INTERACTION OF SULFATE GROUPS WITH THE SURFACE OF ZIRCONIA - AN HRTEMCHARACTERIZATION STUDY

Citation
M. Benaissa et al., INTERACTION OF SULFATE GROUPS WITH THE SURFACE OF ZIRCONIA - AN HRTEMCHARACTERIZATION STUDY, Journal of catalysis, 161(2), 1996, pp. 694-703
Citations number
21
Categorie Soggetti
Chemistry Physical
Journal title
ISSN journal
00219517
Volume
161
Issue
2
Year of publication
1996
Pages
694 - 703
Database
ISI
SICI code
0021-9517(1996)161:2<694:IOSGWT>2.0.ZU;2-W
Abstract
High-resolution transmission electron microscopy (HRTEM) has been used to characterize the morphology and the surface structure at an atomic level of sulfated zirconia and sulfate-free zirconia. Our study shows that HRTEM can be used to directly observe sulfate layers adsorbed on the surface of zirconia crystallites. The results indicate that the p resence of sulfate groups not only stabilizes the tetragonal zirconia phase, but also induces the formation of well-faceted small zirconia c rystallites. In particular, it is observed that the presence of sulfat e groups induces the preferential formation of relatively long-flat (1 10) plane of tetragonal zirconia. HRTEM images of this plane revealed the presence of an adsorbed sulfate layer. It is proposed that the geo metry of the (110) plane is such that it can accommodate sulfate group s in a two- or threefold coordination. Although, zirconia crystallites with relatively long-flat {110} planes containing adsorbed sulfate-gr oups were clearly predominant in the sulfated zirconia catalyst; its r ole in the formation of the highly acidic sites is not clear. Our stud y also reveals the presence of few zirconia crystallites containing ro ugh surfaces, crystallographically speaking high-Miller-index surfaces , which if they were to contain sulfate groups, they could be the locu s of the highly acidic sites. Thus, it is suggested that caution must be taken when performing spectroscopic studies using techniques such a s IR, NMR, XPS, and Raman to distinguish between spectator sulfate gro ups, which could be a majority if they were the ones observed on the ( 110) plane, and those participating in the formation of the highly aci dic site, which could be associated to the few high-Miller-index-conta ining zirconia crystallites. (C) 1995 Academic Press, Inc.