煤层顶板承压含水层涌水模式与疏放水钻孔优化设计

Mine water inflow modes and scientific design of drainage boreholes in roof confined aquifer of coal seam

针对煤层顶板承压含水层涌水模式不清的问题,从煤层回采过程中顶板含水层涌水的时空变化特征入手,提出顶板含水层涌水量由静态储存量和动态补给量构成,认为静态储存量主要受来压步距、顶板垮落和导水裂隙(合称冒裂)影响区含水层厚度、含水层给水度控制,动态补给量主要受冒裂影响区外围含水层厚度、渗透性流场中水力梯度和过水断面面积控制;根据导水裂隙波及含水层情况,将顶板含水层涌水模式划分为井底进水的触及井涌水、井壁及井底进水的非完整井涌水和井壁进水的完整井涌水3种模式,并基于地下水渗流理论给出不同涌水模式下动态补给水量计算公式;针对以往疏放水钻孔数量多及疏放水量大的问题,以实现工作面顶板含水层静态储存量疏放后动态补给量可控为目的,提出冒裂区高度控制钻孔深度、单孔水位影响半径控制钻孔布置间距、钻孔疏放水量稳定时间控制超前疏放时间的疏放水钻孔优化设计理念,对疏放水及疏放钻孔布置进行优化,形成系统的顶板含水层水疏放体系。研究结果丰富了煤层顶板含水层涌水量计算和控制方法,对顶板水害防控具有实际的指导意义。

Aiming at the uncertainty of mine water inflow mode, this paper analyzes the spatiotemporal variation characteristics of mine water inflow at first, and get a conclusion that the mine water is composed of static storage and dynamic recharge. And the static storage is mainly affected by weighting interval, the aquifer thickness of caving and fracture zone height and specific yield;the dynamic recharge is mainly affected by caving and fracture zone height and specific yield, hydraulic gradient in permeable flow field and discharge section area. According to the spatial relationships between water conducted fissure and roof aquifer of coal seam, the mine water inflow mode is classified into 3 types: partially penetrating well with water entering from well bottom, partially penetrating well with water entering from well bottom and wall, and completely penetrating well with water entering from well wall. And then the different calculation formulas of dynamic recharge for three mine water inflow modes are given based on groundwater seepage theory. For the large quantity drainage boreholes and excess quantity drainage, the optimal design concept of drainage borehole is proposed, which consists of caving and fracture zone height controlling boreholes depth, influence radius of single hole controlling borehole layout, and stable time of drainage controlling advanced drainage time, so as to optimize the layout of drainage water and drainage borehole, and establish the system of drainage of roof aquifers. The results offer an alternative for the scientific connotation of calculus formula and control methods for mine roof water inflow, which has practical guiding significance for prevention and control of mine roof water disaster.