Water structure at coal/water interface: Insights from SFG vibrational spectroscopy and MD simulation

被引:5
|
作者
Wang, Chengyong [1 ,2 ]
Xing, Yaowen [2 ]
Zhang, Chenhu [1 ]
Chen, Peng [1 ]
Xia, Yangchao [1 ,2 ]
Li, Jihui [3 ]
Gui, Xiahui [2 ]
机构
[1] Liupanshui Normal Univ, Sch Min & Mech Engn, Liupanshui 553004, Guizhou, Peoples R China
[2] China Univ Min & Technol, Chinese Natl Engn Res Ctr Coal Preparat & Purifica, Xuzhou 221116, Jiangsu, Peoples R China
[3] China Univ Min & Technol Beijing, Sch Chem & Environm Engn, Beijing 100083, Peoples R China
关键词
Coal/water interface; Hydrogen bond; SFG vibrational spectroscopy; MD simulation; Oxygen-containing group; MOLECULAR-DYNAMICS SIMULATION; HYDROGEN-BOND; SURFACE HYDRATION; ADSORPTION; COAL; MODEL; MICA; ORIENTATION; COLLECTOR;
D O I
10.1016/j.colsurfa.2024.133604
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The coal/water interface plays a significant role in coal processing and utilization, and hydrogen bonds (HBs) are the primary factors affecting the interfacial water structure. Sum frequency generation (SFG) vibrational spectroscopy was used in this study to analyze HBs at the coal/water interface, and molecular dynamics (MD) simulations were conducted to investigate the molecular dynamics properties of interfacial water. The results showed that water molecules formed strong HBs with the lignite surface using both oxygen and hydrogen atoms, whereas HBs at bituminous coal/water and anthracite/water interfaces mainly occurred through the hydrogen atoms of water molecules. Fewer HBs existed at the bituminous coal/water interface, resulting in more free hydroxyl groups of water molecules. HBs at the anthracite/water interface were weaker than those at the lignite/ water interface but stronger than those at the bituminous coal/water interface. Stronger HBs facilitated the adsorption of water molecules onto coal surfaces, reducing the number density and diffusion coefficient of water molecules within the water layer. For both properties, the MD simulation results showed the following order of decreasing magnitude: bituminous coal/water interface > anthracite/water interface > lignite/water interface.
引用
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页数:9
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