A two-dimensional finite-element solution scheme for the saturated-unsaturated flow with applications to flow through ditch-drained soils
- 1 January 1981
- journal article
- research article
- Published by Elsevier in Journal of Hydrology
- Vol. 50 (1-3) , 333-353
- https://doi.org/10.1016/0022-1694(81)90077-9
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Finite element method for subsurface hydrology using a mixed explicit-implicit schemeWater Resources Research, 1978
- Coupled saturated-unsaturated transient flow in porous media: Experimental and numeric modelWater Resources Research, 1975
- The calculation of steady-state water-table heights in drained soils by means of the finite-element methodJournal of Hydrology, 1975
- Equation for one‐dimensional vertical flow of groundwater: 1. The Rigorous TheoryWater Resources Research, 1973
- Functional coefficients in the analysis of groundwater flowWater Resources Research, 1973
- Three‐Dimensional, Transient, Saturated‐Unsaturated Flow in a Groundwater BasinWater Resources Research, 1971
- Curved, isoparametric, “quadrilateral” elements for finite element analysisInternational Journal of Solids and Structures, 1968
- SOME FACTORS DETERMINING WATER-TABLE HEIGHTS IN DRAINED HOMOGENEOUS SOILSEuropean Journal of Soil Science, 1958
- THE WATER TABLE, EQUIPOTENTIALS, AND STREAMLINES IN DRAINED LAND: IIISoil Science, 1945
- CAPILLARY CONDUCTION OF LIQUIDS THROUGH POROUS MEDIUMSJournal of Applied Physics, 1931