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Heterotrophic nitrification in soils

机译:土壤中的异养硝化作用

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The contribution of heterotrophic microorganisms to nitrification processes in soils of different types under natural vegetation and in agrocenoses was estimated. The intensity of heterotrophic nitrification was higher in soils of native biocenoses than in croplands. In cultivated soils, the population of autotrophic nitrifying bacteria increased. They had a dominant role in the production of nitrates (84 to 99%). The heterotrophic nitrification was more active in soddy-podzolic soil of the wood sorrel spruce forest (Pinetum oxalidosum). In the gray forest soil of the birch forest and in the virgin dark chestnut soil, heterotrophic microorganisms were responsible for the production of 33-46% of nitrates. In leached brunizems of the pine and oak forests and in soils of different-aged laylands in the forb-grass prairie, the participation of heterotrophic microorganisms in nitrification was estimated at 25%. The additional application of nitrogen fertilizers 2-5 times decreased the activity of heterotrophic organisms.
机译:估计了异养微生物对自然植被和农杆菌条件下不同类型土壤中硝化过程的贡献。天然生物群落土壤中异养硝化的强度高于农田。在耕作土壤中,自养硝化细菌的数量增加。它们在硝酸盐的生产中起主要作用(84%至99%)。木质or浆云杉林(Pinetum oxalidosum)的多土壤土壤中的异养硝化作用更为活跃。在白桦林的灰色森林土壤和原始的深色栗树土壤中,异养微生物负责产生33-46%的硝酸盐。在松树和橡树林的浸出的青草中,以及在草丛草原上不同年龄的产地的土壤中,异养微生物参与硝化作用的比例估计为25%。氮肥的额外施用2-5倍会降低异养生物的活性。

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