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pro vyhledávání: '"鄭允嘉"'
Autor:
Yun-Chia Cheng, 鄭允嘉
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, j
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, j
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/zqj478
