C. Bremard et al., MONTE-CARLO SIMULATIONS AND SPECTROSCOPIC STUDIES OF THE SORPTION ANDCOSORPTION OF GROUP-VI METAL HEXACARBONYLS IN FAUJASITIC ZEOLITES, Journal of the American Chemical Society, 117(36), 1995, pp. 9274-9284
Molecular simulations of the sorption and cosorption energetics and si
ting locations of M(CO)(6) (M = Cr, Mo, W) in faujasitic M'(n)FAU zeol
ites (n = 0-96, Si/Al = 100-1, extraframework cations M' = Li+, Na+, K
+, Rb+, Cs+, Mg2+, and Ca2+) have been presented in combination with D
iffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFTS), A
ttenuated Total Reflectance (ATR-FTIR), and Raman scattering experimen
tal study at low temperature. From the present Monte Carlo calculation
s and the earlier and present experimental works a coherent picture of
the sorption and the cosorption of M(CO)(6) has been drawn as a funct
ion of the Si/Al ratio of the zeolite framework, the cation size, and
the cationic site occupancy as well as the coverage of the sorbates. T
he most favorable siting regions of the completely siliceous FAU zeoli
te pore space are the windows of the supercages, with intercage and in
tracage rapid motions of the M(CO)(6) molecules. In aluminated M'(n)FA
U zeolites the calculated average energy provides evidence to the cont
ribution of significant site II cation/sorbate interactions whereas th
e site I,I' cation/ sorbate and sorbate/sorbate interactions remain we
ak even at high loading. In M'(56)FAU zeolites with bulky cations (M'
= K+, Rb+, Cs+), the M(CO)(6) molecules are rigidily held within the w
indows of the supercages to the six octahedral disposed site II cation
s. The sorption sites are randomly filled from low coverage to saturat
ion. In M'(56)FAU zeolites with small cations (M' = Li+, Na+), the dis
tribution of positions occupied by M(CO)(6) is located in the vicinity
of the windows. It is suggested that M(CO)(6) is predominently entrap
ped as an isolated molecule at low coverage whereas at high loading th
e filling is primarily pairwise. In M'(28)FAU zeolites with site II pa
rtial occupancy (M' = Mg2+, Ca2+), the distribution of positions occup
ied by M(CO)(6) is located in the vicinity of the windows in two sligh
tly different sorption sites.