Masscheleyn et al., 1991). The mobility of As is a function of its oxidation state with arsenite exhibiting greater Arsenic adsorption on amorphous Al and Fe oxides and the clay mobility through sand columns than arsenate (Gulens et minerals, kaolinite, montmorillonite, and illite was investigated as a function of solution pH and As redox state, i.e., arsenite [As(III)] al., 1979). However, und...