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Microbial complexes of therapeutic mud from Lake Tinaki-1

机译:蒂纳基湖1号的治疗泥微生物复合物

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The number and biomass of prokaryote microorganisms in the therapeutic mud from the saline Lake Tinaki-1 (Astrakhan oblast) were studied. In the therapeutic mud of this lake, the organic matter decomposition is performed by bacteria, whose number is250 million/g, which is an order of magnitude lower than the number of bacteria in the soils of the Volga River delta. The therapeutic mud is of the chloride type of salinization. It has a low organic carbon content, which is related to the low bacterialpopulation in it. Among the ecological-trophic groups of microorganisms in the mud of Lake Tinaki-1, halophilic ones prevail. The highest carbon content of the microbial biomass (0.06 mg/g) was characteristic of the therapeutic mud, which is interpretedas an organic horizon of the soil profile studied. The share of carbon of the microbial biomass in the carbon of the mud organic matter varied from 0.5 to 1.4%.
机译:研究了盐湖Tinaki-1(阿斯特拉罕州)的治疗泥中原核生物的数量和生物量。在该湖的治疗性泥浆中,有机物的分解是由细菌进行的,细菌的数量为2.5亿个/克,比伏尔加河三角洲土壤中的细菌数量低一个数量级。治疗性泥浆是氯化物盐碱化类型。它的有机碳含量低,这与其中细菌含量低有关。在Tinaki-1湖泥中的微生物中,有生态营养的群体占优势。微生物生物量的最高碳含量(0.06 mg / g)是治疗泥的特征,这被解释为研究土壤剖面的有机视野。泥浆有机质碳中微生物生物量碳的比例为0.5%至1.4%。

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