烃源岩中粘土对有机质保存的研究进展

新疆石油地质 ›› 2009, Vol. 30 ›› Issue (3): 390-392.

烃源岩中粘土对有机质保存的研究进展

樊馥, 叶文青, 蔡进功, 包于进

同济大学海洋与地球科学学院海洋地质国家重点实验室,上海200092

收稿日期:2008-10-08 修回日期:2008-12-22 出版日期:2009-06-01 发布日期:2020-10-29
作者简介:樊馥(1982-),女,内蒙古赤峰人,在读博士研究生.油气地球化学,(E-mail)fanfu2005612033@sina.rom.
基金资助:
国家自然基金(40672085)和中国石化科技局基金项目共同资助

Advances on Organic Matter Preservation by Clay in Source Rock

FAN Fu, YE Wen-qing, CAI Jin-gong, BAO Yu-jin

State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai 200092, China

Received:2008-10-08 Revised:2008-12-22 Online:2009-06-01 Published:2020-10-29

摘要/Abstract

摘要： 有机质通过与粘土结合而获得长期保存,这在自然界是普遍存在的。通过总结前人在粘土与有机质关系方面的研究成果,包括粘土结合有机质的数量,结合有机质的类型,二者结合的差异性,为探讨烃源岩中有机粘土复合体保存方式及生烃机理问题奠定基础。

关键词: 有机质, 粘土, 烃源岩, 有机粘土复合体.

Abstract: It is ubiquitous in nature that organic matter is chronically preserved by combining with clay. The article summarizes the studied results of relationship between clay and organic matter, including the related quantity, type and othemess of it for the purpose of promoting in-depth studies on the preserving way of organic clay complex and the mechanism of hydrocarbon generation.

Key words: organic matter, clay, source rock, organic clay complex

中图分类号:

TE112.11

樊馥, 叶文青, 蔡进功, 包于进. 烃源岩中粘土对有机质保存的研究进展[J]. 新疆石油地质, 2009, 30(3): 390-392.

FAN Fu, YE Wen-qing, CAI Jin-gong, BAO Yu-jin. Advances on Organic Matter Preservation by Clay in Source Rock[J]. Xinjiang Petroleum Geology, 2009, 30(3): 390-392.

参考文献

[1] 王行信,蔡进功,包于进.粘土矿物对有机质生烃的催化作用[J].海相油气地质,2006, 11(3):27-38.
[2] 王飞宇,傅家漠.煤和烃源岩镜质体中超微细类脂体检出及意义[J].科学通报, 1995, 38(2): 151-154.
[3] Carter M R, Angers D A, Gregorich E G, et al. Characterizing organic matter relention for surface soils in eastemCanada using density and particle size fractions[J]. Can. J. Soil Sci,2003,83(1): 11-23.
[4] Dexter A R, Richard C, Arrouays D,et al.Complexed organie matter controls soil physical properties[J]. Geoderma, 2008,(8):1-8.
[5] Kennedy M J, Pevear D R, Hill R J.Mineral surface control of organic carbon in black shale[J]. Science, 2002, (295):657-660.
[6] LU Xiancai, LIU Qing, ZHANG Lingye, et al.Desorption sequence of organic matter froom organoclay complexes in source rocks[J]. Goldschmidt Conference Abstracts, 2006.
[7] 蔡进功. 泥质沉积物和泥岩中有机粘土复合体[M].北京:科学出版社.2004:95-107.
[8] 张永刚,蔡进功,许卫平.泥质烃源岩中有机质富集机理[M].北京:石油工业出版社,2007:133-144.
[9] 蔡进功. 泥质沉积物和泥岩中有机粘土复合体[M].北京:科学出版社.2004:95-107.
[10] 吴宏海,郭杏妹,杜娟,等.土壤和沉积物中NOM稳定性矿物学机制研究的理论和方法[J].地学前缘,2007,14(5):254-263.
[11] Baldock J A, Oades J M,Waters A G, et al.Aspects of the chemical structure of soil organic material as revealed by solid -state13C, NMR spectroscopy[J]. Biogeochemistry,1992,(16):1-42.
[12] Chen Jennshing, Chiu ChinYu. Characterization of soil organic matter in different particle -size fractions in humid subalpine soils by CP/MASI3C NMR[J]. Geoderma, 2003,(117): 129-114.
[13] Wang Kaijun, Xing Baoshem.Structural and sorption characterstics of adsorbed humic acid on clay minerals[J].Enbiron. Qual, 2005,(34):342-349.
[14] 蔡进功,包于进, 杨守业,等.泥质沉积物和泥岩中有机质的赋存形式与富集机制[J].中国科学(D辑),2007,37(2):234-243.
[15] Rebecca Sutton, Garrison Sposito.Molecular simulation of humic substance-Ca-montomoillonite complex[J]. Geochi-mica, 2006, (70):3 655-3 581.
[16] Anita Parbhakar, Javier Cuadros, Mark A.et al.Adsorption of L-lysine on montmoillonite[J]. Colloids and Surfaces,2007,(307): 142-149.
[17] Chenu C, Plante A F .Clay sized organo-mineral complexes in a cultivation chronosequence:revisting the concept of the priminary organo-mineral complex[J]. Eurpean Joumal of Soil Science, 2006,(57):596-607.
[18] Mayer L M.Extent of coverage of mineral surfaces by organic matter in marine sediments,s[J] Geochim. Cosmochim. Acta,1999, (63):207-215.
[19] 关平,徐水昌,刘文汇.烃源岩有机质的不同赋存状态及定量估算[J].科学通报,43(14):1 556-1 559.