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managing soil organic matter - Grains Research & Development ...

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Soil <strong>organic</strong> <strong>matter</strong> has a reservoir of nutrients boundwithin its <strong>organic</strong> structure, which are released intothe <strong>soil</strong> solution as <strong>soil</strong> microorganisms mineralise(break down) the <strong>organic</strong> <strong>matter</strong> for their ownmetabolism and growth.The amount of nutrients provided to plants viamicrobial breakdown of <strong>organic</strong> <strong>matter</strong> depends onthe type of material that is being mineralised and itsratio of carbon and other nutrients such as nitrogen,phosphorus and sulphur.As a rule, for every tonne of carbon in <strong>soil</strong> <strong>organic</strong><strong>matter</strong> about 100 kg of nitrogen, 15 kg of phosphorusand 15 kg of sulphur becomes available to plants as<strong>organic</strong> <strong>matter</strong> is broken down. As well as releasingplant nutrients, the microbes also release between50-90 per cent of the carbon in <strong>organic</strong> <strong>matter</strong>as carbon dioxide.The rate at which <strong>organic</strong> <strong>matter</strong> is broken downdetermines how rapidly the nutrients within the<strong>organic</strong> structure become available to plants. Theparticulate <strong>organic</strong> <strong>matter</strong> fraction breaks downrapidly, so its nutrients are made readily availableto plants and microbes. In contrast, the humusfraction breaks down over decades and providesa large but slow-release supply of plant-availablenutrients. Other more recalcitrant forms of carbonare relatively inert, taking hundreds to thousandsof years to break down and having little influenceon the amount of nutrients released into the<strong>soil</strong> solution.31MANAGING SOIL ORGANIC MATTER: A PRACTICAL GUIDE

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