唐口煤矿断层构造带含导水性分析与探讨
韦荣律¹，王栋²，李彪¹
（1. 山东能源淄矿集团唐口煤业公司，山东 济宁 272000；2. 济宁市能源综合执法支队，山东 济宁 272000）
摘要： 唐口井田为一大地堑构造，边界断层较发育，井田内包含多个含水层、隔水层，地质构造及水文地质条件复
杂。依据井田的地质构造特征及水文地质情况，结合断层带的岩性特征、抽水试验成果、物探及井下实际揭露等资料对
断层构造带含导水性发育规律进行分析研究。结果表明，唐口井田断层带岩层富水性弱，但受采动影响，断层沟通局部
含水层富水区，或与富水性强的含水层对接，使断层可能导水，对生产造成一定的影响。最后针对煤矿的安全生产提出
了一系列的防治水措施。
关键词： 唐口煤矿；水文地质条件；断层；含导水性
中图分类号： TD163     文献标志码： A     文章编号： 2095-0802-(2022)08-0057-03
Water Conductivity of Fault Tectonic Zone in Tangkou Coal Mine
WEI Ronglv¹, WANG Dong², LI Biao¹
(1. Tangkou Coal Industry Company, Shandong Energy Zikuang Group, Jining 272000, Shandong, China;
2. Jining Energy Comprehensive Law Enforcement Detachment, Jining 272000, Shandong, China)
Abstract: Tangkou minefield is a graben structure with well-developed boundary faults. There are many aquifers and waterresisting
layers in the minefield, and the geological structure and hydrogeological conditions are complex. According to the
geological structure characteristics and hydrogeological conditions of the mining field, combined with the lithologic characteristics
of the fault zone, the results of pumping test, geophysical exploration and actual disclosure of underground, the development law of
water conductivity in the fault tectonic zone was analyzed and studied. The results show that the water-rich strata in the fault zone
of Tangkou minefield is weak, but due to the influence of mining, the fault communicates with the water-rich areas of local
aquifers, or connects with the aquifers with strong water-rich, so that the fault may conduct water, which has certain influence on
production. Finally, a series of water control measures were put forward for the safety production of the coal mine.

 Key words: Tangkou Coal Mine; hydrogeological conditions; fault; water conductivity