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加氢催化裂解技术用于高演化源岩有机质表征研究

孙永革  Will Meredith  Colin E Snape  柴平霞 

摘 要:加氢催化裂解技术作为近年来新发展起来的有机质大分子裂解技术,专门应用于大分子中共价键结合小分子的释放.本研究探索该技术应用于含油气沉积盆地高演化油气源岩原生有机质提取的可能性.以塔里木盆地下古生界油气源岩为例,选取了障壁泻湖相、欠补偿盆地相、闭塞欠补偿陆源海湾相、灰泥丘相等四类典型潜在源岩进行了加氢催化裂解实验,结果表明,加氢催化裂解产物中正构烷烃与甾烷的分布特征与上述源岩相完全吻合,证明加氢催化裂解实验可以有效地提取高演化油气源岩的原生有机质,为下一步实现该技术应用于油气源的对比奠定了基础.
关键词:加氢催化裂解;高演化烃源岩;生物标志化合物;塔里木盆地
分类号:TE135  文献标识码:A

文章编号:0253-9985(2008)02-0276-07

Study on the application of hydropyrolysis technique to the description of organic matter in highly mature source rocks

Sun Yongge  Will Meredith  Colin E Snape  Chai Pingxia 

 

基金项目:国家自然科学基金(40472060);国家重点基础研究发展规划(973)项目(2006CB202303).
作者简介:孙永革(1969-),男,研究员、博士生导师,有机地球化学.
作者单位:孙永革(中国科学院,广州地球化学研究所,有机地球化学国家重点实验室,广东,广州,510640) 
     Will Meredith(School of Chemical,Environmental and Mining Engineering(SCHEME),University of Nottingham, University Park, NG7 2RD, United Kindom) 
     Colin E Snape(School of Chemical,Environmental and Mining Engineering(SCHEME),University of Nottingham, University Park, NG7 2RD, United Kindom) 
     柴平霞(中国科学院,广州地球化学研究所,有机地球化学国家重点实验室,广东,广州,510640) 

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