δ13C and δD Values of n-Alkanes from In-Reservoir Biodegraded Oils: Implications for Understanding the Mechanisms of Biodegradation and for Petroleum Exploration

Geosciences

Steve Larter¹  Nikolai Pedentchouk¹  Barry Bennett² 

[1] Petroleum Reservoir Group (PRG), Department of Geosciences, University of Calgary, Calgary, AB T2N 1N4, Canada;Schlumberger Reservoir Laboratories, 8087-54 Street, SE Calgary, AB T2C 4R7, Canada;

关键词: oil biodegradation;    n-alkanes;    carbon;    hydrogen;    isotopes;    correlation;   

DOI  :  10.3390/geosciences11090365

来源: DOAJ

【 摘 要 】

This study investigates the magnitude and direction of stable C and H isotope shifts of n-C_15–30 alkanes from biodegraded oils sourced from Type II (Oil suite S) and Type II/III (Oil suite H) kerogens. Compound-specific isotope data show a 2.0‰ ¹³C-enrichment and no D-enrichment of n-alkanes in the most biodegraded oil from sample suite S. Similarly, there is a 1.5–2.5‰ ¹³C-enrichment and no D-enrichment in Oil suite H. Overall, there is a <2.5‰ δ¹³C and <20‰ δD variability among individual n-alkanes in the whole sequence of biodegradation. N-alkanes from the least biodegraded Oil H samples are 2–4‰ ¹³C-enriched in comparison with the least biodegraded Oil S. However, there are no differences in the δD values of n-alkanes in these samples. Our indirect isotopic evidence suggests (1) a site-specific biodegradation process, most likely at position C-2 and/or C-3 or another site-specific process, and (2) a significant D/H exchange between organic compounds in the source rock and isotopically similar marine formation waters. We conclude that, unlike δD methodology, investigation of δ¹³C composition of n-alkanes has strong potential as a supplementary tool for oil–oil and oil–source-rock correlation even in biodegraded oils when n-alkanes are present.

【 授权许可】

Unknown