Structural Changes in Nanoporous MFI Zeolites Induced by Tetrachloroethene Adsorption: A Joint Experimental and Simulation Study

被引:10
|
作者
Jeffroy, Marie [1 ,2 ,6 ,7 ]
Weber, Guy [3 ]
Hostachy, Sarah [1 ,2 ]
Bellat, Jean-Pierre [3 ]
Fuchs, Alain H. [4 ,5 ]
Boutin, Anne [1 ,2 ]
机构
[1] Ecole Normale Super, CNRS, F-75231 Paris 05, France
[2] UPMC, F-75231 Paris 05, France
[3] Univ Bourgogne, CNRS, Lab Interdisciplinaire Carnot Bourgogne, F-21078 Dijon, France
[4] Chim ParisTech, F-75005 Paris, France
[5] CNRS, F-75005 Paris, France
[6] CNRS, Chim Phys Lab, F-91405 Orsay, France
[7] Univ Paris 11, F-91405 Orsay, France
来源
JOURNAL OF PHYSICAL CHEMISTRY C | 2011年 / 115卷 / 10期
关键词
CANONICAL MONTE-CARLO; RAY-POWDER DIFFRACTION; ORTHORHOMBIC PHASE-TRANSITION; ORGANIC-INORGANIC FRAMEWORKS; MOLECULAR SIMULATION; SINGLE-CRYSTAL; SILICALITE-1; ZEOLITE; WATER CONDENSATION; GUEST MOLECULES; CO2; ADSORPTION;
D O I
10.1021/jp109447n
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
A joint experimental and molecular simulation study was performed to investigate the,adsorption of tetrachloroethene on two MFI zeolites, ZSM-5 with a Si/Al ratio of 26.5, and silicalite-1, which is the pure silica form of ZSM-5. Adsorption isotherms and isosteric heats of adsorption of tetrachloroethene were measured and compared to molecular simulation results, Experimental curves for both MFI zeoliteS show a step at loading of 4 molecules.uc(-1) that was interpreted in terms of a structural change of the host framework. A thermodynamic analysis based on the Osmotic ensemble scheme allowed attributing this Step to a symmetry Change from ORTHO (orthorhombic form With Pnma symmetry) to PARA (orthorhombic form with P2(1)2(1)2(1) symmetry) of both adsorbents upon micropore filling. The adsorption. mechanism was also characterized. The first tetrachloroethene molecules adsorbs in the channel intersections of the MONO (monoclinic form with P2(1)/n11 symmetry) and ORTHO structures of silicalite-1 and ZSM-5, respectively. Then, the above mentioned structural change from ORTHO to PARA occurs, leading to a filling of Sinusoidal channels Until saturation was reached, i.e. similar to 8 molecules.uc(-1) for silicalite-1 and 6 molecules.nc(-1) for In addition simulation results indicate that the sodium cations in the ZSM-5 zeolite are located at the channel intersections during the,whole adsorption process.
引用
收藏
页码:3854 / 3865
页数:12
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