Hydrologic Mechanisms Governing Fluid Flow in a Partially Saturated, Fractured, Porous Medium
- 1 December 1985
- journal article
- Published by American Geophysical Union (AGU) in Water Resources Research
- Vol. 21 (12) , 1861-1874
- https://doi.org/10.1029/wr021i012p01861
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- A case study on infiltration into dry clay soil I. Morphological observationsPublished by Elsevier ,2003
- Numerical calculation of saturated‐unsaturated infiltration in a cracked soilWater Resources Research, 1985
- Role of Roughness and Edges During Imbibition in Square CapillariesPublished by Society of Petroleum Engineers (SPE) ,1984
- Macropores and water flow in soilsWater Resources Research, 1982
- WATER FLOW IN SOIL MACROPORES II. A COMBINED FLOW MODELEuropean Journal of Soil Science, 1981
- A Simulation Model for Predicting Infiltration into Cracked Clay SoilSoil Science Society of America Journal, 1980
- A Numerical Study of the Effects of Noncapillary‐Sized Pores Upon InfiltrationSoil Science Society of America Journal, 1979
- Numerical model for saturated‐unsaturated flow in deformable porous media: 2. The algorithmWater Resources Research, 1978
- A new model for predicting the hydraulic conductivity of unsaturated porous mediaWater Resources Research, 1976
- Summary of tectonic and structural evidence for stress orientation at the Nevada Test SitePublished by US Geological Survey ,1974