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September 18, 2000
Study of San Francisco Bay contamination shows persistence of lead from gasoline
By Tim Stephens
The use of lead as a gasoline additive was phased out years ago in California, but
an enormous reservoir of lead-contaminated soils and river sediments remains in the
Central Valley and will continue to contaminate the waters of San Francisco Bay for
decades to come, according to a study by UCSC researchers.
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UCSC researchers have been monitoring water quality in San Francisco Bay for over
ten years. A recent analysis shows chronic lead contamination resulting from past
use of leaded gasoline.
Photo courtesy of UCSC's Department of Environmental Toxicology |
The findings, published in the September 12 issue of the Proceedings of the National
Academy of Sciences, are based on an analysis of lead in water samples collected
over a ten-year period in San Francisco Bay and the mouths of the Sacramento and
San Joaquin Rivers.
Although there is no evidence that lead pollution in San Francisco Bay threatens
the health of humans or marine organisms, the study has implications for the persistence
of a wide range of potentially harmful contaminants, said Russell Flegal, professor
and chair of environmental toxicology.
"We can use this as a model for other contaminants, and it shows that many contaminants
simply don't go away once you stop polluting the environment," Flegal said.
"We're seeing lead contamination from the 1960s still coming into the bay, and
our calculations indicate it will be another 50 to 100 years before all the lead
from gasoline emissions in the Central Valley is washed into the bay."
Even after lead stops entering the bay, lead-contaminated sediments are likely to
remain there indefinitely, he added. These findings contrast with those of other
researchers who have reported significant reductions of lead contamination in other
types of environments. Since the phaseout of leaded gasoline, lead concentrations
have fallen in urban air, ocean surface water, polar ice and snow, and even human
blood. But the UCSC researchers now show that contaminated rivers and estuaries can
retain pollutants like lead for a very long time.
Douglas Steding, a graduate student in Flegal's lab, is the first author of the study.
The coauthors are Flegal and Charles Dunlap, a research fellow in the Environmental
Toxicology Department and an assistant professor at the American University of Armenia.
Three factors conspire to maintain elevated levels of lead in the waters of San Francisco
Bay, Steding said. One is the large amount of lead that remains in the Central Valley
watershed, where it is associated with soils that gradually wash into the Sacramento
and San Joaquin Rivers and flow into the bay. A second factor is the large amount
of lead-contaminated sediments within the bay, which continually release lead into
the water. The third factor is the limited transport of contaminated sediments from
the bay into the open ocean.
"The bay just doesn't clean itself efficiently," Steding said. "The
only outflow is through the Golden Gate, so sediment flow out of the bay is limited."
Furthermore, that flow has been drastically reduced by diversions of water from streams
around the bay for urban, industrial, and agricultural uses. Contaminated sediments
in the southern reach of the bay seem likely to remain there indefinitely, the researchers
found.
"There is very little movement of sediments out of the South Bay," Steding
said. "It's akin to a stagnant lagoon, and only during periods of high water
flow does it get any substantial flushing."
Steding was able to analyze water samples from the bay and determine not only how
much of the lead in a given sample came from gasoline, but how much came from, for
example, gasoline produced in the 1960s and 1970s. Lead's unique elemental properties
made this possible, he said. Different forms of lead, called stable isotopes, occur
naturally, and their proportions can indicate the origins of the lead in a sample.
"Lead has a unique isotopic variability that allows us to fingerprint the sources,"
Steding said.
The results showed that gasoline emissions from the 1960s and 1970s still account
for most of the lead in water samples from the rivers and bay. Leaded gasoline consumption
peaked in the mid-1970s. The researchers estimated that cars burning leaded gasoline
emitted 33,000 tons of lead in the Sacramento and San Joaquin drainage basins in
the 1960s and 1970s.
In the South Bay, 1960s and 1970s gasoline lead still accounts for 90 percent of
the lead found in water samples. Moreover, this percentage remained unchanged throughout
the study period, from 1989 to 1998. In the North Bay and the rivers, however, the
proportion of lead from the 1960s and 1970s declined by 5 to 10 percent relative
to lead from 1980s gasoline emissions.
The researchers found that only 1 to 10 percent of the total amount of lead deposited
in the Central Valley during the drought years of 1986-92 had been washed into the
bay by 1995. The study also indicated that lead from 1980s gasoline is more readily
mobilized by surface runoff than lead from 1960s and 1970s gasoline, which is probably
located deeper in California soils and in the sediments of the river beds.
According to Flegal, other heavy metals and some organic pollutants are likely to
show similar patterns of persistence in the environment. These include contaminants,
such as mercury, that are serious problems in San Francisco Bay, posing threats to
humans and wildlife.
"We can't fingerprint these other contaminants, but we know they cycle like
lead does in the environment," Flegal said.
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