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根据非稳定流抽水试验资料计算含水层参数和分析含水层边界条件的方法已被广泛应用,便我们在江苏某矿区的水文地质工作中,发现有两个主要抽水孔的资料,既不能用稳定流理论解释,也难于用非稳定流的泰斯法或雅可布法解释。受美刊《地下水》1982年第1期Jenkins,D. 所写的“在线性流条件下裂隙岩石含水层试验分析理论”一文的启发,比较满意地解释了这两个孔的抽水试验资料,并加深和验证了对原矿区水文地质条件的认识。该矿区为一矽卡岩型矿床,矿体沿接触
The method of calculating aquifer parameters and analyzing the boundary conditions of aquifers based on unsteady flow pumping test data has been widely used so that we can find that there are two main pumping holes in the hydrogeological work of a mine in Jiangsu Province, Flow theory to explain, but also difficult to explain the non-steady flow Tess method or Jacob law. Inspired by Jenkins, D., “The Theory of Experimental Analysis of Fractured Rock Aquifers under a Linear Flow”, “Groundwater”, 1982, No. 1, 1982, the pumping test data of these two holes are satisfactorily explained. And deepen and verify the understanding of hydrogeological conditions in the original mining area. The mine is a skarn-type deposit with ore bodies in contact