HR: 0800h
AN: H51E-0410    [Abstracts]
TI: Determining Sediment Sources in the Anacostia River Watershed
AU: * Devereux, O H
EM: devereux@umd.edu
AF: University of Maryland, Natural Resource Sciences 0104 HJ Patterson, College Park, MD 20742 United States
AU: Needelman, B A
EM: bneed@umd.edu
AF: University of Maryland, Natural Resource Sciences 0204 HJ Patterson, College Park, MD 20742 United States
AU: Prestegaard, K L
EM: kpresto@umd.edu
AF: University of Maryland, Department of Geology 0214A Chemistry Building, College Park, MD 20742 United States
AU: Gellis, A C
EM: agellis@usgs.gov
AF: U.S. Geological Survey, Water Resources Division 8987 Yellow Brick Road, Baltimore, MD 21237 United States
AU: Ritchie, J C
EM: jritchie@hydrolab.arsusda.gov
AF: USDA Agriculture Research Service, Hydrology and Remote Sensing Laboratory BARC-West Bldg-007, Beltsville, MD 20705 United States
AB: Suspended sediment is a water-quality problem in the Chesapeake Bay. This project is designed to identify sediment sources in an urban watershed, the Northeast Branch of the Anacostia River (in Washington, D.C. and Maryland - drainage area = 188.5 km²), which delivers sediment directly to the Bay. This watershed spans two physiographic regions - the Piedmont and Coastal Plain. Bank sediment and suspended-sediment deposits were characterized using the following techniques: radionuclide (Cs-137) analysis by gamma ray spectrometry, trace-element analysis by ICP-MS, clay mineralogy by XRD, and particle-size analysis by use of a laser particle-size analyzer. Sampling of bank and suspended sediment was designed to: a) characterize tributary inputs from both Piedmont and Coastal Plain sources, and b) differentiate tributary inputs from bank erosion along the main stem of the Northeast Branch. Thirteen sample sites were chosen that represent tributary source areas of each physiographic region and the main stem where mixing occurs. Surface samples of the banks were compared to overbank deposits from a ten year storm (a proxy for the suspended sediments). Fingerprint components are selected from these data. Cesium-137 concentrations were analyzed for bank and overbank deposits for each physiographic region. No clear differences were seen between the two physiographic regions. Significant differences were observed between upland tributaries and the main stem of the Anacostia River. The average activity of Cs-137 for the tributaries was 5.4 bq/kg and the average for the main stem was 1.1 bq/kg. This suggests that there is significant erosion and storage of sediment in the tributaries. The low activity from Cs-137 in the main stem suggests a lack of storage of sediment along the main stem of the river. For the trace-element data, we focused on elements that showed significant variation among the sites. For the bank sediment, these elements include: Sr, V, Y, Ce, and Nd. For the overbank deposits, Zr, V, Ba, Ce, and Cu showed significant variability. In both physiographic regions, Pb is primarily found in bank deposits, while Cu is found in higher concentrations in overbank deposits. The Cs-137 data clearly showed the erosion and storage of sediment patterns in the watershed. The trace-element data indicate that stream banks may be differentiated from overbank deposits.
DE: 0486 Soils/pedology (1865)
DE: 1862 Sediment transport (4558)
DE: 1865 Soils (0486)
DE: 1879 Watershed
SC: Hydrology [H]
MN: Fall Meeting 2005