| 000 | 01913nab a2200229 4500 | ||
|---|---|---|---|
| 005 | 20260520000318.0 | ||
| 008 | 260224s2014 xxu ing | ||
| 041 | _aInglés | ||
| 245 | 0 | 0 |
_aDetermination of the stable isotope composition and total dissolved solids of Athabasca oil sands reservoir porewater _bPart 2. Characterization of McMurray Formation waters in the Suncor–Firebag field |
| 260 |
_a _b _coct. 2014 |
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| 270 | _a10/02/2015 ; 10/02/2015 | ||
| 300 | _a17 p. ; 2143-2160 | ||
| 520 | _aTranscripción del resumen del autor: A new stable isotope approach was used to determine the total dissolved solids concentration and stable isotope composition for oil sands drill core extracted porewater at the Suncor–Firebag oil sands field in northeastern Alberta, Canada. A stable isotope mixing approach was used to correct for contamination by drilling fluids in the porewater samples. The mean isotopic compositions of oxygen (BLTN13193eq1) and hydrogen (BLTN13193eq2) in water for fluid samples from 12 wells at Firebag were -20.5 ± 1.4‰ and -157 ± 11‰, respectively. The mean total dissolved solids (TDS) concentration of the reservoir formation water in 12 sampled wells was 1100 ± 400 mg/L (1s). These results suggest that the McMurray Formation water at Firebag is primarily derived from Holocene groundwater recharge, and that the water within the bitumen reservoir is similar to groundwater well samples obtained within the McMurray Formation at Firebag. The results obtained in this study are consistent with regional trends and previously proposed local hydrogeological flow conditions. | ||
| 581 | _a10 | ||
| 773 | 0 |
_tAAPG Bulletin _g98 |
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| 942 | _cARTICULO | ||
| 100 | 1 |
_aCowie, Benjamin R. _954398 |
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| 100 | 1 |
_aJames, Bruce _954399 |
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| 100 | 1 |
_aNighttingale, Michael _954400 |
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| 100 | 1 |
_aMayer, Bernhard _954401 |
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| 999 |
_c188778 _d188778 |
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