Abstract
Three hundred gas samples recovered from SHSC-4 during China’s first gas hydrate production test in the South China Sea were examined for gas component and isotopic composition. According to the gas chromatography analysis, all the gas samples from SHSC-4 are predominated by CH4, with minor N2 + O2, as well as trace amounts of CO2, C2H6, and C3H8. No H2S was detected. The molecular and isotopic data of the gas samples fall into the region of “mixed origin” on the plot of C1/(C2 + C3) − δ13C1, which is close to the microbial origin. The discrimination diagram of δ13C1 − δDCH4 shows that the methane in all of the samples is of microbial origin, and is derived from the CO2 reduction.
Subject
Energy (miscellaneous),Energy Engineering and Power Technology,Renewable Energy, Sustainability and the Environment,Electrical and Electronic Engineering,Control and Optimization,Engineering (miscellaneous)
Reference16 articles.
1. The first offshore natural gas hydrate production test in South China Sea
2. Global resource potential of gas hydrate—A new calculation;Johnson;Fire Ice Methane Hydrate Newslett.,2011
3. Characterization of natural gas hydrate and its deposits recovered from the northern slope of the South China Sea;Liu;Earth Sci. Front.,2017
4. Light hydrocarbons in recent Texas continental shelf and slope sediments
5. METHANE AND OTHER HYDROCARBON GASES IN MARINE SEDIMENT
Cited by
52 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献