摘要
本工作研制了单裂隙弥散渗透实验装置，在单裂隙实验装置上分别使用了含有１２５Ｉ－ 、１３４Ｃｓ＋ 连续液流进行了核素迁移实验，测定流出液中裂隙表面和岩块空间核素浓度分布。
A device of dispersion and permeability experiment single fractured granite was set up, with which the nuclide migration in the continuously flowing fluid containing I 125 and Cs 134 was examined, and the distribution of nuclide concentration in the flowing out fluid along the fracture surface and rock space was tested. The parameters of nuclide migration along fractured and porous granite ware given.
出处
《水文地质工程地质》
CAS
CSCD
1999年第6期45-47,51,共4页
Hydrogeology & Engineering Geology
