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Coal Geology & Exploration

Authors

ZHANG Jinchao, School of Resources and Earth Sciences, China University of Mining and Technology, Xuzhou 221116, Chin; Key Laboratory of Coal Methane Resources and Reservoir Formation Process of the Ministry of Education, China University of Mining and Technology, Xuzhou 221008, ChinaFollow
SANG Shuxun, School of Resources and Earth Sciences, China University of Mining and Technology, Xuzhou 221116, China; Key Laboratory of Coal Methane Resources and Reservoir Formation Process of the Ministry of Education, China University of Mining and Technology, Xuzhou 221008, China; Carbon Neutrality Institute, China University of Mining and Technology, Xuzhou 221008, China; Jiangsu Key Laboratory of Coal-based Greenhouse Gas Control and Utilization, China University of Mining and Technology, Xuzhou 221008, ChinaFollow
HAN Sijie, Carbon Neutrality Institute, China University of Mining and Technology, Xuzhou 221008, China; Jiangsu Key Laboratory of Coal-based Greenhouse Gas Control and Utilization, China University of Mining and Technology, Xuzhou 221008, China
ZHANG Fengbi, Department of Natural Resources, Zhongshan District, Liupanshui City, Guizhou Province, Liupanshui 553000, China
XU Ang, School of Resources and Earth Sciences, China University of Mining and Technology, Xuzhou 221116, Chin; Key Laboratory of Coal Methane Resources and Reservoir Formation Process of the Ministry of Education, China University of Mining and Technology, Xuzhou 221008, China
LIU Qishan, China Petroleum Pipeline Engineering Corporation, Langfang 065000, China

Abstract

CO2 geological storage in deep coal seams is regarded as an important pathway to achieve “2030 carbon peak and 2060 carbon neutrality goals”. The moisture content in coal seams plays a significant role in the CO2 storage capacity mainly based on CO2 adsorption. In this study, the anthracite from the Qinshui Basin was collected to conduct high-pressure CO2 adsorption isothermal experiments under dry, moisture-equilibrated and moisture-saturated conditions at 45℃. The CO2 excess adsorption curve was corrected by the reduction of CO2 dissolution. The adsorption capacity and adsorption heat were calculated using the modified D-R adsorption model. On the bases of the comparison of three CO2 absolute adsorption curves at different moisture conditions, the microscopic mechanism of moisture saturation enhancing the adsorption capacity was explained. The results show that (1) the CO2 adsorption capacity of dry, moisture-equilibrated and moisture-saturated coal samples are 56.72 cm3/g, 45.19 cm3/g and 48.36 cm3/g, and their adsorption heat are 29.42 kJ/mol, 26.23 kJ/mol and 27.24 kJ/mol, respectively. (2) With the CO2 density less than 0.16 g/cm3 (6.48 MPa), the absolute adsorption capacity of anthracite in descending order is dry coal, moisture-saturated coal, and moisture-equilibrated coal, but when the CO2 is in a supercritical state, the order changes to dry coal, moisture-equilibrated coal, and moisture-saturated coal. (3) The preferential occupation of high-energy adsorption sites by water molecules is the main reason for the reduction of the CO2 adsorption capacity of moisture-equilibrated coal samples. The interaction between the coal-H2O system and CO2 is stronger than that between coal and CO2 under the competitive adsorption of CO2 and H2O, resulting in the higher adsorption capacity of moisture-saturated coal samples being higher than that of dry coal samples in the supercritical stage of CO2. (4) Adsorption storage is the main form of CO2 geological storage in coal. In deep coal reservoirs, moisture saturation plays a more obvious role in increasing the adsorption capacity of supercritical CO2. High-pressure water injection into deep coal seams is an effective way to improve CO2 storage capacity and the permeability of coal seams.

Keywords

moisture saturation, anthracite, adsorption capacity, CO2 geological storage, Qinshui Basin

DOI

10.12363/issn.1001-1986.21.12.0758

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