AGR 2320 Lecture Notes - Lecture 29: Soil Organic Matter, Soil Ph, Corn Stover

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The amount of fertilizer-n required in a given year is dependent on the inputs of inorganic-n from other sources, the demands of the crop and the losses by different mechanisms. The most significant input of inorganic-n is derived from the mineralization of different sources of organic-n. Fertilizer-n is required when the supply of inorganic-n during the peak requirement for n by the crop is not satisfied by mineralization of organic-n. Decomposition of om by heterotrophic organisms to yield nh4, co2, h2o, and other plant nutrients. Factors influencing the rate of decomposition of organic matter. If the amount n ingested from the organic matter is less than the n required to build tissue of microorganisms, then mineral-n in soil can be used by microorganisms to continue growth and reproduction. Still decomposition of om by heterotrophic organisms; however, plant available n is reduced.

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