Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geoscience, Hubei, 430074, Wuhan, China.
School of Earth Resources, China University of Geoscience, Hubei, 430074, Wuhan, China.
Sci Rep. 2021 Mar 11;11(1):5712. doi: 10.1038/s41598-021-85263-w.
Abnormal HS concentration in coal mine gas is a serious threat to normal mining activities, which has caused serious loss of life and property in many coal mines. This study explores the genesis and influencing factors of abnormal HS concentration in coal mine gas, taking the Xishan coal mine in the Fukang mining area as a case study. The HS formation by bacterial sulfate reduction (BSR) is simulated with a bacterial culture experiment and that by thermochemical sulfate reduction (TSR) is simulated with a thermal reduction experiment. The potential for a magmatic genesis is assessed using data regarding the tectonic evolution and history of magma intrusion in the study area. The factors influencing HS formation and enrichment are then analyzed by a comprehensive consideration of the characteristics of coal, the gas composition, the coal seam groundwater geochemistry and other geological factors in the study area. The results show that the study area meets the necessary conditions for the BSR process to operate and that there is widespread BSR derived HS. TSR genesis HS mainly forms in coal fire areas and their vicinity, while there is little contribution from magmatically formed HS. The concentration of HS is negatively correlated with the buried depth of the coal seam, the concentrations of CH, N and CO, and the ash yield; and it is positively correlated with the volatiles yield and total sulfur content. In addition, in areas with abnormally high HS concentration, the concentration of SO is obviously lower, HCO + CO concentration is higher, and the HCO/SO value is larger than that in non-anomalous areas. Geologically, HS enrichment is found to be controlled by lithology, tectonism, and hydrogeological conditions. Moreover, the results of predictive modeling show that areas prone to abnormal HS concentration are generally spatially correlated with coal fire areas. In this study, the genetic types of HS and the factors controlling their formation and retention are discussed, producing research results that have guiding significance for the prediction and prevention of the coal mine disasters that arises from abnormal HS concentration.
煤矿瓦斯中异常高浓度的 HS 是对正常采矿活动的严重威胁,在许多煤矿造成了严重的生命和财产损失。本研究以阜康矿区西山煤矿为例,探讨了煤矿瓦斯中异常高浓度 HS 的成因及其影响因素。通过细菌硫酸盐还原(BSR)的细菌培养实验模拟 HS 的形成,通过热化学硫酸盐还原(TSR)的热还原实验模拟 HS 的形成。利用研究区构造演化和岩浆侵入史的数据评估岩浆成因的可能性。然后,通过综合考虑研究区煤的特征、气体组成、煤层地下水地球化学和其他地质因素,分析了 HS 形成和富集的影响因素。结果表明,研究区满足 BSR 过程运行的必要条件,且存在广泛的由 BSR 衍生的 HS。TSR 成因 HS 主要在煤火区及其附近形成,而岩浆成因 HS 的贡献较小。HS 浓度与煤层埋深、CH、N 和 CO 浓度、灰分产率呈负相关,与挥发分产率和总硫含量呈正相关。此外,在 HS 浓度异常高的区域,SO 的浓度明显较低,HCO+CO 的浓度较高,HCO/SO 的值大于非异常区域。从地质角度看,HS 的富集受岩性、构造和水文地质条件的控制。此外,预测模型的结果表明,异常 HS 浓度易发生区域与煤火区在空间上具有相关性。本研究讨论了 HS 的成因类型以及控制其形成和保留的因素,为预测和预防由异常 HS 浓度引起的煤矿灾害提供了具有指导意义的研究结果。