Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Hugh J. Abercrombie"'
Publikováno v:
Chemical Geology. 195:219-227
Coalbead methane is part of the non-conventional gas reservoirs and makes a significant contribution to gas production in some parts of the world. Initially, it was assumed that coalbed methane was of thermogenic origin, but most recent studies based
Publikováno v:
Hydrogeology Journal. 8:623-635
A three-dimensional, finite-element flow model was used to assess the hydrogeological effects of depressurizing coalbeds lying in the Weary Creek exploration block, Elk River valley, southeastern British Columbia, Canada. The simulation results permi
Publikováno v:
Hydrogeology Journal. 8:608-622
Discovery of high contents of methane gas in coals of the Mist Mountain Formation in the Elk River valley, southeastern British Columbia, Canada, has led to increased exploration activity for coal-seam gas (CSG). CSG production requires groundwater a
Publikováno v:
Canadian Journal of Earth Sciences. 31:489-504
The stratigraphic boundary separating the Mannville and the Colorado groups in Alberta, occupying incised valleys cut within the Upper Mannville strata, has previously been interpreted as an unconformity recording post-Mannville erosion followed by a
Autor:
Hugh J. Abercrombie
Publikováno v:
Applied Geochemistry. 6:495-508
Chemical and isotopic analyses of aqueous species in co-produced waters from cyclic steam bitumen recovery wells at the Leming pilot, Cold Lake, Alberta, Canada, show the dominant control of co-produced water chemistry to be mixing of waters of natur
Publikováno v:
Geochimica et Cosmochimica Acta. 54:165-171
Carbon dioxide, produced at low temperatures, is the dominant gaseous species evolved during steam-assisted thermal recovery of bitumen at the Tucker Lake pilot, Cold Lake, Alberta. Two possible sources for the produced CO2 are considered: pyrolysis
Publikováno v:
ACS Symposium Series ISBN: 9780841233287
Geochemical Transformations of Sedimentary Sulfur
Geochemical Transformations of Sedimentary Sulfur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::270efca59c7c7ad42987390aa8484612
https://doi.org/10.1021/bk-1995-0612.ch024
https://doi.org/10.1021/bk-1995-0612.ch024
Autor:
Ian Hutcheon, Hugh J. Abercrombie
Thermal recovery projects, in which steam-water mixtures are injected into oil-bearing rocks at high temperatures, provide a laboratory to study rock-water interactions. The temperature range of 80°-220°C is appropriate for diagenetic settings and,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98c5a37a851d2a6770af36dd31e7a1a9
https://doi.org/10.1306/m49520c10
https://doi.org/10.1306/m49520c10