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Abandoned mining sites with deep scars and overburden contribute to severe land degradation.
Proper discharge and disposal of industrial effluents and wastes after treatment can reduce land and water degradation.
Soil formation is extremely slow, taking millions of years to form up to a few centimetres, so its conservation is important.
Relief, parent rock, climate, vegetation and time are important factors in soil formation.
Soil consists of organic material such as humus and inorganic materials.
Alluvial soils are fertile and contain suitable proportions of potash, phosphoric acid and lime for crops including wheat and sugarcane.
Bangar is old alluvial soil and has a higher concentration of kanker than Khadar.
Khadar is the newer alluvial soil. It has more fine particles and is more fertile than Bangar.
Black soil is ideal for cotton and is well known for its capacity to retain moisture.
Deep cracks developed during hot weather help in proper aeration of black soil.
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