School of Resource and Environment Science, Key Laboratory for Catalysis and Materials Science of the State Ethnic Affairs Commissions &Ministry of Education, South Central University for Nationalities, Wuhan 430074, China.
Emergencies Science and Technology Section, Science and Technology Branch, Environment and Climate Change Canada, Ottawa, ON, Canada.
Sci Rep. 2017 Feb 6;7:42037. doi: 10.1038/srep42037.
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.
在中国湖北江汉平原,分析了受高浓度砷(As)污染的含水层中不同沉积深度(0-30m)的代表性生物标志物(如正烷烃)、多样性和微生物群落,以研究地下水砷富集的潜在机制。砷的浓度在表土和砂中丰富,但在粘土中不丰富。正烷烃的分布、CPI 值和蜡与总正烷烃比(Wax(n)%)的分析表明,浅层沉积物中含有丰富的新鲜陆地植物来源的有机质。然而,从 16m 到 30m 的深度,正烷烃已经受到了严重的生物降解。新鲜陆地衍生有机物质的沉积可能有利于 0-16m 沉积层中砷从沉积物向地下水中释放。然而,在更深的钻孔(16m 至 30m)中,石油衍生的有机物质可能有利于释放砷。16S rRNA 基因序列鉴定表明,在含高砷的沉积物中,酸杆菌、放线菌和噬氢菌丰富。因此,不同来源的微生物和有机质可能在研究区含水层中砷的迁移中发挥重要作用。