A computational study of the adsorption of n-perfluorohexane in zeolite BCR-704

被引:15
作者
Bai, Peng [1 ,2 ,3 ,4 ]
Ghosh, Pritha [5 ]
Sung, Jeffrey C. [1 ,2 ,3 ,4 ]
Kohen, Daniela [6 ]
Siepmann, J. Ilja [1 ,2 ,3 ,4 ]
Snurr, Randall Q. [5 ]
机构
[1] Univ Minnesota, Dept Chem, Minneapolis, MN 55455 USA
[2] Univ Minnesota, Dept Chem Engn, Minneapolis, MN 55455 USA
[3] Univ Minnesota, Dept Mat Sci, Minneapolis, MN 55455 USA
[4] Univ Minnesota, Chem Theory Ctr, Minneapolis, MN 55455 USA
[5] Northwestern Univ, Dept Chem & Biol Engn, Evanston, IL 60208 USA
[6] Carleton Coll, Dept Chem, Northfield, MN 55057 USA
基金
美国国家科学基金会;
关键词
Monte Carlo simulation; Adsorption isotherm; Zeolite; FAUJASITE-TYPE ZEOLITES; MONTE-CARLO; CARBON-DIOXIDE; MOLECULAR-DYNAMICS; PHASE-EQUILIBRIA; SILICALITE; ALKANES; SIMULATIONS; MIXTURE; WATER;
D O I
10.1016/j.fluid.2013.07.018
中图分类号
O414.1 [热力学];
学科分类号
摘要
Monte Carlo simulations in the grand canonical and Gibbs ensembles were carried out to predict the adsorption isotherms of argon, nitrogen, and n-perfluorohexane in BCR-704, a faujasite-type calcium aluminosilicate with a Si/Al ratio of 1.6. Starting from existing force fields for the sorbate molecules and a transferable force field for all-silica zeolites, attempts were made to develop a force field that would reproduce the experimentally determined argon and nitrogen adsorption isotherms in BCR-704. However, good agreement for the nitrogen adsorption isotherm could only be obtained either for a set of force field parameters with a greatly reduced partial charge on the calcium cation or using a larger partial charge and assuming that co-adsorbed water molecules are present at the temperature used for the argon and nitrogen adsorption isotherms. Predictions of the adsorption isotherm for n-perfluorohexane in BCR-704 using the latter force field parameters and the FAU-X structure with a water/calcium ratio of 1 yield good agreement with the experimental benchmark data. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:146 / 151
页数:6
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