Intergrowths of cubic (fau) and hexagonal (em t) structural phases in a number of faujasite-related zeolite materials have been studied using transmission electron mi croscopy, and high-resolution powder X-ray diffraction. In Y, CSZ-1, CSZ-3, ZSM-2, ZSM-3, ZSM-20, ECR-35, ECR-30 and EMC-2 materials, the fau and emt com ponents segregate non-randomly into contiguous blocks. This segregation is most pronounced in ZSM-20 and ECR-35. ECR-30 and EMC-2 are both predominantly emt framework materials, within which fau intergrowths occur in clumps of 1, 2 or 3 layers. No evidence is found for extended superlattice ordering of intergrowths. Intergrowth segregation acts to reduce both the configurational entropy associated with the stacking statistics and the elastic energy associated with coherency strain.
In tr o d u c tio nIt was first reported by Breck (1974) that the cubic faujasite (fau) framework could support recurrent twinning on 111 planes to produce a hexagonal framework struc ture. The hexagonal framework possesses straight 12-ring channels axially aligned along the six-fold axis, each channel being connected to its six neighbours through the 12-ring apertures of a secondary cage. It has been referred to in the literature as 'Breck structure 6' (bss)-in reference to Breck's list of six frameworks, including the faujasite framework fau, that can be generated by connecting sodalite cages (Breck 1974), and, erroneously, as 'hexagonal faujasite'. More recently, the Structure Com mission of the International Zeolite Association has assigned the framework code emt to the hexagonal polymorph, with material EMC-2 designated as the type species (Meier & Olson 1992; Newsam Sz Treacy 1993).Evidence for the existence of domains of the emt framework was originally limited to sightings of twin faults in fau framework materials. The framework in the vicinity of each twin plane would support cages that, locally, were topologically equivalent to those found in the emt framework. Audier et al. (1982) observed low densities of 111 twin planes in transmission electron micrographs of zeolite Y samples. In some materials, twin faults were observed to occur close to one another, suggestive of a superlattice structure (Audier et al. 1982). Kokotailo & Ciric (1976) reported a recurrently twinned ca. 7 nm superstructure in ZSM-3 materials based on selectedarea electron-diffraction data, implying that ZSM-3 contained ca. 20% of EMT-type cages.