Fluid percolation through single fractures
Authors:
- 1 October 1988
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 15 (11) , 1247-1250
Abstract
Large deviations from "cubic‐law" dependence of laminar fluid flow through fractures on the apparent mechanical aperture of a fracture can be explained by assuming: 1) cubic‐law dependence of flow on the actual local aperture at the microscopic level; 2) conservation of rock volume when deforming the fracture; and 3) macroscopic flow properties are dominated by the critical neck (the smallest aperture along the path of highest aperture through the fracture).Keywords
This publication has 14 references indexed in Scilit:
- The Fractal Geometry of Flow Paths in Natural Fractures in Rock and the Approach to Percolation1989
- Fluid flow through rock joints: The effect of surface roughnessJournal of Geophysical Research, 1987
- Correlation between the surfaces of natural rock jointsGeophysical Research Letters, 1986
- Water flow in a natural rock fracture as a function of stress and sample sizeInternational Journal of Rock Mechanics and Mining Sciences, 1985
- Closure of random elastic surfaces in contactJournal of Geophysical Research, 1985
- The Fractal Geometry of NatureAmerican Journal of Physics, 1983
- Percolation and conductivity: A computer study. IPhysical Review B, 1974
- Percolation and conductivity: A computer study. IIPhysical Review B, 1974
- A percolation treatment of dc hopping conductionJournal of Non-Crystalline Solids, 1972
- Hopping Conductivity in Disordered SystemsPhysical Review B, 1971