摘要
本文研究厂地质、水文地质和水文地球化学资料以后,把碴场区的水文地质条件概化为以碴场下渗的污水补给、地下径流排泄的水文地质模型,把含水介质简化为一组矿物集合体,把地下水和含水介质间的各种作用利用地球化学反应来描述。在此基础上,利用能量最低原理和质量守恒、电子守恒、电中性方程来构造线性规划数学模型,并用单纯形法求得水-岩之间的物流量。
Based on a liturature survey on geology, hydrogeology and hydrogeochemistry, this paper presents a hydrogeological model for the ground-water system at the dross-dumpping-ground area. It is considered that the groundwater-bearing medium is a mineral assemblage and the interactions between groundwater and groundwater-bearing medium are described as a series of geochemical reactions. On this basis, the principle of minimum energy and the equations of mass balance, electron balance and electric neutrality are applied to constructing a linear programming mathematical model and calculating the amount of mass transfer between water and rock with the simplex method.
出处
《地球化学》
CAS
CSCD
北大核心
1990年第3期270-276,共7页
Geochimica
