Biodegradation of occluded hydrocarbons and kerogen macromolecules of the Permian Lucaogou shales, Junggar Basin, NW China

被引:2
|
作者
Chen, Yan'e [1 ,2 ]
Li, Longlong [1 ,2 ]
Zhang, Zhirong [1 ,2 ,3 ]
Greenwood, Paul F. [4 ,5 ]
Liu, Yumin [3 ,6 ]
机构
[1] SINOPEC Petr Explorat, Dev Res Inst, Wuxi Branch, Wuxi 214126, Jiangsu, Peoples R China
[2] SINOPEC Key Lab Petr Accumulat Mech, Wuxi 214126, Jiangsu, Peoples R China
[3] Yangtze Univ, Hubei Key Lab Petr Geochem & Environm, Wuhan 430100, Hubei, Peoples R China
[4] Univ Western Australia, Sch Earth Sci, Crawley, WA 6009, Australia
[5] Curtin Univ, Western Australia Organ & Isotope Geochem Ctr, Sch Earth & Planetary Sci, GPO Box U1987, Perth, WA 6845, Australia
[6] Yangtze Univ, Hubei Key Lab Petr Geochem & Environm, Wuhan 430100, Peoples R China
来源
ENERGY GEOSCIENCE | 2023年 / 4卷 / 01期
基金
中国国家自然科学基金;
关键词
Biodegradation; Stepwise pyrolysis; Occluded hydrocarbon; Bitumen II; Kerogen; Source rock; Permian Lucaogou shale; Junggar Basin; TARIM BASIN; ATHABASCA ASPHALTENE; ORGANIC-MATTER; CRUDE OILS; HEAVY OILS; PYROLYSIS; 25-NORHOPANES; GEOCHEMISTRY; PETROLEUM; DISTRIBUTIONS;
D O I
10.1016/j.engeos.2022.10.001
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Three kerogen samples (JJZG-1, JJZG-2 and JJZG-3) isolated from the Permian Lucaogou shales of varying biodegradation levels (BLs z 0, 3 and 7, respectively) were subjected to sequential stepwise pyrolysis combined with on-line detection of gas chromatography-mass spectrometry (GC-MS). Occluded fractions (bitumen II) released at low-temperature steps (<= 410 degrees C) show consistent biodegradative signatures with that reported for solvent-extracted fractions (bitumen I) of the original shales, e.g., broad range of abundant n-alkanes, isoprenoids and regular hopanes for the non-biodegraded JJZG-1; trace n-alkanes and abundant hopanes for the moderately biodegraded JJZG-2; and no n-alkanes but still prominent hopanes including the microbially produced 25-nohopanes for the severely biodegraded JJZG-3. This consistency between bitumen II and bitumen I fractions indicates the biodegradability of the kerogenoccluded bitumen II with limited protection from host kerogen. A minor level of protection was suggested by the trace distribution of n-alkanes in the bitumen II of JJZG-2, whereas the bitumen I had no nalkanes. The kerogen itself was more resistant to biodegradation as reflected by the persistence of high abundances of both n-alkanes and hopanes in the high temperature (>= 460 degrees C) products of all three kerogen samples. However, the relative abundances of these product groups did show some evidence of biodegradation alteration, e.g., ratios of n-C15 alkene/C27 hop-17(21)-ene at 510 degrees C pyrolysis decreased by order of magnitude from the non-biodegraded (JJZG-1 = 27.4) to highly biodegraded (0.3 for JJZG-3) samples. The reduced biodegradation impact on the kerogen fraction (Cf. bitumen fractions) was also evident by the absence of 25-norhopanes in the high-temperature analysis of the JJZG-3 kerogen. (c) 2023 Sinopec Petroleum Exploration and Production Research Institute. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:179 / 184
页数:6
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