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Sedimentology, geochronology, and trace metals in the Nanticoke and Choptank Rivers, and the Chesapeake Bay. Technical report

Technical Report ·
OSTI ID:5014894
Marsh and subtidal sediments in the Nanticoke and Choptank Rivers and Blackwater Wildlife Refuge of Maryland's Eastern Shore were analyzed for historic changes in trace metal and polycyclic aromatic hydrocarbons (PAH) content. Long-term accretion rates, determined from /sup 210/Pb geochronology and historical land-use changes recorded in fossil pollen, ranged from 0.18 to 0.74 cm/yr and decreased down the estuary. Changes in pine pollen concentrations suggest marsh accretion rates have accelerated since the late 19th century. Most core profiles indicate recent regional enrichment in Pb, Zn, and Cu.
Research Organization:
Maryland Univ., College Park (USA). Water Resources Research Center
OSTI ID:
5014894
Report Number(s):
PB-86-235645/XAB; TR-84
Country of Publication:
United States
Language:
English