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L. Richards (1931)
Capillary conduction of liquids through porous mediumsPhysics, 1
F. Fayers, J. Sheldon (1962)
The use of a high-speed digital computer in the study of the hydrodynamics of geologic basinsJournal of Geophysical Research, 67
R. Everdingen (1963)
Groundwater flow-diagrams in sections with exaggerated vertical scale
J. Tóth (1963)
A Theoretical Analysis of Groundwater Flow in Small Drainage BasinsJournal of Geophysical Research, 68
Kirkham Kirkham (1958)
Seepage of steady rainfall through soils into drainsTrans. Am. Geophys. Union, 39
D. Kirkham (1958)
Seepage of steady rainfall through soil into drainsEos, Transactions American Geophysical Union, 39
D. Panov, Charles Stern (1963)
Formulas for the numerical solution of partial differential equations by the method of differences
S. Davis (1963)
Discussion of a paper by J. Tóth, ‘A theory of groundwater motion in small drainage basins in central Alberta, Canada’Journal of Geophysical Research, 68
Remson Remson, Appel Appel, Webster Webster (1965)
Ground‐water models solved by a digital computerJ. Hydraul. Div., Proc. Am. Soc. Civil Eng., 91
Meyboom Meyboom (1963)
Patterns of groundwater flow in the prairie profileNatl. Res. Council Canada, Proc. Hydrol. Symp. 3: Groundwater
Hubbert Hubbert (1940)
Theory of groundwater motionJ. Geol., 48
I. Remson, C. Appel, R.Alden Webster (1965)
Ground-Water Models Solved by Digital ComputerJournal of Hydraulic Engineering, 91
Reply to Davis ( 1963 ) re T 6 th ( 1962 )
J. Tóth (1962)
A theory of groundwater motion in small drainage basins in central Alberta, CanadaJournal of Geophysical Research, 67
A. Liakopoulos (1965)
Variation of the permeability tensor ellipsoid in homogeneous anisotropic soilsWater Resources Research, 1
R. Freeze, P. Witherspoon (1966)
THEORETICAL ANALYSIS OF REGIONAL GROUNDWATER FLOW..
J. Luthin, P. Day (1955)
Lateral Flow Above a Sloping Water Table 1Soil Science Society of America Journal, 19
M. Hubbert (1940)
The Theory of Ground-Water MotionThe Journal of Geology, 48
J. Tóth (1963)
Reply [to “Discussion of a paper by J. Tóth, ‘A theory of groundwater motion in small drainage basins in central Alberta, Canada’”]Journal of Geophysical Research, 68
Luthin Luthin, Day Day (1955)
Lateral flow above a sloping water‐tableSoil Sci. Soc. Am. Proc., 19
D. Young (1954)
Iterative methods for solving partial difference equations of elliptic typeTransactions of the American Mathematical Society, 76
It is possible to represent steady‐state regional groundwater flow in a three‐dimensional, nonhomogeneous, anisotropic basin by a mathematical model. The numerical finite‐difference approach can be used to solve the general case; the analytical separation of variables technique is restricted to two‐dimensional layered mediums. The numerical method is more versatile, mathematically simpler, and well suited to computer oriented methods of data storage. Computer results are in the form of plotted potential nets from which flow patterns can be constructed.
Water Resources Research – Wiley
Published: Dec 1, 1966
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