Samples of two differently prepared zeolite rho loaded with different
amounts of dimethylamine (DMA) were studied in their hydrated forms by
X-ray diffraction. Both zeolites are partially dealuminated, as indic
ated by nonframework Al which is assumed to be Al2O3 or AlOOH. Series
I was prepared from dry-calcined NH4-rho at 873 K, series II from stea
m-calcined NH4-rho at 773 K. The samples were loaded with different am
ounts of DMA. Rietveld refinements yielded the following results for s
eries I: (1) H-3.8(H-DMA)(5)Cs0.2Al9Si39O96.Al2O3.21H(2)O, X-ray data
collection at room temperature, <Im(3)over bar m>, a = 15.0590 (2) Ang
strom, R-wp = 0.089; (2) (H-DMA)(8.8)-Cs0.2Al9Si39O96.Al2O3.18H(2)O, X
-ray data collection at room temperture, <Im(3)over bar m>, a = 15.068
0 (2) Angstrom, R-wp = 0.091. Series II: (3) 0.3(H-DMA)(5)Cs0.7Al6Si42
O96.2.5Al(2)O(3).24H(2)O, X-ray data collection at room temperature, <
Im(3)over bar m>, a = 15.096 (2) Angstrom, R-wp = 0.120. DMA resides o
n the center axis through the alpha-cage with the N atoms pointing to
the single eight-ring and the two methyl groups oriented towards the c
enter of the alpha-cage.