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Bulk and molecular composition variations of gold-tube pyrolysates from severely biodegraded Athabasca bitumen 被引量:2

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摘要 Gold-tube pyrolysis experiments were performed on two Athabasca oil sand bitumens at 300℃to 525℃with 2℃/h rate and 25℃step under 50 MPa.Pyrolysis temperature of 425℃is critical for weight loss of bulk bitumen and hydrocarbon generation and destruction.Polar compounds are the main source of saturated and aromatic hydrocarbon,gas and coke fractions.Molecular compositions in pyrolyzates vary systematically with increasing pyrolysis temperatures.High molecular weight n-alkanes(C26^+) are gradually destructed during pyrolysis due to thermal cracking.Moderate molecular weight n-alkanes(C21-C25)show the highest thermal stability in designed pyrolysis temperatures.The loss of low molecular weight n-alkanes(C20^-)might be caused by volatilization during pyrolysis,which may alter commonly used molecular parameters such as∑n-C20^-/∑n-C21^+,Pr/n-C17 and Ph/n-C18.Aromatic hydrocarbons were generated from 300 to 425℃,then condensation and dealkylation have been initiated at 425℃as evidenced by decreased summed alkylnaphthalenes to alkylphenanthrenes ratios and increased unsubstituted aromatics to substituted homologs ratios in higher temperatures.The occurrence of anthracene and benz[a]anthracene in pyrolysates indicates pyrogenic origin,while fluoranthene shows unexpected behaviors during pyrolysis.Ratios derived from them are not always reliable for pyrogenic source input diagnosis in environmental samples.
出处 《Petroleum Science》 SCIE CAS CSCD 2020年第6期1527-1539,共13页 石油科学(英文版)
基金 supported by National Natural Science Foundation of China(Grant Number 41573035,41873049) the Mitacs project at University of Calgary。
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  • 1Adams J J,,Rostron B J,Mendoza C A.Coupled fluid flow,heat andmass transport,and erosion in the Alberta basin:implications forthe origin of the Athabasca oil sands[].Canadian Journal of EarthSciences.2004
  • 2Adams J,Riediger C,Fowler M,et al.Thermal controls onbiodegradation around the Peace River oil sands:Paleo-pasteurization to the west[].Journal of Geochemical Exploration.2006
  • 3Anfort S J,Bachu S,Bentley L R.Regional-scale hydrogeology of theUpper Devonian-Lower Cretaceous sedimentary succession,south-central Alberta basin,Canada[].American Association of Petroleum Geologists Bulletin.2001
  • 4Bennett B,Fustic M,Farrimond P,et al.25-Norhopanes:Formationduring biodegradation of petroleum in the subsurface[].Organic Geochemistry.2006
  • 5Brooks P W,Fowler M G,MacQueen R W.Biological markerconventional organic geochemistry of oilsands/heavy oils,WesternCanada Basin[].Organic Geochemistry.1988
  • 6Connan J.Biodegradation of crude oils in reservoirs[].Advances in Petroleum Geochemistry I.1984
  • 7Fowler M G,Stasiuk L D,Hearn M,et al.Devonian hydrocarbon sourcerocks and their derived oils in the Western Canada SedimentaryBasin[].Bulletin of Canadian Petroleum Geology.2001
  • 8Huang H P,Bennett B,Oldenburg T,et al.Geological controls onthe origin of heavy oil and oil sands and their impacts on in-siturecovery[].Journal of Canadian Studies.2008
  • 9Huang H P,Bowler B F J,Zhang Z W,et al.Influence of biodegradationon carbazole and benzocarbazole distributions in single oil columnsfrom the Liaohe basin,NE China[].Organic Geochemistry.2003
  • 10Huang H P,Larter S R,Bowler B F J,et al.A dynamic biodegradationmodel suggested by petroleum compositional gradients withinreservoir columns from the Liaohe basin,NE China[].Organic Geochemistry.2004

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