Borehole sediment samples (n = 2235) from each 3.03 m or 6.06 m interval from 112 boreholes and arsenic-rich water residues from arsenic-affected areas of West Bengal were studied to find out the geochemical environment and the chemistry involved in leaching out of arsenic from mineral phase and their mode of occurrence and origin. Arsenic-rich grains were characterized by petrologically (Binocular, Thin section, Polish section study), mineralogically, X-Ray Diffraction (XRD), Scanning Electron Microscopy... Mehr