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SPE 073

Regional Groundwater Quality Appraisal, Cold Lake-Beaver River Drainage Basin, Alberta

The Alberta Geological Survey (AGS) of the Alberta Energy and Utilities Board (EUB) has partnered with Alberta Environment (AENV) Northern Region to compile and analyze groundwater data in the Cold Lake-Beaver River Drainage Basin. The project ... Show Abstract

Lemay, T.G.  Parks, K.  Andriashek, L.D.  Michael, K.  Jean, G.M.  Stewart, S.A.  Kempin, E.  2005-02-01

SPE 074

Regional Groundwater Resource Appraisal, Cold Lake-Beaver River Drainage Basin, Alberta

Regional Groundwater Resource Appraisal, Cold Lake-Beaver River Drainage Basin, Alberta The Alberta Geological Survey (AGS) of the Alberta Energy and Utilities Board (EUB) has partnered with Alberta Environment (AENV) Northern Region to compile and ... Show Abstract

Parks, K.  Andriashek, L.D.  Michael, K.  Lemay, T.G.  Stewart, S.A.  Jean, G.M.  Kempin, E.  2005-02-01

GEO 2002-04

Arsenic Concentrations in Quaternary Drift and Quaternary-Tertiary Buried Channel Aquifers in the Athabasca Oil Sands (In Situ) Area, Alberta

The purpose of the sampling program was to obtain high-quality water samples that could be used to better define baseline groundwater chemistry in these geological units.Twenty-one water samples were collected from Quaternary intertill-intratill ... Show Abstract

Lemay, T.G.  2003-07-01

GEO 2002-08

Static Water Levels and Completion Details of Nested Piezometers in the Quaternary-Tertiary(?) Succession, Athabasca Oil Sands (In Situ) Area, Alberta

Abstract: NOTE: In October 2011, AGS staff noted and corrected an error in the naming of the piezometers. Text referring to piezometer WEPA 00-1-158 was corrected to now refer to the correct piezometer WEPA 00-3-158.In 2000, Alberta Geological Survey installed nine piezometers. The piezometers were completed within both Quaternary drift aquifers and a Quaternary-Tertiary buried channel aquifer. Water levels were measured within these piezometers. The results of these measurements indicate that, at all three sites, vertical hydraulic gradients are downwards. At one of the sites (WEPA 00-1), the calculated vertical gradients between three of the nested piezometers are small. This may indicate that the three stratigraphically distinct aquifers monitored by these piezometers may be part of a larger, vertically connected aquifer system, even though they are separated by intervening till packages. Place Keywords 73l 73m 74d 74e 83i 83o 83p 84a 84b 84g 84h athabasca oil sands area Theme Keywords athabasca oil sands in situ quaternary tertiary water water level

Lemay, T.G.  Jean, G.M.  2002-12-01