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Soil organic matter (SOM) is the organic matter component of soil, consisting of plant and animal detritus at various stages of decomposition, cells and tissues of soil microbes, and substances that soil microbes synthesize.
When the organic component of a soil is substantial, the soil is called organic soil rather than mineral soil. A soil is called organic if: Mineral fraction is 0% clay and organic matter is 20% or more; Mineral fraction is 0% to 50% clay and organic matter is between 20% and 30%; Mineral fraction is 50% or more clay and organic matter 30% or ...
In classical [1] soil science, humus is the dark organic matter in soil that is formed by the decomposition of plant and animal matter. It is a kind of soil organic matter. It is rich in nutrients and retains moisture in the soil. Humus is the Latin word for "earth" or "ground". [2]
The increased percentage of organic matter improves water infiltration and retention, aeration, and other soil characteristics. The soil is more easily turned or tilled than non-aggregated soil. Further aeration of the soil results from the ability of the root systems of many green manure crops to efficiently penetrate compact soils.
RA's primary contributions to soil health is the enhancement of organic matter and microbial activity. A myriad of practices can be used to increase soil organic content, like cover cropping, composting, and crop rotation to improve soil fertility, water retention, and ability to resist soil erosion.
Microorganism function is in long duration, causing improvement of the soil fertility. It maintains the natural habitat of the soil. It increases crop yield by 20-30%, replaces chemical nitrogen and phosphorus by 30%, and stimulates plant growth. It can also provide protection against drought and some soil-borne diseases.
Organic amendments improve biological activity, water permeability, and soil structure. [4] Mulch, for example, reduces erosion and helps to maintain the temperature of the soil. [3] Compost is rich in organic matter, [4] it is composed of decomposed matter such as food, vegetation, and animal wastes. [3]
The organic matter in soil derives from plants, animals and microorganisms. In a forest, for example, leaf litter and woody materials fall to the forest floor. This is sometimes referred to as organic material. [9] When it decays to the point in which it is no longer recognizable, it is called soil organic matter.