The
Big Storm
In
the 1996 Annual Report, the water monitoring discussion focused
on seasonal and spatial patterns that emerged over the first four
years of the RMP. While these general patterns largely persisted
in 1997, the extremely unusual hydrology of early 1997 did have
a conspicuous impact on the concentrations of some contaminants.
As described by Cloern et al. (see Water-Quality
Variability in San Francisco Bay: General Patterns of Change During
1997, this Chapter), 1997 was the year of the Big Storm, with
record-setting precipitation in the watershed in December and January
(Hunrichs et al., 1998). Heavy rainfall and record streamflow in
January was then followed by unusually dry weather in February and
March and low freshwater inflow for the rest of the year. This discussion
will focus on ways in which the 1997 results were unusual in comparison
to the persistent general patterns observed in RMP water monitoring
from 1993 to 1996.
The
extreme hydrological variation in early 1997 created a sharp contrast
in conventional water quality parameters between the first two sampling
cruises of the year. During the January sampling, the surface waters
of the Bay were approximately 90% freshwater, with low salinity
waters pushing well into Central Bay. By the April cruise the surface
waters of the Bay were down to about 50% freshwater. The January
sampling therefore characterized a very different water mass than
the April sampling, with the January sampling overwhelmingly influenced
by the high flows from the Sacramento and San Joaquin rivers and
the April sampling more equally influenced by the Rivers and saline
waters within the Bay. The January flows also carried a relatively
large load of suspended solids, producing the highest baywide mean
concentration of total suspended solids (TSS) observed in the five
years of the RMP. The mean TSS in April was less than half of the
January mean.
The
Effect of the Big Storm on Contaminant Concentrations
Dissolved
concentrations of several trace elements, including chromium, lead,
mercury, nickel, and zinc, were relatively high in January. Dissolved
concentrations of chromium, mercury, and lead were especially high,
leading to the highest baywide average concentrations (including
all stations shown in figures
3.43.23) of these elements for any cruise since the beginning
of the RMP.
The
average concentration of dissolved mercury in January (0.0045 µg/L)
was four times higher than the average concentrations in April and
August (0.0011 and 0.0010 µg/L, respectively). The January
average was heavily influenced by an extremely high value (the second
highest observed in the RMP) at the Petaluma River (BD15). Dissolved
mercury was also elevated in January at the other Northern Estuary
and Rivers stations. The average concentration of dissolved chromium
in January (1.86 µg/L) was even more sharply elevated over
the April average (0.24µg/L), an eight fold difference. Concentrations
were uniformly elevated at the Northern Estuary and Rivers stations.
Ten of the eleven highest chromium concentrations recorded in the
RMP were measured in the northern reach. The highest chromium concentration
(8.79 µg/L) was measured at the Petaluma River station (BD15).
The average dissolved lead concentration in January (0.17µg/L)
was three times higher than the April average (0.05 µg/L).
In the South Bay, concentrations of dissolved mercury, chromium,
and lead were not strongly affected by the Big Storm. The high dissolved
concentrations observed during high flow conditions in the watershed
suggest mobilization and transport of large masses of more bioavailable
forms of these elements during this period.
Total
(dissolved + particulate) concentrations of some trace elements
that are transported primarily in the particulate phase were also
sharply elevated in January. The highest baywide average total concentrations
of chromium, copper, mercury, nickel, lead, and zinc since the beginning
of the RMP were measured in January. Baywide average TSS concentrations
fell from 91 mg/L in January to 38 mg/L in April, and baywide average
concentrations of these elements showed similar declines, generally
dropping to about 50% of the January concentrations. Total mercury,
for example, fell from a baywide average of 0.036 µg/L in January
to 0.014 µg/L in April. The largest drop was observed for chromium,
from 17.7 µg/L in January to 5.3 µg/L in April, a 3.3-fold
difference. As for the dissolved concentrations, the high baywide
averages in January were principally due to high concentrations
in the northern reach, and the South Bay was relatively unaffected
by the Big Storm. The dissolved and particulate forms of trace elements
mobilized during the Big Storm were likely derived from both natural
and anthropogenic sources.
High
concentrations of some organics were also observed in January. Dissolved
chlordanes and DDTs were highest in January at all Northern Estuary
stations, although the magnitude of this seasonal difference was
not as great as for dissolved mercury, chromium, and lead. The Petaluma
River (BD15) and Napa River (BD50) stations in January had the highest
concentrations of dissolved DDTs and chlordanes observed in the
northern reach. Dissolved chlordanes and DDTs did not exhibit clear
seasonal variation in the southern reach.
Diazinon
is found almost entirely in the dissolved phase in RMP samples.
Unlike chlordanes and DDTs, diazinon concentrations showed seasonal
variability in both the northern and southern portions of the Bay.
The highest concentrations for the year were observed at the Northern
Estuary and Rivers stations in January, ranging between approximately
10 and 40 ng/L. These concentrations were high relative to RMP data
from other years, but not the highest.
Total
(dissolved + particulate) chlordanes and DDTs were also elevated
in the January sampling. Total DDT concentrations at the Rivers
were the highest yet observed for these stations in the RMP. Total
DDT concentrations were also elevated in January at the Northern
Estuary stations. Total concentrations of dieldrin and chlordanes
at the Northern Estuary stations were the highest yet observed for
these stations in the RMP. The high dissolved + particulate concentrations
of DDTs, chlordanes, and dieldrin in the Northern Estuary suggest
transport of contaminated sediment particles from the Central Valley
during the high flows in January.
In
contrast to the organochlorine pesticides, dissolved + particulate
PCB concentrations at the Rivers and Northern Estuary stations were
not elevated during the Big Storm. This suggests that the sediment
particles washing into the Estuary from the Central Valley were
relatively uncontaminated with respect to PCBs. This observation
is consistent with previous observations of relatively low TSS-normalized
concentrations of PCBs at the Northern Estuary and Rivers stations
(Jarman and Davis in the 1995 Annual Report).
Overall,
due to a combination of high flows and elevated concentrations,
the mass loading of many contaminants to the Bay was greatly increased
during the Big Storm of 1997.
Comparison
to Water Quality Guidelines
This
section provides a brief overview of how 1997 data compare to relevant
water quality guidelines (Table 3.7).
Of the ten trace elements measured, concentrations of chromium,
copper, mercury, nickel, and zinc were higher than guidelines on
one or more occasions (Table 3.8).
Nickel, mercury, and chromium concentrations were most frequently
above guidelines. Several trace organics also had concentrations
above guidelines, including PCBs, DDTs, chlordanes, dieldrin, and
PAHs (Table 3.9). Congener-based
ÂPCBs were well above the congener-based 170 pg/L guideline
in most of the samples.
Effects
of Water Contamination
Clear
statistically and biologically significant toxicity was observed
in the Mysidopsis test in January 1997 at Sacramento River
(BG20) and San Joaquin River (BG30). Statistically significant toxicity
with higher percent survival was also observed at Grizzly Bay (BF20)
and Napa River (BD50). In August 1997 clear toxicity was also observed
in the Mysidopsis test at four South Bay stations: Redwood
Creek (BA40), Coyote Creek (BA10), Sunnyvale (C-1-3), and San Jose
(C-3-0). Percent survival was 33% at Redwood Creek (BA40), and 0%
at the other three stations.
Toxicity
tests using Mytilus larvae indicated statistically significant
toxicity in January at Grizzly Bay (BF20), Pinole Point (BD30),
Redwood Creek (BA40), and Sunnyvale (C-1-3), but percent normal
development in these samples was relatively high. The statistical
significance of these results is due to the low variability in the
control treatments and does not indicate toxicity in the samples.
In
1996 a special study was initiated to investigate episodic toxicity
following storm events, as described in detail in Ogle and Gunther
(this Chapter). In the winter of 19961997, ambient toxicity
monitoring was conducted at the mouths of Guadalupe Slough and Alviso
Slough in the South Bay and in Napa River and at Mallard Island
in the North Bay. In the winter of 19971998, more temporally-intensive
sampling was performed at Mallard Island, sampling continued at
Guadalupe Slough, and sampling at Pacheco Slough was added. Toxicity
has been detected consistently in this special study. In some instances,
ELISA analysis of diazinon and chlorpyrifos in the samples has yielded
results consistent with these organophosphates being the possible
cause of toxicity. In most samples, however, diazinon and chlorpyrifos
concentrations were below toxic levels, suggesting that other contaminants
were responsible for the observed toxicity.
References
Hunrichs,
R.A., D.A. Pratt, and R.W. Meyer. 1998. Magnitude and frequency
of the flood of January 1997 in northern and central Californiapreliminary
determinations. U.S. Geological Survey Open File Report 98-628.
Sacramento, CA.
SFBRWQCB.
1995. 1995 Basin Plan. San Francisco Bay Regional Water Quality
Control Board, Oakland, CA.
U.S.
EPA. 1997. Water Quality Standards; Establishment of Numeric Criteria
for Priority Toxic Pollutants for the State of California; Proposed
Rule. Federal Register Vol. 62, No. 150, August 5, 1997.
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