TY - JOUR
T1 - The molecular and sulfur isotope distribution of volatile compounds in natural gases and condensates from Alberta, Canada
AU - Kutuzov, Ilya
AU - Said-Ahmad, Ward
AU - Turich, Courtney
AU - Jiang, Chunqing
AU - Luu, Nathalie
AU - Jacksier, Tracey
AU - Amrani, Alon
N1 - Publisher Copyright:
© 2020 Elsevier Ltd
PY - 2021/1
Y1 - 2021/1
N2 - Compound-specific S isotope analysis (CSSIA) of volatile organic sulfur compounds (VOSC) in petroleum gases was applied for the first time to two natural gas samples from the Triassic section of the Alberta Basin in Canada. For comparison, CSSIA was conducted for five condensate samples from adjacent wells. The analysis of VOSC in the gas samples revealed similarity in the sulfur isotope composition for thiols, sulfides, and H2S suggesting an isotopic equilibrium during the reaction between H2S and hydrocarbons in the reservoir. In contrast, one of the gas samples contained alkyl thiophenes with distinct δ34S values that suggest a different source, probably from oil or bitumen. The molecular and isotopic analysis of condensates revealed several phases of thiol interaction with H2S bearing similar δ34S value as the H2S in Gas A and B. Thermally stable OSC such as alkyl-, benzo- and dibenzo- thiophenes of all condensate samples kept their previous δ34S values and not the ones expected in isotopic equilibrium, indicating a recent migration of H2S to the reservoirs. The δ34S value of the H2S reacting with the gas and condensate samples is isotopically similar to H2S which could have generated during complete microbial or thermochemical sulfate reduction of the Charlie Lake anhydrite in the Triassic section, therefore making this process the likely source of the H2S. This study demonstrates the potential of sulfur isotope analysis of VOSC to interpret origin, migration pathways and provide a relative time frame for in-reservoir processes impacting present day natural gas properties.
AB - Compound-specific S isotope analysis (CSSIA) of volatile organic sulfur compounds (VOSC) in petroleum gases was applied for the first time to two natural gas samples from the Triassic section of the Alberta Basin in Canada. For comparison, CSSIA was conducted for five condensate samples from adjacent wells. The analysis of VOSC in the gas samples revealed similarity in the sulfur isotope composition for thiols, sulfides, and H2S suggesting an isotopic equilibrium during the reaction between H2S and hydrocarbons in the reservoir. In contrast, one of the gas samples contained alkyl thiophenes with distinct δ34S values that suggest a different source, probably from oil or bitumen. The molecular and isotopic analysis of condensates revealed several phases of thiol interaction with H2S bearing similar δ34S value as the H2S in Gas A and B. Thermally stable OSC such as alkyl-, benzo- and dibenzo- thiophenes of all condensate samples kept their previous δ34S values and not the ones expected in isotopic equilibrium, indicating a recent migration of H2S to the reservoirs. The δ34S value of the H2S reacting with the gas and condensate samples is isotopically similar to H2S which could have generated during complete microbial or thermochemical sulfate reduction of the Charlie Lake anhydrite in the Triassic section, therefore making this process the likely source of the H2S. This study demonstrates the potential of sulfur isotope analysis of VOSC to interpret origin, migration pathways and provide a relative time frame for in-reservoir processes impacting present day natural gas properties.
KW - Condensate
KW - Hydrogen sulfide
KW - Natural gas
KW - Sulfur isotope
KW - Volatile organic sulfur compounds
UR - http://www.scopus.com/inward/record.url?scp=85096520767&partnerID=8YFLogxK
U2 - 10.1016/j.orggeochem.2020.104129
DO - 10.1016/j.orggeochem.2020.104129
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AN - SCOPUS:85096520767
SN - 0146-6380
VL - 151
JO - Organic Geochemistry
JF - Organic Geochemistry
M1 - 104129
ER -
