咸水含水层是二氧化碳(CO2)封存的主要地址储体,具有巨大的埋存潜力.当CO2封存于咸水含水层时,CO2的注入能耗及注入率在很大程度上取决于CO2与地下含盐水之间的界面特性.本文应用分子动力学仿真的方法,分析了超临界CO2和纯水界面系统中的分子间(内)作用力、分子的结构和virial等对界面张力(IFT)的影响.结果表明,分子间范德华力减小IFT,静电力、分子内的键拉伸和角力均增加IFT;水和水分子间的相互作用占主导地位,CO2和CO2以及水和CO2间的作用影响较小;水和CO2分子在界面处均成规则的有序排布,且CO2分子平行于界面分布.
参考文献
[1] | Xiaofeng Xu;Shiyi Chen;Dongxiao Zhang .Convective stability analysis of the long-term storage of carbon dioxide in deep saline aquifers[J].Advances in water resources,2006(3):397-407. |
[2] | JUAN J. HIDALGO;JESUS CARRERA.Effect of dispersion on the onset of convectionduring CO_2sequestration[J].Journal of Fluid Mechanics,2009:441-452. |
[3] | Nieto-Draghi C;de Bruin T;Perez-Pellitero J;Avalos JB;Mackie AD .Thermodynamic and transport properties of carbon dioxide from molecular simulation[J].The Journal of Chemical Physics,2007(6):64509-1-64509-8-0. |
[4] | Senapati S.;Berkowitz ML. .Computer simulation study of the interface width of the liquid/liquid interface - art. no. 176101[J].Physical review letters,2001(17):6101-0. |
[5] | C. Chalbaud;M. Robin;J-M Lombard;F. Martin;P. Egermann;H. Bertin .Interfacial Tension Measurements And Wettability Evaluation For Geological Co_2 Storage[J].Advances in water resources,2009(1):98-109. |
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