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18.3: Organic Matter and Nutrient Availability

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    The best overall strategy for nutrient management is to enhance the level of organic matter in soils (Figure 18.1). This is especially true for N and P. Soil organic matter, together with any freshly applied residues, are well-known sources of N for plants. (However, as discussed in Chapter 9, unusual residues with high C:N ratios can reduce N availability for a period of time.)

    Mineralization of P and sulfur from organic matter is an important source of these nutrients. Also, organic matter helps hold on to positively charged potassium (K+), calcium (Ca++) and magnesium (Mg++) ions, and provides natural chelates that maintain micronutrients such as zinc, copper and manganese in forms that plants can use. In addition, the improved soil structure (tilth) and the growth-promoting substances produced during organic matter decomposition help the plant develop a more extensive root system, allowing it to obtain nutrients from a larger volume of soil. And a wide diversity of soil organisms helps maintain low populations of plant pathogens.

    residue decomposition nutrient flow chart
    Figure 18.1. Influence of residue decomposition on nutrient availability.

    Cover crop roots (living soil organic matter) also contribute to nutrient management. They provide energy material that allows soil organisms to better thrive and mobilize soil nutrients, keep nutrients from being lost by leaching or runoff, add new N to the soil (if a legume), and maintain plentiful supplies of mycorrhizae spores that lead to better inoculation of the following crop, helping it to take up soil nutrients.


    This page titled 18.3: Organic Matter and Nutrient Availability 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.