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Maceral and Organic Geochemical Characteristics of the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern China
[Image: see text] Compositional characteristics of maceral and extractable organic matter (EOM) of the No. 10 coal from the Yueliangtian mine, Guizhou, Southwestern China, were analyzed by optical microscopy, gas chromatography (GC), and gas chromatography-mass spectrometry (GC-MS). The depositional...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Chemical Society
2021
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7860094/ https://www.ncbi.nlm.nih.gov/pubmed/33553931 http://dx.doi.org/10.1021/acsomega.0c05561 |
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author | Lu, Qingfeng Qin, Shenjun Xu, Fei Chang, Xiangchun Wang, Wenfeng |
author_facet | Lu, Qingfeng Qin, Shenjun Xu, Fei Chang, Xiangchun Wang, Wenfeng |
author_sort | Lu, Qingfeng |
collection | PubMed |
description | [Image: see text] Compositional characteristics of maceral and extractable organic matter (EOM) of the No. 10 coal from the Yueliangtian mine, Guizhou, Southwestern China, were analyzed by optical microscopy, gas chromatography (GC), and gas chromatography-mass spectrometry (GC-MS). The depositional conditions, thermodynamic effect, type and maturity of organic matter, and possible health hazards were evaluated. The random vitrinite reflectance (R(o)) is 1.01%, and the macerals are dominated by collodetrinite, inertodetrinite, collotelinite, and fusinite. The coal seam is a terrestrial sedimentary environment of the lower delta plain through the analysis of coal facies. Additionally, the extracted yield of EOM is 1.01%. The low ratio of saturated to aromatic fraction and the distribution of n-alkanes indicate that the coal-forming plants are primarily terrestrial higher plants. Typical isoprenoid biomarker parameters, including pristane/phytane (Pr/Ph), Pr/n-C(17), and Ph/n-C(18), reflect a weak oxidizing environment of coal. The hopanoid biomarkers, odd–even predominance index (OEP), and carbon preference index (CPI) reveal that the organic matter was mature. More than one hundred polycyclic aromatic compounds (PACs) were eluted and identified, and the phenanthrenes and naphthalenes account for a higher proportion. Thermodynamic stabilities play an essential role in the conversion of molecular structures, which support the relatively high contents of 2-methylnaphthalene, 2- and 3-methylphenanthrenes, and 2,6- and 2,7-dimethylphenanthrenes compared to their respective isomers. The oxygen-containing and sulfur-containing aromatic compounds also indicate the weak oxidization of the coal-formation environment, which is consistent with the results of isoprenoid biomarkers. Because of the carcinogenicity and mutagenicity of PACs, the distribution and toxic equivalency of PACs are briefly summarized. |
format | Online Article Text |
id | pubmed-7860094 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | American Chemical Society |
record_format | MEDLINE/PubMed |
spelling | pubmed-78600942021-02-05 Maceral and Organic Geochemical Characteristics of the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern China Lu, Qingfeng Qin, Shenjun Xu, Fei Chang, Xiangchun Wang, Wenfeng ACS Omega [Image: see text] Compositional characteristics of maceral and extractable organic matter (EOM) of the No. 10 coal from the Yueliangtian mine, Guizhou, Southwestern China, were analyzed by optical microscopy, gas chromatography (GC), and gas chromatography-mass spectrometry (GC-MS). The depositional conditions, thermodynamic effect, type and maturity of organic matter, and possible health hazards were evaluated. The random vitrinite reflectance (R(o)) is 1.01%, and the macerals are dominated by collodetrinite, inertodetrinite, collotelinite, and fusinite. The coal seam is a terrestrial sedimentary environment of the lower delta plain through the analysis of coal facies. Additionally, the extracted yield of EOM is 1.01%. The low ratio of saturated to aromatic fraction and the distribution of n-alkanes indicate that the coal-forming plants are primarily terrestrial higher plants. Typical isoprenoid biomarker parameters, including pristane/phytane (Pr/Ph), Pr/n-C(17), and Ph/n-C(18), reflect a weak oxidizing environment of coal. The hopanoid biomarkers, odd–even predominance index (OEP), and carbon preference index (CPI) reveal that the organic matter was mature. More than one hundred polycyclic aromatic compounds (PACs) were eluted and identified, and the phenanthrenes and naphthalenes account for a higher proportion. Thermodynamic stabilities play an essential role in the conversion of molecular structures, which support the relatively high contents of 2-methylnaphthalene, 2- and 3-methylphenanthrenes, and 2,6- and 2,7-dimethylphenanthrenes compared to their respective isomers. The oxygen-containing and sulfur-containing aromatic compounds also indicate the weak oxidization of the coal-formation environment, which is consistent with the results of isoprenoid biomarkers. Because of the carcinogenicity and mutagenicity of PACs, the distribution and toxic equivalency of PACs are briefly summarized. American Chemical Society 2021-01-15 /pmc/articles/PMC7860094/ /pubmed/33553931 http://dx.doi.org/10.1021/acsomega.0c05561 Text en © 2021 The Authors. Published by American Chemical Society This is an open access article published under a Creative Commons Non-Commercial No Derivative Works (CC-BY-NC-ND) Attribution License (http://pubs.acs.org/page/policy/authorchoice_ccbyncnd_termsofuse.html) , which permits copying and redistribution of the article, and creation of adaptations, all for non-commercial purposes. |
spellingShingle | Lu, Qingfeng Qin, Shenjun Xu, Fei Chang, Xiangchun Wang, Wenfeng Maceral and Organic Geochemical Characteristics of the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern China |
title | Maceral and Organic Geochemical Characteristics of
the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern
China |
title_full | Maceral and Organic Geochemical Characteristics of
the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern
China |
title_fullStr | Maceral and Organic Geochemical Characteristics of
the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern
China |
title_full_unstemmed | Maceral and Organic Geochemical Characteristics of
the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern
China |
title_short | Maceral and Organic Geochemical Characteristics of
the Late Permian Coals from Yueliangtian Mine, Guizhou, Southwestern
China |
title_sort | maceral and organic geochemical characteristics of
the late permian coals from yueliangtian mine, guizhou, southwestern
china |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7860094/ https://www.ncbi.nlm.nih.gov/pubmed/33553931 http://dx.doi.org/10.1021/acsomega.0c05561 |
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