基于矿井突水反演计算水文地质参数方法研究
Study on method of mine water inrush for inverse calculation of hydrogeological parameters
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摘要: 为了准确分析矿井突水原因并进行水文地质条件研究,将矿井突水事故视为井下放水试验。通过综合利用水文地质钻探、物探及矿井水文监测系统等手段,提出了一种地下水原始流场恢复技术,并利用此技术还原了柠条塔煤矿2-2煤上覆直罗组风化基岩含水层地下水初始流场状态,并利用矿井突水监测数据反演计算出该含水层的水文地质参数。通过2个地面钻孔抽水试验获取的含水层渗透系数分别为2.13、2.15 m/d,而利用突水反演计算的含水层渗透系数为6.88 m/d;2个地面钻孔抽水试验获取的影响半径分别是106、89 m,而利用突水反演计算的影响半径为1 941 m。结果表明,利用地面抽水试验获取的水文地质参数较利用突水反演计算的水文地质参数明显偏小。Abstract: In order to accurately analyze the cause of the mine water inrush occurred and study on the hydrogeological conditions,a mine water inrush accident was Co nsidered as a mine water drainage test. With the comprehensive application of the hydrogeological drilling exploration,geophysical exploration,mine hydrology monitoring a nd measuring system and other means,a recovery technology of the underground water original flow field was provided. The technology was applied to restore the undergr ound water initial flow field status of the aquifer in weathered bedrock aquifer of Zhiluo Formation in overburden strata above No. 2-2seam of Ningtiaota Mine,and the mine water inrush monitoring and measuring data were applied to the inverse calculation on the hydrogeological parameters of the aquifer. With the water pumping tests of the t wo boreholes at the surface ground,the permeability cofficients of the aquifer obtained were 2. 13 and 2. 15 m 1 d individually. With the inverse calculation of the mine wat er inrush,the permeability coefficients of the aquifer obtained was 6.88 m 1 d. The influence radius from the two borehole pumping test was 106 and 89 m individually. The i nfluence radius obtained with the mine water inrush inverse calculation was 1 941 m. The results showed that the hydrogeological parameters from the mien water inrush i nverse calculation would be higher than hydrogeological parameters from the surface ground water pumping test and the data would be more accurate and reliable.