiments."

The second field condition worthy of consideration occurs when freshly
cut logs are deposited into relatively stagnant log ponds or some lakes.
In these situations where only minimal water interchange is possible,
a concentration gradient does develop which could alter the rate of
diffusion.  A  laboratory experiment was set up to determine whether  the
leaching rate  from a freshly cut  log is retarded by polluted water.

A freshly cut, unaltered Douglas  fir log was placed into a tank of water
which had previously held a similar log for 38 days.  The rate of leaching
of COD was followed for 42 days and the results plotted  in Figure 18.
The plot shows that nearly 5 grams of COD/ft2  were  lost  in fresh water
whereas a similar freshly cut log  lost only 1.7 grams of COD/ft2 in  the
polluted water.  This  implies that a concentration  limit is approached
in stagnant  log pond waters independent of the quantity  of logs stored
or the  length  of storage period.

BOD,  toxicity, and sugars.  A parallel, static  leaching study was conducted
to determine the BOD,  toxicity  and wood sugar  content of  log  leachates.

Douglas fir, ponderosa pine and hemlock logs,  15  inches  in diameter,
were  cut  into  sections 20  inches  long  and  suspended  in storage  tanks as
described earlier  in  this report.   Bark was completely removed  from  some
of the  log segments.   Water from  a  creek near  Oregon  State University's
Oak Creek  Laboratory  was used in  all  experiments  since this water was
also  used  to rear  test fish for bioassays.
                                  35

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The log segments were held submerged for seven days in the creek water
poisoned with 2 mg/1 Hg-*+ in the form of HgCl2.  Following the storage
period at 20° + 2°C, aliquots removed from each holding tanks were de-
poisoned by chelation (see Appendix B) then analyzed for BOD5, BOD decay
constant, wood sugars and acute toxicity.   COD determinations were also
made to correlate test results with those reported above.   Results of
all analyses except toxicity were expressed as grams leached per square
foot of cylindrical log surface area submerged (g/ft2).

Experimental results summarized in Table 1 include experiments with one
hemlock log, one ponderosa pine log and two Douglas fir logs which differed
considerably in age.  In addition, two adjacent segments from the same
Douglas fir log were tested to determine the reproducibility and reliability
of results.

Results show that leachates from ponerosa pine, hemlock and older Douglas
fir logs, with and without bark, are not acutely toxic to salmon and
trout fry in 96 hour exposure.  The leachate from the younger Douglas fir
log did result in mortality to some test fish.  Log sections without
bark were more toxic than comparable sections with bark intact.  TLmg^
values ranged from 20 to 93%  (v/v) for leachate from the young Douglas
fir logs.  This slight, but measurable, toxicity for the young fir log
might be attributed to the much greater release of soluble substances to
the holding water.

This study also revealed that a considerable portion of the substances
which leach from logs is biodegradable and represents a significant
oxygen demand on holding waters.  Table 1 shows BOD5 values as high as
1.3 g/ft2.  BOD:COD values are commonly used as an indicator of the bio-
degradability of a waste,  BODs represents the oxygen required to bio-
logically degrade a given sample of organic matter, whereas COD represents
the amount of oxygen required to chemically decompose organic matter.
BOD5:COD values for the log leachate were found to range between 0.1 -
0.45.  This compares with a BOD5:COD of about  0.7 for glucose and 0.5
for raw domestic sewage.

A considerable portion of the BOD-exerting compounds in the log leachate
were wood sugars.  Table 1 shows that 0.18 to  0.41 grams of sugar leached
per square foot of submerged  log in 7 days.  The high BOD decay constants,
0.17 - 0.40, determined for log leachate can be attributed to the pre-
sence of this large fraction  of readily degradable wood sugars.  As
expected, ponderosa pine logs which released the highest amount of sugar
also had the highest decay rate.  The BOD decay constant is a measure of
the rate at which oxygen is consumed by bacteria during the biodegradation
of organic matter.  A high rate constant  (0.15 - 0.3) indicates the
presence of a readily degradable substance.

Even though a measurable quantity of biodegradable and toxic substances
leach from floating logs the  severity of pollution problem associated
with this storage depends upon the quantity of logs stored, the age
and species of logs and the flow rate of the holding water.  Each field
situation should be evaluated separately.
                                 36

-------
•
«  5





§  "
o


   3



   2
w-
Dr
•
0 	 C




• i_uy i TVUIC
] Leached Log in Fresh W
) Fresh Log in Polluted W


X
/




ntnr
ater
rf
.-• 	 — o



C
X




&-— -°"


,x


__ — 	

x<
z:


. 	
.^
^^



                                    20
                                       30         40


                                              TIME (days)
50
60
70
80
               FIGURE 18. COD Results for  Unaltered  Douglas Fir  Logs in  Fresh  Water  and  Water  Which


                         Was Polluted  by  a   Submerged  Log.

-------
•'.
O
                                                                  40

                                                            TIME (days)
                 FIGURE 19. PBI  Results  for  Unaltered  Douglas  Fir  Log  in  Fresh Water.

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                                             Table 1.   BOD, COD, FBI and Toxicity Associated with Leachate from Logs
                                                              Held in Static Water Storage for Seven Days
<£>
Log Description
Species Age Bark
Douglas fir
Douglas fir
Douglas fir
Douglas fir
Douglas fir
Douglas fir
Hemlock
Hemlock
Ponderosa pine
Ponderosa pine
50
50
50
50
120
120
50
50
70
70
1 -
g/ft* of submerged
yr with
with
yr w/6
w/o
yr with
w/o
yr with
w/o
yr with
w/o
surface area
BOD
g/ft2l(mg/l)2
0.90
1.20
0.93
1.30
0.11
0.56
0.27
0.93
0.80
1.36

( 84)
( 84)
( 44)
(120)
( 6)
( 42)
( 15)
( 79)
( 42)
( 92)

BOD decay COD BOD:COD
rate
days"1 g/ft2(mg/l)
0.25 3.25(193) 0.28
0.32 3.91(272) 0.31
0.19 3.18(287) 0.29
0.26 3.38(313) 0.38
0.17 1.0 ( 53) 0.11
0.30 1.89(189) 0.30
0.13 1.82(101) 0.15
0.28 2.04(174) 0.45
0.31 4.25(221) 0.19
0.40 2.63(177) 0.52

Reducing
sugars
g/ft2(mg/l)
0. 41 (24)
0.66
0.41 (37)
0. 50 (46)
0.31 (16)
0.41 (31)
0.23 (13)
0.18 (15)
0.84(44)
0.16 (11)

PBI Toxicity
as 10% SSL
g/ft2(mg/l) TLm4g TLmgg
7.11 (426)
12. 5 ( 46) 20% v/v
4.45 (402)
10. 8 (1005) 24% v/v
0.66 ( 35) 10% kill in 60% soln
after 72 hrs
'2.98(233) 93% v/v
2.06(114) n o kill in 96 hrs
1.91 (163)
7. 48 (416) no kill in 96 hrs
0.79 ( 53)

                  mg/1 in test tank

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Log leaching equation.  Based upon results obtained from the static log
leaching tests the following equation was derived for application in
field situations;

          T = [(l-x)(D)(Ac)] + [(x)(C)(Ac)] * [(£1)CB-D)(AE)]


where

      T  =  total pollutant contribution from logs (grams)

      B  =  grams leached from test log (ends unaltered, w/bark)
                           2
                         ft  cylindrical area

      C  =  grams leached from test log (ends sealed, w/o bark)
                           2
                         ft  cylindrical area

      D  =  grams leached from test log (ends sealed, w/bark)
                           2
                         ft  cylindrical area
                                                2
      A  =  total submerged end area of logs (ft )

                                                        2
      A  =  total submerged cylindrical area of logs (ft )


      x  -  fraction of bark missing from logs

      f1 =  cylindrical area of log
               end area of log
The term [(l-x)(D)(A )] represents the contribution from the cylindrical
log area with bark intact.  Correspondingly, the [(x)(C)(Ac)] term is
the contribution from the cylindrical area without bark and the [(f^)
(B-D)(Ag)] term is the contribution from the end areas.

This equation is in slightly different form than the one proposed by
Graham (9) in an earlier study.  Example calculations applying this
equation are given in Appendix D.

The above equation can be used to compare the quantity of organic matter
in log leachate for different storage conditions, species of logs and
surface conditions of logs.  Table 2 summarizes the estimated contribution
of COD, TOG, TS and TVS from Douglas fir and ponderosa pine logs, two
feet in diameter and thirty feet long.  Calculated values are shown for
logs with all bark intact and only 50 percent of the bark intact.  These
values show that pine logs add nearly 22 percent more COD and 99 percent
more TOG than fir logs of comparable size and degree of submergence.
                                 40

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    Table 2. Estimation of Pollutants Contributed by Douglas Fir and Ponderosa Pine Logs Two
          Feet in Diameter and Thirty Feet Long Floating One-half Submerged.
Log
species


Douglas
fir
Water
exposure
period
(days)
10
35
COD
(K)
100%
Bark
144
331
50%
Bark
163
332
FBI
Iz)
100%
Bark
265
683
50 %
Bark
204
522
TVS
(z)
100%
Bark
164
278
50%
Bark
174
249
TOC
(K)
100%
Bark
48
71
50%
Bark
-
-
 Ponderosa

  pine
10

35
210    183

403    344
 710

1375
555

915
211   154

349   268
 98

161
Dynamic Leaching

General.  In rivers,  estuaries,  and flow-through log ponds, water contin-
uously flows past rafted  logs.   This dynamic situation would discourage
the build-up of a concentration  gradient of leached substances at the
water-log interface.  A  laboratory experiment was set-up to evaluate the
influence of hydraulic flow rate on the rate of leaching.  The apparatus
and procedures developed  for this experiment are presented in an earlier
section of this report.

Poisoned log holding  water  was passed through test tanks at rates low
enough that some measurable accumulation of pollutants could be obtained,
yet fast enough to prevent  the development of a concentration gradient.
Flow velocities below 0.01  ft/min were needed to obtain sufficient  leachate
concentration for analysis, even though low velocities in excess of 50 to
100 feet per minute are  not uncommon in natural flowing streams and
estuaries.  Both Douglas  fir and ponderosa pine log segments (unaltered)
were studied.  Samples of overflow were periodically collected and  analyzed
for COD and nitrate and  Kjeldahl nitrogen.

COD.  The plot of cumulative COD in Figure 20 shows that the rate of
leaching of organic substances is nearly the same for static and low flow
rates.  However, at the  higher flow rates, the rate of leaching was rapid
initially then leveled out  after 30 days of immersion.  This indicates
that in swift waters  soluble organics will leach at a more rapid rate
than in more stagnant waters such as overflowing ponds, lakes and sloughs.
Furthermore, leaching from  the ponderosa pine logs will be essentially
complete within 30 to 35 days.   Previous static leaching tests had
indicated that the rate  of  leaching might remain constant for 80 days or
more.
                                  41

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                                             FLOW
                                           VELOCITY
                                           I0's ff/min
                                               -
                          I      I      I      I
       0     4     8     12    16    20    24     28    32    36    40    44
                                    TIME (days)
FIGURE  20.Leachate  COD  from Dynamic Storage Tests with Ponderosa Pine Logs.
                                      42

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Cumulative COD results  from Douglas fir logs plotted in Figure 21 also
reveal that logs held in  dynamic  water systems will contribute leachates
to the water at higher  rates  than in stagnant situations.   The rate of
leaching does not appear  to be  directly related to flow rate, however,
since similar quantities  of soluble organics were leached from the tanks
at all three flow velocities.   Even though the rate of leaching declined
after 25 to 30 days considerable  material was still removed from the
logs.

At the high flow rates  found  in natural streams, the initial leaching
rate would likely be very high.   No high rate studies were run during this
research investigation  because  of the difficulty in collecting sufficient
leachate for reliable quantitative measurement.  A closed recycle system
might have been applicable in the dynamic leaching studies.

Nitrogen.   Total Kjeldahl nitrogen and nitrate nitrogen determinations
were made during the dynamic  leaching experiment on samples of leachate
from Douglas fir logs.  Results in Table 3 show that a close relationship
exists between COD and  Kjeldahl nitrogen in the log leachate.  Values
ranges from 0.055 to 0.073 grams  of nitrogen per gram of COD with an
average of about 0.061.   Nitrate  nitrogen appeared in negligible quan-
tities in the leachate  samples  tested.
        Table 3.  Total Kjeldahl Nitrogen and COD in Leachates from Douglas fir

                    Logs During Dynamic teaching Studies
Storage time
hours
100
200
300
400
500
600

COD
1.28
2.39
3.65
4.77
5.79
6.69

N
g/ft2
0.093
0.156
0.214
0.269
0.322
0.369

N
COD
0.073
0.065
0.059
0.057
0.056
0.055
Avg 0.061
             *grams per ft  of Submerged surface area
                               43

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            8     12    16    20    24    Z8   32    36    <»U
FIGURE 21 .Leochate  COD  from Dynamic Storage Tests with Douglas
            Fir  Logs.
                          44

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Phosphorus.   Total phosphate phosphorus determinations were made on
leachate samples.   Results showed only trace quantities collected through-
out the entire dynamic leaching experiment.
Log Ponds

The pollution potential of logs rafted in lakes and rivers is readily
apparent.  Not so apparent, but very much a pollution threat, are the
numerous log ponds which dot the Pacific Northwest.  A great number of
these ponds are operated on an overflow basis with the overflow being
discharged to the nearest water course.  The fact that there are approx-
imately 12,000 acres of log ponds in Oregon alone, stresses the extent
of the problem.

Four log ponds situated at different locations in Oregon were selected
for evaluation.  These ponds exhibited different physical characteristics
as indicated in Table 4.  Several points were sampled within each pond
to determine if the pond water was homogeneous with respect to chemical
characteristics.

The BOD2Q (20-day BOD) values for each pond were much lower than corre-
sponding COD values.  For example Pond B had a COD of 504 rag/1 and a BOD2Q
of only 167 mg/1.  This difference can be readily explained by recogniz-
ing what each test measures.  The COD test measures all organic compounds
which can be oxidized to carbon dioxide and water by strong chemical
oxidizing agents, whereas the BOD determination measures the oxygen re-
quired to biologically oxidize an organic material.  Since many wastes
contain organic compounds that cannot be stabilized totally through bio-
logical action, the COD values are generally higher than the BOD2Q values.
BOD2o was used to estimate the ultimate BOD of the pond water.  Further-
more, the biodegradable substances which do leach from logs are attacked
immediately by microorganisms in pond water.  This results in a reduction
of BOD and also BOD;COD ratios.

Another important parameter of any waste is the BOD reaction rate con-
stant denoted as k.  Values for k can be found by solving the general
BOD equation  (20) when the BOD5 and BOD2o values are known.  High k values
indicate rapid exertion of BOD.  Very simple substrates such as sugars
are degraded rapidly thus the k rates are high  (0.20 to 0.30 day1).  The
k rates for the four ponds ranged from 0.03 to  0.08 day'1) which indicates
that the organic compounds present in the water were somewhat complex
and difficult to biodegrade.

All of the ponds contained sufficient amounts of nitrogen and phosphorus
to support biological growth.  The concentration of these elements in-
creased as the degree of pollution  (in terms of COD and BOD) increased.
This suggests that  some of the nitrogen and phosphorus must come from
the logs, although  neither pine nor fir contain much of these elements.
An important  source of the nitrogen and phosphorus is from the benthic
deposits in the ponds.  All the ponds tested were fairly old and had
extensive deposits  which consisted of bark, wood, dead algae and aquatic
                               45

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Table 4.  Physical Characteristics of Selected Log Ponds in Oregon
Surface
Pond area,
acres
A 26
B 20
C 2-1/2
D 3
Average
depth,
ft
8
6-8
12
4-5
Age of
pond,
years
11
14
19
39
Type of
logs
stored
Douglas fir
Douglas fir
85% ponderosa pine
15% Douglas fir
over 90% ponderosa
pine
Length
of
storage
l-3yrs
80% of
logs about
one week
two weeks
one week
Water
source
stream
wells
stream
springs:
irrigation
ditch
Remarks
non -overflowing except during
high runoff periods; sanitary
wastes dumped into pond.
non -overflowing except during
high runoff periods; sanitary
and glue wastes from plywood
dumped into pond
overflowing at about 400 gallon
per minute
overflowing at about 16 gallons
per minute

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vegetation.   As these materials undergo decomposition, nitrogen and phos-
phorus are released for reuse by the microorganisms feeding on soluble
leachates.  Other nutrient sources would include surface runoff, the source
water and some sanitary wastes which are dumped into the ponds.

The indices used to define the character of log pond waters included
chemical oxygen demand (COD), biochemical oxygen demand (BOD), dissolved
oxygen (D.O), phosphates, nitrates, total Kjeldahl nitrogen, total solids,
settleable solids, alkalinity, oxygen transfer coefficient, K^a, and
Pearl Benson Index (FBI).  The methods of measurement are described under
the section of this report entitled EXPERIMENTAL APPARATUS AND PROCEDURES.

Table 5 summarizes the results of analyses performed on water samples
from each of the four ponds.  Generally, the ponds proved to be quite
homogeneous with respect to the various parameters measured.  Therefore,
data from only one sampling point for each pond is listed in Table 5.

The length of storage time and hydraulic overflow rate seem to signifi-
cantly influence the chemical nature of the log pond water.  Ponds B and
D, which had short log storage times and low overflow rates, exhibited
much higher values for most all the characteristics studied than ponds
A and C.

As logs are added to a pond, leaching of the water soluble materials
begins immediately.  As time goes on these materials are depleted until
finally no further leaching can take place.  Therefore, the shorter the
log storage period, the greater the amount of substances available to be
leached.  A pond with a mean log storage time of one week will build up
greater concentrations of tannins, wood sugars, etc., than a pond which
stores the same logs for a year.

The high overflow rate shown for Pond C resulted from the addition of
large quantities of fresh water to the pond.  Therefore, the concentra-
tions of leached substances did not build up in Pond C as they did in
ponds with low discharge rates.

As shown in Ponds B and  D, the chemical oxygen demand  (COD) of  a  log
pond can be quite high (504 and 353 mg/1, respectively), indicating that
much of the material leached from the logs was organic.

The Pearl Benson Index (PBI) is a measure of the lignin-like substances
dissolved in water.  In  all cases the PBI values were closely related
with the COD values.  COD values for the four ponds ranged from 24 to
504 mg/1 and the corresponding PBI values ranged from 35 to 545 mg/1.
This could be expected since the same compounds detected by the PBI  test
would also contribute to the COD.

The dissolved oxygen  (D.O)  level in all ponds was  quite  low  (0.0  to  1.5
mg/1), even close to the surface.  This indicates  that extensive  biolog-
ical activity was taking place within the ponds.   The quiescent condition
of the ponds also contributed to the  low D.O. values  since  oxygen trans-
fer is much less effective under these  conditions.
                                 47

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                                       Table 5.  Chemical Characteristics of Log Ponds Studied
Pond
A
B
C
D
TS,a
mg/1
254
747
356
606
*vsb
59
55
31
46
ssc,
mg/1
43
180
4
122
DO,
mg/1
0.1
0.3
1.5
0.7
Temp. ,
°C
22
21.5
23
21.5
PH
6.9
7.1
7.5
7.4
COD,
mg/1
116
504
23
353
mg/1
48
167
10
116
mg/1
29
54
6
68
BOD5
COD
0.25
0.11
0.25
0.19
k,
day"-'-
0.08
0.03
0.08
0.08
mg/1
2.4
10.4
1.0
4,9
N03-Ne
mg/1
0.6
1.5
0.1
0.7
po4
mg/1
0.5
1.2
0.1
2.0
FBI,
mg/1
175
545
35
338
a   = total solids
 1 S


b   = volatile solids



c   = suspended solids
 oo
d   = total Kjeldahl nitrogen (ammonia plus organic nitrogen)
 NO,-N = nitrate nitrogen

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Cold Decks

General.  There  are  several locations in Oregon  and  the Pacific Northwest
where the water  storage of logs is not permitted or  is  not practical.  In
such instances the  industry must store their  inventory  of logs on land in
cold decks.   In  order to minimize losses of timber through splitting of
log ends, the decked logs are frequently sprinkled with water.  Water
which pases over the logs picks up water soluble organics and inorganics
from the wood.   Consequently, underflow from  sprinkled  cold decks contain
similar pollutants  to those extracted during  submerged  water storage.
Cold deck underflow  is sometimes recycled  although more commonly it is
discharged to a  receiving body of water.

A field study was undertaken to obtain cold deck leaching data for com-
parison with  laboratory findings.  The number and surface area of logs
together with hydraulic flow rate and measured BOD of the cold deck run-
off are given in Table 6.  Based upon a BOD to COD ratio of 0.46 (esti-
mated from static leaching experiments)., the  resultant  daily COD con-
tribution in the under flow would be 147 Ibs/day.  Using these data, a
value of 0.085 g COD/ft^ can be calculated per 100 hours of sprinkling.
This value corresponds closely to the slope of the COD  vs time curve in
Figure 18 for ponderosa pine logs with bark intact for  an extended stor-
age period.  Thus,  it may be reasoned that the data  obtained in the
laboratory leaching  tests can provide a good  prediction for cold deck
operation in the field.
                    Table 6.  Ponderosa Pine Cold Deck Data
                parameter                         sampled value


               Mean log diameter                    19.2 inches

               Mean log length                      32. 5 ft

               Number of logs/25 lin. ft               350

               Lineal feet of cold deck                1740 ft

               Estimated number of logs               24, 400
                                                     /-  2
               Estimated surface area                 4.0 y. 10° ft

               Mean BOD of runoff                    19 mg/1

               Flow                              0. 426 mgd

               BOD/day                           67. 5 Ibs/day
                                   49

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                       Part II;  Bark Debris
Introduction

Trees felled in the forest are generally sawed into logs which vary in
length from 20 to 40 feet.  Logs are transported to temporary land or
water storage sites by truck or rail car.  Water storage sites include
lakes, rivers, estuaries and man-made ponds.

Logs are deposited into a water storage area by several methods including
direct vertical dump, sloped slide and cable hoist.  The logs are then
aligned into rafts for subsequent transport and storage.  This repeated
handling results in the loss of considerable amounts of bark from the
logs.  Bark dislodged in water will sink either immediately or after a
short soaking period.  Bark which settles to the bottom of water courses
forms benthic deposits which may have deleterious effects on aquatic
organisms inhabiting the benthic zone.  Additionally, benthic deposits
can exert a demand for dissolved oxygen from overlying waters.  The
methods used in the developmental phases of the bark study are described
in the section of this report entitled EXPERIMENTAL APPARATUS AND PRO-
CEDURES .
Dislodged Bark

The application of two-dimensional photography for estimating losses of
bark from logs required pre-evaluation of several potential sources of
error since logs are three-dimensional and photographs are planar.

First, optical dispersion in the camera field was determined by photograph-
ing one-foot square pieces of paper placed randomly on the ground beneath
the tripod-mounted camera.  The squares were compared in the resulting
photographs.  The degree of dispersion was found to be negligible.

Actual photographic scale was found to be insignificant since the per-
centage of bark missing was computed.  The projection of the curved
surfaces of the logs upon the planar  surfaces of the photographic slides
did not represent the true surface area of the logs.  However, on a
statistical basis, the percentage of  bark missing in any differential
area would be distorted equally.  This rationalization was verified by
physically measuring the total surface area of several logs and the area
of missing bark, then comparing with  photographic results for the same
logs.  Several logs were also rotated in the water and examined for
missing bark on all surfaces to insure that the percentage of bark missing
from the air-exposed surface was representative of the entire log.

Results of numerous photographic measurements of loaded log trucks, and
rafted logs, before and after raft transport, are given in Appendix C
                                  51

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for Douglas fir stored in Yaquina Estuary and for ponderosa pine stored
in the Klamath River.  Results summarized in Table 7 reveal that nearly
22 percent of the original bark was lost from Douglas fir logs during
unloading and raft transport compared to only 6 percent for ponderosa
pine logs.  This large difference can be explained by two factors, the
species of logs studied and the abrasiveness of unloading operations.

Unloading operations examined on the Yaquina Estuary were more abrasive
than the operations on Klamath River due to the greater height the logs
had to fall to the water surface during direct dumping.  At Yaquina
Estuary the elevation difference between the unloading deck and the water
surface varied with tidal fluctuation from 8 to 15 feet.  A fall of only
6 to 8 feet was observed on the inland Klamath River.  This difference
in distance gave the logs a greater impact velocity which increased the
amount of bark dislodged.

Probably the major factor responsible for the wide difference in bark
loss is the difference in character of the two species of logs studied.
As shown in Table 7, 18 percent of the Douglas fir bark was lost during
felling operations compared to only 6 percent for the pine logs.  During
earlier leaching experiments, sections of both the fir and pine logs
were debarked by hand.  Douglas fir bark peeled easily and in large chunks
whereas a chisel had to be used to peel the ponderosa pine logs.

A study was undertaken to compare bark losses caused by different unloading
techniques.  Fortunately for research purposes, the vertical dump appar-
atus used at the Yaquina Estuary site up to 1968 was replaced in 1969 by
a cable sling system.  Therefore, similar log types were studied during
the same month in both years.  Data from 190 photographic observations
were analyzed statistically as shown in Table 8 to ascertain the relative
bark losses from the two methods.  The vertical dump method was found to
be the most abrasive, as expected, with bark losses of 17.1% compared to
only 8.2% for the cable hoist system.  Therefore, the method of dumping
selected by the timber industry can substantially affect the quantity of
bark debris released to a water course.
Bark Sinking Rate

Bark sinking rate is dependent upon the moisture content of the bark
particles, the size of bark particles and the rate at which water diffuses
into, the bark pores.  Most pieces of bark will float for a short period
of time before they soak up moisture which increases their density and
causes them to sink.

The first sinking rate study involved a direct comparison of grab samples
of Douglas fir and ponderosa pine bark randomly collected at log dumping
sites.  The ponderosa pine bark debris consisted mostly of small, thin
chips approximately 1/16-inch thick with a 1/2-inch mean diameter, plus
a few large bark pieces approximately 3/8-inch thick with a 1 to 3-inch
mean diameter.  The Douglas fir bark debris consisted mostly of large
                                  52

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    Table 7.   Incremental Percentages of Bark Dislodged During Logging,
                      Unloading, and Raft Transport
Area studied
(species of logs)
Yaquina Estuary
(Douglas fir)
Klamath River
(ponderosa pine)
Percentage of Bark Dislodged
During During During raft
logging unloading transport
18.2 16.8 4.9

5.7

During
unloading and
transport
21.7

6.2

       Table 8.   Bark Losses from Douglas Fir Logs During Unloading
                        by Two Different Methods
Sample statistic

Bark removed before unloading

    No. of observations
    Mean (Xi)
    Standard deviation (s)
     Vertical Hoisting
           59
           24.8%
           12.1%
Direct Dumping
    38
    18.0%
    11.596
Bark removed after unloading

    No.  of observations
    Mean (X2)
    Standard deviation (s)
           73
           33.094
           13.4%
    20
    35.1%
     6.9%
Bark dislodged during unloading

    Mean (Xg - %)
    Pooled deviation (s)
    Sampled standard error

      (S    -}
            8.2%
           12.7%
            2.5%
    17.1%
    11.6%
     3.2%
1) Percent dislodged represents
debarked area
total surface area
                                                X 100.
                                   53

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pieces approximately 3/8-inch thick, 1 to 3 inches wide and 1 to 6 inches
long, although, there were some small bark chips.

The cumulative amount of bark which had sunk was measured several times
during the 60-day study.  Results plotted in Figure 22 show that about
10% of the bark of both species sank the first day.  These were mainly
the very small bark chips.  After 30 days of storage, nearly 70% of the
pine bark had sunk whereas only 47% of the fir bark had sunk.  This could
be accounted for by the higher quantity of small pine bark particles.  At
the end of 60 days, the quantity of bark of both species which had sunk
leveled out to approximately 75%.  This data indicates that at least 10%
of the bark dislodged during unloading operations will sink within the
first day and probably in the vicinity of the dump site.  Furthermore,
approximately 65% of the bark dislodged during dumping and raft transport
will deposit in the raft transport and storage areas, if the logs remain
rafted for 60 days.  Logs are frequently held in rafts for 60 days or
longer.  The remaining bark which does not sink within 60 days, will
either float with the prevailing currents or become trapped in the log
rafts.  Bark trapped in log rafts is frequently removed from the water
at the log processing site by a skimming mechanism.

Other experiments were undertaken to ascertain the effect of bark particle
size on sinking rate.  Cumulative amounts of sunken bark are plotted in
Figures 23 and 24 for Douglas fir and ponderosa pine bark respectively.
These results clearly indicate that sinking rate is dependent upon par-
ticles size.  All of the 0-1/2" size bark of both  species sank within
20 days of immersion whereas only 3% of the 4" or  greater particles of
ponderosa pine sank during this same period.  The  large Douglas fir bark
sank more rapidly than the pine, i.e., 27% sank within 20 days.

Table 9 shows the relative particle size distribution, on a dry weight
basis, for samples collected around log dumping sites in a random manner.
Approximately 30% of the pine bark was 0 to 1/2-inch in size whereas only
22% was 4 inches or larger
 Benthic Distribution

 Bark debris arising from  log storage activities, eventually sinks and
 becomes incorporated in the benthic deposits if not physically removed
 from the water.  The aim  of this part of the study was to determine the
 amount of bark in the benthic deposits  as a function of depth from the
 water-soil interface.

 Many techniques were considered for obtaining representative benthic
 samples.  The method selected involved  freezing an intact core sample
 followed by analysis of the sample for  volatile solids as a function of
 depth.  COD determinations were considered as an indicator of bark in
 the benthic zone, however, due to the high and variable concentrations
 of chlorides in the overlying water this pollutant index was rejected.
 Chlorides interfere with  COD determinations and require special consid-
 eration during analysis.  The volatile  solids test was finally selected
                                 54

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100
                                   LEGEND
                               D  Douglas fir
                               O  ponderosa pine
                              30       40
                           TIME (days)
 FIGURE 22. Sinkage  for  Composite  Grab Samples  of  Bark.


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                 100
in
LU

z
(0

(E
00
                              10
                          20
30        40        50
      TIME  (days)
60
70
                   FIGURE  23-Percent of Bark  Sunk  for a   Graded  Sample  of  Douglas Fir Bark.

-------

                    20
30
40        50
TIME  (days)
60
70
8O
90
FIGURE  24. Percent  of  Bark Sunk for a  Graded  Sample of  Ponderosa Pine Bark.

-------
                  Table 9.  Size Distribution of Samples of Bark
                  Collected Randomly from Log Damping Areas
Particle size range
inches
0 -
1/2 -
1 -
2 -
3 -
4 +
1/2
1
2
3
4

Pondeiosa pine
% by weight
18.
12.
13.
14.
17.
24.
3
2
3
4
0
8
Douglas fir
% by weight
10.2
12.0
8.5
17.2
25.2
27.0
as  the  index  of bark present in the deposits  since  this measurement  is
a. indicator of organic  substances and is not  influenced by  chlorides.
Organic substances other than bark which are  measured by  the volatile
solids  test could include micro- and macro-organisms, debris from over-
land run-off, industrial waste sludges and others.  The presence  of
significant quantities  of these substances in the deposits  could  have
resulted in a measurement error, however, much of the error was eliminated
by  correcting all readings with volatile solids values taken from control
areas without bark deposits.

The assumption was made in this study that the difference in volatile
solids  in soil samples  taken from log dumping and storage areas and  cor-
responding values for samples from control areas without  bark  storage
represents the volatile solids added by bark  debris.  The volatile solids
content  of bark varied  considerably with the  species of wood and  the
extent  of biodegradation or decay of bark in  deposits.  Therefore volatile
solids values can be correlated to the amount of bark in  a  benthic deposit
but cannot be used as a direct measure of actual bark.  Experimental
results  are reported as grams volatile solids per cubic foot for  the soil
depth sampled.

Benthic  deposits were studied at log dumping  and storage  sites in the
Yaquina  Estuary and the Klamath River.  The sites studied on the  Yaquina
Estuary  are shown in Figure 25 and the Klamath River sites  are shown in
Figure 26.  Volatile solids data obtained at  log storage  site  D in
Yaquina  Estuary are presented in Table 10 and are plotted in Figure  27.
Descriptive maps for the other study sites in Yaquina Estuary  and Klamath
River are presented in  a M.S. thesis by Williamson  (26).

Some general  trends were noted using the core sampling data.   Bark debris
did not  accumulate in the channel of Yaquina  Estuary, probably due to  the
high flow velocity.  Most of the bark was localized in dumping and stor-
age areas and quiescent regions.  Bark debris was found uniformly distri-
buted across  the slow moving upper reaches of the Klamath River,  with  the
largest  accumulations in the dumping regions.   Furthermore, logs  are
stored on a high percentage of the river surface area.

                                 58

-------
                              Toledo
      LEGEND

Q Core  Sample Points



ft Pilinas
                                                       o Pilings
                                                                 •O  Log Booms
                                                                ff     Land/Water
                                                                  •k Sampling  Area
                                                     _ Typical  Graph

                                                          VOLATILE  SOLIDS  (Ibs/ft3)
                                                     !J   0      5       10
                                                     I
                                                             scale:  Horiz l" = 10 ibs
                                                                   Vert  I" = 20 im
"EI8

i 	
H
-
— i
EI7
	 1
                                                                             E 14
                                                         EI6
                                                          EI5

FIGURE   25 .Sampling  Areas  for Bark  Distribution   Study  at
                 Yaquina  Estuary.
                                                                             EI9
                      H E 20


-------
                                  KLAMATH
               LEGEND


          |ii* Bark  Sampling  Area
                                           Lost River
                                               Diversion  Channel
                                     scale  l"= 4000*
FIGURE   26.Sampling  Areas for  Bark  Distribution Study  at
             Klamath  Falls.
                             60

-------
Table 10.   Average Unit Weights, Percentage of Volatile Solids and Volatile Solids per Cubic Foot for



                                Core Samples from Area D (Figure 25*
Depth
(Inches)
0-2
2-4
4-6
6-8
8-10
10 - 12
12 - 14
14 -16
16 - 18
18 -20
20 - 22
Number
of samples
Extending through
Stated Depth
11
12
12
12
11
11
8
8
3
2
1
Unit
Weight
Mean Ave. Deviation
(lbs/ft3)
34.78
50.81
49.39
51.98
54.27
50.13
48.00
57.00
60.88
59.35
43.46
6.75
11.37
6.43
8.34
19.00
14.59
10.29
11.97
6.10
6.92

%
Mean
9.22
8.90
9.53
9.93
12.20
9.85
7.61
7.14
7.86
12.70
11.72
Volatile Solids
Ave. Deviation
3.28
4.59
5.42
4.49
7.51
5.12
3.26
3.92
3.03
2.70

Volatile Solids
lbs/ft3
3.21
4.52
4.70
5.16
6.62
4.94
3.65
4.07
4.79
7.54
5.09

-------
NJ
                                   0D8    OD6
                                                                                      002
                                                             0    0
                                                             Dll    D4
                                                                             ODI2
       OD7
       •o-
                                           ~
                                           OD5
OD9      DQ    o3     O01
  	y	o	o—
                                   LEGEND:

                                      See Figure as for Key
                                                                              scale
                                   \\
                              \\
                      n          vT
                                          DIO
                           D6
             D7
                                                        Dll
                                                                      D4
                                                                                         DI2
                                          D9
                                                                              DI3

D5
                                                        D3
                                                                                             Dl
                 FIGURE   27. Bark Distribution at a  Typical  Log  Storage  Area in  Yaquina Estuary.
                                                                                                       D2

-------
Table 11.   Total and Volatile Solids for Benthic Core Samples as a Function
                of Depth Below the Water-Soil Interface
Depth
(inches)


% volatile Total solids
solids (grams)



^volatile Total solids
solids (grams)

Control - 5
0
2
4
6
8
10


0
2
4
6
8
10
12
- 2
- 4
-6
- 8
- 10
- 12


- 2
- 4
-6
- 8
- 10
- 12
- 14
9.52
7.48
7.72
4.48
6.98
7.34


40.73
36.54
33.56
25.25



12.
15.
18.
25.
18.
14.

A - 3
8.
9.
15.
25.



48
57
61
54
30
77


68
37
14
12



4.
4.
3.
5.
8.



43.
29.
35.





Sample
No.
Control - 6
69
91
82
12
79



57
98
37




22.
19.
22.
24.
31.

Sample
A -4
6.
12.
14.




43
40
38
13
25

No.

07
14
20




% volatile Total solids % volatile
solids (grams) solids

A - 1
31.90 10.92 22.
20.77 18.91 24.
13.75 22.89 20.
25.07 18.12 14.
19.


A - 5
19.27 8.03 16.
25.91 16.55 24.
24.14 19.16 26.
22.
22.
24.
17.

A - 2
65
42
34
94
10


A - 6
35
46
32
37
63
65
12
Total solids
(grams)


13.13
16.18
15.66
23.42
19.87



14.51
18.68
13.94
15.90
14.22
18.28
19.21

-------
--
8   6
UJ

Q_
5



    8
ft
UJ
Q
    10
    2
    14
                                                   O  L°9 Storage Area I



                                                      Log Storage Area 2
     23            4567

                         VOLATILE   SOLIDS  ( Ibs/ff  )

FIGURE  28. Volatile  Solids of  Benthic Deposits at  Selected  Sites  in

              Yaquina   Estuary.
                               64

-------
^   6
 •
 4
UJ



I

1
a.
u
c
    10
    12
    '4
                                                             LEGEND




                                                                  Log Dump I




                                                               -f""l Log Dump 2  	





                                                               -T1 Log Dump 3




                                                               -O Log Storoge Area I





                                                               'O Log Storage Area 2





                                                               "O Log Storage Area 3





                                                                  Log Storage Area 4





                                                                  Log Storage Area 5
\
\
X
b
X
X
X
X
X
X
X
X
•















f.
^s''













X
X,
X
\
X
k
\
\
\
\
\
\
\
\
\
,''h































                         5                 10                 15


                            VOLATILE   SOLIDS   ( Ibs/ft5  )
20
  FIGURE   29. Volatile   Solids  of  Benthic  Deposits  at  Selected  Sites  in

                the  Klamath  River.


-------
To characterize  a  given segment of the benthic  zone, the  average volatile
solids were  computed.  For each small area sampled the  average percent-
age  of volatile  solids and the average dry weight were  computed for
successive  2-inch  wafers  cut  from core samples  beginning  at the soil-
water interface.   From these  data the average pounds of volatile solids
per  cubic  foot of  soil was computed.  A complete report of all core test
results  is  given by Williamson  (26).  Typical results are presented in
Table  11.   A plot  of volatile solids as a function of depth is shown in
Figures  28  and 29.  The control samples noted in Figure 28 had volatile
solids values ranging from 2  to 3 pounds per cubic foot.  These volatile
solids were probably contributed by biological  growth in  benthic deposits
and  volatile portions  (humus) of the soil.
 Figure 28 shows an average increase  of  0.1  to  2.8  pounds  of  volatile
 solids per cubic foot for samples  from  the  log storage  area  over  samples
 from the control area.   The average  of  the  increases  is approximately
 equal to two pounds of volatile  solids  per  cubic foot.  In the  log  dump-
 ing area, increases from 1.9 to  3.8  pounds  of  volatile  solids per cubic
 foot over the control samples are  shown with an average increase  of ap-
 proximately 2.5 Ib VSS/cu ft.

 Figure 29 shows an average volatile  solids  content in the log storage
 areas of approximately two pounds  per cubic foot at the Klamath River
 site.   No control samples were taken because no area  could be found which
 was not affected by log rafting.   Since the soil is of  volcanic origin,
 the background volatile solids content  from soil humus  would probably
 be  small.   A large algae bloom does  occur, however, in  the upper  Klamath
 River,  which could add  some organic  matter  to  the  benthic zone.

 The volatile solids in  the log dumping  areas at Klamath River sites
 averaged  about six pounds per cubic  foot for the first  six inches of
 depth.  This is an increase of approximately four  pounds  of volatile
 solids  per  cubic foot over the log storage areas.  At Yaquina Estuary
 an  increase in volatile solids of  only  0.5  lb/ft3  was found for the log
 dumping areas  over adjacent log  storage areas.

 The  large difference  in bark distribution between  the two study areas is
 probably due to swifter moving water at Yaquina Estuary as compared to
 the  Klamath River.   In  the  Klamath River the debris would tend  to stay
 in the  log  dumping and  storage areas after sinking, whereas at the
 Yaquina Estuary the tides  would  tend to redistribute  the  sunken debris
 over a wide  area.

The curve in Figure 29  corresponding to the log dumping area on the Klamath
River, shows a  volatile  solids content  of approximately 15 Ibs/cu ft for
samples taken from  a  depth  of  6  to 16 inches.  Visual observation revealed
that this sample was  nearly 100 percent bark.  The volatile solids  content
of bark alone would vary, however, depending upon  stage of decomposition.
                                 66

-------
—
UJ
*:
 :
a.
2
UJ
X
 LEGEND
O  RUN 4A
D  RUN 4B
                   Oxygen Uptake Rate   =
                            234
                    TIME FROM START  OF RUN  (hrs)
FIGURE    30.  Insitu  Benthic Oxygen Demand Results for Two  Respiro-
               meter Runs  at the  Same  Test  Site on  the  Little
               Deschutes  River near  Gilchrist, Oregon.


-------
Benthic Oxygen Uptake

The rate of oxygen consumption by benthic bark deposits was evaluated
at four locations in central and western Oregon.  Ponderosa pine logs
were stored at the two interior locations and Douglas fir was the pre-
dominant species stored at the coastal sites.

Oxygen uptake readings as mg/1 02 were recorded continuously during each
test run and test results were plotted as shown in Figure 30.  Using
these plots together with the volume enclosed by the respirometer and the
planar surface area covered by the respirometer, values with units rag
02/m2/day were calculated.  Following each experimental run (2 to 8 hours
duration), the respirometer was removed and core samples were taken at
the exact location of the respirometer emplacement.  The top two inches

of  the  cores were tested  for volatile  solids  content.   Experimental runs
were  conducted  in areas  containing different  amount  of  bark  in  the benthic
deposits.   Control  areas, with  little  or no  bark in  benthic deposits  were
also  tested.

Volatile  solids values and  oxygen uptake readings  were  modified by sub-
tracting  comparable values  from control samples.   The results summarized
in  Table  12 represent the averages of  several  runs at each different  lo-
cation.   The volatile solids and oxygen uptake values for the control
areas indicate  the  presence of  biodegradable organic matter  from  sources
other than  log  storage activities.  These  sources  could include dead  and
living  organisms, debris  washed from the watershed,  man-made wastes  and
others.

Figure  31  is  a  plot of oxygen uptake versus  volatile solids  content  of
benthic deposits, corrected for the contribution from control samples.
The curve  shows that as  the concentration  of volatile solids increases,
oxygen  uptake increases  up  to  approximately  2 to 2.5 g  0 /m^/day.  These
values  can  be compared with the results obtained by  Stein, et.al.  (25)
for cellulose deposits in the  vicinity of  pulp mills.   They  found uptake
values  of 3.6 g 02/m2/day,  however, they did not relate their uptake
readings  to the volatile solids content of the benthic  samples.  They
also  discovered that benthic oxygen demand is related  only to the surface
area  of the deposit and  not to the depth.  Therefore, very deep undisturbed
deposits  are  no more of  a problem from an  oxygen depletion standpoint
than  are  shallow deposits.
                                 68

-------
                                                Table 12.   In Situ Benthic Oxygen Uptake as a Function of Volatile Solids
                                                         Content in the Top Two Inch Layer of Bark Deposits
<£>
Run No. Location

Control Bend
1
2 "
3 "
Control Gilchrist
4 "
5 "
6
7 "
Control* N. Fork Coos River
8n 11
9 ii "
Control S. Fork Coos River
10 " "
11
12 "
13 " "
Species of logs

Ponderosa pine
M
II
M
Ponderosa pine
n
n
n
it
Douglas fir
M
it
Douglas fir
n
n
M
II

Average
top 2"
0.009
0.026
0.048
0.084
0.009
0.089
0.083
0.136
0.150
0.013
0.046
0.079
0.018
0.032
0.030
0.032
0.031
Volatile solids
(g/cm3)
of Increase above
control values
	
0.017
0.039
0.075
	
0.080
0.074
0.127
0.141
	
0.023
0.056
	
0.014
0.012
0.014
0.013
Oxygen
(g/m
Average
0.25
0.79
1.0
1.7
0.40
1.7
1.8
3.2
2.6
1.9
3.0
4.4
1.7
2.6
3.8
2.3
2.3
uptake
2 -day)
Increase above
control values
	
0.54
0.7
1.5
	
1.3
1.4
2.8
2.2
	
1.1
2.5
	
0.9
2.1
0.6
0.6
                        *Average of five runs

-------
        3.0
    N
     E
     ui
     *
     r
     i
     Z3
     ?
     X
     o
        2.5-
2.0-
 15 -
 1.0-
        0.5 -


D
0^




                                                                   LEGEND
STORAGE
SITE
D BEND
O OILCHRIST
O ALLEGANEY
A DELLWOOD
AVG. CONTRC
02 UPTAKE
—
0.4 g/m2
1.90
0.79
)L VALUES
VS.
	
0.009 g
0.023
0.016
                                   0.05
                                                    0.10
0.15
                              VOLATILE  SOLIDS  IN   TOP   2"   ( g/cm* )
FIGURE  31  Benthic  Oxygen  Demand  as a   Function  of  Volatile  Solids. (all  values
            corrected  for  corresponding  control   area  values)

-------
               Part III;   Comprehensive Field Studies


Introduction

During the initial phases of this research investigation, apparatus and
procedures were developed for the prediction of pollution from log storage
activities based upon the quantity of logs in water storage, length of
storage period, and the hydraulic characteristics of the body of holding
water.  All experimental results were reported with units which could be
directly extrapolated for field application.  In order to determine the
reliability and validity of the predictive information, field studies
were conducted at four log storage sites:  one in central Oregon near
Bend, on the Deschutes River; another south of Bend on the  Little Deschutes
River; and the third and fourth on the north and south forks of the Coos
River in western Oregon.  Ponderosa pine  logs were stored at the interior
sites whereas Douglas fir and hemlock logs were stored on the Coos River.
The quantity of logs in storage and approximate length of storage period
were determined through cooperation with  the appropriate mill personnel
at the various sites and by direct measurement.  Hydraulic  flow data
were determined at each site with current meters and flow,cross-section
measurements; water quality measurements  were made on samples taken up-
stream and downstream of the log storage  sites.


Log Volume-Area Relationship

All  leachate data  (with the exception of  toxicity) taken during the de-
velopmental phases of this study are reported  in the units, grams  of
pollutant  leached  per square foot of log  area  submerged.  Therefore,  for
extrapolation  of  this information to field  application,  the degree of
log  submergence had to be determined.   This  was  accomplished by taking
numerous  field measurements  of logs at  different stages  of  storage.
Depth of  submergence was measured with  a  steel  ruler  and expressed as
percentage of  diameter  submerged.   Results  of  measurements  on Douglas
fir  and ponderosa pine  logs  are presented in Table 13.   Freshly dumped
fir  logs  were  found to  be  submerged up  to 66%  of their diameter,  whereas
similar  logs  stored for more than  30 days were only 70% submerged.
Ponderosa pine logs,  held  in water  over 30 days, were found to be ap-
proximately 69%  submerged.

 Since the timber industry generally uses board feet as an  expression of
 log volume held in storage,  a relationship had to  be developed between
board feet stored and square feet of raft area.   This was  done using log
 scaling notes from the timber industry and the Scribner log rule   (5).

 Then by combining the log submergence  data with the log surface area-
 volume information,  a reasonable estimate could be made of log area
 submerged per 1,000 board feet stored.   A summary of these calculations
 is given in Table 14.
                                  71

-------
Table 13.  Percentage of Log Submergence in Water (Based on Diameter)
Parameter
Number of logs
measured
Mean (X)
Standard deviation
95% confidence limit
Douglas fir
(freshly dumped)
118
66. 0*
46.8
64.8 -67.2
Douglas fir
(stored for an
extended period)
323
70.5%
70.4
69.6 -71.4
Ponderosa pine
(stored for an
extended period)
278
69. 0%
117.2
67. 7 - 70. 3
      Table 14.   Statistical Data for Raft Volume-area Parameters
Species
Douglas fir
mean (X)
no. of observations
standard deviation
95% confidence
interval
Ponderosa pine
mean (X)
no. of observations
standard deviation
95% confidence
interval
Board ft/sq ft
of raft area
4.8
5
0.61

4. 1 - 5. 6

7.2
4
0.85

5.9-8.6
End area submerged/1000 bd ft
(ft2)
7.2
5
0.42

6. 6 - 7. 7

6. 5
4
0.48

5.7-7.3
Cylindrical area submerged
/1000 bd ft (ft2)
249.0
5
10.8

235.6 - 262.

157.1
4
67.10

50. 2 - 264.




4





0
                                  72

-------
Gilchrist Lake

The first comprehensive field study was undertaken on the Little Deschutes
River near Gilchrist in central Oregon.  Ponderosa pine logs were stored
in a small reservoir created by a dam on the river.  Logs have been stored
for many years at this site which has resulted in a benthic accumulation
of bark debris in various stages of degradation.  However, since 1969, all
logs stored at this site have been completely debarked prior to dumping,
consequently, very little bark now enters the reservoir from log handling
activities.  No attempts have been made to remove existing bark deposits.
The volume of the reservoir was determined by depth measurements to be about
8.7 million cubic feet.

Flow in the Little Deschutes River during the study period (June 19 to
29, 1970) was measured with a Pygmy current meter at a control section
in the stream.  Average flow during the sampling period was 46.5 cfs  (30
mgd) which corresponded to a theoretical hydraulic detention time of 52
hours.  A plot of measured flow during the test period is shown in Figure
32.  A Rhodamine dye tracer was added at the inlet end of the pond to
determine the actual detention time.  Results of the dye dump plotted in
Figure 33 show a peak dye concentration in the reservoir outlet of 23 hours
after injection at the inlet.  This is 0.6 of the theoretical detention
time.  Even though some short circuiting of flow was noted, it was not
judged to be critical for subsequent water quality measurements.

Grab samples were taken daily at six intermediate stations within the
reservoir.  In addition, samples were collected every four to six hours
at the inlet and outlet ends of the reservoir.  Samples were analyzed for
BOD, COD, PBI, and total organic carbon.  Results of tests on samples
taken within the reservoir indicated that the reservoir was nearly com-
pletely mixed.  The inlet and outlet sample data were used to measure the
contribution of pollutants from the stored logs.  Analytical results are
shown in Tables 15 and 16.

The predicted quantity of pollutants based upon the equation developed
during the laboratory  leaching studies  (see Appendix D) is also included
in Table 16.  An estimated 70,000 board feet of peeled ponderosa pine
logs were held in storage for a mean storage period of 30 days.  Based
upon this input information, the following values were calculated:  COD,
18  Ibs/day; BOD5, 4 Ibs/day; PBI, 40 Ibs/day; and TOC, 8  Ibs/day.  As-
suming a mean flow rate through the storage area of 46.5  cfs, the con-
centration of pollutants leached could be calculated to be BOD, 0.01 mg/1,
COD, 0.06 mg/1; PBI,  0.16 mg/1; and TOC, 0.03 mg/1.

It  is readily apparent from Table 16 that a considerably  higher quantity
of  pollutants were measured  in the  system than were predicted from lab-
oratory studies.  This can be accounted for by the extreme difficulty in
measuring BOD, COD, PBI and TOC at  low concentrations, and in obtaining
consistent values at  each sampling  point during the sampling period.
First, BOD values below 1.0 mg/1 have questionable significance.  Further-
more, the average influent BOD value was 0.25 with a standard deviation
                                 73

-------
    80


~  70
•
o
3
    60
    50
    40
    30
        period of pond sampling- average
      I2N
     6/22
I2M
 I2N
6/23
I2M
 I2N
6/24
I2M
 12 N
6/25
I2M
 FIGURE  32. Little  Deschutes River Flow  Curve  Upstream
              from  Gilchrist  Pond.
    70 -
 FIGURE  33. Results  of  Dye  Tracer Study  at Gilchrist  Pond.


-------
         Table 15.  Measured Concentration of COD. BOD, FBI and TOC at the
                   Inlet and Outlet of the Gilchrist Log Storage Site
Date
6/23/70
6/24/70




6/25/70



Mean
Std. dev.
Inlet samples
COD, mg/1 BOD, mg/1
	 _ 	 _ 	
inlet outlet inlet outlet
5.4 8.5 0.4 1.9
14.2 	 0.1 0.8
4.8 14.7
12.1 7.6 0.2 1.5
5.2 	 0.3 0.8
	
8.7 	
8.3 	
13.5 14.0
5.7 5.4
8.7 10.0 0.25 1.25
3.7 4.1 0.13 0.55
taken at 4 hour intervals
PBI,ppm SSL
(10% solids)
inlet
0.18
	
1.00
2.30
6.76
2.30

1.87
2.00

1.61
0.83

outlet
---
1.45
2.09
1.21
25.3
.._

11.23
2.37

1.78
0.54

TOC,
inlet
3
14
4
3.5
5
4
2
5
3.5
3.5
3.7
0.95

mg/1
outlet
9
--
16
12,3
25
16
4
25
12
12
4.7
1.87

Outlet samples taken 30 minutes after inlet samples


Pollution
index
BOD
COD
FBI1
TOC
Table 16. BOD, COD, PBI and TOC
from Gilchrist Log Storage
Inflow Outflow
mean mean
concentration concentration
mg/1 mg/1
0.25±0. 13 1.25±0. 55
8.7± 3.7 10. 0± 4.1
1.6± 0.83 1. 8± 0.54
3.7± 0.95 3.9± 1.87
in Inflow and
Reservoir
Measured
mg/1
1.0
1.3
0.2
0.2
Outflow

increase
lb/day2
250
325
50
50




Predicted increase
mg/1
0.02
0.07
0.16
0.03
lb/day
4
18
40
8
FBI is expressed as ppm SSL (1Q% by weight)

lb/day based on a flow of 46. 5 cfs (30 mdg)
                                        75

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of  0.13 mg/1 and the mean effluent concentration was only 1.25 rag/1 with
a standard deviation of 0.55 mg/1.  Therefore, with this spread of data,
the 1.0 mg/1 difference in BOD must be considered insignificant.  However,
when 1.0 mg/1 is multiplied by the flow of 46.5 cfs, a large daily BOD
contribution  (540 Ibs) is calculated; yet only four pounds of BOD were ex-
pected in the leachate per day.  Similar reasoning can be applied to
explain the variation in FBI, COD, and TOG results.

Perhaps a closer comparison in results could have been obtained if more
logs would have been held in storage or the flow rate would have been
reduced substantially.  Regardless of which values are used, it is im-
portant to note that the storage of peeled ponderosa pine logs in this
particular situation did not have a significant effect on the quality of
the holding water, even though a slight increase in pollutant level was
detected.
Deschutes River Storage

The second log storage area studied was on the Deschutes River near Bend,
Oregon.  Approximately 2.5 million board feet of ponderosa pine logs were
stored in the river in the area under study.  Most of the bark remained
intact on the logs.  River flow was measured to be 1,360 cfs during the
study period.

Water samples were collected immediately upstream and downstream from
the storage area at six to eight hour intervals for three days.  Samples
were analyzed for BOD, COD, FBI and TOC.  Average results from eight
samples at each site are shown in Table 17.  The predicted contribution
of pollutants is also given in Table 17.  Refer to Appendix D for com-
putation of predicted leachate values.

These results clearly show that the quantity of pollutants picked up by
log storage was not detectable within the limits of test accuracy and
sample variability.  The average BOD values for influent and effluent
samples were exactly the same.  Again, when trace concentrations are
multiplied by very large flows, a considerable number of pounds are
calculated.  Therefore, it appears more reasonable to determine the
quantity and species of logs in water storage, then predict the effect
on the holding water, rather than rely upon direct water quality measure-
ments .
Coos Bay^ Study

The final log storage sites selected were on the north and south forks
of the Coos River in western Oregon.  Douglas fir and hemlock logs with
bark intact (except for that lost during dumping and raft transport) were
held in rafts for one or more days.  The rafts were then taken by tug to
the lower bay for processing.  The log storage areas were in the upper
tidal water, very near to the free flowing streams.  Therefore, the log
                                  76

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          Table 17.  BOD, COD, FBI and TOC in Inflow and Outflow from
                 the Log Storage Area on the Deschutes River
Pollution
index
BOD
COD
FBI1
TOC
Inflow
concentration
mg/1
1.9±0. 5
6.0± 1.6
2.2± 2.17
0. li 0.15
Outflow
concentration
mg/1
1.9±0. 5
6. 5± 1.6
3.9± 0.99
1.1± 1.4
Measured
mg/1
0
0.5
1.7
1.0
increase
lb/day2
0
70
220
130
Predicted
mg/1
<0.01
<0.01
<0.01
<0.02
increase
lb/day
50
110
40
360
  FBI is expressed as ppm SSL (10% by weight)


  lb/day is based on a flow of 1360 cfs (880 mdg)
holding water moved both up-  and  downstream during each tidal cycle, with
some net movement downstream  due  to stream inflow.  This tidal fluctuation,
combined with the large volume of fresh water inflow, greatly complicated
the direct measurement of  differences in water quality upstream and down-
stream from the rafted logs.

Predicted values for  the  logs stored in the North Fork area are given in
Table 18 and those for the South  Fork are given in Table 19.  Supporting
calculations are included  in  Appendix D.

Results shown in these tables reveal that less than 1.0 mg/1 of all pol-
lution indices measured were  added to the log handling water.  Since this
quantity is too small to verify by field measurement, especially in a
situation in which the stream and tidal hydraulics are complicated, only
limited effort was made to determine the "actual" impairment to water
quality fron. the log  rafts.   The  direct measurements that were made proved
to be widely variable, and in some instances showed a decrease in pollutant
level during water passage through the log storage area.

Benthic oxygen demand determinations were made at several points in and
around the log storage areas.  Values of 1.7 to 3.8 g (H/m /day were
determined for the south  fork storage area, whereas values ranged from
1.9 to 4.4 g 02/m2/day for the north fork storage site.  A summary of
oxygen uptake values  is  given in  Table 12.  Assuming an average demand of
3.0 g 02/m2/day and  a log  storage area of 200 meters by 20 meters  (4,000
m2), the total demand for  oxygen  would be 12,000 grams or 26.5 Ibs per
day.  With a stream  flow  of 20 mgd, the resulting depletion of dissolved
oxygen from the overlying  water would be only 0.16 mg/1.  This deficit
could not be determined by conventional analytical methods used in the
field.
                                  77

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Table 18.  Predicted Increases in BOD, COD, PBI and TOC from the
          Log Storage Area on lie North Fork Coos River
Pollution
index
BOD
COD
PBI1
TOC
mg/12
0.20
0.69
0.54
0.27
Ib/day
33
112
86
43
     PBI is expressed as ppm SSL (10& by weight)
     Concentration is based on a flow of 30 cfs (19.4 mgd)
 Table 19.  Predicted Increases in BOD,  COD, PBI and TOC from the
            Log Storage Area on the South Fork Coos River
Pollution
index
BOD
COD
PBI1
TOC
mg/12
0.09
O.30
0.62
0.12
Ib/day
12
40
83
16
     PBI expressed as ppm SSL (10« by weight)
    2
     Concentration is based on a flow of 40. 3 cfs (26.0 mgd)
                               78

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                 Part IV:  Magnitude of the Problem


One of the specific aims of this research program was to survey the
magnitude of the pollution problem in the Pacific Northwest resulting from
log handling and storage.  Such a survey requires the active participation
of saw mills, pulp mills, and other industries which utilize raw timber.
Several attempts were made to organize this survey through various timber
industry associations, without success.  The industry was found to be re-
luctant to divulge information regarding log inventories, length of storage
and conditions for storage.  Perhaps as state and federal pollution con-
trol authorities press for tighter control of all pollution discharges,
information of this type will become more readily obtainable.  Some semi-
quantitive information was obtained, however, during visits to the states
in the Northwest region which have log storage problems.


Oregon

Several species of timber including Douglas fir, ponderosa pine, white
pine, hemlock and cedar are harvested in Oregon.  Nearly one-half of the
5000 manufacturing firms in the state depend upon this timber resource  (19),
Furthermore, the 400 billion board feet of raw timber produced in Oregon
ranks as the largest single state output in the nation.

Large inventories of logs are held in lakes, rivers, estuaries, and man-
made ponds.  Oregon has over 12,000 acres of log ponds and 2,000 acres of
sloughs and canals used for log storage (18).  In some areas of the state
the Department of Environmental Quality has required that all logs be
peeled before storage in a water course.  Land storage of logs, with and
without sprinkling, is also widely practiced.
Washington

Vast quantities of logs are stored in rivers, lakes, estuaries, and man-
made log ponds in the state of Washington.  Land storage of logs is also
widely practiced.  No estimate was obtainable regarding the quantity and
species of logs stored.
California

California officials in Sacramento indicate that little, if any, water
storage is permitted in the northern California timber regions.  Most all
logs are held in cold decks on land.
Alaska

There are only two major log storage sites in Alaska at the present time.
These are located near Sitka and Ketchikan.  Logs are primarily held in
                                  79

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saline water bays and estuaries.  The logs are strapped into bundles,
then the bundles are rafted for transport and storage.  No attempt was
made in this investigation to study the effect of bundling on the loss
of bark, however, this procedure should reduce bark losses.  Furthermore,
it is likely the rate of leaching and benthic oxygen uptake rate would
be reduced in the very cold Alaskan waters.
                                 80

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                             DISCUSSION
Storage of vast quantities of logs is extremely important to the timber
industry in the Pacific Northwest due to the prevailing regional weather
pattern.  Timber cutting and overland hauling activities are essentially
limited to the dry summer and fall months.  Heavy winter and spring rains
and snows restrict field activities.  Yet, production at saw mills, pulp
mills, and other forest products industries must continue throughout the
entire year.

Logs can be stored on  land or floated in rafts in rivers, lakes, or man-
made ponds.  Logs which are not kept moist soon dry out at the ends and
cracks develop.  This  phenomenon! referred to as "checking" enhances insect
attack and results in  extensive wastage of the resource.  Logs stored
upon dry land can be sprinkled to retard checking.

The presence of logs in water can cause several problems.  Log rafts fre-
quently cover large areas of streams, lakes and estuaries which have other
benefical uses such as boating, fishing, crabbing, etc.  Some logs become
water soaked, escape from the raft and float partially  submerged in the
water course creating  a hazard to boaters.  Other logs  sink and accumulate
on the bottom of the water course.  There is also some  objection to the
presence of rafted logs for aesthetic reasons.  Two other problems are
associated with log storage which perhaps are not so obvious but are of
concern i.e., the quantity and effect of substances which leach  (or dis-
solve) out of the logs and the bark which is dislodged  from the logs.
These latter two problems were dealt with in detail in  this research
investigation.

Leachates from logs in water storage contained mostly organic substances
which exert both a chemical and biochemical oxygen demand  (COD and BOD).
This organic chemical  composition was also shown by the fact that  60 to
80 percent of the solids  leached were volatile.  The tannins and lignin-
like substances added  a brownish color to the  leachates and were quantita-
ted by  the Pearl Benson  Index  (PBI).  Even though these substances are
not known to be injurious to aquatic organisms or humans, the added color
is often aesthetically undesirable.

Laboratory results with  20-inch  long  log  sections of ponderosa pine and
Douglas fir  logs showed  that when  logs  are held  in  stagnant, non-flowing
systems, leachates emerge at a relatively  constant  rate for up to  80 days.
However, when water  is passed by  the  logs  in  a flow-through  system the
initial  leaching rate  is  substantially  higher  but declines  after 20 to
30 days.  No  studies were attempted  at  the high  flow rates  experienced  in
some natural  streams  and estuaries.   Apparently,  a  concentration gradient
builds  up  around the  logs in  a  static  system  which  retards  the rate of
leaching.   This  gradient would not  likely  exist  in  free flowing  systems.

The  leaching  rates  determined  in  this  study  are  absolute  rates,  and as
such would tend  to  be  conservative.   In actual field  situations  where
                                  81

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microbial  biodegradation  of  leached  substances would  take place, the
measured amount  of  BOD, COD, solids,  etc., would  generally be  less than
predicted.   This was found to be the  case with log pond waters.  Log pond
waters  tested  generally had much lower  BOD to COD ratios than  would have
been  predicted from the leachate studies in which biological activity was
arrested with  chemical poison.  This  low ratio resulted since  only bio-
degradable  substances are measured by the BOD test whereas both biodegrad-
able  and non-biodegradable organic substances are measured in  the COD test.

The technique  developed during this  investigation for poisoning samples
then  depoisoning at a later time for  biological analyses such  as BOD and
acute toxicity could be applied to many other types of experiments and
for routine  sample  preservation  (21).

Experimental data shows that more color-producing and soluble  organic
substances were  leached from ponderosa  pine logs  than from comparable
Douglas fir  logs.   This observation  is  consistent with the findings re-
ported by Kurth, et.al. (17).  They  found that the leachates extracted
from  pine bark contain nearly ten times more soluble  sugar than the ex-
tracts from  Douglas fir.

As expected, log sections with bark  intact imparted much more  color to
the water than pine with  the bark removed.  Bark  is known to contain many
water soluble  extraneous  components,  including tannins and lignin-like
substances which can produce color.   The exposed  cut  ends of the logs
tend  to expedite the release of color and soluble organics.  A comparison
of data shown  in Figure 12 for unaltered test logs with those  for logs with
ends  sealed  clearly illustrate this  fact.  This observation was not un-
expected since the physiological flow pattern of  water and nutrients is
longitudinally through a  living tree.

Leaching rate  does not appear to be  affected by saline water as shown by
COD results  in Figure 17a.  A significantly smaller value for FBI did
result in saline water, however.  This  may be explained by the precip-
itation of lignin-like substances which have a net positive surface charge,
through the  formation of  a complex with chloride  ions present in high
concentrations in the saline water.  Andrews (2)  observed this phenomenon!
during his study of the fate of color in kraft waste  when discharged in-
to sea water.

Log leachates  were found  to be relatively non-toxic to salmon  and trout
fry during exposure periods of up to  four days.   Similar observations
have been reported by Servizi (22) for  leachate from  bark using adult
sockeye salmon as the test fish.

Only trace amounts of nitrogen and phosphous were found in the log leach-
ates.   This is understandable since ponderosa pine and Douglas fir con-
tain very small amounts of these nutrients.

Results from brief laboratory and field studies on runoff from sprinkled
cold decks showed that this water leaches soluble organics from the logs
                                 82

-------
as it trickles across the log surfaces.  Consequently, cold deck runoff
will probably require some form of treatment prior to discharge into a
receiving body of water.  An alternate solution would be to form a closed
recycle loop and avoid discharging the polluted water.

Loss of bark from logs during storage is related to the species of timber
and the method of log handling.  Ponderosa pine bark tends to adhere more
tightly to the wood surface than does Douglas fir bark.  Consequently,
fir logs would be expected to lose more bark than pine under similar han-
dling conditions.  This hypothesis was verified by direct field measure-
ment.  Approximately 22% of the bark was lost from Douglas fir logs during
unloading and transport compared to only 6% for ponderosa pine.  Similarly,
Douglas fir logs lost 18% of their bark during felling operations and
truck loading compared to less than 6% for ponderosa pine.

The rate at which barks sinks when placed in water is a function of bark
density,, water absorption rate and particle sizes.  Laboratory studies on
ponderosa pine bark revealed that all particles less than 1/2-inch in
mean diameter sank within 20 days whereas only 3%  (by weight) of the bark
pieces 4 inches or larger sank during this period.  Generally, a large
fraction of dislodged pine bark is in the small size classification which
would result in a high overall rate of sinking.  Sinking studies on bark
samples collected at random near log dumps verified that overall, on a
dry weight basis, pine bark tends to sink at a faster rate than Douglas
fir bark.

Sunken bark accumulates on the bottom of holding water systems to form
benthic deposits.  Bark deposits were found to range in thickness from
several feet at log dumping sites to less than an inch in adjacent log
storage sites.  Since some bark floats for a period of time, it can be
carried considerable distances with prevailing currents before sinking.
Consequently, bark can be found in benthic deposits at locations far
removed from the dumping and storage areas.  Volatile solids measurements
on core samples revealed an average increase of 2 to 2.5 pounds of
volatile solids per cubic foot in log storage areas compared to samples
from control areas  (without log handling).

The presence of bark in the benthic deposits could result in several
problems.  Bark is a form of biodegradable organic matter which when
undergoing biodegradation results in the consumption of dissolved oxygen
from overlying waters.  Fortunately, the rate of bark decomposition is
very slow due to its complex chemical composition and to the low water
temperatures at many storage sites.  This low rate was shown by in situ
benthic respirometric measurements in log storage and control areas.
The maximum oxygen uptake values found ranged from 2 to 2.5 g 02/m2/day
greater than control values and the rate appeared to be independent of
depth of deposit.   It is apparent from these results that benthic oxygen
demand will only become a significant problem in situations where an
extensive area of a water body is covered with bark and/or the hydraulic
flow is very small.  Such conditions could be found in lakes, sloughs,
and man-made ponds.  Davison and Hanes  (4) have also found that oxygen
uptake rate is independent of depth for compacted sludge deposits.
                                  83

-------
Since the quantity of substances leaching from logs in water storage is,
in general, minute when diluted with the large hydraulic flows found in
many water courses used for storage, it is virtually impossible to detect
an increase in pollutant level due to the logs.   The recommended procedure
for evaluating the impact of log storage on water quality is to apply the
predictive equations developed in this study.   Several unsuccessful attempts
were made in the field to directly measure an increase in pollutatnt load
resulting from water storage of logs.  This is not to infer that log stor-
age does not add pollutants to the holding water, but only that the input
from leaching is generally small.  Dislodged bark is another matter.
Methods for controlling bark losses must be developed and implemented,
such as improved methods of depositing logs into the holding water.  De-
barking of logs prior to water storage has been successfully used at
several locations in Oregon and could possibly be applied in other sit-
uations.  Banding logs in bundles may be another effective method for
reducing bark losses.

Based upon the information generated in this three-year investigation, it
appears that the widely practiced water storage of logs does not have a
severe impact on water quality in the Pacific Northwest.  Improved methods
of handling logs during dumping, rafting and transport could significantly
reduce bark losses and thereby prevent the build up of benthic deposits.
Research is currently being conducted by this investigator to evaluate
the effects of bark deposits on aquatic organisms.
                                 84

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                         ACKNOWLEDGEMENTS
     The invaluable assistance of Mr. Kenneth J. Williamson and Mr.  John
Cristello throughout the entire study is gratefully acknowledged.

     The cooperation of many timber companies in the Pacific Northwest
for allowing on-site studies and providing logs is sincerely appreciated.

     The support and suggestions offered by Dr. Kirk Willard, EPA project
officer is acknowledged.  Also, the financial support of EPA, which
made this study possible, is acknowledged.

     The bioassay work performed by the Oregon  State University Department
of Fisheries and Wildlife is appreciated.

     The principal project  investigator was Frank U. Schaumburg, Associate
Professor of Civil Engineering, Oregon State University, Corvallis, Oregon
97331.
                                 85

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                            BIBLIOGRAPHY


1.  American Public Health Association.  Standard methods for the ex-
        amination of water and wastewater.  12th ed. New York, 1965.

2.  Andrews, B.N./A study of the coagulation of kraft effluent by sea
        water." M.S. Thesis, Oregon State University, 1968.

3.  Atkinson, S.R., ''"BOD  and toxicity  of log leachates/ M.S. Thesis,
        Oregon State University, 1971.

4.  Davison, B.I. and N.B. Hanes, " Effect of sludge depth on oxygen uptake
        of a benthal system/Water and sewage works, August 1969.

5.  Dilworth, J.R.,  Log  scaling and timber cruising.  OSU Book Stores,
        Inc., Corvallis,  Oregon, 1966.

6.  Farmer, R.H.,  Chemistry  in the utilization of  wood.  Pergamon
        Press,  1967.

7.'  Felicetta, V.F.  and J.L. McCarthy, "The Pearl-Benson , or nitroso,
        method  for the  estimation  of  spent  sulfite  liquor  concentration
        in water." Tappi 48:337-347.   1963.

8.  Ellwood, E.L.  and  B.A.  Ecklund/"  Bacterial  attack  of pine  logs  in
        pond storage."  Forest  Products Journal  9_: 283-292.  1959.

9.  Graham, J.L.  and F.D. Schaumburg.t Pollutants leached  from selected
         species of wood in log storage waters ''  Presented  at  the  24th
         Purdue  Industrial Wastes  Conference,  Purdue University,  Lafayette,
         Indiana,  May 6, 1969.

10.   Graham,  J.L., " Pollutants leached from selected species  of wood in
         log storage  waters/ M.S.  Thesis, Oregon State  University, 1970.

11.   Henriksen,  A.  and J.E. Sandal, ^Centralized log barking and water
         pollution/''  Vattenhygien 2:55-60.   1966.

12.   Hodge, J.E. and B.T. Hofreiter, '"'Determination of reducing sugars
         and carbohydrates."  Methods in Carbohydrate Chemistry.

13.   Jeris, J.S./'A rapid COD test."   Water_aidjfastw^n£^ering.
         4:89-91.  May, 1967.

14.   Kurth, E.F., '"Chemicals from Douglas fir bark? Tappi, 36_: 119A-122A
         1953.

15.   Kurth, E.F., H.J.  Kiefer and J.K.  Hubbard/ Utilization of Douglas
         fir barkf  The Timberman  49:8.  1948.
                                  87

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16.   Kurth,  E.F.  and J.K.  Hubbard, ''Extractives from ponderosa pine bark.
         Industrial and Engineering  Chemistry 43:896.  1951.

17.   Kurth,  E.F., J.K.  Hubbard and J.D.  Humphrey, "Chemical composition
         of  ponderosa and sugar pine barks f  Paper presented at the Third
         Annual National Meeting of  the  Forest Products Research Society,
         Grand Rapids,  Michigan, May 3,  1949.

18.   McHugh, R.A., L.S. Miller and I.E.  Olsen, //rThe ecology and naturalistic
         control of log pond mosquitoes  in the Pacific Northwest.7 Portland,
         Oregon State Board of Health, 1964.

19.   Oregon.  Dept. of Commerce.  The economy and outlook, Salem, 1968.

20.   Sawyer, Clair N. and Perry L. McCarty,  Chemistry for sanitary
         engineers.  New York, McGraw-Hill Book Company, 1967.

21.   Schaumburg, F.D.,"A new concept in sample preservation - poisoning
         and depoisoning," Journal Water Pollution Control Fedej-j-tion.,
         (In press).

22.  Servisi, J.A., D.W. Martens and R.W. Gordon, " Effects of decaying
         bark on incubating salmon eggs/'' Progress Report No. 24 for
         International  Pacific  Salmon Fisheries Commission, 1970.

23.  Somogyi, M., "*A new reagent for the determination of sugars/7  Journal
         of Biological  Chemistry. 160:61-68,   1945.

24.  Sproul, O.J.  and  C.A. Sharpe,  Water quality degradation by wood
         bark pollutants/" Water Resources Center, University of Maine,
         Orono, Maine,  1968.

25.  Stein, J.E.  and J.G. Denison, "In  situ  benthal  oxygen demand of
         cellulose fibers,"' Proceedings, Third International Conference
         on Pollution  Research, Munich,  1966.

26.  Williamson,  K.J.,  "A study of the  quantity and  distribution of bark
         debris  resulting from log rafting,"  M.S. Thesis,  Oregon State
         University, 1969.

27.  Wise,  L.E., "Extraneous  components of wood,"  Forest  Products Journal
         224-227,  1959.
                                 88

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                          PUBLICATIONS
Graham, J. and F.D. Schaumburg,  "Pollutants Leached for Selected Species
     of Wood in Log Storage Waters, Proceedings, 24th Purdue Industrial
     Wastes Conference, May 1969.

Schaumburg, F.D.,  "Log Pollution," Northwest Magazine  (Oregonian Newspaper),
     September 7, 1969.

Williamson, K.J. and F.D.  Schaumburg,  "Bark Debris from Log Unloading
     Operation," Pulp  and  Paper  (In Press).

Schaumburg, F.D.,  "Influence  of Log Handling on Water  Quality, Water
     Resources Research  Institute  (OSU)  Bulletin, January  1970.

Hoffbuhr, J., G. Blanton and F.D.  Schaumburg,   "The Character  and Treatability
     of Log Pond Waters."  Water and Sewage Works_, July 1971.
                              Theses
Williamson,  K.J.,   "A Study of the  Quantity and  Distribution  of  Bark  Debris
      Resulting  from Log  Storage,  OSU  M.S.  Thesis,  June  1970.

Atkinson,  S.R.,"BOD and  Toxicity  of Log Leachates,"   OSU M.S.  Thesis
      June  1971.

Blanton, G.I.,   "The Characterization and  Physical-Chemical Treatability
      of'Log Pond Waters," OSU M.S.  Thesis  June 1970.

Hoffbuhr,  J.W.,  "The Character and Biological Treatability  of Log Pond
      Waters," OSU M.S. Thesis June  1970.

Graham, J.L.,  "Pollutants Leached  from Selected Species of  Wood in Log
      Storage Waters," OSU M.S. Thesis, June 1970.


                  Conference Paper and Presentations

 Schaumburg, F.D. and S.R. Atkinson,"BOD5 and Toxicity Associated with
      Log Leachates," Western Division American Fisheries Society Meeting,
      August 1970.

 Williamson  K J  and F.D.  Schaumburg,   "The Quanity and Distribution of
      Bark Debris Resulting  from  Water Storage of  Logs,"  PNW-WPCF Meeting,
      October,  1969.
                                  89

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                             APPENDIX A

                 DEVELOPMENT OF MASKING PROCEDURES
Soluble leachates from logs immersed in water emerge from both the cross-
cut ends and the cylindrical surface of the logs.  Evaluation of the rel-
ative contribution from each of these types of surface was accomplished
by masking the cross-cut ends of some of the log section to prevent
leaching through the ends.  The procedures followed in the selection of
an appropriate masking substance and subsequent application of the sub-
stance are described below.  Four commercially available products were
tested as sealants or masking agents.  These included: (1) Teflon spray
supplied by Connecticut Hard Rubber Co., New Haven, Connecticut;  (2)
Epoxy sealer supplied by Travaco Laboratories Inc., Chelsea, Mass.;  (3)
Paraffin wax. supplied by Union Oil Co. of California; and (4) silicone
lubricant supplied by Dow Corning Corp., Midland, Michigan.  The effective-
ness of each product was evaluated by total carbon determinations of log
holding water.  Other important factors considered were: ease of appli-
cation, durability, sealing quality and product cost.  The first exper-
iment involved a determination of the contribution of carbonaceous sub-
stances to the holding water by each sealant.  Plexiglas blocks, 1/8"
thick and 0.4 ft^ were used as the base material for the sealants, since
no measurable quantities of organics leach from plexiglas.  Each sealant
was applied to individual pieces of plexiglas and allowed to harden.
Two blocks of epoxy sealer were prepared, one air-dried, the other oven-
dried for 3 hours at 103°C.  All blocks were then immersed in 1000 ml
beakers containing 850 ml of distilled water.

Two rag/1 of mercury  (as Hg++) was added to the water in  the form  of a
solution of mercuric chloride  (HgCl2), to prevent any  interference from
biological growth.  The water temperature was held at  20°C ^0.5  through-
out the experiment.  Samples were taken from each beaker and tested for
total carbon content.

The total carbon data given in Table 20 for the  plexiglas blocks  showed
that the silicone grease  contributed the  least carbonaceous material.
The other sealants,  listed  in order  of increasing total  carbon  contri-
bution, were paraffin, Teflon spray, oven-dried  epoxy  sealer and  air-
dried epoxy sealer.

The second experiment was designed  to determine  the  sealing quality of
each product.   Several uniform cubical blocks were cut  from the same
Douglas fir log.  The total  surface  area  of each block  was  approximately
0.73 square feet.  Each  of  the four  sealants was applied to a separate
block so that  the  surface was completely  covered.  Each block was  com-
pletely immersed  in  1500 ml  of water poisoned with 2 mg/1  Hg+ +  and  held
submerged by  a clamp.   An unsealed  control block was also  prepared  and
handled in the  same  manner.  The  temperature was held  at 20°C +_ 0.5
throughout the  experiment.   Samples  taken from each  beaker were analyzed
for  total carbon  content.
                                91

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         Table 20.   Total Organic Carbon (TOC) in Leachate from Plexiglas Blocks
                and Wood Blocks Coated with Different Masking Substances.
                                   Plexiglas Blocks
Time
(houre)
0
24
96
154
A
0
30.3
6.9
5.9
B

70.5
109.
95.0
C

25.4

27.4
D

39.2
7.9
8.8
E

25.4
38.2
18.6
F

23.5
36.2
45.0

Time
(hours)
0
31
72
120


Wood
Mg TOC/ft2
A
0
171
243
280
B

34.
38.
29.


3
0
8
Blocks
of
C

16.
16.
15.
surface area


4
2
1


37
61
62
D

.3
.5
.8
submerged





A  - Uncoated control
B - Epoxy sealer - air dried
C  - Paraffin
D  - Silicone  grease
E - Teflon
F - Epoxy sealer - air dried
                                          92

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Total carbon data for the wood blocks showed that the greatest total car-
bon contribution was from the block sealed with silicone grease, and the
least contribution was from the paraffin-coated block.  The total carbon
value of the epoxy sealed (air-dried) block after five days immersion was
approximately 30 mg/ft^ or about twice that of the paraffin covered block
for which the TOG value was about 15 mg/ft^.

Teflon spray was eliminated from practical, full scale application because
it was non-viscous and failed to seal the cracks in the wood block.

The total carbon contribution of the epoxy sealer compared favorably with
the other products only after pre-drying in an oven.  Since this method
of drying was not practical for the large log sections and because of the
possible detrimental effect it could have on the leaching characteristics
of the logs, the epoxy sealer was eliminated from consideration.

The total carbon data for the wood block indicated that the silicone
grease did not seal effectively.  A possible explanation for this is that
the silicone grease remained in a highly viscous state and therefore was
easily displaced when the sample was handled.  This problem could prob-
ably have been reduced by covering the sealed area with a plexiglas sheet,
but this was not a practical solution considering the time and  materials
involved.

Paraffin was chosen as the most desirable sealer because it satisfactorily
met the requirements of low carbon contribution to the surrounding water,
excellent sealing quality, ease of application and relatively  low cost.
Paraffin sealant was applied by dipping the end of each log in  liquid
paraffin and allowing it to solidify onto the appropriate wood  surface.
A double boiler arrangement was used to melt the paraffin and  to keep it
at a constant temperature of 60°C during application.  While the paraffin
was cooling on the  log, any bubble present was rubbed away by  hand.  This
process  was repeated until a coating of paraffin approximately 1/4-inch
thick was secured on the  log end.
                                    93

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                             APPENDIX B

            LEACHATE PRESERVATION WITH THE MERCURIC ION
Many substances which leach from logs during water storage are biodegrad-
able.  Since non-sterile systems were used in these studies, bacteria
and other microorganisms were very likely present in the holding water,
in the test tanks and on the log sections.  Consequently, organic sub-
stances which leached into the log holding water were subject to bio-
degradation before qualitative and quantitative measurements could be
made.  The rate of leaching measured would have been the net result of
addition of leachate minus losses due to biodegradation.

Several methods were considered for the preservation of organic substances
during leaching tests which lasted from 4 to 40 days, including alteration
of pH, heat sterilization, organic toxicants, and heavy metal toxicants.
Only the heavy metal toxicants appeared feasible since the other methods
would have affected rate of leaching or the character of leached substances.

Since biological tests such as BOD and toxicity by bioassay, were to be
performed on the leachate some procedure was required for complete removal
of the toxic agent added during the log storage period.  For other chemical
tests such as COD, solids, PBI, etc., removal of the toxic agent was not
required since there was no interference with the analytical procedures.

Schaumburg  (21) describes a sample preservation technique in which the
mercuric ion can be added to water samples as a chemical preservative
then removed by chelation prior to biological analyses such as BOD or a-
cute bioassay.  This sample preservation method was used in this study
to prevent biodegradation of organic substances which leached from logs
floating in water.  The mercuric ion was added to test tanks filled with
tap water and holding submerged log sections.  Following a storage period
of seven days, samples of the holding water were withdrawn and the mercuric
ion was removed by selective chelation.  Samples were then analyzed for
BOD and acute toxicity.

In order to verify the effectiveness of the chelating agent in removing
mercury from aqueous solution a bioassay experiment was performed using
Chinook salmon fry as test fish.  Twenty liters of the Oak Creek water
used for rearing test fish was allowed to stand quiescent for seven days
after which time, the mercury was removed by chelation.  Three grams per
liter of chelex  100  (50 mesh) size was mixed with the poisoned water  for
30 minutes.  The resin was then allowed to settle out during a 60 minute
holding period.  Supernatant water was tested for acute toxicity by the
standard bioassay procedure  (1).  Results showed that all ten test fish
died in a control sample  containing 2 mg/1 Hg++ and not chelated.  One
fish died in an unpoisoned Oak Creek water control and none of the test
fish died during a  96-hour exposure period in the poisoned  sample which
had been treated with a  chelating agent.
                                   95

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This preservative technique was applied in all subsequent experiments in
which log leachate was preserved during a seven day holding period then
tested for acute toxicity following chelation.

A detailed account of the developmental work leading to the application
of this poisoning-depoisoning procedure for bioassay is given by Atkinson
(3).
                                  96

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                              APPENDIX C
        QUANTITY OF BARK DISLODGED DURING LOG  HANDLING
                  Douglas Fir Logs on Trucks (Yaquina Estuary)
Slide no.
Total area
Area of bark dislodged
Percent dislodged
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
31
32
33
34
35
36
37
38
TOTAL


180. 29
121. 99
152. 71
194. 79
287.40
215. 57
234. 12
108. 35
218. 70
201. 13
189. 78
259. 13
259. 76
213.69
206. 19
178. 71
274. 43
249. 05
221.17
258.27
264. 56
218.19
227. 58
255. 42
207. 72
176. 26
188.14
194. 82
199.06
173. 70
204. 23
124.40
209. 02
207. 27
185.44
166.48
112.23
124. 17
7663. 92


31.00
29.37
10.19
13.82
43.32
21.13
30.39
57.68
39.63
21.57
17.57
29.91
20.42
15.73
29.88
6.76
41.25
41.28
69.99
37.75
74.90
41.00
26.48
47.71
47.55
36.85
4.04
13.73
24.30
63.52
94.74
34.39
9.35
8.83
33.83
26.04
23.05
37.10
1306.05
Average
Deviation
17.19
24.08
6.67
7.09
15.07
9.80
12.98
43.23
18.12
10.72
9.26
11.54
7.86
7.36
14.49
3.78
15.03
16.57
31.65
14.62
28.31
18.79
11.64
18.68
22.89
20.91
2.16
7.05
12.21
36.57
46.39
67.84
4.47
4.26
18.24
15.64
20.54
29.88
18.25

9.60
                                     97

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                  Douglas Fir Logs After Dumping (Yaquina Estuary)
Slide no.
Total area
Area of bark dislodged
Percentage dislodged
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
TOTAL



Slide no.
1
2
3
4
5
6
7
8
9
10
11
282. 65
248.55
250.36
237.46
205. 53
265. 18
269.27
272.05
278. 20
215.30
223. 68
254.83
266.64
292.42
257. 57
257. 72
213.25
217. 42
198.07
214. 68
4920. 83


Douglas Fir Logs
Total area
307. 34
276.44
252.26
225. 87
228.21
200.41
161. 73
241.92
243.60
240.70
176. 31
118. 59
74.29
65.42
95.19
53.18
113.61
77.75
93.66
111.33
67.02
54.56
117. 45
73.70
133.04
77.16
86.03
86.52
84.56
70.68
81.33
1735.07
Average
Deviation
After Raft Transport (Yaquina Estuary)
Area of bark dislodged
121.78
76.55
56.47
95.11
54.21
79.57
115.81
115.64
111.52
108.40
59.72
41.96
29.89
26.13
40.09
25.87
42.84
28.87
34.43
40.02
31.13
24.39
46.09
27.64
45.50
29.96
33.38
40.57
38.89
35.68
37.88
35.06

5.89

Percentage dislodged
39.74
27.69
22.39
42.11
23.75
39.70
71.61
47.80
45.78
45.06
33.87
TOTAL
 2554.79
                                             994. 78
                                                          Average
                                                          Deviation
                                   39.95

                                    9.57
                                       98

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               Ponderosa Pine Logs on Trucks and Trains (Klamath River)
Slide no.
Total area
Area of bark dislodged
Percent dislodged
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
31
32
33
34
35
36
TOTAL


150.54
124. 55
118.71
138.30
143. 78
172.82
172.62
144.90
134.84
170. 78
170. 36
160. 11
145.50
145. 92
130.14
119. 58
160. 86
171.75
163.30
128. 85
167.03
139.44
128.54
179.27
181.32
107. 84
138. 10
126. 60
148. 21
149. 57
176. 42
137.16
140.31
128.32
140.47
155. 31
5334.02


2.73
2.86
3.82
4.76
5,12
12.22
6.85
8.19
8.59
26.22
39.60
8.50
5.61
5.24
5.09
4.97
4.92
9.72
6.02
8.77
4.77
7.13
6.30
7.97
3.75
14.77
4.00
5.24
6.75
6.60
7.70
12.34
8.86
6.00
9.55
14.99
306. 52


1.81
2.30
3.22
3.44
3.56
7.07
3.97
5.65
6.37
15.65
20.59
5.31
3.85
3.59
3.91
4.16
3.06
5.66
3.87
6.81
2.86
5.11
4.90
4.45
2.07
13.70
2.90
4.14
4.55
4.41
4.36
9.00
6.32
4.68
6.80
9.65
5.66
Average
Deviation 3.49
                                          99

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        Ponderosa Pine Logs After Unloading and Raft Transport (Klamath River)
Slide no
Total area
Area of bark dislodged
Percent dislodged
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
TOTAL


270. 08
247. 61
282.44
318. 53
271.49
266. 25
244.49
142. 08
252. 77
284. 37
301.59
223. 34
250,71
277.70
243. 82
290.28
4167. 80


15.01
74.82
22.19
47.04
39.17
26.52
22.61
11.01
57.64
36.53
7.94
21.90
43.90
17.79
18.16
33.11
495. 34


5.56
30.22
7.86
14,77
14.43
9.96
9.25
7.75
22.80
12.85
2.63
9.81
17.51
6.41
7.45
11.41
11.92
Average
Deviation 5. 14
                                        100

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                             APPENDIX D

        METHOD FOR EXTRAPOLATION OF LABORATORY TEST DATA FOR
             FIELD APPLICATION WITH EXAMPLE CALCULATION
Several types of surface conditions are found for logs in water storage
which tend to influence the rate at which soluble substances leach from
the logs.  Some of the original bark is dislodged and lost from logs
during dumping and transport activities.  The percentage of bark missing
depends upon the species of log and the abrasiveness of handling.  The
presence or absence of bark affects the character and quantity of leachate.
There is also a difference in leaching rate between the exposed ends and
cylindrical surface of the logs.

All of these conditions were examined in controlled laboratory experiments
reported in the EXPERIMENTAL FINDINGS section of this report.  The fol-
lowing equation was generated from observed laboratory data for application
in field situations:

               T= [(l-x)(D)(Ac)] +  [(x)(C)Ac)] + [(f1)(B-D)(AE)]


      T  =  total pollutant contribution from field logs  (grams)

      B  =  grams leached from test  log  (ends unaltered, w/bark)
                          2
                        ft  of cylindrical area          (from Figures  13-16)

      C  =  grams leached from test  log  (ends sealed, w/o bark)
                        ft  of cylindrical area          (from Figures  13-16)

      D  =  grams leached from test  log  (ends sealed, w/bark)
                          __
                        ft  of cylindrical area          (from Figures  13-16)
                                                      O
      Ap =  total submerged end area of  field logs  (ft^)
       c
      A  =  total submerged cylindrical  area of field logs

      x  =  fraction  of bark missing from  field logs

      f  =  cylindrical area of test log
                 end  area of test  log

         =  2.66 for  Douglas fir  test  logs

         =  2.71 for  ponderosa pine  test logs

The following  calculations  demonstrate  the application  of the  leachate
equation at four  log  storage sites  in  Oregon.
                                 101

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Gilchrist Reservoir Site
Storage Conditions --
                                       2
      1.  area of log rafts - 70,000 ft  (based on actual field measure-
          ment)
      2.  species - ponderosa pine
      3.  all logs peeled before storage
      4.  average length of storage - 30 days
Calculations --
      1.  board feet = (70,000 ft ) (7'2 boar^ ft ) = 5.04 x 105 board  ft
                       v            ^ square ft
          See Table 14 for conversion factor
      2.  AE - (504 M bd ft) (y') = 3.28 x 103 ft2 of end area  submerged
          See Table 14 for conversion factor
      3.  AC = (504 m bd ft) (^53^-) = 8-06 x 1C)4 f*2 of cylindrical  area
                                                              submerged
          See Table 14 for conversion factor
      4.  Constants B,C, and D from Figures 13, 14 and 15.
Constant
B

C

D

Time
Basis
1/30 d
I/day
1/30 d
I/day
1/30 d
I/day
COD
g/ft2
6.0
0.20
2.35
0.077
3.55
0.12
TOC
g/ft2
2.2
0.073
0.8
0.027
1.4
0.046
FBI
g/ft2
17.0
0.57
4.0
0.13
12.0
0.40
      5.  "fj" factor - 2.71
      6.  "x" factor - 1.0  (all logs completely peeled)
      7.  Solving the leachate equation:
                                 102

-------
          TCOD  =  [tt-l)(0.12)(8.06 x 106)] + [(1.0)(0.077)(3.06 x


                    + [(2.71) (0.08)(3.28 x 103)]


                    0 + 6.2 x 103 + 0.71 x 103


                =   6.91xl03 grams COD leached per day



                    15.2 Ibs COD leached perday



          TpBI  =  [(1-1)(0.40)(8.06 x 104)] +  [(1.0)(0.13)(8.06 x 104)]



                    + [(2.71)(0.17)(3.28 x 103)]



                    0 + 10.5 x 103 + 1.5 x 103


                    12 x 103 grams FBI leached per day


                =   26.4 Ibs FBI leached per day  (equivalent SSL - 10%

                    by weight)



          TTnr  =  [(1-1) (0.046)(8.06 x 104)] + [(2.71)(0.027)(3.28  x 103)]
           1 L/C*


                    +  [(2.71)(0.027)(3.28 x 103)]


                    0 + 2.18 x 103 + 0.24 x 103


                =   2.42 x  103 grams TOG leached  per day


                    5.3 Ibs TOG  leached per day




      8.  BOD   Apply  a BOD/COD  factor of 0.19  for ponderosa pine  logs

                without bark  (refer to Table  1) to estimate BOD  added:


                    0.19 x  15.2  Ibs COD/day = 2.9 Ibs  BOD leached  per day





Deschutes River Site


Storage Conditions --


      1.  quantity of  logs  in  storage  -  2.5 x 106 board feet  (mill estimate)


      2.  species and  condition  -  ponderosa pine, unpeeled (assume 12%

          bark missing)


      3.  average length of storage  -  30  days
                                 103

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Following the calculation procedure outlined above for the Gilchrist site,
the following values are obtained:
Pollution
Index
COD
BOD
FBI
TOC
Quantity Leached
Ibs/day
109
50
356
43
Coos River North Fork Site

Storage Conditions --
                                                 2
      1,  quantity of logs in storage - 69,000 ft   (based On field
          measurements)

      2.  species and condition  - Douglas fir, 12 percent bark missing

      3.  average length of storage period  -  1 day

Following the calculation procedure outlined  above  for  the Gilchrist
site, the following vslues are obtained:
Pollution
Index
COD
BOD
PBI
TOC
Coos River South Fork Site
Quantity Leached
Ibs/day
112
33
86
48

 Storage Conditions --

       1.   quantity of  logs stored - 23,000 ft2 (based on field measure-
           ments)

       2.   species and  condition - Douglas fir, 12 percent bark missing

       3.   average length of storage period - 1 day
                                  104

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Following the calculation procedure  outlined above  for  the Gilchrist
site, the following values are obtained:
                    Pollution       Quantity Leached
                       Index	Ibs/day
                        COD                  40
                        BOD                  12
                        FBI                  83
                        TOC                  17
                                     105              OU.S. GOVERNMENT PRINTING OFFICE: 1973  514-153:198 1-3

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  .SELECTED WATER
   RESOURCES ABSTRACTS
   INPUT TRANSACTION FORM
                                             1. Report No.
  4.  Title
       The Influence of Log Handling  on Water  Quality
3. Accession No.
                                                                 w
   7.  Authoi(s)
     Schaumburg, Frank D.
   9. Organization

     Oregon State University
     Corvallis, OR  97331
. J  Sponsoring O.-ganizatioa
   P. S. EPA, Research & Monitoring
/.i- Supplementary Notes
                                                                 5. Report Date
                                                                 6.
                                                                 8. Performing Organization
                                                                   Report No.

                                                                10. Project No.
                                                                   12100 EBG
                                                                //. Contract/Grant No.
                                                                  13. Type of Report and
                                                                     Period Covered
                                                                     5-1-68 to 10-1-72
                 Environmental Protection Agency report
                 number,  EPA-R2-73-085,  February 1973.
  >. Abstract  The water storage  of  logs  is  widely practiced in the Pacific Northwest.  An
 investigation has been made to determine  the effect of this practice on water quality.

j      Soluble organic matter and some inorganics leach from logs floating in water and
(from logs held in sprinkled land  decks.   The character and quantity of leachate from
 Doublas fir, ponderosa pine and hemlock logs have been examined.  Measurements including
 BOD, COD (1.0-4.2gm/ft2 per week),  PBI, solids  and toxicity (no kill to 20% TLm 96) have
|shown that in most situations  the contribution  of soluble leachates to holding water is
jnot a significant water pollution problem.

      The most significant problem associated with water storage appears to be the loss of
 bark from logs during dumping,  raft transport and raft storage.  Bark losses from 6.2%   :
 to  21.7% were measured during  logging  and raft  transport.  Dislodged bark can float until
 it  becomes water logged and sinks,  forming  benthic deposits.  Floating bark is aesthetic-
jally displeasing and could interfere with other beneficial uses of a lake, stream or
'estuary.  Benthic deposits exert  a  small, but measurable oxygen demand and may influence
'the biology of the benthic zone.  Implementation of corrective measures by the timber
'industry to reduce bark losses could make the water storage of logs a practice      *
jwhich is compatible with a high quality environment.
|  I7a. Descriptors
jbark,  leachate, bark sinkage,  toxicity, water  pollution,  oxygen demand, log storage,
jbark deposits, benthic deposits
I  17b. Identifiers

jbark,  BOD, forest industry pollution, logging  wastes,  Pacific NW logging, leachate
characteristics.
1 7c. COWRR Field 4 Group
IS. Availability
H. Kirk Willard
Abstractor
19. Security Class. 21. No. of
(Report) Pages
20. Security Class. 22. Price
(Page)
Send To:
WATER RESOURCEb SCIENTIFIC INFORMATION CENT Ff,
U S DEPARTMENT OF THE INTERIOR
WASHINGTON, D. C Z02iO
^Institution Environmental Protection Agency
WRSIC 102 (REV JUNE 1971)
                                                                                G P 0 9 I 3. 7 « 1

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