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Kuiper, Logan K. (1978) The computational efficiency and taylor expansion derivation of approximating equations to the groundwater flow equation. Water Resources Research, 14 (6). 1171-1181 doi:10.1029/wr014i006p01171

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Reference TypeJournal (article/letter/editorial)
TitleThe computational efficiency and taylor expansion derivation of approximating equations to the groundwater flow equation
JournalWater Resources Research
AuthorsKuiper, Logan K.Author
Year1978 (December)Volume14
Issue6
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/wr014i006p01171Search in ResearchGate
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Mindat Ref. ID8204900Long-form Identifiermindat:1:5:8204900:9
GUID0
Full ReferenceKuiper, Logan K. (1978) The computational efficiency and taylor expansion derivation of approximating equations to the groundwater flow equation. Water Resources Research, 14 (6). 1171-1181 doi:10.1029/wr014i006p01171
Plain TextKuiper, Logan K. (1978) The computational efficiency and taylor expansion derivation of approximating equations to the groundwater flow equation. Water Resources Research, 14 (6). 1171-1181 doi:10.1029/wr014i006p01171
In(1978, December) Water Resources Research Vol. 14 (6) American Geophysical Union (AGU)

See Also

These are possibly similar items as determined by title/reference text matching only.

Kuiper, Logan K. (1983) A numerical procedure for the solution of the steady state variable density groundwater flow equation. Water Resources Research, 19 (1). 234-240 doi:10.1029/wr019i001p00234
Kuiper, L. K. (1973) Analytic solution of spatially discretized groundwater flow equations. Water Resources Research, 9 (4). 1094-1097 doi:10.1029/wr009i004p01094
Kuiper, Logan K. (1986) A Comparison of Several Methods for the Solution of the Inverse Problem in Two-Dimensional Steady State Groundwater Flow Modeling. Water Resources Research, 22 (5). 705-714 doi:10.1029/wr022i005p00705
Kuiper, L. K. (1981) A comparison of the incomplete cholesky-conjugate gradient method with the strongly implicit method as applied to the solution of two-dimensional groundwater flow equations. Water Resources Research, 17 (4). 1082-1086 doi:10.1029/wr017i004p01082
Kuiper, L. K. (1972) Groundwater flow in an inhomogeneous aquifer. Water Resources Research, 8 (3). 722-724 doi:10.1029/wr008i003p00722
Morel-Seytoux, Hubert J. (1978) Derivation of equations for variable rainfall infiltration. Water Resources Research, 14 (4). 561-568 doi:10.1029/wr014i004p00561
Nutbrown, D. A. (1975) Normal mode analysis of the linear equation of groundwater flow. Water Resources Research, 11 (6). 979-987 doi:10.1029/wr011i006p00979
Kuiper, Logan K. (1979) Comment on ‘A two-dimensional linearized view of one-dimensional unsaturated-saturated flow’ by John Cushman and Don Kirkham. Water Resources Research, 15 (3). 719-720 doi:10.1029/wr015i003p00719
Gureghian, A. B. (1978) Solutions of Boussinesq's Equation for seepage flow. Water Resources Research, 14 (2). 231-236 doi:10.1029/wr014i002p00231
Gray, William G. (1982) Derivation of vertically averaged equations describing multiphase flow in porous media. Water Resources Research, 18 (6). 1705-1712 doi:10.1029/wr018i006p01705
Gambolati, Giuseppe (1974) Reply [to “Comments on ‘Equation for one-dimensional vertical flow of groundwater’ by Giuseppe Gambolati”]. Water Resources Research, 10 (6). 1262 doi:10.1029/wr010i006p01262
 
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