Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6306789 | Chemosphere | 2016 | 8 Pages |
Abstract
The release dynamics of dissolved Cr and Pb as affected by redox potential (EH), pH, Fe, Mn, dissolved organic carbon, and sulfate was quantified using an automated biogeochemical microcosm apparatus. Soil pH decreased under oxic conditions. The release of Cr, Pb, Fe, and Mn increased under acidic oxic (pHÂ =Â 3.7, EHÂ =Â 521Â mV) conditions due to the associated decrease of pH (7.1-3.7). The mobilization of Cr and Pb was affected by the Fe and Mn. In conclusion, our multi-technique approach identified the geochemical distribution of Cr and Pb and verified major factors that explain mobilization of Cr and Pb in floodplain soils.
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Authors
Jörg Rinklebe, Sabry M. Shaheen, Felix Schröter, Thilo Rennert,