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| 02085nam 2200325za 4500 |
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001 | 9.862911 |
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003 | CaOODSP |
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005 | 20221107161141 |
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007 | cr ||||||||||| |
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008 | 181009s1972 oncb ob f000 0 eng d |
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040 | |aCaOODSP|beng |
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041 | |aeng|bfre |
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043 | |an-cn-sn |
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086 | 1 |aEn36-515/59E-PDF |
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100 | 1 |aVan Everdingen, R. O. |
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245 | 10|aObserved changes in groundwater regime caused the creation of Lake Diefenbaker, Saskatchewan |h[electronic resource] / |cR.O. Van Everdingen. |
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260 | |aOttawa : |bInland Waters Branch, Dept. of the Environment, |c1972. |
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300 | |avi, 65, [3] p. : |bchart, ill., maps. |
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490 | 1 |aTechnical bulletin ; |vno. 59 |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references (p. 23). |
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520 | 3 |a"Measurements between 1964 and 1971 of piezometric levels in 35 piezometers installed in 9 groups in a multiple aquifer system and in unconsolidated sediments in a section across the valley of the South Saskatchewan River near Riverhurst, Saskatchewan, have revealed increased piezometric pressures as a result of the creation of Lake Diefenbaker. The increases in pressure, which vary with the water level in the reservoir, reflect a hydraulic connection between the aquifers and the reservoir, and not a classical loading effect. The stability of the area immediately downstream from the dam may have been adversely affected by these pressure increases. Groundwater discharge rates have been reduced significantly, and some loss of water from the reservoir appears to take place"--Abstract, p. vi. |
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546 | |aIncludes abstract in French. |
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693 | 4|aGroundwater flow |
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693 | 4|aSaskatchewan--Diefenbaker, Lake |
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710 | 1 |aCanada. |bEnvironment Canada. |
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710 | 1 |aCanada. |bInland Waters Branch. |
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830 | #0|aTechnical bulletin (Canada. Inland Waters Branch)|vno. 59.|w(CaOODSP)9.861115 |
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856 | 40|qPDF|s4.97 MB|uhttps://publications.gc.ca/collections/collection_2018/eccc/En36-515-59-eng.pdf |
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