Carbon and hydrogen isotopes of methane, ethane, and propane: A review of genetic identification of natural gas

• Published in: Earth-science reviews Vol. 190; pp. 247 - 272
• Main Authors: Liu, Quanyou, Wu, Xiaoqi, Wang, Xiaofeng, Jin, Zhijun, Zhu, Dongya, Meng, Qingqiang, Huang, Shipeng, Liu, Jiayi, Fu, Qi
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.03.2019
• Subjects: Alkane; Carbon isotope; Genetic identification; Hydrogen isotope; Natural gas; Secondary process; Genetic identification; Hydrogen isotope; Natural gas; Carbon isotope; Alkane; Secondary process
• ISSN: 0012-8252; 1872-6828
• DOI: 10.1016/j.earscirev.2018.11.017

The genetic identification of different types of natural gas is notably important for assessment of its sources and exploration potential. The chemical and isotopic (C and H, in particular) compositions of natural gas vary significantly due to the complexity of its generation, migration, and accumulation processes. The “coal-type” gas generated from humic matter is generally enriched in 13C as compared to "oil-type" gas generated from sapropelic organic matter. However, gas originating from fresh-brackish water environments is depleted in 13C whereas gas from saline environments is enriched in 13C. Notwithstanding organic precusors and sedimentary environments, both isotope compositions of alkanes tend to become enriched both in 13C and 2H with prograde thermal evolution. Therefore, in addition to thermal maturity, source material is the major controlling factor of carbon isotope compositions, whereas sedimentary environment is predominant in governing hydrogen isotopes. Secondary processes, including thermochemical sulfate reduction (TSR) and diffusion, result in an enrichment of the gases in 13C and 2H due to mass-dependent kinetic isotope effect. Microbial degradation causes a decrease in propane content and an enrichment in 12C and 2H of the residual propane. The abiogenic gases may include methane from deep mantle and high molecular weight hydrocarbons through Fischer-Tropsch type (FTT) synthesis. Methane of mantle origin possesses a narrow range of isotope compositions, although it is still a tall task to determine the exact values. In contrast, isotopes of alkane gases synthesized from FTT processes are in a wide range. In sedimentary basins, the mixing of gases from multiple sources and/or through different secondary processes may pose a challenage to identification of their origins. The detailed assessment is provided here with case studies from major oil and gas basins in China. This review provides identification of misconceptions in genetic types of natural gas using carbon and hydrogen isotopes of alkanes, and sheds insights into using isotope geochemistry as an important diagnostic tool for energy exploration as well. Classification of natural gas and traditional geochemical methods for genetic identification of natural gas are reviewed.The effect of geological background and secondary alteration on δ13C and δ2H of light alkanes is assessed.New diagnostic tools for genetic classification of natural gas are suggested.