| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6335396 | Applied Geochemistry | 2012 | 11 Pages |
Abstract
⺠Seasonal storativity changes in clay-peat layers affect groundwater chemistry. ⺠During dry season, DOC is released and total mineralization increases. ⺠In rainy season, recharge leads to dilution and decrease of total mineralization. ⺠Depth-dependent As-distribution confirms DOC-driven reduction of iron hydroxides. ⺠Seasonal peak arsenic concentration follows peak DOC with an unexplained time lag.
Related Topics
Physical Sciences and Engineering
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Geochemistry and Petrology
Authors
Britta Planer-Friedrich, Cornelia Härtig, Heidi Lissner, Jörg Steinborn, Elke SüÃ, M. Qumrul Hassan, Anwar Zahid, Mahmood Alam, Broder Merkel,