论文部分内容阅读
《水力均衡法》是评价地下水资源的一种使用广泛的方法,它的基础是建立在对既定均衡区一定时间范围内地下水流入和流出各项均衡要素的详细研究上。如果对一个均衡区内的各项均衡要素能够取得比较可靠的数据,利用这种方法可以对地下水资源做出较为理想的评价。苏联水文地质学家斯巴卡拉诺维奇把这种方法简化之后,建立了预测矿坑涌水量的《水力均衡》方程。五十年代初斯巴卡拉诺维奇的这一方程引入我国,直至七十年代末期,我国出版的有关书刊中都相继引用了这一矿坑涌水量的预测方法。本文试从我国的气候条件、固体矿床的充水特征和矿山防排水设计的实际需要出发,拟定出预测矿坑涌水量的《水力均衡》方程与同行共议,敬希得到批评指正。
The Water Equilibrium Method, a widely used method of evaluating groundwater resources, is based on a detailed study of the various elements of the inflow and outflow of groundwater over a given period of time in a given equilibrium zone. If reliable data can be obtained for all the equilibrium elements in an equilibrium area, this method can make a more satisfactory assessment of groundwater resources. After this method was simplified by the Soviet hydrogeologist Spacca Norovic, a “hydraulic equilibrium” equation was established for predicting the amount of water in the mine. In the early 1950s, this equation of 斯巴卡拉诺维奇 introduced into our country, until the late seventies, the publications published in our country have cited the prediction method of the mine water inflow. Based on the climatic conditions in our country, the filling characteristics of solid mineral deposits and the actual needs of mine drainage and drainage design, this paper draw up a “hydraulic equilibrium” equation to predict the gushing capacity of mine and discuss with colleagues.