Get Online Soil Formation Assignment Help

Soils all over the world have varied properties which make a difference in their ability for the transportation of water and nutrients and these differences are due to various factors and they also differ from one place to another. The age of the soil and also the kind of rock it is made up of are responsible for their properties. Some of the factors such as climate, soil age, parent material, and soil slopes, relief, and soil depth contribute to soil formation. Along with these four major factors, the other factors that are responsible for the soil formation are microbes, vegetation, and animals. The process of soil formation has an effect on the crop production. Human activity has impacts on soil formation in a major way, either by upgrading the productivity or by destroying it. Soil formation forms a part of the Geography course curriculum.

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Formation of Soils

The soil is the layer of material that covers the surface of the earth. The soil is formed because of the weathering of rocks. It consists of the organic materials, mineral particles, water, air, and living organisms that interact in a slow but constant manner. Most of the plants get the available nutrients from the soil and these nutrients are a major source of food for the animals, birds, and humans. Living beings are dependent on soil for their survival and existence. The soil is a very valuable resource and it is required to be managed in a careful manner because it gets damaged and blown away quite easily.

Soil Formation Process

Accumulation of materials– Materials get added to the soil like the decomposing materials, new materials, and organic matter and they all accumulate with time. This usually happens at the topsoil layer. Deposits also take place through wind forces, ice, and water.
Leaching and losses– The accumulated soils are leached or eroded are taken up by plants from the soil. Due to this, the physical, as well as the chemical composition of the parent soil material, also changes.
Transformation and illuviation– The chemical weathering of the sand, clay, and silt and also the change of the organic materials to the decay organic matter is called transportation. Plants and animals also contribute to soil transformation by breaking the materials both physically and chemically.
Podsolization and translocations– Podsolization happens when the acidic solutions are broken down into the clay materials.

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