Discrimination of abiogenic and biogenic alkane gases

We have combined the analytical data of the carbon isotope distribution pattern, R/Ra and CH 4 / 3 He values of abiogenic and biogenic (referring to the thermogenic and bacterial or microbial) alkane gases in China with those of alkane gases from USA, Russia, Germany, Australia and other countries....

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Published inScience in China. Series D, Earth sciences Vol. 51; no. 12; pp. 1737 - 1749
Main Authors Dai, JinXing, Zou, CaiNeng, Zhang, ShuiChang, Li, Jian, Ni, YunYan, Hu, GuoYi, Luo, Xia, Tao, ShiZhen, Zhu, GuangYou, Mi, JingKui, Li, ZhiSheng, Hu, AnPing, Yang, Chun, Zhou, QingHua, Shuai, YanHua, Zhang, Ying, Ma, ChengHua
Format Journal Article
LanguageEnglish
Published Heidelberg SP Science in China Press 01.12.2008
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Summary:We have combined the analytical data of the carbon isotope distribution pattern, R/Ra and CH 4 / 3 He values of abiogenic and biogenic (referring to the thermogenic and bacterial or microbial) alkane gases in China with those of alkane gases from USA, Russia, Germany, Australia and other countries. Four discrimination criteria are derived from this comparative study: 1) Carbon isotopic composition is generally greater than −30‰ for abiogenic methane and less than −30‰ for biogenic methane; 2) Abiogenic alkane gases have a carbon isotopic reversal trend (δ 13 C 1 > δ 13 C 2 > δ 13 C 3 > δ 13 C 4 ) with δ 13 C 1 > −30‰ in general; 3) Gases with R/Ra >0.5 and δ 13 C 1 − δ 13 C 2 >0 are of abiogenic origin; 4) Gases (methane) with CH 4 / 3 He⩽10 6 are of abiogenic origin, whereas gases with CH 4 / 3 He⩽10 11 are of biogenic origin.
ISSN:1006-9313
1862-2801
DOI:10.1007/s11430-008-0133-1