GEOCHEMICAL JOURNAL
Online ISSN : 1880-5973
Print ISSN : 0016-7002
ISSN-L : 0016-7002
Influence of water on yields and isotopic fractionations of gas hydrocarbons generated from oil cracking
YONGBIN JINXIANMING XIAOYONGCHUN TANGHUI TIANJINZHONG LIU
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2009 年 43 巻 4 号 p. 247-255

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Few investigations have been made to discuss the influence of water on the yields and carbon and hydrogen isotopic ratios of gas hydrocarbons generated from oil cracking although water occurs in oil reservoirs. In this study, a pyrolysis experiment for a crude oil under hydrous and anhydrous conditions in a gold tube confined system was performed at T = 370°C, P = 21 MPa and times from 1 to 7 days. It is found that water has an obvious inhibition on the gas yields generated from oil cracking and a pronounced influence on the carbon and hydrogen isotopic fractionations of the cracking gas. Compared with the anhydrous pyrolysis, the hydrous pyrolysis has a smaller C1-5 alkane yields and lighter carbon and hydrogen isotopic ratios of the C1-3 hydrocarbons within maturity levels investigated. The differences in their C1-5 alkane yields reach 3-12 ml/g, in their δ13CH4, δ13C2H6 and δ13C3H8 values reach 1.0-2.7‰, 0.2-0.8‰ and 0.2-0.3‰, respectively, and in their δDCH4, δDC2H6, δDC3H8 values reach 5-16‰, 22-80‰ and 4-13‰, respectively. Moreover, the hydrous pyrolysis experiment formed a greater amount of H2 and alkenes and a smaller amount of CO2 than the anhydrous pyrolysis experiment did. The differences of H2, ethene, propene and CO2 between the two experiment conditions are 0.44-2.12 ml/g, 0.03-0.05 ml/g, 0.20-0.34 ml/g and 0.08-0.98 ml/g, respectively. These results indicate that these differences in carbon and hydrogen isotopic ratios of generated gases between the hydrous and anhydrous experiments is possibly because water affects the free radical reactions of oil cracking and inhibits the combination between alkyl and hydrogen to form alkane to some extent, rather than due to the isotopic exchange reactions between water and some pyrolysates as usually believed for kerogen hydrous pyrolysis.

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© 2009 by The Geochemical Society of Japan
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