Study on Microstructure Differences of Coal Samples before and after Loading

The microscopic pore structure of coal affects the content of adsorbed gas. The microstructure of coal sample before and after loading is different, which will affect the adsorption and permeability of coal seam gas. In order to study this difference, the authors carried out mercury intrusion experi...

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Main Authors: Jiajia Liu, Yingxiang Fang, Gaini Jia, Shouqi Chen, Jianmin Hu
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Shock and Vibration
Online Access:http://dx.doi.org/10.1155/2020/8840051
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author Jiajia Liu
Yingxiang Fang
Gaini Jia
Shouqi Chen
Jianmin Hu
author_facet Jiajia Liu
Yingxiang Fang
Gaini Jia
Shouqi Chen
Jianmin Hu
author_sort Jiajia Liu
collection DOAJ
description The microscopic pore structure of coal affects the content of adsorbed gas. The microstructure of coal sample before and after loading is different, which will affect the adsorption and permeability of coal seam gas. In order to study this difference, the authors carried out mercury intrusion experiments on coal containing different coal samples and used nondestructive nuclear magnetic resonance (NMR) techniques, scanning electron microscopy, and transmission electron microscopy, to study the microstructure of coal samples before and after loading. The experimental results show that the pores of coal samples are mainly micropores and small pores, and the mesopores and macropores are relatively few. The T2 spectrum area of the coal sample is significantly increased after loading, and the parallel-layer coal samples’ T2 spectrum area is 46735, which is 9112 more than the vertical layer coal samples. The T2 spectrum of the vertical coalbed of saturated water samples shows a three-peak shape, the peak of the T2 spectrum is 12692, and the parallel bedding shows a bimodal morphology. The peak area of the T2 spectrum is 11277. The permeability of the parallel bedding coal sample is good, and the coal sample exhibits anisotropic properties. The pores and cracks of the coal samples increased after loading, and the localized area of the coal sample collapsed and formed a fracture zone, which was not conducive to the occurrence of coal seam gas. Further explanation of the changes in the permeability of the coal sample before and after loading will affect the gas storage and transportation.
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institution Kabale University
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publishDate 2020-01-01
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series Shock and Vibration
spelling doaj-art-847b9ddc64244dadb496b0fad05c34462025-02-03T05:53:52ZengWileyShock and Vibration1070-96221875-92032020-01-01202010.1155/2020/88400518840051Study on Microstructure Differences of Coal Samples before and after LoadingJiajia Liu0Yingxiang Fang1Gaini Jia2Shouqi Chen3Jianmin Hu4State Collaborative Innovation Center of Coal Work Safety and Clean-Efficiency Utilization, Jiaozuo 454000, ChinaSchool of Safety Science and Engineering, Henan Polytechnic University, Jiaozuo 454000, ChinaSchool of Safety Science and Engineering, Henan Polytechnic University, Jiaozuo 454000, ChinaSchool of Safety Science and Engineering, Henan Polytechnic University, Jiaozuo 454000, ChinaSchool of Safety Science and Engineering, Henan Polytechnic University, Jiaozuo 454000, ChinaThe microscopic pore structure of coal affects the content of adsorbed gas. The microstructure of coal sample before and after loading is different, which will affect the adsorption and permeability of coal seam gas. In order to study this difference, the authors carried out mercury intrusion experiments on coal containing different coal samples and used nondestructive nuclear magnetic resonance (NMR) techniques, scanning electron microscopy, and transmission electron microscopy, to study the microstructure of coal samples before and after loading. The experimental results show that the pores of coal samples are mainly micropores and small pores, and the mesopores and macropores are relatively few. The T2 spectrum area of the coal sample is significantly increased after loading, and the parallel-layer coal samples’ T2 spectrum area is 46735, which is 9112 more than the vertical layer coal samples. The T2 spectrum of the vertical coalbed of saturated water samples shows a three-peak shape, the peak of the T2 spectrum is 12692, and the parallel bedding shows a bimodal morphology. The peak area of the T2 spectrum is 11277. The permeability of the parallel bedding coal sample is good, and the coal sample exhibits anisotropic properties. The pores and cracks of the coal samples increased after loading, and the localized area of the coal sample collapsed and formed a fracture zone, which was not conducive to the occurrence of coal seam gas. Further explanation of the changes in the permeability of the coal sample before and after loading will affect the gas storage and transportation.http://dx.doi.org/10.1155/2020/8840051
spellingShingle Jiajia Liu
Yingxiang Fang
Gaini Jia
Shouqi Chen
Jianmin Hu
Study on Microstructure Differences of Coal Samples before and after Loading
Shock and Vibration
title Study on Microstructure Differences of Coal Samples before and after Loading
title_full Study on Microstructure Differences of Coal Samples before and after Loading
title_fullStr Study on Microstructure Differences of Coal Samples before and after Loading
title_full_unstemmed Study on Microstructure Differences of Coal Samples before and after Loading
title_short Study on Microstructure Differences of Coal Samples before and after Loading
title_sort study on microstructure differences of coal samples before and after loading
url http://dx.doi.org/10.1155/2020/8840051
work_keys_str_mv AT jiajialiu studyonmicrostructuredifferencesofcoalsamplesbeforeandafterloading
AT yingxiangfang studyonmicrostructuredifferencesofcoalsamplesbeforeandafterloading
AT gainijia studyonmicrostructuredifferencesofcoalsamplesbeforeandafterloading
AT shouqichen studyonmicrostructuredifferencesofcoalsamplesbeforeandafterloading
AT jianminhu studyonmicrostructuredifferencesofcoalsamplesbeforeandafterloading