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Far infrared study of cation motion in dry and solvated mono- and divalent zeolites x and y. Technical report

Technical Report ·
OSTI ID:7220866
Far infrared ion motion bands have been observed and assigned in the spectra of dry synthetic zeolites X and Y containing Li/sup +/, Na/sup +/, K/sup +/, Rb/sup +/, Cs/sup +/, Ag/sup +/, Ca2/sup +/, Sr2/sup +/, and Ba2/sup +/ cations. The site I' and site II cation vibrational bands overlap and form the strongest feature in the spectra of samples exchanged with monovalent ions. The site I cation band appears at lower frequency than the site II envelope in these samples, but in divalent ion exchanged zeolites the opposite order occurs. A very low frequency site III cation band, typical of monovalent X zeolites, has been observed in CsY. For a given cation, the frequency on X is higher than on Y due to the higher framework charge of X zeolites. The vibrational frequencies also follow an approximate m raised to minus 1/2 power dependence for the two types of cation and the two forms of the zeolite. Solvation of the monovalent zeolites with H/sub 2/O, THF, DMSO, pyridine, and CH/sub 2/Cl/sub 2/ results in the appearance of a new band at higher frequency than the ion-framework modes which concurrently diminish in intensity, especially the site III band. The high frequency band is due to ion motion in a solvation shell which is unsymmetric at low hydration levels and at all solvation levels with organic adsorbates.
Research Organization:
Brown Univ., Providence, RI (USA). Dept. of Chemistry
OSTI ID:
7220866
Report Number(s):
AD-A-038665
Country of Publication:
United States
Language:
English