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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 term comes from humus, which in turn comes from the Latin word humus, meaning "soil, earth". [1] Humic substances represent the major part of organic matter in soil, peat, coal, and sediments, and are important components of dissolved natural organic matter (NOM) in lakes (especially dystrophic lakes), rivers, and sea water.
Mor humus has three distinct layers: A litter (L) layer, atop a fermentation (Fm) layer, followed by a humus (H) layer, before the transition to mineral soil (Ae, Bf). ). Unlike other types of forest floor humus, the litter layer is well-differentiated from the fermentation layer, and the fermentation layer remains distinct from the humus la
In terms of soil and humus creation, the most important fungi tend to be saprotrophic; ... Soil and Water Conservation Society, 2000, Soil Biology Primer. Tate, 2000 ...
Soil has a crucial function in the global carbon cycle, with the global soil carbon pool estimated to be 2,500 gigatons. This is 3.3 times the amount of the atmospheric pool at 750 gigatons and 4.5 times the biotic pool at 560 gigatons.
Muck farming on drained swamps is an important part of agriculture in New York, Ohio, Illinois, Indiana, Michigan, Wisconsin, and Florida, where mostly vegetables are grown. The muckland of Torrey Farms of Elba, New York , which covers the counties of Orleans , Niagara , and Genesee , is thought to be the largest continuous section of muckland ...
The formation of mull humus form results from various factors, including regional climate, parent rock, vegetation, and soil organism. [3] Mull order presents in deciduous forests, and the development is often associated with a mild climate in terms of warm temperature and moderate precipitation, also rich soil parent materials. [4]
Above-ground and below-ground biodiversities are tightly interconnected, [157] [208] making soil protection of paramount importance for any restoration or conservation plan. The biological component of soil is an extremely important carbon sink since about 57% of the biotic content is carbon.