Molecular modeling of carbonaceous compounds formed inside the pores of FER zeolite during skeletal isomerization of n-butene

Citation
P. Andy et al., Molecular modeling of carbonaceous compounds formed inside the pores of FER zeolite during skeletal isomerization of n-butene, J PHYS CH B, 104(20), 2000, pp. 4827-4834
Citations number
39
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF PHYSICAL CHEMISTRY B
ISSN journal
15206106 → ACNP
Volume
104
Issue
20
Year of publication
2000
Pages
4827 - 4834
Database
ISI
SICI code
1520-6106(20000525)104:20<4827:MMOCCF>2.0.ZU;2-A
Abstract
Molecular mechanics calculations of isobutene, its dimer (2,4,4-trimethyl-2 -pentene), its trimer (2,4,4,6,6-pentamethyl-2-heptene), and seven families of coke molecules formed during n-butene isomerization were carried out wi thin the ferrierite pore system. Monte Carlo docking showed that most of th ese molecules are well solvated by the zeolite framework and are preferenti ally sited within one or two intersections along the 10-membered ring chann el. The locations of most of the larger coke molecules in two adjacent inte rsections account for the significant influence of dehydrogenative coupling in the formation of coke molecules in FER-structured zeolites. The stabili ty of the butene dimer is close to that of molecules of carbonaceous compou nds, which are known to be trapped inside the zeolite pores, whereas the st ability of a trimer intermediate is much lower. This is consistent with the bimolecular isomerization mechanism and autocatalytic process proposed pre viously. Of the coke molecules investigated, only,fluoranthene is unstable in the FER pores. This suggests that fluoranthene is not completely located in the zeolite pores, and it is proposed that this molecule is formed at t he pore mouth. The results of simulated diffusion calculations confirmed th e minimum energy locations of biphenyl and naphthalene found by docking and were consistent with experimental data regarding the mobility of these two species in ferrierite.