Chromium Geochemistry in a Wetland Environment
Author(s) -
Patrick Longmire,
M. Dale,
Kim Granzow
Publication year - 2013
Publication title -
procedia earth and planetary science
Language(s) - English
Resource type - Journals
ISSN - 1878-5220
DOI - 10.1016/j.proeps.2013.03.010
Subject(s) - chromium , wetland , geochemistry , geology , mining engineering , metallurgy , materials science , ecology , biology
Cooling tower water ranging between 7 to 18mg/L of Cr(VI) was released to a stream channel entering a wetland at Los Alamos National Laboratory, New Mexico, USA from 1956 to 1972. The wetland contains between 5700 and 27,000kg total Cr mainly as Cr(III), with a median mass of 11,000kg total Cr, representing 21 to 49% of the total Cr. Chemical analyses conducted on wetland sediments show that 97.3 to 99.9% of the Cr is stable as Cr(III). Mass balance calculations confirm that there are sufficient concentrations of Fe(II) along with the organic-rich sediments to maintain Cr(III) stability within the wetland
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