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Functioning of microbial complexes in aerated layers of a highmoor peat bog.

机译:微生物复合物在高泥炭沼泽的充气层中的功能。

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Monitoring was carried out using the luminescent-microscopic method of the abundance parameters of different groups of microorganisms in a monolith and in the mixed layers of a highmoor peat bog (oligotrophic residual-eutrophic peat soil) in a year-long model experiment. The increase of the aeration as a result of mixing of the layers enhanced the activity of the soil fungi. This was attested to by the following changes: the increase of the fungal mycelium length by 6 times and of the fungal biomass by 4 times and the double decrease of the fraction of spores in the fungal complex. The response of the fungal complex to mixing was different in the different layers of the peat bog. The maximal effect was observed in the T1 layer and the minimal one in the T2 layer. The emission of CO2 in the mixed samples was 1.5-2 times higher than that from the undisturbed peat samples. In contrast with the fungi, the bacteria and actinomycetes were not affected by the aeration of the highmoor layers.
机译:在长达一年的模型实验中,使用发光显微镜方法对整块土壤和高沼泥炭沼泽(贫营养剩余富营养化泥炭土壤)的混合层中不同微生物群的丰度参数进行了监测。由于各层混合而增加的通气量提高了土壤真菌的活性。下列变化证明了这一点:真菌菌丝体长度增加了6倍,真菌生物质增加了4倍,并且真菌复合物中的孢子含量也减少了两倍。在泥炭沼泽的不同层中,真菌复合物对混合的反应不同。在T1层中观察到最大效果,在T2层中观察到最小效果。混合样品中CO 2 的排放是未扰动泥炭样品的1.5-2倍。与真菌相反,细菌和放线菌不受高沼气层通气的影响。

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