Effects of Soil Microorganisms on Soil Fertility

The nutrient elements in organic matter can only be released for plant absorption and utilization through the decomposition of microorganisms. The decomposition and metabolites of microorganisms are the basic materials for the formation of soil humus. Microbial cells, such as fungal hyphae, themselves participate in the formation of soil aggregates and play an important role in the physical structure of the soil. Many microorganisms with special functions in the soil, such as nitrogen-fixing bacteria, phosphorus-solubilizing bacteria, and potassium-releasing bacteria, can increase the content of available N, P, and K in the soil and their supply intensity. Soil nitrification and re-nitrification bacteria are closely related to the efficient use of soil nitrogen. Nitrification inhibitors are used in agriculture to inhibit the nitrification of ammonium, thereby reducing nitrate denitrification and reducing nitrogen loss. Through the decomposition of microorganisms, the toxic substances in the soil can be decomposed.

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