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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.
The process that converts soil organic matter into humus feeds the population of microorganisms and other creatures in the soil, and thus maintains high and healthy levels of soil life. [ 53 ] [ 54 ] The rate at which soil organic matter is converted into humus promotes (when fast, e.g. mull ) or limits (when slow, e.g. mor ) the coexistence of ...
In terrestrial ecosystems detritus is present as plant litter and other organic matter that is intermixed with soil, known as soil organic matter. The detritus of aquatic ecosystems is organic substances suspended in the water and accumulated in depositions on the floor of the body of water ; when this floor is a seabed , such a deposition is ...
Organic matter, organic material, or natural organic matter refers to the large source of carbon-based compounds found within natural and engineered, terrestrial, and aquatic environments. It is matter composed of organic compounds that have come from the feces and remains of organisms such as plants and animals . [ 1 ]
Only fungi produce the enzymes necessary to decompose lignin, a chemically complex substance found in wood. A decaying tree trunk in Canada's boreal forest. Decaying wood fills an important ecological niche, providing habitat and shelter, and returning important nutrients to the soil after undergoing decomposition. Detritivore nutrient cycling ...
Decomposition is largely inhibited during advanced decay due to the loss of readily available cadaveric material. [15] Insect activity is also reduced during this stage. [ 16 ] When the carcass is located on soil, the area surrounding it will show evidence of vegetation death. [ 15 ]
In terrestrial environments, decomposition happens mainly in or on soil, and decomposers' activities lead to increased soil fertility. [7] The main nutrients plants have to derive from soils are nitrogen, phosphorus, and potassium, and all three have to be available in forms that are accessible to and absorbable by the plants.
Water is a critical agent in soil development due to its involvement in the dissolution, precipitation, erosion, transport, and deposition of the materials of which a soil is composed. [39] The mixture of water and dissolved or suspended materials that occupy the soil pore space is called the soil solution. Since soil water is never pure water ...