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《Acta Sedimentologica Sinica》 2002-04
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A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin

ZHANG Xiao bao XU Yong-chang LIU Wen hui SHEN Ping JI Li ming MA Li yuan (State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000)  
The chemical composition and carbon isotope of the six water dissolved gas samples in the Turpan Hami basin are measured and the characteristic of formation mechanism and the possibility of application of the composition and isotope to natural gas geology are discussed by comparison with the natural gas in the basin. The characteristic of the composition of the water dissolved gas hydrocarbons is mainly controlled by dissolution degree of the hydrocarbons. They are derived from the same source rocks as the natural gases, but they are different from the natural gases, e.g., the C 1/C 1~5 of the water dissolved gas should be higher than that of the natural gas, but in fact it is lower; the homologue of the water dissolved gas CH 4 is enriched in 13 C than that of the natural gas. the above characteristic was thought to be related with that the dissolved content of the natural gases in the dissolved water was less than the migrated content. It is considered that the differences of the composition and isotope between the water dissolved gas and the natural gas indicate the relation of between the sampling members and natural gas dynamics pool forming system.
【Fund】: 国家自然科学基金项目 (批准号 :49972 0 51 ;;40 1 72 0 53);; 中国科学院资源环境领域知识创新工程重大 (重要方向 )项目 (KZCX2 1 1 1 )资助
【CateGory Index】: P593
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