Groundwater development and electric and digital modelling of the Upper Carbonate aquifer, Metropolitan Winnipeg area
An extensive confined aquifer, currently pumped at a rate of 3 billion gallons per year, occurs in the fractured and jointed upper 100 feet of the thick Paleozoic carbonate rock sequence underlying metropolitan Winnipeg. The karstic bedrock surface, a controlling parameter of the groundwater flow...
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2012
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| Online Access: | http://hdl.handle.net/1993/5645 |