Abstract: | From a comparison of the X-ray difractograms for various ZSM-5 zeolites the isomorphous substitution of framework Si4+ by large cations (Al3+, Ga3+, Fe3+) is suggested to be ordered as contrasted to the statistical substitution by small ones (B3+).
ZSM-5 , Si4+ (Al3+, Ga3+, Fe3+) , (B3+). |