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本文中所指的层状含水层是由几层透水性不同的岩层所组成的非均质含水层,而任何两个岩层的交界面都是水平的。计算在层状含水层中完整潜水井涌水量是水文地质计算中常遇到的问题。例如计算在层状含水层中作供水用的完整潜水井涌水量。又例如当用钻孔进行设在层状岩层上的建筑场地疏干时,为了决定所需钻孔数目和其分布位置必须事先精确地计算每
The layered aquifer referred to in this paper is a heterogeneous aquifer composed of several layers of rock with different water permeability. The interface between any two rock formations is horizontal. Calculating the total submerged well inflow in a layered aquifer is a problem often encountered in hydrogeological calculations. For example, calculate the amount of water infused from a complete submerged well used to supply water in a layered aquifer. As another example, when drilled for laying of a building site on a layered rock formation, in order to determine the required number of holes and their distribution locations, it must be accurately calculated beforehand