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Soil organic matter (SOM) plays a key role in the improvement of soil physical, chemical and biological properties. Cultivation has caused reductions in C content of agricultural soils, contributing to increases in atmospheric CO2 concentration. Organic carbon is a key attribute of soil fertility, as it serves as soil conditioner, nutrients source and substrate for microbial activity, preserver of the environment and sustainer of agricultural productivity (Benbi et al., 2011). Application of manures and fertilizers at an optimum rate increases the crop production which, in turn, results in greater residueinput balanced application of inorganic fertilizers or organic manure plus inorganic fertilizers can increase.

Soil Carbon Fractions as Influenced by Long-Term Integrated Nutrient Management under Rice-Wheat Cropping System in Calcareous Soil of North Bihar