Inherent and stress-dependent anisotropy of permeability for jointed rock masses
碩士 === 國立中央大學 === 應用地質研究所 === 94 === The fracture networks are major flow paths in jointed rock masses. Experiment results suggest that a marked difference exist between the permeabilities measured in the laboratory and in situ. The difference is due to the presence of faults, joints and other disco...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Others |
| Language: | zh-TW |
| Published: |
2006
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| Online Access: | http://ndltd.ncl.edu.tw/handle/zqj478 |