Abstract
Tidal seawater inundation of coastal acid sulfate soils can generate Fe- and SO4-reducing conditions in previously oxic-acidic sediments. This creates potential for mobilization of As during the redox transition. We explore the consequences for As by investigating the hydrology, porewater geochemistry, solid-phase speciation, and mineralogical partitioning of As across two tidal fringe toposequences. Seawater inundation induced a tidally controlled redox gradient. Maximum porewater As (400 i??g/L) occurred in the shallow (
Original language | English |
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Pages (from-to) | 1968 - 1973 |
Number of pages | 6 |
Journal | Environmental Science and Technology |
Volume | 44 |
Issue number | 6 |
DOIs | |
Publication status | Published - 2010 |