“…However, anions other than OH − can be released, as is the case for SO 2− 4 , PO 3− 4 or organic anions, which is in concordance with the correlations found between adsorbed As(V) and DOC (r = 0.810, for fine shell, and r = 0.919 and r = 0.913, for the granitic material amended with 12 and 24 t ha −1 mussel shell, respectively, p < 0.005). Moreover, other mechanisms that can be responsible for anion retention (such as retention on calcite or H and van der Waals bindings) do not implicate OH − release (Boddu et al, 2003). Different authors remark on the influence of pH on As(V) adsorption (Maji et al, 2007;Partey et al, 2008;Stanic et al, 2009), but in the case of our granitic material, Al, Fe, Al o , Fe o , organic matter and organoaluminum complexes, contents must also be relevant.…”