Lj. Puckett et al., SINKS FOR TRACE-METALS, NUTRIENTS, AND SEDIMENTS IN WETLANDS OF THE CHICKAHOMINY RIVER NEAR RICHMOND, VIRGINIA, Wetlands, 13(2), 1993, pp. 105-114
The Chickahominy River drains 790 km2 in southeastern Virginia, includ
ing approximately 155 kM2 of dense commercial, industrial, and urban d
evelopment in the upper basin near Richmond, Virginia. Previous studie
s have shown that total stream concentrations of trace metals and nutr
ients increased during storms, suggesting resuspension of contaminated
sediments and (or) stormwater influxes of pollutants. The possible ro
le of wetlands in maintaining water quality is of concern because the
river furnishes about 46 percent of the water supply for the City of N
ewport News. Particle sizes of sediments and their corresponding total
concentrations of carbon, nitrogen, copper, nickel, lead, and zinc we
re determined to assess their distribution within wetlands adjacent to
the river. Except for Zn, concentrations of all measured constituents
in the <63-mum-particle fraction were lower downstream of Richmond, s
uggesting that most contaminants are retained in the upper basin. Zinc
concentrations increased along downstream reaches, peaking at 5 1 0 m
g kg-1 approximately 8 km below the confluence of Upham Brook with the
Chickahominy River. Lead concentrations up to 192 mg kg-1 were measur
ed in sediments along Upham Brook near Richmond. Concentrations of Zn
and Cu were highest in streambed sediments and lowest in elevated fore
sted wetlands. The results suggest that the developing regions of the
basin have a significant effect on sediment chemistry within the basin
and that wetlands play a role in retaining these sediment-borne conta
minants in upper reaches of the basin. Studies are underway to assess
the stablity of these sediments and the capacity of these contaminated
wetlands to continue to assimilate them.