Abstract
Samples of two differently prepared zeolite rho loaded with different amounts of monomethylamine (MMA) were studied in their hydrated and dehydrated forms by X-ray and neutron diffraction. Both zeolites are partially dealuminated, as indicated by nonframework alumina, which is assumed to be Al2O3 or AlOOH. Series I was prepared from dry-calcined NH4-rho at 873 K, series II from steam-calcined NH4-rho at 773 K. The samples were loaded with different amounts of deuterated MMA, Rietveld refinements yielded the following results for series I (dry): (1) H3.8(H-MMA)5Cs0.2Al9Si39O2.Al2O3.28H2O, X-ray data collection at room temperature, Im3̅m, a = 14.9991 (2) Å, Rwp = 0.095; (2) composition as in (1), anhydrous and deuterated, neutron data collected at 5 K, disproportionation into two phases in I4̄3m, with a = 14.8410 (7) and 14.5273 (11) Å, Rwp = 0.038; (3) (H-MMA)8.8Cs0.2Al9Si39O96.Al2O3.25H2O, X-ray data collection at room temperature, I4̄3m, a = 14.9771 (2) Å, Rwp = 0.090. Series II (steam): (4) H0.3(H-MMA)5Cs0.7Al6Si42O96.2.5Al2O3.23H2O, X-ray data collected at room temperature, Im3̅m, a = 15.0323 (2) Å, Rwp = 0.124; (5) composition as in (4), anhydrous and deuterated, neutron data collected at 5 K, disproportionation into two phases in I4̄3m with a = 14.9151 (2) and 14.6475(8) Å, Rwp = 0.031. In the hydrated samples MMA resides on the center axis in the α-cage with the N atoms pointing to the single eight-ring; upon dehydration it migrates into the double eight-rings.