An in-situ X-ray powder diffraction study of the adsorption of hydrofluorocarbons in zeolites

Citation
Mf. Ciraolo et al., An in-situ X-ray powder diffraction study of the adsorption of hydrofluorocarbons in zeolites, J PHYS CH B, 105(13), 2001, pp. 2604-2611
Citations number
21
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF PHYSICAL CHEMISTRY B
ISSN journal
15206106 → ACNP
Volume
105
Issue
13
Year of publication
2001
Pages
2604 - 2611
Database
ISI
SICI code
1520-6106(20010405)105:13<2604:AIXPDS>2.0.ZU;2-Y
Abstract
A time resolved in-situ synchrotron X-ray powder diffraction study of hydro fluorocarbon (HFC)-134 (CF2HCF2H) and -134a (CF3CFH2) adsorption on NaY has been performed, as a function of the temperature of the zeolite molecular sieve. Use of an image plate, allowed kinetic processes to be followed with a resolution of the order of a few seconds. The 111 reflection of the zeol ite framework is very intense and particularly sensitive to adsorption of g ases, whereas the weaker 220 reflection is fairly insensitive to gas sorpti on. The adsorption process could, therefore, be readily monitored by using a ratio of the integrated intensities of these two reflections. This ratio was found to be an accurate measure of gas loading level and loading levels could be estimated from this ratio by using a calibration curve establishe d with samples loaded es-situ. Furthermore, good agreement was found betwee n the experimentally measured value of this ratio, and that obtained by cal culating the 111 and 220 structure factors from our earlier structural mode l for the HFC-134 bound to NaY (Grey, C. P.; Poshni, F. I.; Gualtieri, A. F .; Norby, P.; Hanson, J. C.; Corbin, D. R. J. Am. Chern. Sec. 1997, 119, 19 81). A contraction of the unit cell parameter was observed that correlated with the HFC loading level. This contraction occurred abruptly at room temp erature but was both smoother and slower at higher temperatures (100 degree sC). The kinetics of sorption depended strongly on temperature, lower tempe ratures reaching equilibrium more rapidly. This result was explained by an increase in the interparticle diffusion rate at higher temperatures, so tha t equilibrium is not reached until all the zeolite particles in the whole c apillary tube are uniformly loaded with HFC molecules. At low temperatures, the HFC molecules are strongly bound to the crystallite particles so that the adsorption front fills the particles sequentially, moving steadily and rapidly through the sample.