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Microbial distribution and diversity in saturated, high pH, uranium mine tailings, Saskatchewan, Canada.

机译:加拿大萨斯喀彻温省饱和高pH铀矿尾矿中的微生物分布和多样性。

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摘要

Microbiological analyses were conducted on core samples collected along a vertical profile (0-66 m below surface) from the tailings management facility (TMF) at the Rabbit Lake uranium mine in northern Saskatchewan, Canada. Bacterial numbers in the core materials were similar to surrounding soils and surface waters, regardless of the seemingly unfavorable pH (mean=9.9) and temperature (approximately 0 degrees C) in the TMF. The greatest number of viable cells (105 CFU/g) was detected at the interface between the tailings and overlying standing water, below which cell counts decreased rapidly with depth. Whole-community metabolic profiles for samples from the different depths grouped into 3 clusters; however, these groups could not be positively correlated with sampling depth, temperature, redox potential, pH, or ore-mill feed. Flow-cell studies demonstrated microbial communities in the tailings surface water could develop biofilms and maintain cell activity at both pH 10 and 7, and altering the pH between these 2 values had little effect on biofilm viability. These results demonstrate the resilience and adaptive nature of naturally occurring microbial communities and signify a potential role of microbial activity in the long-term geochemical evolution of the TMF.
机译:对从加拿大萨斯喀彻温省Rabbit Lake铀矿的尾矿管理设施(TMF)沿垂直剖面(地下0-66 m)收集的岩心样品进行了微生物分析。核心材料中的细菌数与周围的土壤和地表水相似,而与TMF中看似不利的pH值(平均值= 9.9)和温度(约0摄氏度)无关。在尾矿和上覆死水之间的界面处检测到最大数量的活细胞(105 CFU / g),在此以下,细胞数量随深度迅速减少。来自不同深度的样品的全社区代谢谱分为3个组;但是,这些组与采样深度,温度,氧化还原电位,pH值或矿石厂进料之间没有正相关。流式细胞研究表明,尾矿表面水中的微生物群落可以形成生物膜并在pH值为10和7时保持细胞活性,而在这两个值之间改变pH值对生物膜的活力影响很小。这些结果证明了天然存在的微生物群落的弹性和适应性,并表明了微生物活性在TMF的长期地球化学演化中的潜在作用。

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