| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.879041 |
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| 003 | CaOODSP |
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| 005 | 20221107165416 |
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| 006 | m go d f |
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| 007 | cr |n||||||||| |
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| 008 | 190909s1969 onca |ob f00| 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cnp-- |
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| 086 | 1 |aM26-502/3E-PDF |
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| 100 | 1 |aFreeze, R. A., |eauthor. |
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| 245 | 10|aTheoretical analysis of regional groundwater flow / |cR.A. Freeze. |
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| 264 | 1|aOttawa : |bInland Waters Branch, Department of Energy, Mines and Resources, |c[1969] |
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| 264 | 4|c©1969 |
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| 300 | |a1 online resource (ix, 147 pages, 53 unnumbered pages) : |billustrations. |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aScientific series ; |vno. 3 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references (pages 120-122). |
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| 520 | 3 |a"A mathematical model representing steady-state regional groundwater flow in a three dimensional, non-homogeneous, anisotropic groundwater basin is developed. Two independent methods of solution are presented: the analytical separation of variables technique is used to solve the two-dimensional, three-layer case; the numerical finite-difference approach is used to solve the general case. The numerical method is more versatile, mathematically simpler, and well-suited to computer oriented methods of data storage. Computer programs have been written for both methods; the output consists of plotted potential nets from which flow patterns can be constructed"--Abstract. |
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| 692 | 07|2gccst|aGroundwater |
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| 692 | 07|2gccst|aMathematics |
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| 692 | 07|2gccst|aModelling |
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| 710 | 1 |aCanada. |bDepartment of Energy, Mines and Resources. |
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| 710 | 1 |aCanada. |bInland Waters Branch. |
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| 830 | #0|aScientific series (Canada. Inland Waters Branch)|vno. 3.|w(CaOODSP)9.853476 |
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| 856 | 40|qPDF|s8.82 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/M26-502-3-eng.pdf |
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