Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods

The study of pore characteristics in tectonic coal is essential for a deeper understanding of gas diffusion, seepage, and other transport processes within coal seams, and plays a crucial role in the development of coalbed methane resources. Based on low-temperature N<sub>2</sub> and CO&l...

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Main Authors: Jinbo Zhang, Huazhou Huang, Wenbing Zhou, Lin Sun, Zaixing Huang
Format: Article
Language:English
Published: MDPI AG 2025-02-01
Series:Energies
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Online Access:https://www.mdpi.com/1996-1073/18/4/887
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author Jinbo Zhang
Huazhou Huang
Wenbing Zhou
Lin Sun
Zaixing Huang
author_facet Jinbo Zhang
Huazhou Huang
Wenbing Zhou
Lin Sun
Zaixing Huang
author_sort Jinbo Zhang
collection DOAJ
description The study of pore characteristics in tectonic coal is essential for a deeper understanding of gas diffusion, seepage, and other transport processes within coal seams, and plays a crucial role in the development of coalbed methane resources. Based on low-temperature N<sub>2</sub> and CO<sub>2</sub> adsorption experiments, this study investigated the pore structure characteristics of four tectonic coal samples collected from the Hegang and Jixi basins in China. The results show that the mylonitic coal sample exhibits a clear capillary condensation and evaporation phenomenon around a relative pressure (<i>P</i>/<i>P</i><sub>0</sub>) of 0.5. The degree of tectonic deformation in coal has a significant impact on its pore characteristics. As the degree of deformation increases, both the pore volume and specific surface area of the coal gradually increase. The pore volume and specific surface area of micropores are primarily concentrated in pores with diameters of 0.5–0.7 nm and 0.8–0.9 nm, while those of mesopores are mainly distributed in pores with diameters of 2.3–6.2 nm. The proportion of pore volume and specific surface area contributed by micropores is much greater than that of mesopores. The fractal dimension is positively correlated with the degree of tectonic deformation in coal. As the fractal dimension increases, the average pore diameter decreases, closely tied to the destruction and reconstruction of the coal’s pore structure under tectonic stress. These findings will contribute to a deeper understanding of the pore structure characteristics of tectonic coal and effectively advance coalbed methane development.
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spelling doaj-art-91d4ea245f80451996159510d3bdf6572025-08-20T02:44:53ZengMDPI AGEnergies1996-10732025-02-0118488710.3390/en18040887Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption MethodsJinbo Zhang0Huazhou Huang1Wenbing Zhou2Lin Sun3Zaixing Huang4Key Laboratory of Coalbed Methane Resources and Reservoir Formation Process, China University of Mining and Technology, Ministry of Education, Xuzhou 221008, ChinaKey Laboratory of Coalbed Methane Resources and Reservoir Formation Process, China University of Mining and Technology, Ministry of Education, Xuzhou 221008, ChinaAnhui Transport Consulting & Design Institute Co., Ltd., Hefei 230088, ChinaKey Laboratory of Coalbed Methane Resources and Reservoir Formation Process, China University of Mining and Technology, Ministry of Education, Xuzhou 221008, ChinaNational Engineering Research Center of Coal Preparation and Purification, China University of Mining and Technology, Xuzhou 221116, ChinaThe study of pore characteristics in tectonic coal is essential for a deeper understanding of gas diffusion, seepage, and other transport processes within coal seams, and plays a crucial role in the development of coalbed methane resources. Based on low-temperature N<sub>2</sub> and CO<sub>2</sub> adsorption experiments, this study investigated the pore structure characteristics of four tectonic coal samples collected from the Hegang and Jixi basins in China. The results show that the mylonitic coal sample exhibits a clear capillary condensation and evaporation phenomenon around a relative pressure (<i>P</i>/<i>P</i><sub>0</sub>) of 0.5. The degree of tectonic deformation in coal has a significant impact on its pore characteristics. As the degree of deformation increases, both the pore volume and specific surface area of the coal gradually increase. The pore volume and specific surface area of micropores are primarily concentrated in pores with diameters of 0.5–0.7 nm and 0.8–0.9 nm, while those of mesopores are mainly distributed in pores with diameters of 2.3–6.2 nm. The proportion of pore volume and specific surface area contributed by micropores is much greater than that of mesopores. The fractal dimension is positively correlated with the degree of tectonic deformation in coal. As the fractal dimension increases, the average pore diameter decreases, closely tied to the destruction and reconstruction of the coal’s pore structure under tectonic stress. These findings will contribute to a deeper understanding of the pore structure characteristics of tectonic coal and effectively advance coalbed methane development.https://www.mdpi.com/1996-1073/18/4/887tectonic coalsmesoporemicroporepore specific areapore volumefractal dimension
spellingShingle Jinbo Zhang
Huazhou Huang
Wenbing Zhou
Lin Sun
Zaixing Huang
Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
Energies
tectonic coals
mesopore
micropore
pore specific area
pore volume
fractal dimension
title Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
title_full Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
title_fullStr Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
title_full_unstemmed Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
title_short Study on Pore Structure of Tectonically Deformed Coals by Carbon Dioxide Adsorption and Nitrogen Adsorption Methods
title_sort study on pore structure of tectonically deformed coals by carbon dioxide adsorption and nitrogen adsorption methods
topic tectonic coals
mesopore
micropore
pore specific area
pore volume
fractal dimension
url https://www.mdpi.com/1996-1073/18/4/887
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AT wenbingzhou studyonporestructureoftectonicallydeformedcoalsbycarbondioxideadsorptionandnitrogenadsorptionmethods
AT linsun studyonporestructureoftectonicallydeformedcoalsbycarbondioxideadsorptionandnitrogenadsorptionmethods
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