以城郊井田深部煤层底板典型泥岩为研究对象,测试其在3种不同溶液浸泡条件下的电导率变化规律;以典型砂岩为研究对象,测试其在3种不同溶液浸泡条件下的总溶解性固体物质量化数据,总结其矿化度变化规律,为探究典型岩石的水岩相互作用机理提供了有益依据。 Taking the typical mudstone of the deep coal seam floor in the suburbs of the suburb as the research object, the conductivity of the samples was tested under three different solution immersion conditions. The typical sandstone was taken as the test object to test its total dissolved solids under three kinds of solution immersion conditions Material quantitative data, summarizes the variation of mineralization degree, and provides a useful basis for exploring the mechanism of water-rock interaction of typical rocks.