Cargando…

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...

Descripción completa

Detalles Bibliográficos
Autores principales: Lu, Qingfeng, Qin, Shenjun, Xu, Fei, Chang, Xiangchun, Wang, Wenfeng
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2021
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
_version_ 1783646871786356736
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
work_keys_str_mv AT luqingfeng maceralandorganicgeochemicalcharacteristicsofthelatepermiancoalsfromyueliangtianmineguizhousouthwesternchina
AT qinshenjun maceralandorganicgeochemicalcharacteristicsofthelatepermiancoalsfromyueliangtianmineguizhousouthwesternchina
AT xufei maceralandorganicgeochemicalcharacteristicsofthelatepermiancoalsfromyueliangtianmineguizhousouthwesternchina
AT changxiangchun maceralandorganicgeochemicalcharacteristicsofthelatepermiancoalsfromyueliangtianmineguizhousouthwesternchina
AT wangwenfeng maceralandorganicgeochemicalcharacteristicsofthelatepermiancoalsfromyueliangtianmineguizhousouthwesternchina