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REP 01

First Annual Report on the Mineral Resources of Alberta

First Annual Report on the Mineral Resources of Alberta Much has yet to be done, and considerable field investigation must be carried out before the extent of the mineral resources of the Province of Alberta can be determined.The details given in ... Show Abstract

Allan, J.A.  1920-02-17

SPE 092

Subsurface Characterization of the Edmonton-Area Acid-Gas Injection Operations

Abstract: Injection of acid gas in the Edmonton region takes place at five sites into three different stratigraphic intervals. Acid gas dissolved in water in the Redwater oil field, and the resulting weak acidic solution ("sour" water) is injected into the depleted Leduc Formation Redwater reef trough 47 alternating wells. Dry acid gas is injected at four other sites. At Golden Spike and Watelet, the acid gas is injected into deep Devonian carbonate aquifers (Beaverhill Lake Group and Cooking Lake Formation, respectively). At Acheson and Strathfield, the acid gas is injected into depleted gas reservoirs in the Cretaceous Lower Mannville Group. Acheson, operating since 1990, is actually the oldest acid-gas injection operation in Canada and the world. By the end of 2003, more than 200 kt of acid gas have been injected into deep geological formations in the Edmonton region. If only the natural setting is considered, including geology and flow of formation waters, the basin and local-scale hydrogeological analyses indicate that injecting acid gas into these deep geological units in the Edmonton region is basically a safe operation with no potential for acid-gas migration to shallower strata, potable groundwater and the surface. At Redwater, the acid gas is already dissolved in water and it will dissolve further in the formation water, with no possibility for migration or leakage, being contained in the Redwater reef. At Golden Spike, the acid gas injected into an isolated, confined reefal carbonate in the Beaverhill Lake Group is contained by the surrounding and overlying low-permeability argillaceous limestone at the top of the Beaverhill Lake Group. At Watelet, upward migration is impeded by the overlying thick and tight shales of the Ireton Formation. While the acid-gas plume may migrate updip, it will dissolve in formation water long before it may reach the sub-Cretaceous unconformity. Even there, thick overlying Cretaceous shales will impede any upward migration. At Strathfield and Acheson, the acid gas will be contained within the gas reservoir that is the respective injection target. Upward migration is not possible, as a result of thick and tight overlying shales of the Clearwater Formation and its equivalents. Lateral migration within the gas reservoir has been recorded in 2003 at Acheson, where, after 13 years of injection, CO2 has been detected at an offset producing well at 3625 m distance in the same gas pool. However, migration within the same unit, particularly in a gas reservoir, is expected and its occurrence should not come as a surprise.The entire stratigraphic interval from the Beaverhill Lake Group to the Lower Mannville Group is overlain by thick shales of the Colorado Group and Lea Park Formation. There are many barriers to acid-gas migration from an injection zone into other strata, and the flow process, if it will ever happen, would take an extremely long time on a geological time scale. Any acid-gas plume would disperse and dissolve in formation water during flow on such large time and spatial scales.There is no potential for acid-gas leakage through fractures. However, the possibility for upward leakage of acid gas exists along wells that were improperly completed and/or abandoned, or along wells whose cement and/or tubing have degraded or may degrade in the future as a result of chemical reactions with formation brine and/or acid gas. A review of the status and age of wells that penetrate the respective injection unit at each site shows that most wells were drilled in the 1950s and 1960s, and that the majority of wells are abandoned. Although no leakage has been detected and reported, the potential for this occurring in the future should be considered. Place Keywords 83a 83g 83h 83i alberta canada edmonton Theme Keywords acid gas geology hydrogeology injection lithology mannville group stratigraphy

Bachu, S.  Buschkuehle, B.E.  Haug, K.  Michael, K.  2008-04-14

MAP 600

Bedrock Geology of Alberta

The geology of the Rocky Mountains and the Rocky Mountain Foothills is also the product of compilation with rare instances of new geological interpretation (e.g., the interpretation of bedrock geology beneath drift-filled valleys). The Cretaceous ... Show Abstract

Prior, G.J.  Hathway, B.  Glombick, P.M.  Pana, D.I.  Banks, C.J.  Hay, D.C.  Schneider, C.L.  Grobe, M.  Elgr, R.  Weiss, J.A.  2013-06-17

ESN 1980-A

Potential industrial clays of Alberta : a preliminary assessment, Part II

From the same area, samples of Kaskapau Formation dry well, firing range is moderate to long, and the milk chocolate brown colour could be acceptable in "earth colour" pottery or structural clay products. A sample from the Bearpaw Formation in the ... Show Abstract

Scafe, D.W.  1980-01-01

ECO 3

Alberta clays and shales : summary of ceramic properties

Ceramic test data for more than 200 deposits of clays and shales in Alberta resulted largely from early investigations of the Federal Department of Mines (1912-15, 1932) supplemented by more recent work of Alberta Research ... Show Abstract

Hamilton, W.N.  Babet, P.H.  1975-03-01

ECO 4

Limestone resources of Alberta

Seven areas in Alberta, close to transportation facilities, were studied to determine quality and reserves of high-calcium limestone.Three formational units in the foothills and mountain regions are of importance. Formerly a cement plant operated ... Show Abstract

Holter, M.E.  1976-01-01

ECO 2

Alberta Bentonites

Low yields, high grit content, or thick overburden reduce the desirability of other deposits.The paucity of glass shards and the mineralogy of the sand and silt fractions suggest rhyodacite as the composition of the parent volcanic ash for each ... Show Abstract

Scafe, D.W.  1975-01-01

ECO 5

Bromide, iodide and boron in Alberta formation waters

Bromide contents up to 2786 mg/L were found in high calcium and magnesium brines associated with evaporites in the Upper Devonian Beaverhill Lake Formation and Middle Devonian Elk Point Group. The most extensive regions of high-iodide formation ... Show Abstract

Hitchon, B.  Levinson, A.A.  Horn, M.K.  1977-01-01

MAP 602

Bedrock Topography of Alberta, Canada

Bedrock Topography of Alberta, Canada Explanatory notes, references, and data sources appear on a supplementary page to accompany the map. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d 74e 74l 74m 82g 82h 82i 82j 82n 82o 82p 83a 83b 83c 83d 83e ... Show Abstract

MacCormack, K.E.  Atkinson, N.  Lyster, S.  2015-05-12

ECO 7

The ceramic potential of Alberta clays and shales

Many geographical areas and geological formations were missed when the ceramic suitability of materials was studied early this century. Geological formations that are useful for the production of structural clay products or pottery are Pleistocene ... Show Abstract

Scafe, D.W.  1982-01-01

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