Water flow in a natural rock fracture as a function of stress and sample size
- 1 August 1985
- journal article
- Published by Elsevier in International Journal of Rock Mechanics and Mining Sciences
- Vol. 22 (4) , 251-261
- https://doi.org/10.1016/0148-9062(85)92952-3
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Fluid Flow Along Very Smooth Joints at Effective Pressures Up to 200 MegapascalsGeophysical Monograph Series, 2013
- Hydromechanical behavior of a deformable rock fracture subject to normal stressJournal of Geophysical Research, 1981
- Flow through fracturesWater Resources Research, 1981
- Validity of Cubic Law for fluid flow in a deformable rock fractureWater Resources Research, 1980
- Observations of a potential size effect in experimental determination of the hydraulic properties of fracturesWater Resources Research, 1979
- The permeability of whole and jointed Barre GraniteInternational Journal of Rock Mechanics and Mining Sciences, 1979
- A new model for analyzing the effect of fractures on compressibilityJournal of Geophysical Research, 1979
- Variation of whole and fractured porous rock permeability with confining pressureInternational Journal of Rock Mechanics and Mining Sciences, 1978
- Elastic and transport properties of an in situ jointed graniteInternational Journal of Rock Mechanics and Mining Sciences, 1977
- A Laboratory Study of the Effects of Confining Pressure on Fracture Flow and Storage Capacity in Carbonate RocksJournal of Petroleum Technology, 1975