Humus
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In soil science, humus (coined 1790–1800; ) refers to any organic matter that has reached a point of stability, where it will break down no further and might, if conditions do not change, remain as it is for centuries, if not millennia. Humus significantly influences the texture of soil and contributes to moisture and nutrient retention.
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See also
- Soil Profile
- Biomass
- Terra preta
- Biotic material
- Soil horizon
- Detritus
- Glomalin
- Humic acid
- Organic matter
- Plant litter
- Hummus
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