Novel cation sited in a dehydrated divalent copper-exchanged zeolite

Abstract
Single-crystal X-ray analysis has shown that in dehydrated divalent copper-exchanged faujasite the so-called site III-type cations are located at the pore entrances to the supercage and are effectively bonded to only one framework oxygen, thus being present in a highly unsaturated co-ordination geometry.
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