United States
Environmental Protection
Agency
Environmental
Research Laboratory
Athens, GA 30605-2720
Research and Development
EPA/600/SR-93/048  May 1993
Project  Summary
South  San  Francisco  Bay
Water  Quality  Modeling  and
Waste  Load  Allocation  Study

Pei-Fang Wang, Robert B. Ambrose, Jr., and Kevin J. Novo-Gradac
  A waste load allocation  modeling
study was conducted  in South San
Francisco  Bay, California.  Relatively
numerous  reports  on  hydrodynamics
and less complete data  for water qual-
ity,  especially sediment levels,  in the
Bay were reviewed for use in  the study.
Simulations were based  on the premise
that  sediments maintain equilibrium
over long periods of time. Copper con-
centrations were simulated  using dif-
ferent loading  conditions describing
different scenarios. Nontidal transport
results were  obtained for suspended
solids, copper, nickel,  and  lead. The
wide ranges of historical water quality
data were addressed through sensitiv-
ity  analysis  of unsteady  nonpoint
source loads. For demonstration pur-
poses, the domain for tidal simulations
covered only the  regions  south  of
Dumbarton Bridge. The effects  of the
reduction of  point-source loads over
the past few years and of the droughts
that began in 1987  were simulated us-
ing appropriate loading  conditions.
  This Project Summary was  developed
by  EPA's  Environmental  Research
Laboratory, Athens, GA, to  announce
key findings  of the research  project
that is fully documented in a separate
report of the same title (see  Project
Report ordering information  at back).

Background
  In response to a. request from the Cali-
fornia Regional Water Quality Board, San
Francisco Ekty Region, the U.S. Environ-
mental Protection Agency's Center for Ex-
posure Assessment  Modeling  conducted
a water quality study of  the  South Bay
portion of San Francisco Bay from April
1991 to  December 1992 to  support the
determination  of waste load  allocations
for copper. South Bay, which receives rela-
tively little fresh water, has near-oceanic
salinity characteristics for much of the year
and usually is well mixed. The embayment
is generally shallow with a deep channel
in the middle.
  South  Bay has very irregular geometry
and bathymetry and poses great model-
ing problems in the representation of tidal
flats. Hydrodynamics data were sufficient
for calibration of tidal and nontidal mod-
els. More solids data were needed for the
calibration of sediment transport and wa-
ter quality models. Both point and non-
point source loading data were available
for simulations predicting copper concen-
trations in South Bay. It is uncertain, how-
ever, what fraction of the nonpoint source
loads is  delivered from different source
areas in the Bay.
  Because most usable  data were not
collected concurrently, extrapolation was
required  for modeling purposes. Extrapo-
lation may cause inaccuracies in the setup
of input data and make interpretations cf
the  modeling results difficult.  While  some
of the data can be used for nontidal water
quality simulations, the information  is net
sufficient for the verification of more so-
phisticated sediment transport models.
  The speciation of  copper in the South
Bay was of interest because of increased
concentrations of the metal and its poten-
tial bioavailability. The geochemical model
MINTEQA2 was employed, using histori-
cal data, to assess the degree of impor-
tance of  competing factors on dissolved
copper levels  and to determine an  effec-
                                                  Prmted on Recycled Pap<>:

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live partition coefficient for the transport
modeling.

Results
  MINTEQA2 modeling indicated adsorp-
tion-based control of dissolved copper lev-
els,   controlled  primarily  by   iron
oxyhydroxide phases on sediments. A rela-
tively constant  partition  coefficient  of
14,000  L/kg  was  observed  for copper
throughout  South Bay.  Dissolved organic
carbon may not play an important role in
copper speciation.  Small changes in pH,
however, can cause larger  changes in the
sorptive properties of iron oxyhydroxide in
South Bay. Any  small pH  changes, such
as those related to runoff  or phytoplank-
ton blooms, could  alter the copper parti-
tioning  behavior. Better datasets were
needed  on pH,  the  binding capacity  of
dissolved organic carbon, and the readily
extractable iron in the sediments.
  Water quality in South Bay was investi-
gated under  historical  flow  and loading
conditions using WASP4 to simulate sedi-
ment and contaminant transport. A nontidal
approach was employed to elucidate the
large-scale response of the system to cop-
per,  nickel, and  lead loadings. A coarse
network of  ten water column and ten un-
derlying benthic segments  was set up be-
tween Oakland Bay Bridge and the sloughs
south of Dumbarton Bridge.
  The modeling strategy  involved  using
previously  determined  dispersion coeffi-
cients along with net  advective flows from
point  and  nonpoint sources.  Suspended
solids were simulated based on observa-
tions that sediments are in  long-term equi-
librium  in  South  Bay,  with little net
deposition or  erosion. A constant deposi-
tion velocity was specified based on an
earlier study. Resuspension velocities were
calibrated to match historical data on sus-
pended  solids in the  water column. Parti-
tion coefficients were specified based on
historical data and  geochemical consider-
ations.
  Simulations of annual  average  water
quality parameters  were conducted using
the annual mean loading  and flow data.
Results wera  compared  with  various
datasets spanning the period 1976 through
1990. Calibrated suspended solids lie, in
general, between the medians for dry and
wet weather data collected between 1969
and 1975. The field data exhibit wide varia-
tions that the steady-state simulation does
not capture.
  Simulated total copper  concentrations
lie within the ranges of field data from the
Oakland Bay  Bridge to the  area just south
of Dumbarton Bridge. Simulated results,
however,  overestimate the  Discharger's
Two-Year Study data in the southern-most
portion of the Bay. Simulated dissolved
copper tends to overpredict measured val-
ues, particularly  in the southernmost re-
gions.  Observed differences could have
been caused  by the model parameteriza-
tion for sediment transport, partitioning, or
loading.
  Similar simulations were conducted for
nickel and lead. While simulated total nickel
concentrations slightly underpredict ob-
served data,  simulated  dissolved  nickel
follows the data desirably. Simulated total
lead concentrations overpredict observed
data by a factor of about two,  whereas
simulated dissolved lead concentrations
overpredict by a large  margin. More study
is needed on lead  sorption and sediment
transport,
  A simulation was conducted using an-
nually  varying flow and  copper loading
data from 1977 through  1990 in order to
understand the  concentration response
dynamics. Observed data are available at
the  beginning and end of this period. The
model  prediction of very little change in
the  northern and middle reaches of South
Bay during this  period  is confirmed  by
data. The historic data  south of Dumbarton
Bridge  seem  to  indicate net constant  or
perhaps slightly declining copper concen-
trations. The  model simulates increasing
concentrations until 1986, and  declining
concentrations thereafter, with a small net
increase  over the period. Sensitivity stud-
ies  indicate that  more vigorous sediment
exchange or  net deposition in this  region
would cause the model to predict  a mini-
mal net increase during this period.
  Because of the prolonged drought from
1987 through 1991, the model was  set  up
to  simulate this  period using greatly re-
duced nonpoint source loads. Steady state
results were  compared  with  data taken
during  1989 through 1991.  In the  south-
ern reaches of South Bay, reduced flow
and loads resulted in  lowered concentra-
tions of sediment, copper, and nickel, and
improved modeling results as compared
with field datn.
  Field data  in the southern reaches of
South Bay exhibit large temporal variabil-
ity.  Tc  better  understand possible causes
for the high variability, a study of concen-
tration  responses to different runoff load-
ing  conditions was  conducted.
  Hypothetical 13.5-hour runoff  events
composed of  1/10 and  1/29 of the total
wet weather period flows and loads were
simulated. In some simulations, resuspen-
sion velocities during  post-storm periods
were  reduced to  75% and  50%  of the
annual means for 6 days.
  The analysis showed most sensitivity to
changes in  loading  and  sedimentation
south of  Dumbarton Bridge.  In this area,
runoff loading  produced small short-term
concentration pulses.  The predicted wet
weather dissolved copper concentration
variations were smaller than the  sus
pended solids and total copper responses
which is consistent with the field data
Regions north of Dumbarton Bridge are
not very sensitive to the runoff loadings
due  to  their very large volumes. Sus
pended solid concentrations in South Bay
are primarily a result of the resuspension
deposition processes.
  Tidal  variations south of Dumbarton
Bridge were investigated using the three
dimensional estuarine circulation model
HYDRO3D linked with WASP4.  The hy
drodynamic model network was composed
of vertically integrated  rectangular cells
measuring 200 m by 200 m. Tidal eleva
tions were specified at Dumbarton Bridge
Simulations  compared well in ranges and
trends with  data at Coyote Creek in the
extreme southern end of the  bay.
  Tidal  flows  and volumes  were linked
with  a  3-segment and a  15-segment
WASP4 model  The tidal analysis predicts
the water transport in  extreme South Bay
within several  tidal cycles. Results show
that  mass is conserved through  the link
ing process. Variations of concentrations
over a tidal cycle reach more than plus or
minus 15% of the annual mean value.
  Possible copper load reductions were
studied for South Bay based on  the cali
brated model.  To gain perspective on the
gross response of  South Bay to waste
loads, future concentrations following elimi-
nation of  various  loads  were  examined
under annually averaged conditions. Fol
lowing the  elimination of all loads,  ap-
proximately  3 years would be required to
bring total  copper concentrations in  the
southernmost segment down by  half. The
decrease of copper in interior segments
proceeds at a much slower  rate; the ei
fective half-life in this  area is as much  as
16 years.
  Next, we examined  the  response  of
South Bay to  the elimination of  various
classes of waste loads, assuming as  a
base the  calibrated  average profile for
1977-1989.  Elimination of all loads north
of Dumbarton  Bridge  has little effect on
the extreme South Bay, whereas elimina-
tion of all loads south of Dumbarton Bridge
should reduce concentrations throughout
South Bay to below 2  u,g/L. Although con-
centrations would decline considerably fol-
lowing the  elimination of all  point source
loads, nonpoint sources would continue to
cause concentrations  above  4 u,g/l_ south
of Dumbarton Bridge.
  If  drought conditions are  taken as  a
base, then the  response of South Bay to
the  elimination of loadings  changes.  In

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this case, the largest contribution is from
point  source  loads  south  of  Dumbarton
Bridge. Nonpoint source loads from south
of Dumbarton Bridge contribute much less.
If  nonpoint source  loads during drought
conditions could be maintained, the elimi-
nation of all point source loads would lead
to concentrations below 3 u.g/L throughout
South Bay.
  Finally, calculations of copper concen-
trations were  made for eight loading sce-
narios of management interest. Given the
numerous assumptions that were made in
order to compensate for lack of data, the
model results are better viewed as predic-
tions of the general type, extent, and term
of response rather  than as precise nu-
merical predictions. Following realistic load
reductions, copper concentrations are ex-
pected to decrease  at  slow  rates. The
slowly  decreasing copper concentrations
demonstrate that sediment deposition and
resuspension  constitute important pro-
cesses controlling the long term transport
of metals in the water column of  South
Bay.

Conclusions
  With the reduction of point source efflu-
ent concentrations to 2.9 u,g/L and the
reduction of nonpoint source loads by 50%,
the concentrations  of copper decrease
most rapidly. After 20 years following load
reduction, total copper concentrations de-
crease by about half, falling below the 4.9
u.g/L standard in regions north of Dumbar-
ton Bridge. Regions south of Dumbarton
Bridge are expected to maintain average
concentrations above this standard. Su-
perimposing the effects  of tidal fluctua-
tions and storm pulses, even higher con-
centration excursions are expected.
  The effects of reducing the copper loads
from the publicly owned treatment works
discharges south  of  Dumbarton  Bridge
were examined to identify conditions re-
flecting  both  average and  drought  non-
point source loads. Reducing the effluent
concentrations to  4.0 u.g/L had about the
same effect as  reducing the flows and
loadings by 30%.  During drought condi-
tions,  average  copper  concentrations
should fall below the 4.9 u.g/L  standard
except in extreme South Bay, where slight
exceedances are  expected.  During aver-
age nonpoint source years, concentrations
north of Dumbarton Bridge should still re-
main below the standard.  Exceedances
below Dumbarton Bridge, however, would
be higher and more widespread.
                                                                                      'U.S. Government Printing Office: 1993 — 750-071/6024 ?

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 The EPA author, Robert B. Ambrose, Jr. (also the EPA Project Officer, see below)
   is with the Environmental Research Laboratory, Athens, GA  30605-2720.
   Pel-Fang Wang and Kevin J. Novo-Gradac are with AScI Corporation, Athens,
   GA 30605.
 The complete report, entitled "South San Francisco Bay Water Quality Modeling and
   Waste Load Allocation Study," (Order No. PB93-166981/AS;   Cost: $27.00;
   subject to change) will be available only from:
         National Technical Information Service
         5285 Port Royal Road
         Springfield, VA 22161
         Telephone: 703-487-4650
 The EPA Project Officer can be contacted at:
         Environmental Research Laboratory
         U.S. Environmental Protection Agency
         Athens, GA 30605-2720
United States
Environmental Protection Agency
Center for Environmental Research Information
Cincinnati, OH 45268

Official Business
Penalty for Private Use $300
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         EPA
   PERMIT No. G-35
EPA/600/SR-93/048

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