A continuum model for water movement in an unsaturated fractured rock mass
- 1 March 1988
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 24 (3), 416-430
- https://doi.org/10.1029/wr024i003p00416
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- Hydrologic Mechanisms Governing Fluid Flow in a Partially Saturated, Fractured, Porous MediumWater Resources Research, 1985
- A conceptual model of deep unsaturated zones with negligible rechargeWater Resources Research, 1984
- Double‐Porosity Models for a Fissured Groundwater Reservoir With Fracture SkinWater Resources Research, 1984
- An Effective Stress Principle for Partially Saturated Granular MediaPublished by Elsevier BV ,1983
- A Closed-form Equation for Predicting the Hydraulic Conductivity of Unsaturated SoilsSoil Science Society of America Journal, 1980
- Flow in fractured porous mediaWater Resources Research, 1977
- A new model for predicting the hydraulic conductivity of unsaturated porous mediaWater Resources Research, 1976
- The frequency and apertures of fractures in rockInternational Journal of Rock Mechanics and Mining Sciences, 1970
- CAPILLARY CONDUCTION OF LIQUIDS THROUGH POROUS MEDIUMSPhysics, 1931