“…In the soil solution, Ni occurs as free ionic form (Ni 2+ ) and complexed form with organic and inorganic ligands (Reddy and DeLaune 2008). Approximately 50% of Ni in soils and sediments might be associated with the residual fraction and about 20% in the Fe/Mn oxides fraction, the rest might be attached to the carbonate fraction, and to the exchangeable and organic fractions (Pacifico et al 2007;Jordán et al 2009). Redox potential (E H ) and soil reaction (pH) are master variables controlling Ni dynamics, mobilities, and partitioning in soils.…”