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Characteristics and the Model of Thermal Evolution and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based on Hydrous Pyrolysis
[Image: see text] The Qinshui basin is an important coal-accumulating basin in China, and its Late Paleozoic coal is an important source rock of coalbed methane in the basin. Its thermal evolution and gas generation characteristics determined the grade of coalbed methane resources, especially the co...
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/PMC8280706/ https://www.ncbi.nlm.nih.gov/pubmed/34278151 http://dx.doi.org/10.1021/acsomega.1c02211 |
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author | Hao, Ruilin Huang, Wenhui Jiu, Bo |
author_facet | Hao, Ruilin Huang, Wenhui Jiu, Bo |
author_sort | Hao, Ruilin |
collection | PubMed |
description | [Image: see text] The Qinshui basin is an important coal-accumulating basin in China, and its Late Paleozoic coal is an important source rock of coalbed methane in the basin. Its thermal evolution and gas generation characteristics determined the grade of coalbed methane resources, especially the coal measure free gas resources in the basin. Late Paleozoic coal samples were collected for organic geochemical analysis, a high-volatile bituminous coal was used for hydrous pyrolysis, to propose the thermal evolution characteristics, gas generation characteristics, thermal evolution, and free gas accumulation model, and the Ordos Basin is compared. The results show that the variation trends of various geochemical parameters are different with the increase in R(o). Hydrous pyrolysis shows that the gas production potential of coal is excellent. The gases produced consist mainly of CH(4), C(2–), CO(2), and H(2). C(2–) is produced only before the simulated temperature of 550 °C, and oil is produced only before the temperature of 500 °C. The thermal evolution stages can be divided into the immature stage, symbiosis stage, wet gas stage, and dry gas stage, and the symbiosis stage can be divided into the preliminary stage and mainly gas stage. R(o), T(max), (2+3)MP/(1+9)MP, saturated+arene, V(daf), and H/C can be used as indicators of the thermal evolution stages. On the plane, the distribution of thermal evolution stages of the Shanxi Formation and the Taiyuan Formation is very alike. The gas generating strength of the Taiyuan Formation is higher than that of the Shanxi Formation. The gas generating strength in the north of the Taiyuan Formation is higher, while that in the south of the Shanxi Formation is higher. The second gas generation stage has a good spatio-temporal configuration relationship with accumulation factors, and the gas production is large, which is beneficial to the enrichment of the coal measure free gas resources. Relatively, the Ordos Basin has better prospects for exploration and development. |
format | Online Article Text |
id | pubmed-8280706 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2021 |
publisher | American Chemical Society |
record_format | MEDLINE/PubMed |
spelling | pubmed-82807062021-07-16 Characteristics and the Model of Thermal Evolution and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based on Hydrous Pyrolysis Hao, Ruilin Huang, Wenhui Jiu, Bo ACS Omega [Image: see text] The Qinshui basin is an important coal-accumulating basin in China, and its Late Paleozoic coal is an important source rock of coalbed methane in the basin. Its thermal evolution and gas generation characteristics determined the grade of coalbed methane resources, especially the coal measure free gas resources in the basin. Late Paleozoic coal samples were collected for organic geochemical analysis, a high-volatile bituminous coal was used for hydrous pyrolysis, to propose the thermal evolution characteristics, gas generation characteristics, thermal evolution, and free gas accumulation model, and the Ordos Basin is compared. The results show that the variation trends of various geochemical parameters are different with the increase in R(o). Hydrous pyrolysis shows that the gas production potential of coal is excellent. The gases produced consist mainly of CH(4), C(2–), CO(2), and H(2). C(2–) is produced only before the simulated temperature of 550 °C, and oil is produced only before the temperature of 500 °C. The thermal evolution stages can be divided into the immature stage, symbiosis stage, wet gas stage, and dry gas stage, and the symbiosis stage can be divided into the preliminary stage and mainly gas stage. R(o), T(max), (2+3)MP/(1+9)MP, saturated+arene, V(daf), and H/C can be used as indicators of the thermal evolution stages. On the plane, the distribution of thermal evolution stages of the Shanxi Formation and the Taiyuan Formation is very alike. The gas generating strength of the Taiyuan Formation is higher than that of the Shanxi Formation. The gas generating strength in the north of the Taiyuan Formation is higher, while that in the south of the Shanxi Formation is higher. The second gas generation stage has a good spatio-temporal configuration relationship with accumulation factors, and the gas production is large, which is beneficial to the enrichment of the coal measure free gas resources. Relatively, the Ordos Basin has better prospects for exploration and development. American Chemical Society 2021-07-01 /pmc/articles/PMC8280706/ /pubmed/34278151 http://dx.doi.org/10.1021/acsomega.1c02211 Text en © 2021 The Authors. Published by American Chemical Society Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works (https://creativecommons.org/licenses/by-nc-nd/4.0/). |
spellingShingle | Hao, Ruilin Huang, Wenhui Jiu, Bo Characteristics and the Model of Thermal Evolution and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based on Hydrous Pyrolysis |
title | Characteristics and the Model of Thermal Evolution
and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based
on Hydrous Pyrolysis |
title_full | Characteristics and the Model of Thermal Evolution
and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based
on Hydrous Pyrolysis |
title_fullStr | Characteristics and the Model of Thermal Evolution
and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based
on Hydrous Pyrolysis |
title_full_unstemmed | Characteristics and the Model of Thermal Evolution
and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based
on Hydrous Pyrolysis |
title_short | Characteristics and the Model of Thermal Evolution
and Gas Generation of Late Paleozoic Coal in the Qinshui Basin, Based
on Hydrous Pyrolysis |
title_sort | characteristics and the model of thermal evolution
and gas generation of late paleozoic coal in the qinshui basin, based
on hydrous pyrolysis |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8280706/ https://www.ncbi.nlm.nih.gov/pubmed/34278151 http://dx.doi.org/10.1021/acsomega.1c02211 |
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