多含水层稳定流非干扰多孔混合井流理论及示踪测井方法

The multi well hybrid flow theory and tracer logging method in multi layered aquifer non disturbance steady flow

本文提出了一种多含水层稳定流非干扰混合多孔井流理论，研究了在不抽水（或不注水）条件下，通过测定多含水层中各层的垂向流速、流向、渗透流速等求解各含水层的渗透系数、静水头、降深与流量的关系等水文地质参数的一种方法．该方法完全是在天然流场下进行渗流场的测试。

A new multi well hybrid flow theory in the multi layered aquifer non disturbance steady flow is introduced in this article.According to this theory the permeability coefficient,hydrostatic head and flow rate graph of each aquifer can be found out by measuring the direction and velocity of vertical flow and permeability rate etc.without pumping or injecting.With this theory and method the permeability in the flow field can be determined and more information about hydrogeology can be obtained without pumping.