高级检索

山底河流域煤矿酸性矿井水微生物群落结构特征

Structure characteristics of microbial community in acid mine drainage in Shandi River Basin

  • 摘要: 为了揭示不同氧化还原环境条件下酸性矿井水微生物群落结构特征及其与水环境相互作用关系,选取娘子关泉域内典型废弃煤矿区山底河流域,采集不同氧化还原环境的AMD水样,用于水化学同位素分析和微生物16S rRNA基因V4、V5区测序。水化学同位素分析得出AMD水化学特征主要受pH和围岩水岩作用影响,好氧和厌氧环境下AMD的pH与Eh呈负相关;缺氧厌氧环境下AMD的pH与 Fe3+、Eh呈负相关。AMD中Ca、Mg离子则主要来源于围岩和煤中方解石、白云石的溶解;K、Na主要来源于长石等硅酸岩在酸性条件下的溶解;\mathrmSO_4^2- 、Fe含量主要来源含煤地层中黄铁矿氧化;AMD的硫同位素演化特征为好氧环境下AMD的δ34S–\mathrmSO_4^2- 较低,缺氧厌氧环境下AMD的δ34S–\mathrmSO_4^2- 较高。山底流域AMD微生物多样性影响分析,得出pH越低,样品的细菌丰度和多样性越低;温度越高样品的细菌丰度和多样性越高。通过AMD的微生物群落与环境因子的相关性分析,得出柳沟AMD的优势菌属为FerrovumGallionellaFerritrophicum。庙沟露天矿AMD的优势菌属为FerrovumGallionellaAcidithiobacillus。榆林垴钻井AMD的优势菌属为FerrovumGallionella。山底河流域AMD的微生物群落受pH、温度和降水的影响较大。

     

    Abstract: In order to reveal the structural characteristics of microbial communities in acid mine drainage(AMD) under different redox environmental conditions and the interaction between microbial communities and groundwater environment, Select the typical abandoned coal mining area in the Shandi River basin of the Niangziguan Spring area, and collect AMD samples from different redox environments for Hydrochemical characteristics and isotope analysis and the high-throughput sequencing of the V4, V5 region of microbial 16S rRNA. The analysis of Hydrochemical characteristics and isotope indicates that the hydrochemical characteristics of AMD are mainly influenced by pH and surrounding rock. The analysis of hydrochemical isotopes shows that the hydrochemical characteristics of AMD are mainly influenced by pH and rock water interaction. Under aerobic and anaerobic environments, the pH of AMD is negatively correlated with Eh; The pH of AMD in anaerobic and hypoxic environments is negatively correlated with Fe3+and Eh.The Ca and Mg ions in AMD mainly come from the dissolution of calcite and dolomite in the surrounding rock and coal. The K and Na ions in AMD mainly come from the dissolution of silicate rocks such as feldspar under acidic conditions; The main source of \mathrmSO_4^2- and Fe content in AMD is the oxidation of pyrite in coal-bearing strata; The sulfur isotope evolution of AMD is characterized by lower δ34S–\mathrmSO_4^2- values in aerobic environments and higher δ34S–\mathrmSO_4^2- values in anaerobic and hypoxic environments. The analysis of the microbial diversity impact of AMD in the bottom of the mountain basin shows that the lower the pH, the lower the bacterial abundance and diversity of the sample; The higher the temperature, the higher the bacterial abundance and diversity of the sample. Through the correlation analysis between the microbial community and environmental factors of AMD, it was found that the dominant bacterial genera in the Liugou are Ferrovum, Gallionella and Ferritrophicum. The dominant genera of AMD in the Miaogou open-pit mine are Ferrovum, Gallionella and Acidithiobacillus. The dominant genera of AMD in Yulinnao drilling are Ferrovum and Gallionella. The microbial community of AMD in the Shandi River Basin is greatly affected by pH, temperature and precipitation.

     

/

返回文章
返回