STORM WATER CONTROLLED TRACE METAL LOADING IN THE CHESAPEAKE BAY WATERSHED
An investigation in the Patapsco River Watershed, a subordinate drainage system with in the Chesapeake Bay Watershed, has determined that the ultimate source of most trace metals being transported to Baltimores Inner Harbor are soils that are being eroded within the watershed. Furthermore, the flux of suspended sediments and associated trace metals are dominated by storm water discharge events. The geochemical characteristics of the suspended sediments being transported to the Inner Harbor are consistent with material derived from the chemically weathered UCC and as much as 50% of the total trace metal flux associated with suspended sediments is potentially bio-available.
The sediment yield of the Patapsco River Watershed, which in some cases is >30,000 t/km2/yr, is closely correlated with impermeable ground cover. The ground cover conditions within the Patapsco River Watershed have created non-equilibrium denudation conditions leading to an unusually high sediment flux and corresponding trace metal transport into Baltimores Inner Harbor. Resultantly, any effort to limit and/or control the accumulation of trace metals in the Harbor must include storm water management and erosion control measures through out the watershed.