Abstract
Hydrogen sulfide (H2S) is one of the important factors that control safety in coal mines because it could cause fatalities and could contribute to serious health problems. Based on the widely accepted genesis models of BSR, TSR, TDS and magmatic activity that may occur in coal mines, the formation, preservation migration and enrichment of hydrogen sulfide are closely related to the geological conditions of the coal seams. Analysis of H2S occurrences in a few typical coal basins indicates that the major geological conditions are sedimentary environments, regional tectonic characteristics and the characteristics of the surrounding strata. Others factors include coal seam porosity, groundwater activities, sulfate content in groundwater, depth and cover strata of the coal seams and magmatic intrusion.
Cite
CITATION STYLE
Deng, Q., Wang, Q., Liu, M., & Zhao, F. (2014). Geological Factors Controlling H2S in Coal Seams. In Mine Planning and Equipment Selection (pp. 619–627). Springer International Publishing. https://doi.org/10.1007/978-3-319-02678-7_59
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