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Specific features of the structure of microbial biomass in soils of annular mesodepressions in Lipetsk and Volgograd oblasts

机译:利佩茨克州和伏尔加格勒州环形中压下土壤微生物生物量结构的特殊特征

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摘要

In the studied mesodepressions, the total microbial biomass in the gray forest and chernozemic soils decreases by two-three times under the impact of hydrogen flux from the subsoil horizons and soil waterlogging. The biomass decrease is especially pronounced in the lower soil horizons. The population density of bacteria in the soil samples subjected to the impact of hydrogen fluxes and temporary waterlogging decreases by two-three times in the upper horizons and by ten times in the lower horizons in comparison with that in the control samples. These factors also affect the length of fungal mycelium: it decreases by three-four times in the upper horizons and may completely disappear in the lower horizons. The reduction of the microbial biomass can be explained by the fact that hydrogen and waterlogging sharply decrease the soil redox potential, which retards the development of most microbes, except for methanogens and some other specialized groups of microorganisms. The domination of bacteria with diameter a parts per thousand yen0.23 and a parts per thousand yen0.38 mu m and the decrease in the total number of bacteria have been found with the use of the cascade filtration method.
机译:在所研究的中压下,灰土和黑钙土中微生物的总生物量在地下土壤水平和土壤涝的氢通量的影响下减少了三倍。在较低的土壤层中,生物量的减少尤为明显。与对照样品相比,受到氢通量和暂时性内涝影响的土壤样品中细菌的种群密度在上层减少了三倍,下层减少了十倍。这些因素也影响真菌菌丝体的长度:其在上层减少了三到四倍,在下层可能会完全消失。微生物和生物量的减少可以用以下事实来解释:氢和涝渍会大大降低土壤的氧化还原电位,这会阻碍大多数微生物的发展,除了产甲烷菌和某些其他专门的微生物群。通过级联过滤法,发现直径为千分之0.23和千分之0.38μm的细菌占优势,细菌总数减少。

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