Soil indeed alive and dynamic system consisting of minerals and microorganisms, the top-most layer of soil is comparatively richer in nutrients and supports maximum bio-resource. The profile character varies distinctly from place to place, particularly with respect to their depth, colour and composition. The mineral composition of the soil, organic matter within it and environment, all these are resolute by chemical, physical and biological properties of soil. Soil organic carbon is necessary for improving soil quality, sustaining food production and sinking CO 2 in the atmosphere, whereas its inorganic counterpart (free CaCO 3 ) is the cause of organic carbon decomposition, restricting root proliferation, developing salinity (Eswaran and Van den