石油学报 ›› 2022, Vol. 43 ›› Issue (12): 1770-1787.DOI: 10.7623/syxb202212008
页岩有机孔研究现状和展望
聂海宽1,2, 张光荣3, 李沛2, 丁江辉4, 党伟5, 孙川翔1,2, 张培先3, 王进6, 杨超7, 李鹏1,2, 王鹏威1,2, 苏海琨8
- 1. 页岩油气富集机理与有效开发国家重点实验室 北京 102206;
2. 中国石油化工股份有限公司石油勘探开发研究院 北京 102206;
3. 中国石油化工股份有限公司华东油气分公司 江苏南京 210019;
4. 中国石油集团工程技术研究院有限公司 北京 102206;
5. 西安石油大学地球科学与工程学院 陕西西安 710300;
6. 中国石油化工股份有限公司江汉油田分公司勘探开发研究院 湖北武汉 430223;
7. 中国科学院广州能源研究所, 中国科学院天然气水合物重点实验室 广东广州 510640;
8. 中国地质大学(北京)能源学院 北京 100083
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收稿日期:2022-03-19修回日期:2022-08-22出版日期:2022-12-25发布日期:2023-01-06 -
作者简介:聂海宽,男,1982年4月生,2010年获中国地质大学(北京)矿产普查 与勘探专业博士学位,现为中国石油化工股份有限公司石油勘探开发研究院研究员,主要从事非常规油气地质研究工作。Email:niehk.syky@sinopec.com -
基金资助:国家自然科学基金项目"四川盆地五峰组—龙马溪组页岩储层演化机理及评价方法"(No.41872124)、国家自然科学重点基金项目"复杂构造带常压页岩气动态赋存机理与可动性研究"(No.42130803)和中国石油化工股份有限公司重点科技项目"深层页岩气勘探/开发/工程一体化设计技术"(P20046)资助。
Research status and prospect on organic matter pores in shale
Nie Haikuan1,2, Zhang Guangrong3, Li Pei2, Ding Jianghui4, Dang Wei5, Sun Chuanxiang1,2, Zhang Peixian3, Wang Jin6, Yang Chao7, Li Peng1,2, Wang Pengwei1,2, Su Haikun8
- 1. State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Beijing 102206, China;
2. Sinopec Petroleum Exploration and Production Research Institute, Beijing 102206, China;
3. Sinopec East China Oil & Gas Company, Jiangsu Nanjing 210019, China;
4. CNPC Engineering Technology R & D Company Limited, Beijing 102206, China;
5. School of Earth Sciences and Engineering, Xi'an Shiyou University, Shaanxi Xi'an 710300, China;
6. Research Institute of Petroleum Exploration and Development, Sinopec Jianghan Oilfield Company, Hubei Wuhan 430223, China;
7. Guangzhou Institute of Energy Conversion, Key Laboratory of Natural Gas Hydrate, Chinese Academy of Sciences, Guangdong Guangzhou 510640;
8. School of Energy Resources, China University of Geosciences, Beijing 100083, China
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Received:2022-03-19Revised:2022-08-22Online:2022-12-25Published:2023-01-06
摘要： 有机孔是页岩气储层的主要储集空间,也是页岩气储层区别于常规油气储层的重要孔隙类型。目前对有机孔的类型和特征、发育载体及其影响因素等的认识还存在较大争议。系统回顾国内外页岩有机孔的研究现状,调研分析有机孔发育特征及其控制因素,展望有机孔的攻关研究方向,研究认为,页岩的有机质类型是控制有机孔发育的根本因素,矿物类型与组成、成岩作用以及由脆性矿物形成的刚性格架是有机孔形成并保持的重要保障,热演化程度和地层压力对有机孔的发育和保持具有重要的影响。建议加强有机质类型(成烃生物)、不同有机质类型的生烃和排烃模式、矿物类型及其成岩作用(刚性格架形成时间)、页岩生-排烃与矿物成岩作用之间的有机—无机协同演化机制研究,探讨有利的页岩有机孔类型及其发育模式,加强页岩不同尺度储集空间定量表征、有机孔连通性及其影响因素等研究。未来需进一步关注深层—超深层页岩有机孔的发育特征及其保存机制研究。
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引用本文
聂海宽, 张光荣, 李沛, 丁江辉, 党伟, 孙川翔, 张培先, 王进, 杨超, 李鹏, 王鹏威, 苏海琨. 页岩有机孔研究现状和展望[J]. 石油学报, 2022, 43(12): 1770-1787.
Nie Haikuan, Zhang Guangrong, Li Pei, Ding Jianghui, Dang Wei, Sun Chuanxiang, Zhang Peixian, Wang Jin, Yang Chao, Li Peng, Wang Pengwei, Su Haikun. Research status and prospect on organic matter pores in shale[J]. Acta Petrolei Sinica, 2022, 43(12): 1770-1787.
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