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From Atmosphere to Basement: Development of a Framework for Groundwater Assessment in CanadaCanadian Journal of Earth Sciences
Evidence of discharging saline formation water to the Athabasca River in the oil sands mining region, northern Alberta2013 •
This paper summarizes various lines of evidence, including new geophysical and geochemical surveys indicating the discharge of naturally occurring saline formation water from Cretaceous and Devonian formations to the Athabasca River downstream of Fort McMurray — an active oil sands extraction area. The following features are indicative of saline water discharge: (i) the hydrogeological setting of the reach which is situated near the western, up-dip, and subcropping, edge of the Western Canada Sedimentary Basin; (ii) springs and seepage along area rivers and tributaries that have been observed and reported in previous studies; and (iii) a significant increase in dissolved solids in the river, particularly chloride, occurring in a downstream direction from Fort McMurray. Further evidence of the saline groundwater discharge was obtained from electromagnetic surveys conducted along a 125 km reach from the Clearwater River to the Firebag River. This technique was used to map the distribu...
Hydrological Processes
A hydrologic assessment of a saline-spring fen in the Athabasca oil sands region, Alberta, Canada - a potential analogue for oil sands reclamation2015 •
2008 •
Hydrogeology Journal
Geostatistical mapping of leakance in a regional aquitard, Oak Ridges Moraine area, Ontario, Canada2001 •
Water Resources Management
Quantitative Assessment of Regional Rock Aquifers, South-Western Quebec, Canada2006 •
The population of the St. Lawrence Lowlands platform in south-western Quebec, Canada, is heavily dependent on groundwater. The present study summarizes the quantity, quality and sustainability estimations of the groundwater resources found mainly in sedimentary rock aquifers. Results show that the regional groundwater flow in the considered domain of 1,500 km2 is 97.7 Mm3/y with: 86.6% infiltration from precipitation, 9.6% inflow from neighboring aquifers, and 3.8% induced recharge. The regional sustainability is defined with simulated drawdowns from uniform withdrawal scenarios. The current withdrawal rate of 18 Mm3/y results in median drawdown of 0.6 m, compared to pre-development conditions. This drawdown is situated well in the sustainable range, an indication that regional aquifers are not overexploited. Hypothetical pumping rate of 24 Mm3/y resulting in an average drawdown of 2.2 m is estimated as sustainable limit. Increasing exploitation from 24 to 51 Mm3/y would need tight control and planning. Pumping rates beyond 51 Mm3/y are judged not sustainable as regional drawdowns become high, ∼8 m. The water levels in recharge areas are the most sensitive to groundwater extraction. Combining drawdown maps, groundwater quality zones, and aquifer vulnerability to surface contamination delineated the areas most suitable for future groundwater developments.
Uluslararası Siyaset Dergisi / US Journal
ERMENİ KAMU DİPLOMASİSİNDE TÜRK KARŞITLIĞIPensar Iberoamérica, revista de cultura
Cultura, Economía y derecho, tres conceptos implicados”2002 •
2014 •
Türk hijiyen ve deneysel biyoloji dergisi
Increased Mean Platelet Volume, Red Blood Cell Distribution Width and Platelet/ Red Blood Cell Distribution Width in Patients With Hepatitis B2019 •
Revista Brasileira de Cancerologia
Anorexia: um Desafio Alimentar em Cuidados Paliativos2019 •
Infection Control and Hospital Epidemiology
Impact of coronavirus disease 2019 (COVID-19) pre-test probability on positive predictive value of high cycle threshold severe acute respiratory coronavirus virus 2 (SARS-CoV-2) real-time reverse transcription polymerase chain reaction (RT-PCR) test results2021 •
Applied Business and Economics Journal
Technological Advancements and Their Impact on Organisational Information Security2024 •