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Sediment biomarker, bacterial community characterization of high arsenic aquifers in Jianghan Plain, China

机译:沉积物生物标志物,江汉平原高砷含水层的细菌群落特征

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Representative biomarkers (e.g., n-alkanes), diversity and microbial community in the aquifers contaminated by high concentration of arsenic (As) in different sediment depth (0–30?m) in Jianghan Plain, Hubei, China, were analyzed to investigate the potential mechanism of As enrichment in groundwater. The concentration of As was abundant in top soil and sand, but not in clay. The analysis of the distribution of n-alkanes, CPI values, and wax to total n-alkane ratio (Wax(n)%) indicated that the organic matter (OM) from fresh terrestrial plants were abundant in the shallow sediment. However, n-alkanes have suffered from significant biodegradation from the depth of 16?m to 30?m. The deposition of fresh terrestrial derived organic matters may facilitate the release of As from sediment to groundwater in the sediment of 0–16?m. However, the petroleum derived organic matters may do the favor to the release of As in the deeper section of borehole (16?m to 30?m). The 16S rRNA gene sequences identification indicated that Acidobacteria, Actinomycetes and Hydrogenophaga are abundant in the sediments with high arsenic. Therefore, microbes and organic matters from different sources may play important roles in arsenic mobilization in the aquifers of the study area.
机译:通过高浓度的砷(AS)污染的含水层中的代表性生物标志物(例如,正烷烃),多样性和微生物群落在江汉普平原的不同沉积物深度(0-30?m)中,湖北,中国湖北省,探讨了作为地下水富集的潜在机制。顶部土壤和沙子的浓度丰富,但不含粘土。分析N-烷烃,CPI值和蜡的分布至总N-烷烃比(蜡(N)%)表明来自新鲜陆生植物的有机物(OM)在浅沉积物中丰富。然而,N-烷烃从16μm至30μm的深度遭受显着的生物降解。新鲜陆地衍生的有机物的沉积可以促进从沉积物中释放到0-16Ω·m的沉积物中的地下水。然而,石油衍生的有机物质可以对钻孔更深部分(16μm至30μm)的释放来释放。 16S rRNA基因序列鉴定表明,抗酸体,放线菌和氢气在高砷的沉积物中丰富。因此,来自不同来源的微生物和有机物可能在研究区域的含水层中的砷动员中起重要作用。

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