摘要
从减小矿坑涌水量计算误差的角度出发 ,分析了厚弱含水层深部抽、排水时地下水的运动特征 ,提出了运用区域二维流和矿区地段三维流数值耦合模型计算涌水量 ,并对北氵名河铁矿坑下涌水量进行了重新计算 ,所得结果与实际相近 ,简化了运算程序。
To reduce the error in the calculation of underground waterinflow in mine, the kinematic characteristics of underground water in deep water pumping and draining from thick weakly water-carrying stratum are analysed and a numerical coupling model of 2-dimensional flow for area and 3-dimensional flow for mining district is proposed for waterinflow calculation. The underground waterinflow of Beiminghe Iron Mine is recalculated with the model, with the result close to the real value and the operation sequence simplified.
出处
《金属矿山》
CAS
北大核心
2004年第4期44-46,共3页
Metal Mine
关键词
矿坑涌水量
数值耦合
厚弱含水层
铁矿
Thick weakly water-carrying stratum, Underground waterinflow, Numerical coupling
