Nikolaos P Nikolaidis1, Gregory M Dobbs, Jing Chen
1Department of Environmental Engineering, Technical University of Crete, Polytechnioupolis, 73100 Chania, Greece. nnikolai@mred.tuc.gr
Arsenic mobility in lake sediment is influenced by groundwater flow and sediment geochemistry. Iron co-precipitation significantly reduces arsenic leaching into water, leading to accumulation at the groundwater/lake interface.
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