Technical Papers
Aug 5, 2021

Differences of the Pore Structure and Methane Adsorption/Desorption between Vitrain and Durain of Low-Rank Coals: Case Study in the Huanglong Coalfield, Southern Ordos Basin, China

Publication: Journal of Energy Engineering
Volume 147, Issue 5

Abstract

Coal reservoirs are highly heterogeneous, and different macrolithotypes of coal have differences in material composition and pore structure, resulting in different coalbed methane (CBM) adsorption/desorption performance and gas-water migration characteristics. In order to explore the pore development characteristics of different macrolithotypes in low-rank coal and their influence on adsorption and desorption, the low-rank coal of the Yan’an Formation in the Huanglong coalfield is taken as the sample of the research object. Vitrain and durain are collected and then separated. The results show that the porosity of coal is 2.92%–11.81%, and the total porosity is relatively developed. The porosity of durain is slightly higher than that of vitrain, the pore throat of durain is thicker, and the macropores are more developed. The Brunauer-Emmett-Teller (BET) specific surface area (SSA) and Barrett-Joyner-Halenda (BJH) total pore volume (TPV) of vitrain is slightly larger than durain, the micropores are more developed, and most of them are semiclosed and ink-bottle-shaped pores. The pore-fracture connectivity of the durain is better than vitrain via nuclear magnetic resonance (NMR). Vitrain has more developed micropores than durain, with larger specific surface area and stronger adsorption capacity. In the process of methane adsorption/desorption, the phenomenon of desorption hysteresis generally exists. Moreover, the pore connectivity of durain is relatively good, the degree of desorption hysteresis is weaker than vitrain, and the theoretical desorption efficiency is higher than vitrain. Temperature has a significant influence on adsorption and desorption of methane. The increase in temperature is beneficial to desorption and weakens the hysteresis effect of desorption. At the same temperature, the isosteric adsorption heat in the desorption process is greater than the adsorption process, which further explains the incomplete reversibility of the adsorption and desorption process. Under the same conditions, the isosteric adsorption heat of vitrain in the adsorption process is greater than durain, and adsorption capacity of vitrain is stronger than durain. Similarly, the isosteric adsorption heat of vitrain in the desorption process is greater than durain, and desorption needs to absorb more heat. The desorption capacity is weaker than durain.

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Data Availability Statement

All data, models, and code generated or used during the study appear in the published article.

Acknowledgments

This work is supported by National Natural Science Foundation of China (Grant No. 41902175), the Shanxi Province Science and Technology Major Special Funding Project (Grant No. 20201101002), the Shaanxi Province Natural Science Basic Research Program Funding Project (Grant Nos. 2019JQ-245, 2020JQ-1000, and 2019JLZ-03), the Open Funding Project of the Key Laboratory of Coal Resources Exploration and Comprehensive Utilization of the Ministry of Natural Resources of China (Grant No. KF2019-2), and the Projects Funded by China Postdoctoral Science Foundation (Grant No. 2019M653873XB). The authors also thank the editors and anonymous reviewers for valuable comments and suggestions that have greatly improved the article.

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Go to Journal of Energy Engineering
Journal of Energy Engineering
Volume 147Issue 5October 2021

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Received: Mar 5, 2021
Accepted: Apr 30, 2021
Published online: Aug 5, 2021
Published in print: Oct 1, 2021
Discussion open until: Jan 5, 2022

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Lecturer, Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xi’an 710021, China; Lecturer, College of Geology and Environment, Xi’an Univ. of Science and Technology, Xi’an 710054, China (corresponding author). Email: [email protected]
Hongyi Fu
Undergraduate Student, College of Geology and Environment, Xi’an Univ. of Science and Technology, Xi’an 710054, China.
Dongmin Ma
Professor, Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xi’an 710021, China; Professor, College of Geology and Environment, Xi’an Univ. of Science and Technology, Xi’an 710054, China; Academic Adviser, Jinneng Holding Group Co. Ltd., National Key Laboratory of Coal and CBM Co-Mining Technology, Jincheng 048000, China.
Zhonghui Duan
Senior Engineer, Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xi’an 710021, China.
Yuping Zhang
Senior Engineer, Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xi’an 710021, China.
Fu Yang
Senior Engineer, Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Natural Resources, Xi’an 710021, China.
Weibo Li
Senior Engineer, Geological Survey Institute of Shaanxi Province, Shaanxi Geological Science and Technology Center, Xi’an 710054, China.
Chao Zheng
Lecturer, College of Geology and Environment, Xi’an Univ. of Science and Technology, Xi’an 710054, China.
Jinxiang Teng
Master’s Student, College of Geology and Environment, Xi’an Univ. of Science and Technology, Xi’an 710054, China.

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