Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage
Underground coal gasification and exploitation of geothermal mine resources can effectively improve coal conversion and utilization efficiency, and the basic theory of the above technologies generally relies on the change law of the coal pore structure under thermal damage. Therefore, the influence...
Saved in:
Main Authors: | , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Wiley
2020-01-01
|
Series: | Geofluids |
Online Access: | http://dx.doi.org/10.1155/2020/8864571 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
_version_ | 1832560200429600768 |
---|---|
author | Zhen Liu Mingrui Zhang Shijian Yu Lin Xin Gang Wang Liutao Sun |
author_facet | Zhen Liu Mingrui Zhang Shijian Yu Lin Xin Gang Wang Liutao Sun |
author_sort | Zhen Liu |
collection | DOAJ |
description | Underground coal gasification and exploitation of geothermal mine resources can effectively improve coal conversion and utilization efficiency, and the basic theory of the above technologies generally relies on the change law of the coal pore structure under thermal damage. Therefore, the influence mechanism of the development of the coal pore structure under thermal damage is analyzed by the nuclear magnetic resonance experiment, and the temperature-permeability fractal model is created. The results show that compared with microtransitional pores, the volume of meso-macropores in the coal body is more susceptible to an increase in temperature, which was most obvious at 200-300°C. During the heating process, the measured fractal dimension based on the T2 spectral distribution is between 2 and 3, indicating that the fractal characteristics did not disappear upon a change in external temperature. The temperature has a certain negative correlation with DmNMR, DMNMR, and DNMR, indicating that the complexity of the pore structure of the coal body decreased gradually with the increase of the temperature. Compared with the permeability calculated based on the theoretical permeability fractal model, the permeability obtained from the temperature-permeability fractal model has a similar increasing trend as the permeability measured by the NMR experiment when the temperature increases. The experimental study on pore structure and permeability characteristics of the low metamorphic coal under thermal damage provides a scientific theory for underground coal gasification and geothermal exploitation. |
format | Article |
id | doaj-art-a493d45e06c240b7bf658b1d2014c9cd |
institution | Kabale University |
issn | 1468-8115 1468-8123 |
language | English |
publishDate | 2020-01-01 |
publisher | Wiley |
record_format | Article |
series | Geofluids |
spelling | doaj-art-a493d45e06c240b7bf658b1d2014c9cd2025-02-03T01:28:09ZengWileyGeofluids1468-81151468-81232020-01-01202010.1155/2020/88645718864571Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal DamageZhen Liu0Mingrui Zhang1Shijian Yu2Lin Xin3Gang Wang4Liutao Sun5College of Safety and Environmental Engineering, Shandong University of Science and Technology, 579 Qianwangang Rd, Huangdao District, Qingdao 266590, ChinaCollege of Safety and Environmental Engineering, Shandong University of Science and Technology, 579 Qianwangang Rd, Huangdao District, Qingdao 266590, ChinaCollege of Safety and Environmental Engineering, Shandong University of Science and Technology, 579 Qianwangang Rd, Huangdao District, Qingdao 266590, ChinaCollege of Safety and Environmental Engineering, Shandong University of Science and Technology, 579 Qianwangang Rd, Huangdao District, Qingdao 266590, ChinaCollege of Safety and Environmental Engineering, Shandong University of Science and Technology, 579 Qianwangang Rd, Huangdao District, Qingdao 266590, ChinaSchool of Management, China University of Mining and Technology, 1 Daxue Rd, Tongshan District, Xuzhou 221116, ChinaUnderground coal gasification and exploitation of geothermal mine resources can effectively improve coal conversion and utilization efficiency, and the basic theory of the above technologies generally relies on the change law of the coal pore structure under thermal damage. Therefore, the influence mechanism of the development of the coal pore structure under thermal damage is analyzed by the nuclear magnetic resonance experiment, and the temperature-permeability fractal model is created. The results show that compared with microtransitional pores, the volume of meso-macropores in the coal body is more susceptible to an increase in temperature, which was most obvious at 200-300°C. During the heating process, the measured fractal dimension based on the T2 spectral distribution is between 2 and 3, indicating that the fractal characteristics did not disappear upon a change in external temperature. The temperature has a certain negative correlation with DmNMR, DMNMR, and DNMR, indicating that the complexity of the pore structure of the coal body decreased gradually with the increase of the temperature. Compared with the permeability calculated based on the theoretical permeability fractal model, the permeability obtained from the temperature-permeability fractal model has a similar increasing trend as the permeability measured by the NMR experiment when the temperature increases. The experimental study on pore structure and permeability characteristics of the low metamorphic coal under thermal damage provides a scientific theory for underground coal gasification and geothermal exploitation.http://dx.doi.org/10.1155/2020/8864571 |
spellingShingle | Zhen Liu Mingrui Zhang Shijian Yu Lin Xin Gang Wang Liutao Sun Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage Geofluids |
title | Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage |
title_full | Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage |
title_fullStr | Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage |
title_full_unstemmed | Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage |
title_short | Experimental Study on the Fractal Features and Permeability Characteristics of Low Metamorphic Coal Pore Structure under Thermal Damage |
title_sort | experimental study on the fractal features and permeability characteristics of low metamorphic coal pore structure under thermal damage |
url | http://dx.doi.org/10.1155/2020/8864571 |
work_keys_str_mv | AT zhenliu experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage AT mingruizhang experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage AT shijianyu experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage AT linxin experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage AT gangwang experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage AT liutaosun experimentalstudyonthefractalfeaturesandpermeabilitycharacteristicsoflowmetamorphiccoalporestructureunderthermaldamage |