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Methane production and growth of microorganisms under different moisture conditions in soils with added chitin and without it

机译:添加甲壳素和不添加甲壳素的土壤在不同湿度条件下甲烷的产生和微生物的生长

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The limits of soil moisture providing the possibility of methane production and growth of microorganisms in soils with added chitin and without it were determined. Samples of gray forest, soddy-podzolic, gley taiga, chestnut, and chernozemic soils were studied. It was found that methane emission increases significantly under a high soil moisture content in the presence of chitin. The increase of the soil moisture up to the maximum water-holding capacity enhanced the emission of methane by two-six times. The dynamics of the methane emission from the soils in the course of microbial successions initiated by the addition of chitin or by the soil moistening to different levels were studied by the gas-chromatographic method. The population density and biomass of fungal, bacterial, and actinomycetic complexes under different moister levels were studied by the method of luminescent microscopy. It was determined that many microorganisms participate in the transformation of chitin in the soil under conditions of oxygen deficiency (upon the increased moisture content). Prokaryotes dominated by actinomycetes were the group that increased its biomass most actively (the biomass doubling took place).
机译:确定了土壤湿度的极限值,从而确定了添加甲壳质和不添加甲壳质的土壤中甲烷的产生和微生物生长的可能性。研究了灰色森林,泥泞的土壤,针叶林针叶林,栗子和黑钙土的样品。发现在甲壳质存在下,在高土壤湿度下甲烷排放显着增加。土壤水分增加到最大持水量,甲烷排放量增加了六倍。通过气相色谱法研究了通过添加几丁质或将土壤润湿至不同水平引发的微生物演替过程中土壤甲烷排放的动力学。通过发光显微镜的方法研究了不同水分含量下真菌,细菌和放线菌复合物的种群密度和生物量。已确定在缺氧条件下(随着水分含量的增加)许多微生物参与了土壤中几丁质的转化。以放线菌为主的原核生物是最活跃地增加其生物量的组(发生了生物量加倍)。

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