T176 Chemical and Hydrological Interactions in the Evolution and Control of Coal and Metal Mine Drainage (Posters)
DISSOLVED METALS AND ASSOCIATED CONSTITUENTS IN ABANDONED COAL-MINE DISCHARGES, PENNSYLVANIA, 1999
Paper number: T176-9
Program: Technical Sessions
Time: 1:30 PM – 5:30 PM
Authors
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R. SealU.S. Geological Survey, Reston, VA
Abstract
Predominant trace metals, in order of median concentration (range in ug/L), were Zn (0.6 to 10,000), Ni (2.6 to 3,200), Co (0.27 to 3,100), Ti (0.65 to 28), Cu (0.4 to 190), Cr (<0.5 to 72), Pb (<0.05 to 11), and Cd (<0.01 to 16). Predominant rare-earth elements, in order of median concentrations (range in ug/L), were Y (0.11 to 530), Ce (0.01 to 370), Sc (1.0 to 36), Nd (0.006 to 260), La (0.005 to 140), Gd (0.005 to 110), Dy (0.002 to 99), and Sm (<0.005 to 79). Concentrations of most trace metals and rare earths were negatively correlated with pH, consistent with sorption control. In contrast, As (<0.03 to 64 ug/L) was positively correlated with pH and negatively correlated with dissolved O2. These associations could indicate As mobilization by desorption from, or reduction of, hydrous ferric oxides under neutralizing conditions. All 140 samples exceeded USEPA continuous-concentration criteria for Al, Fe, Co, Ni, and/or Zn for protection of freshwater organisms. Ten percent of the samples exceeded USEPA drinking-water standards for As, and 33 percent exceeded those for Be.