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Soil formation is a process in which interaction takes place between parent material, topography, climate, and organism to form soil. Theres another term used for soil Formation and that is Pedogenesis. When the soil is formed through the disintegration of parent rock by climate changes and biological agents it is also regarded as the formation of soil. A living organism that is found on ground levels such as insects, leeches, and microorganisms assist soil to get ready for plantation.
Several forms of soil are formed through environmental factors and made factors. Soil is characterized into various forms such as
Sandy Soil:
It is light and dry, and a low amount of nutrients are found in sandy soil. The proportion of sand in sand-clay is high which makes it lighter and clay is present in significantly less amount. Water can be easily drained from this soil and it can be more vibrant fir growing plants when nutrients and water capacity is enlarged.
Clay Soil:
Heavy soil that controls an ample amount of nutrients is classified as clay soil. It contains 255 clay soils, therefore; it can hold a high amount of water. They do not warm up easily in summer.
Silt Soil:
Along with high fertility and moisture, silt soil is made up of medium size particles. They are prone to be carried away with the rainwater. One can bond silt soil with other table clumps to make better use of it.
Chalk Soil:
Soil that is high in alkaline as there is a high presence of calcium carbonate in them is known as chalk soil. Chalk soil does not support ericaceous plant growth. When calk soil starts showing visible lumps of white colour then the gardener should prefer plants that would grow in the presence of alkaline.
Loam Soil:
Loam soil is formed when sand, clay, and silt are mixed. The negative effects of each type of soil are eliminated through this. It is fertile soil and more organic matter can be added to it. It is the most effective form of soil to work with and is preferably used by most of the gardeners.
Peat Soil:
A high amount of organic matter is present in peat soil, therefore, enabling it to hold excess moisture. It acts as an effective soil base for plantation of various crops.
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