Abstract
Groundwater of the arsenic affected areas demonstrates that the water is Ca-bicarbonate type and typical anoxic in nature. High arsenic groundwater is distributed in patches and hot spots are identified in palaeo-meander belt. Iron rich arsenic traps undergo reduction and release redox sensitive species (As and Fe) under local reducing conditions. Releases of redox species are often depends on land-use pattern and the abundance of bioavailable forms of iron oxides/minerals.
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