Groundwater flow characterization in the vicinity of the underground caverns in fractured rock masses by numerical modeling

被引:12
作者
Yang, HS
Kang, JG [1 ]
Kim, KS
Kim, CS
机构
[1] Chonnam Natl Univ, Dept Geosyst Engn, Kwangju 500757, South Korea
[2] Korea Atom Energy Res Inst, Taejon 305353, South Korea
关键词
3D fractured media; anisotropic hydraulic conductivitiy; DFN model; CPM model; groundwater inflows;
D O I
10.1007/BF02910476
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Groundwater inflow into the caverns constructed in fractured bedrock was simulated by numerical modeling: NAP-SAC (DFN, discrete fracture network model) and NAMMU (CPM continuous porous media model), which is a finite-element software package for groundwater flow in 3D fractured media develop by AEA Technology, UK. The input parameters for modeling are based on surface fracture survey, core logging and single hole hydraulic test data. In order to predict the groundwater inflow as accurately as possible, the anisotropic hydraulic conductivity was considered. The anisotropic hydraulic conductivities were calculated from the fracture network properties and the in-situ fracture data. With a minor adjustment during model calibration, the numerical modeling is able to reasonably reproduce groundwater inflows into the cavern as well as the travel lengths and the surface arrival times through the flow paths.
引用
收藏
页码:401 / 413
页数:13
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