Manganese
Manganese is liable to oxidation in soil depending on pH, oxygen supply and organic matter content of soil. In acid soils it is present in a bivalent state (Mn++) in which state it is easily available for absorption by plants. In neutral and alkaline soils, on the other hand, manganese occurs in trivalent or tetravalent state (Mn++++) when the element is not easily available for absorption by plants. Therefore, the oxidation state of the element is the primary factor affecting its absorption by plants.





