摘要
研究了在饱和水流条件下，花岗岩单裂隙中核素迁移的连续注入数学模型，给出了裂隙中和岩块中核素浓度的解析解，并结合裂隙流出水样实验数据分析了影响核素迁移的主要参数。
The mathematical model of radionuclide transport in the saturated fractured porous granite is obtained,and the analytical solution of concentration distribution in the contiuous steay state in both fracture and rock matrix is also obtained for Dirichlet boundary conditions. The main effect of the transport of radionuclide in single fracture channel is described.
出处
《核化学与放射化学》
CAS
CSCD
北大核心
1998年第4期221-227,共7页
Journal of Nuclear and Radiochemistry
