Characteristics and Evolution of Water-Occurrence in Coal Based on a New Classification Method

• Published in: Natural resources research (New York, N.Y.) N.Y.), 2024-10, Vol.33 (5), p.2155-2171
• Main Authors: Liu, Ding, Xu, Hao, Tang, Dazhen, Chen, Shida, Xin, Fudong, Wu, Heng, Wang, Qiong, Zong, Peng, Zhao, Tiantian
• Format: Article
• Language: English
• Subjects: Chemistry and Earth Sciences; Coal; Coalbed methane; Computer Science; Dehydration; Differential equations; Earth and Environmental Science; Earth Sciences; Fossil Fuels (incl. Carbon Capture); Functional groups; Geography; Mathematical Modeling and Industrial Mathematics; Mineral Resources; Original Paper; Oxygen; Physics; S curves; Statistics for Engineering; Sustainable Development; Water
• ISSN: 1520-7439; 1573-8981
• DOI: 10.1007/s11053-024-10370-0

The presence of water in coal and its interaction plays pivotal roles in the storage and migration of coalbed methane (CBM), making it imperative to understand the water-occurrence across different coal ranks to guide CBM exploitation effectively. Here, a novel method for categorizing water into condensed and adsorbed forms based on their dehydration dynamics is proposed using differential thermogravimetric curve and the Arrhenius equation, offering a straightforward process and enabling the assessment of the interaction strength between water and coal. The result indicates that the total water capacity decreases initially before subsequently increasing as coal rank increases from 0.28 to 2.33% R o,max , with the ratio of condensed water exhibiting an S-shaped curve. Remarkably, the condensed water capacity is correlated linearly with the total pore volume. The adsorbed water in low-rank coal is controlled primarily by the level of oxygen functional groups, whereas in medium-high rank coal it is controlled primarily by the specific surface area. Based on this, the controlling equations of water capacity and coal–water structure models were established. Additionally, coal–water interaction strength decreases significantly after the first coalification jump, with the strength of low-rank coal being approximately 2.54 times higher than that of medium-high rank coal. This discrepancy arises from the combined influence of multiple oxygen functional groups in low-rank coal on adsorbed water. This paper enhances the understanding of drainage process in coal reservoirs of varying ranks, which can facilitate the efficient extraction of CBM.