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2.4: Summary

  • Page ID
    25011
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    Soil organic matter is the key to building and maintaining healthy soils because it has such great positive influences on essentially all soil properties—aggregation, nutrient availability, soil tilth and water availability, biological diversity and so on— helping to grow healthier plants. Organic matter consists mainly of the living organisms in the soil (“the living”), the fresh residue (“the dead”), and the well-decomposed (or burned) material physically or chemically protected from decomposition (“the very dead”). Residue trapped inside aggregates (a portion of “the dead” organic matter), especially small ones, is protected also from decomposition because organisms are unable to access the material. Each of these types of organic matter plays an important role in maintaining healthy soils. Soil organic matter transformations are a key part of plant nutrition and the ability to achieve good crop yields. Soil organic matter is also an integral part of local and global cycles of carbon, nitrogen and water, impacting many aspects that define the sustainability and future survival of life on earth.


    This page titled 2.4: Summary is shared under a CC BY-NC 4.0 license and was authored, remixed, and/or curated by Fred Magdoff & Harold van Es (Sustainable Agriculture Research and Education (SARE) program) via source content that was edited to the style and standards of the LibreTexts platform.