“…However, in the case of monovalent cation forms of zeolite X, a significant proportion of the cations are often undetected in X-ray studies. In hydrated NaX, KX, and TlX, for example, the proportion of undetected cations is almost 50%, leading Baur to conclude that many of the water molecules and exchangeable cations in faujasite zeolites move freely through the aluminosilicate framework. The dehydrated forms of zeolites find utility in a number of commercial separation processes, including air − and hydrocarbon separations, and a comprehensive determination of the cation positions in such materials is an important prerequisite for understanding their properties. , It is surprising to find, therefore, that in the prototypical system, NaX, where the numbers of cations in the SI, SI‘, and SII sites (Figure ) appear to be well-established, the precise location of the remaining cations remains uncertain.…”