徐州矿区奥灰岩溶水突出的原因与防治
THE RESOURCES AND CONTROL OF ORDOVICIAN KARST WATER BURSTING IN XUZHOU COAL MINING AREA
-
摘要: 徐州矿区开采深度大,水文地质条件复杂,水害严重。主要突出水源为奥陶系含水层。突水原因主要有:底板隐伏陷落柱或断层导水;底(顶)板含水层与奥灰含水层对接;顶板冒落裂隙带导通断层对盘的奥灰含水层;奥灰水通过基岩隐伏露头侧向补给矿井。其防治对策为:引进先进技术手段,探查分析奥灰岩溶水发育规律;分区隔离开采,完善防排水系统;注浆封堵突水通道;排供结合,综合利用。Abstract: In Xuzhou Coal Mining Area the groundwater hazard is serious due to the larger mining depth and complicated hydrogeological conditions.The causes of water bursting,which source is Ordovician(O) aquifer,are as follows:hidden collapse column in coal seam floor or the fault is transmissible for groundwater;the floor(roof) aquifer connects to O aquifer,fracture zone of coal seam roof conducts with O aquifte that is located in opposite side of the fault;O groundwater recharges the mine through buried outcrop of bedrock laterally.The measures of groundwater hazard control are as follows:the development regularity of O karst water should be explored by advance technique;mining by areas and perfecting drainage system;plugging water bursting points with grouting;combining drainage with water supply and synthetically utilizing water resources.