摘要
为了研究柠条塔煤矿中央运输大巷掘进到112 m时,发生涌水并有H2S逸出的原因,通过对煤层煤质、地质构造、水文地质条件等的分析,探讨了H2S异常的成因。研究认为主要是通过煤层自燃、微生物硫酸盐还原作用和热化学成因所形成。地下水的流动和泄压最终导致H2S逸出。
In oredr to study the reason that was caused water inrushing and H2 S escaping when Ningtiaota coal mine central transport roadway heading to 112 m,based on the analysis of coal quality,geological structure and hydrogeological condition,the H2 S origin of anomaly is discussed. The research shows that it is mainly formed by the spontaneous combustion of coal seam,the effect of microbial sulfate reduction and the groundwater flow and pressure eventually lead to H2 S escape.
引文
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