Geochemical implications of the carbon isotope compositions of individual polycyclic aromatic compounds in coals from the Junggar and Ordos basins, NW China
Ziao Geng , Meijun Li , Shuichang Zhang , Shengbao Shi , Wenqiang Wang , Lei Zhu , Tiantian Li , Jianfeng Zhang
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引用次数: 0
Abstract
This study analyzes the δ13C values of various polycyclic aromatic compounds (PACs), including dibenzofuran, and methyldibenzofurans in two sets of coals from the Junggar and Ordos basins in NW China. The results reveal that the δ13C values of individual PACs are primarily influenced by the source of degraded organic matter rather than thermal maturity. The significant differences in δ13C values (−11.7 ‰) between dibenzofuran (DBF) and its methylated homologues (MDBFs) imply different sources. DBF is primarily derived from higher plants, while MDBFs have multiple sources from both lichens and higher plants. However, the δ13C values of DBF and MDBF in predominantly pyrogenic samples are relatively similar. This is due to two factors: (1) The kinetic isotope effect leads to preferential demethylation of 12C-enriched MDBF isomers, and the residual MDBFs are consequently enriched in 13C isotopes. The DBF produced by this process is enriched in 12C isotope, leading to depletion of δ13C for DBF in the combustion products. (2) Greater higher plant than lichen inputs result in higher δ13C values of MDBFs also potentially causes lower δ13C values in DBF. These two factors combine to produce similar δ13C values for DBF and MDBFs in samples heavily affected by wildfires.
期刊介绍:
Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology.
The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements.
Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.