烃源岩中无机矿物对有机质生烃的影响

蔡郁文; 张水昌; 何坤; 米敬奎; 张文龙; 王晓梅; 王华建; 吴朝东

doi:10.11781/sysydz201702253

烃源岩中无机矿物对有机质生烃的影响

doi: 10.11781/sysydz201702253

蔡郁文^1,2,3,
张水昌^2,3, ,,
何坤^2,3,
米敬奎^2,3,
张文龙^2,3,
王晓梅^2,3,
王华建^2,3,
吴朝东¹

1.
北京大学地球科学与空间科学学院, 北京 100871
2. 中国石油勘探开发研究院, 北京 100083
3. 中国石油天然气股份有限公司油气地球化学重点实验室, 北京 100083

基金项目: 国家油气专项（2016ZX05007001）及中国石油天然气股份有限公司项目（2014D-3209）资助。

详细信息

作者简介:
蔡郁文(1989-),女,博士研究生,从事油气地球化学研究。E-mail:caiyuwen1@aliyun.com。

通讯作者:
张水昌(1961-),男,教授,博士生导师,从事有机地球化学方面研究工作。E-mail:sczhang@petrochina.com.cn。

中图分类号: TE122.11
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出版历程
- 收稿日期: 2016-08-19
- 修回日期: 2017-02-03
- 刊出日期: 2017-03-28

Effects of inorganic minerals in source rocks on hydrocarbon generation from organic matter

Cai Yuwen^1,2,3,
Zhang Shuichang^{2,3
, ,},
He Kun^2,3,
Mi Jingkui^2,3,
Zhang Wenlong^2,3,
Wang Xiaomei^2,3,
Wang Huajian^2,3,
Wu Chaodong¹

1.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
2. Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China
3. Key Laboratory of Petroleum Geochemistry, CNPC, Beijing 100083, China

摘要

摘要: 对华北下花园地区下马岭组及鄂尔多斯盆地延长组2组低成熟泥岩全岩及分离的干酪根样品开展有水热解实验，探讨了烃源岩源内无机矿物对有机质生烃及同位素分馏的影响。实验结果表明，两组全岩有水体系液态烃及气态烃产率不同程度低于干酪根有水体系，CO₂及H₂产率则明显偏高。同时，全岩有水热解体系气体产物异构烃含量相对较低，表明烃源岩中无机矿物的加入抑制了水-有机质的反应并一定程度上改变了反应途径。稳定同位素的分析结果表明，相同热演化程度下，2组全岩及相应干酪根热解生成的甲烷碳同位素变化不大，但前者生成的二氧化碳碳同位素显著升高，且气态烃氢同位素更低。表明全岩有水热解体系下，烃源岩中的无机矿物参与到有机质热解过程中，改变了CO₂产率及同位素组成，并存在H₂间接加氢作用。
- 有水热解 /
- 氢同位素 /
- 碳正离子机理 /
- 无机矿物 /
- 烃源岩
Abstract: The effects of inorganic minerals in source rocks on gas generation and isotopic fractionation of organic matter were studied by hydrous pyrolysis using two sets of whole rocks and their kerogens, which were separated from the low maturity shale of the Yanchang Formation in the Ordos Basin and the Xiamaling Formation in Huayuan area of North China. The liquid and gaseous hydrocarbon yields indicated that hydrous pyrolysis with whole source rocks were lower than those in pyrolysis of kerogen, but the amounts of CO₂ and H₂ in the former experiments were much higher, and the i-C₄/n-C₄ ratios in the whole rock hydrous pyrolysis were also lower. The results indicated that the presence of inorganic minerals in source rocks inhibited the interaction between water and organic matter, and the reaction mechanism between them also changed. Stable isotopic analyses revealed that little difference exists between the carbon isotopes of methane generated from two different types of hydrous pyrolysis, whereas the isotopic values of CO₂ were much more enriched due to the inorganic minerals present in source rocks, and the hydrogen isotopic values of gaseous hydrocarbons decrease significantly. These results demonstrated that inorganic minerals in source rocks have participated in and affected the isotopic compositions of hydrocarbon gases, and there exists indirect hydrogenation controlled by the presence of hydrogen.
- hydrous pyrolysis /
- hydrogen isotopes /
- carbocation mechanism /
- inorganic minerals /
- source rock

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