Research on preservation and enrichment mechanisms of organic matter in muddy sediment and mudstone

• Published in: Science China. Earth sciences Vol. 50; no. 5; pp. 765 - 775
• Main Authors: Cai, JinGong, Bao, YuJin, Yang, ShouYe, Wang, XingXin, Fan, DaiDu, Xu, JinLi, Wang, AiPing
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer Nature B.V 01.05.2007; State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China; Institute of Earth Sciences, Shengli Oil Company, Dongying 257015, China%Institute of Earth Sciences, Shengli Oil Company, Dongying 257015, China%State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
• Subjects: Carbon cycle; Chloroform; Clay minerals; Minerals; Organic matter; Sediments; dissoluble organic matter; clay minerals; organic-matter enrichment mechanisms; organo-clay complexes
• ISSN: 1006-9313; 1674-7313; 1862-2801; 1869-1897
• DOI: 10.1007/s11430-007-0005-0

Using multidiscipline methodologies, the differences in preservation and enrichment mechanisms of organic matter (OM) in muddy sediment and mudstone are investigated. In clay fractions, concentrations of TOC and chloroform bitumen "A" are significantly higher than those in coarser fractions. This indicates that clay minerals (CM) play an important role in enriching OM. The content of chloroform bitumen "A" increases obviously in the clay fraction, which reveals that dissolvable OM is the main composition of coalesce with clay minerals. Furthermore, TG and DTA data show that OM enrichment mechanisms and preservation forms have multiplicity. Several exothermic peaks in the DTA curves demonstrate that muddy sediment and mudstone contain a number of bioclasts and amorphous OM besides dissolvable OM. Through analyzing with XRD and DTA after mudstone samples were pretreated, the conclusions can be arrived at. Firstly, CM interlayer space of XRD curves and exothermic peaks of DTA curves both change as temperature increases. Secondly, the changes of CM interlayer space and exothermic peaks are concordant and stable around 350 degree C. All these are the features that OM enters CM interlayers to form stable organo-clay complexes. Therefore, the combination format of OM with CM is not only surface adsorption, partial OM enters CM interlayers to form stable organo-clay complexes. Finally, through the research on OM preservation forms and enrichment mechanisms in muddy sediment and mudstone, the hydrocarbon-generation processes and the global carbon cycle and budget can be explained.