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Sulfate-reducing bacterial activity and pyrite formation in sediments from Qinghai Lake in China

机译:中国青海湖沉积物中的硫酸盐还原细菌活性和黄铁矿形成

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The foul odor ofurban rivers is often attributed to the activity of sulfate-reducing bacteria (SRB),i.e. bacterial production of H2S fixed with iron ions into FeS or pyrite (FeS2) in river sediments. This process has been examined at the estuaries of urban rivers and in cultivation of SRB, and a close relationship between the activity of SRB and the presence of pyrite was confirmed. Our previous studies in Japan and at Qinghai Lake in China revealed similar findings. Three kinds of SRB, Desulfovibrio sp., an uncultured bacterium, and Desulfomicrobium apsheronum, were isolated from Qinghai Lake sediments, as was pyrite. This is the first report to describe the environmental bacteria of Qinghai Lake and to examine the relationship between bacterial activity and pyrite in its sediments.
机译:城市河流的恶臭通常归因于硫酸盐还原细菌(SRB)的活性,即细菌生产的铁离子将H2S固定为河流沉积物中的FeS或黄铁矿(FeS2)。已经在城市河流的河口和SRB的种植过程中检查了这一过程,并证实了SRB的活性与黄铁矿的存在之间存在密切的关系。我们之前在日本和中国青海湖进行的研究也发现了类似的发现。从青海湖沉积物中分离出三种SRB,一种未经培养的细菌Desulfovibrio sp。,和一种绿皮棉Desulfomicrobium apsheronum,以及黄铁矿。这是描述青海湖环境细菌并研究其沉积物中细菌活性与黄铁矿之间关系的第一份报告。

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