地下水多组分反应溶质迁移模型的研究进展  

Advances in study on transport models of multicomponent reacting solutes in groundwater

作　　者：钱天伟[1] 李书绅[1] 武贵宾[1] 

机构地区：[1]中国辐射防护研究院,山西太原030006

出　　处：《水科学进展》2002年第1期116-121,共6页Advances in Water Science

基　　金：中国辐射防护研究院 (CIRP) ;日本原子力研究所 (JEARI)的国际合作项目资助

摘　　要：描述多孔介质中地下水中溶质迁移行为的模型有两类 :一为溶质的多组分水化学平衡模式 ;二为溶质的水动力迁移模式 (对流 -弥散模式 )。对这两类模型进行了回顾 ,着重介绍了近年来两者耦合模型的发展 ,提出了尚需解决的问题。The model describing migration behavior of groundwater solutes in porous media can be divided into two parts: the first is the multicomponent aquatic chemistry model, and the second is the hydraulic transport model (advection dispersion model) This paper presents a short review about two kinds of models aforementioned, mainly introducing the development of transport model of reacting solutes in recent years. In the meantime, some existing problems of the model are also suggested

关 键 词：多组分 地下水 反应溶质 耦合模型 迁移模型 

分 类 号：P641.2[天文地球—地质矿产勘探]