1. Irrigation produces elevated arsenic in the underlying groundwater of a semi-arid basin in Southwestern Idaho
- Author
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Montague W. Busbee, Shawn G. Benner, and Benjamin D. Kocar
- Subjects
Hydrology ,geography ,geography.geographical_feature_category ,Water table ,chemistry.chemical_element ,Aquifer ,Groundwater recharge ,Pollution ,chemistry ,Geochemistry and Petrology ,Groundwater pollution ,Environmental Chemistry ,Environmental science ,Water quality ,Leaching (agriculture) ,Groundwater ,Arsenic - Abstract
The shallow aquifer beneath the Western Snake River Plain (Idaho, USA) exhibits widespread elevated arsenic concentrations (up to 120 μg L−1). While semi-arid, crop irrigation has increased annual recharge to the aquifer from approximately 1 cm prior to a current rate of >50 cm year−1. The highest aqueous arsenic concentrations are found in proximity to the water table (all values >50 μg L−1 within 50 m) and concentrations decline with depth. Despite strong vertical redox stratification within the aquifer, spatial distribution of aqueous species indicates that redox processes are not primary drivers of arsenic mobilization. Arsenic release and transport occur under oxidizing conditions; groundwater wells containing dissolved arsenic at >50 μg L−1 exhibit elevated concentrations of O2 (average 4 mg L−1) and NO3 (average 8 mg L−1) and low concentrations of dissolved Fe (
- Published
- 2009
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