Nickel (Ni) is an abundant element found in soils at an average of 50 mg/kg. Soil Ni can commonly range from 5 to 500 mg, and serpentine soils have the highest natural levels of Ni. Elevated Ni levels may occur due to industrial activity such as metal refining or the agricultural application of heavy metal-contaminated sewage sludge.
Nickel can be found in oxidation states ranging from -1 to +4, but Ni2+ is the most common state in biological systems. Nickel availability in soil may be as low as 0.2 mg/kg, but proper soil Ni deficiencies are rare. Nickel availability may be considerably lower than total nickel concentration. Above pH 6.5, Ni forms insoluble hydroxide complexes with iron, aluminum, and manganese. Liming has been demonstrated to reduce Ni uptake in acidic soils.
Below pH 6.5, most Ni compounds are relatively soluble. Organic soils adsorbed more Ni than sandy soils, and amino acids and other organic acids can mobilize Ni. Thus, acidic, organic-rich soils may promote Ni uptake.
Ni enters plants via passive diffusion and active transport. Ni may share a common transport system with other ions such as Cu2+ or Zn2+. Thus, Ni cations carry a double positive charge which can induce deficiency via excessive fertilization with competing ions (Zn2+, Cu2+, Mg2+, Mn2+, Fe2+, Ca2+).