Organic matter in soils resulting from decay of plant and animal materials
This article is about the organic matter in soil. For the food, see Hummus. For the band, see Humus (band).
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]
In agriculture, "humus" sometimes also is used to describe mature or natural compost extracted from a woodland or other spontaneous source for use as a soil conditioner.[3] It is also used to describe a topsoilhorizon that contains organic matter (humus type,[4]humus form,[5] or humus profile[6]).
Humus has many nutrients that improve the health of soil, nitrogen being the most important. The ratio of carbon to nitrogen (C:N) of humus commonly ranges between 8:1 and 15:1 with the median being about 12:1.[7] It also significantly improves (decreases) the bulk density of soil.[8] Humus is amorphous and lacks the cellular structure characteristic of organisms.[9]
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Popkin, Gabriel (27 July 2021), A soil-science revolution upends plans to fight climate change, Quanta Magazine, retrieved 9 June 2024, "The latest edition of The Nature and Properties of Soils, published in 2016, cites Lehmann's 2015 paper and acknowledges that "our understanding of the nature and genesis of soil humus has advanced greatly since the turn of the century, requiring that some long-accepted concepts be revised or abandoned."