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坑道涌水的量和动态,多半不仅决定于地质构造和水文地质条件,正如舍戈列夫早在1948年指出的,同样也决定于矿区的地形特点。以后开采矿床的实践查明必须详细弄清这些情况。根据地表的地形矿床可分为:(工)在分水岭和地形纵横交错的山区中的矿床;(2)在分水岭斜坡上的矿床;(3)在河谷中而非直接邻近地表水流的矿床;我们较详细地来研究一下这些问题。1.对分布在分水岭上和山区高地上的矿床来说,
The volume and dynamics of the gushing water are mostly determined not only by geological structure and hydrogeological conditions, but also by the topographic features of the mining area, as pointed out by Chegoriev in 1948. The practice of prospecting the future deposits identified these conditions in detail. According to the topography of the surface deposits can be divided into: (workers) in the mountains and watersheds criss-cross the topography of deposits; (2) in the watershed slope deposits; (3) in the valley rather than directly adjacent surface water deposits; Study these questions in more detail. 1. For deposits distributed over watersheds and mountainous heights,