Deformation and reservoir properties of tectonically deformed coals

Tectonic deformation and pore structure characteristics of tectonically deformed coals (TDC) collected from the Hancheng area, Weibei block, eastern Ordos Basin were characterized through scanning electron microscope, micro-CT, mercury porosimetry and low-temperature nitrogen adsorption experiments....

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Main Authors: Huifang YAO, Zhiqin KANG, Wei LI
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2014-08-01
Series:Petroleum Exploration and Development
Online Access:http://www.sciencedirect.com/science/article/pii/S1876380414600525
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spelling doaj-24b83ed7573142a68df0cf975d0708342021-02-02T03:37:12ZengKeAi Communications Co., Ltd.Petroleum Exploration and Development1876-38042014-08-01414460467Deformation and reservoir properties of tectonically deformed coalsHuifang YAO0Zhiqin KANG1Wei LI2Corresponding author; Taiyuan University of Technology, Taiyuan 030024, ChinaTaiyuan University of Technology, Taiyuan 030024, ChinaTaiyuan University of Technology, Taiyuan 030024, ChinaTectonic deformation and pore structure characteristics of tectonically deformed coals (TDC) collected from the Hancheng area, Weibei block, eastern Ordos Basin were characterized through scanning electron microscope, micro-CT, mercury porosimetry and low-temperature nitrogen adsorption experiments. The isothermal adsorption experiment of lumpy TDC was also performed to investigate the gas storage behavior. The results show that the primary layer structure can be observed in cataclastic coals and granulated coals. These coals show sub-angular particles of 1–3 cm. For scaled coals and mylonitic coals, the primary structure and coal bedding have been destroyed, and the coal is sheared with directional arrangement of grains. The pore volume, pore surface area, micro-pore volume and pore connectivity increase with the increase in deformation extent. The CH4 adsorption capacity of coals shows an increasing trend from brittle deformation to ductile deformation. It is concluded that the coal structure, pore and fracture characteristics of TDC control the gas adsorption capacity of coals. Key words: tectonically deformed coal (TDC), deformation characteristics, pore structure, adsorptionhttp://www.sciencedirect.com/science/article/pii/S1876380414600525
collection DOAJ
language English
format Article
sources DOAJ
author Huifang YAO
Zhiqin KANG
Wei LI
spellingShingle Huifang YAO
Zhiqin KANG
Wei LI
Deformation and reservoir properties of tectonically deformed coals
Petroleum Exploration and Development
author_facet Huifang YAO
Zhiqin KANG
Wei LI
author_sort Huifang YAO
title Deformation and reservoir properties of tectonically deformed coals
title_short Deformation and reservoir properties of tectonically deformed coals
title_full Deformation and reservoir properties of tectonically deformed coals
title_fullStr Deformation and reservoir properties of tectonically deformed coals
title_full_unstemmed Deformation and reservoir properties of tectonically deformed coals
title_sort deformation and reservoir properties of tectonically deformed coals
publisher KeAi Communications Co., Ltd.
series Petroleum Exploration and Development
issn 1876-3804
publishDate 2014-08-01
description Tectonic deformation and pore structure characteristics of tectonically deformed coals (TDC) collected from the Hancheng area, Weibei block, eastern Ordos Basin were characterized through scanning electron microscope, micro-CT, mercury porosimetry and low-temperature nitrogen adsorption experiments. The isothermal adsorption experiment of lumpy TDC was also performed to investigate the gas storage behavior. The results show that the primary layer structure can be observed in cataclastic coals and granulated coals. These coals show sub-angular particles of 1–3 cm. For scaled coals and mylonitic coals, the primary structure and coal bedding have been destroyed, and the coal is sheared with directional arrangement of grains. The pore volume, pore surface area, micro-pore volume and pore connectivity increase with the increase in deformation extent. The CH4 adsorption capacity of coals shows an increasing trend from brittle deformation to ductile deformation. It is concluded that the coal structure, pore and fracture characteristics of TDC control the gas adsorption capacity of coals. Key words: tectonically deformed coal (TDC), deformation characteristics, pore structure, adsorption
url http://www.sciencedirect.com/science/article/pii/S1876380414600525
work_keys_str_mv AT huifangyao deformationandreservoirpropertiesoftectonicallydeformedcoals
AT zhiqinkang deformationandreservoirpropertiesoftectonicallydeformedcoals
AT weili deformationandreservoirpropertiesoftectonicallydeformedcoals
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