Laboratory measurement of capillary pressure‐saturation relationships in a rock fracture
- 1 April 1994
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 30 (4) , 865-878
- https://doi.org/10.1029/93wr03451
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- Leakage of dense, nonaqueous phase liquids from waste impoundments constructed in fractured rock and clay: theory and case historyCanadian Geotechnical Journal, 1992
- The Behavior of Dense, Nonaqueous Phase Liquids in Fractured Clay and RockGroundwater, 1991
- Groundwater contamination: pump-and-treat remediationEnvironmental Science & Technology, 1989
- A continuum model for water movement in an unsaturated fractured rock massWater Resources Research, 1988
- Channel model of flow through fractured mediaWater Resources Research, 1987
- Correlation between the surfaces of natural rock jointsGeophysical Research Letters, 1986
- Laboratory Studies of Gas Flow Through a Single Natural FractureWater Resources Research, 1986
- A Closed‐form Equation for Predicting the Hydraulic Conductivity of Unsaturated SoilsSoil Science Society of America Journal, 1980
- A new model for predicting the hydraulic conductivity of unsaturated porous mediaWater Resources Research, 1976