Soil

Soil

Soil is the loose surface material that covers most land. It consists of inorganic particles and organic matter. Soil provides the structural support to plants used in agriculture and is also their source of water and nutrients. Soils vary greatly in their chemical and physical properties. Soil is the biologically active and porous medium that has developed in the uppermost layer of Earth's crust. It serves as the reservoir of water and nutrients and a medium for the filtration and breakdown of injurious wastes.

Technically, the soil is a mixture that contains minerals, organic matter, and living organisms. But broadly speaking, soil can refer to any loose sediment. Moreover, there are many types of soil that are distributed around the world and these are generally classified into the following: Clay Soil.