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. SOM provides numerous benefits to the physical and chemical properties of soil and its capacity to provide regulatory ecosystem services.[1] SOM is especially critical for soil functions and quality.[2]
The benefits of SOM result from a number of complex, interactive, edaphic factors; a non-exhaustive list of these benefits to soil function includes improvement of soil structure, aggregation, water retention, soil biodiversity, absorption and retention of pollutants, buffering capacity, and the cycling and storage of plant nutrients. SOM increases soil fertility by providing cation exchange sites and being a reserve of plant nutrients, especially nitrogen (N), phosphorus (P), and sulfur (S), along with micronutrients, which the mineralization of SOM slowly releases. As such, the amount of SOM and soil fertility are significantly correlated.[3]
SOM also acts as a major sink and source of soil carbon (C). Although the C content of SOM varies considerably,[4][5] SOM is ordinarily estimated to contain 58% C, and "soil organic carbon" (SOC) is often used as a synonym for SOM, with measured SOC content often serving as a proxy for SOM. Soil represents one of the largest C sinks on Earth and is significant in the global carbon cycle and therefore for climate change mitigation.[6] Therefore, SOM/SOC dynamics and the capacity of soils to provide the ecosystem service of carbon sequestration through SOM management have received considerable attention.[7]
The concentration of SOM in soils generally ranges from 1% to 6% of the total mass of topsoil for most upland soils. Soils whose upper horizons consist of less than 1% of organic matter are mostly limited to deserts, while the SOM content of soils in low lying, wet areas can be as great as 90%. Soils containing 12% to 18% SOC are generally classified as organic soils.[8]
SOM can be divided into three genera: the living biomass of microbes, fresh and partially decomposed detritus, and humus. Surface plant litter, i. e., fresh vegetal detritus, is generally excluded from SOM.[9]
^Weil, Ray R.; Brady, Nyle C. (2016). The nature and properties of soils (15th ed.). Upper Saddle River, New Jersey: Pearson. ISBN 978-0133254488. Retrieved 17 December 2023.
^Beare, Mike H.; Cabrera, Miguel L.; Hendrix, Paul F.; Coleman, David C. (1994). "Aggregate-protected and unprotected organic matter pools in conventional and no-tillage soils". Soil Science Society of America Journal. 58 (3): 787–95. doi:10.2136/sssaj1994.03615995005800030021x. Retrieved 17 December 2023.
^Tiessen, Holm; Cuevas, Elvira; Chacón, Prudencio (1994). "The role of soil organic matter in sustaining soil fertility" (PDF). Nature. 371: 783–85. doi:10.1038/371783a0. Retrieved 17 December 2023.
^Périé, Catherine; Ouimet, Rock (2008). "Organic carbon, organic matter and bulk density relationships in boreal forest soils". Canadian Journal of Soil Science. 88 (3): 315–25. doi:10.4141/CJSS06008. Retrieved 24 December 2023.
^Jain, Terri; Graham, Russell T.; Adams, David L. (1997). "Carbon to organic matter ratios for soils in Rocky Mountain coniferous forests". Soil Science Society of America Journal. 61 (4): 1190–95. doi:10.2136/sssaj1997.03615995006100040026x. Retrieved 24 December 2023.
^"Restoring soils could remove up to '5.5bn tonnes' of greenhouse gases every year". Carbon Brief. London, United Kingdom. 2020-03-16. Retrieved 24 December 2023.
^Ontl, Todd A.; Schulte, Lisa A. (2012). "Soil carbon storage". The Nature Education Knowledge Project. Cambridge, Massachusetts. Retrieved 24 December 2023.
^"Organic matter in soil: overview of composition, distribution, and content". Ocean Agro LLC. Nandesari Vadodara, India. 2018. Retrieved 25 December 2023.
^Bot, Alexandra; Benites, José (2005). "The importance of soil organic matter: key to drought-resistant soil and sustained food production. Chapter 1. Introduction". Food and Agriculture Organization of the United Nations. Rome, Italy. Retrieved 25 December 2023.
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