深部采区复杂含水层顶板综合富水性研究

    Study on comprehensive water-rich roof of complex aquifer in deep mining area

    • 摘要: 煤炭是我国最主要的能源。华北型煤田占我国煤田资源总量的60%,多数采区已进入深部开采阶段,面临着顶板含水层富水性分布规律不清晰等诸多问题。本次研究基于采区的地质与水文地质情况,选择了典型华北型煤田—田陈井田七一采区3煤上覆含水层作为研究对象,将含水介质的厚度乘以一个折算系数,并考虑砂岩含量、砂泥组合层数等因素,构建“岩性发育影响指数”(Lithology Influencing Index,简称LII),对含水层的富水性进行定量评价,为煤矿水害的防治提供地质保障。

       

      Abstract: Coal is the main energy source in China. The North China type coalfields account for 60% of China's total coalfield resources, and most mining areas have entered the deep mining stage, facing many problems such as unclear distribution patterns of water abundance in roof aquifers. Based on the geological and hydrogeological conditions of the mining area, this study selected the typical North China type coal field - Tianchen Well Tianqi No. 1 mining area 3 coal overlying aquifer as the research object. The thickness of the water-bearing medium was multiplied by a conversion coefficient, and factors such as sandstone content and sand mud combination layers were considered to construct the "Lithology Influencing Index" (LII), which quantitatively evaluates the water richness of the aquifer, Provide geological support for the prevention and control of coal mine water hazards.

       

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