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Microbial communities in a porphyry copper tailings impoundment and their impact on the geochemical dynamics of the mine waste

机译:斑岩型铜尾矿库中的微生物群落及其对矿山废弃物地球化学动力学的影响

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The distribution and diversity of acidophilic bacteria of a tailings impoundment at the La Andina copper mine, Chile, was examined. The tailings have low sulfide (1.7% pyrite equivalent) and carbonate (1.4% calcite equivalent) contents and are stratified into three distinct zones: a surface (0-70-80 cm) 'oxidation zone' characterized by low-pH (2.5-4), a 'neutralization zone' (70-80 to 300-400 cm) and an unaltered 'primary zone' below 400 cm. A combined cultivation-dependent and biomolecular approach (terminal restriction enzyme fragment length polymorphism and 16S rRNA clone library analysis) was used to characterize the indigenous prokaryotic communities in the mine tailings. Total cell counts showed that the microbial biomass was greatest in the top 125 cm of the tailings. The largest numbers of bacteria (10(9) g(-1) dry weight of tailings) were found at the oxidation front (the junction between the oxidation and neutralization zones), where sulfide minerals and oxygen were both present. The dominant iron-/sulfur-oxidizing bacteria identified at the oxidation front included bacteria of the genus Leptospirillum (detected by molecular methods), and Gram-positive iron-oxidizing acidophiles related to Sulfobacillus (identified both by molecular and cultivation methods). Acidithiobacillus ferrooxidans was also detected, albeit in relatively small numbers. Heterotrophic acidophiles related to Acidobacterium capsulatum were found by molecular methods, while another Acidobacterium-like bacterium and an Acidiphilium sp. were isolated from oxidation zone samples. A conceptual model was developed, based on microbiological and geochemical data derived from the tailings, to account for the biogeochemical evolution of the Piuquenes tailings impoundment.
机译:检查了智利拉安迪纳铜矿尾矿库中嗜酸细菌的分布和多样性。尾矿的硫化物含量低(黄铁矿当量为1.7%)和碳酸盐含量(方解石当量为1.4%),并且被分为三个不同的区域:以低pH值(2.5-2.5%)为特征的表面(0-70-80 cm)“氧化区”。 4),“中和区”(70-80至300-400 cm)和400 cm以下的未更改“主要区”。结合培养依赖和生物分子方法(末端限制性酶片段长度多态性和16S rRNA克隆文库分析)来表征矿山尾矿中的原核生物群落。总细胞数表明,在尾矿的顶部125 cm处,微生物量最大。在氧化前沿(氧化和中和区之间的交界处)发现了最大数量的细菌(尾矿干重为10(9)g(-1)干重),其中同时存在硫化物和氧气。在氧化前沿鉴定出的主要的铁/硫氧化细菌包括钩端螺旋体属细菌(通过分子方法检测)和与硫杆菌相关的革兰氏阳性铁氧化嗜酸菌(通过分子方法和培养方法均可鉴定)。也检测到了酸性氧化铁硫杆菌,尽管数量相对较少。通过分子方法发现了与荚膜嗜酸杆菌有关的异养嗜酸菌,而另一种嗜酸杆菌样细菌和嗜酸菌属嗜酸菌。从氧化区样品中分离。根据源自尾矿的微生物和地球化学数据,开发了概念模型,以解释皮乌肯斯尾矿库的生物地球化学演化。

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