An accurate knowledge of zeolite structure is required for understanding th
eir selective sorption capacities and their catalytic properties. In partic
ular, the positions of the exchangeable cations and their interactions with
the framework are essential. The present study deals with the accurate cry
stal structure determination of a fully exchanged and fully dehydrated CaA
zeolite (Ca48Al96Si96O384,Fm (3) over bar c, a = 24.47 Angstrom) using sing
le-crystal high-resolution synchrotron X-ray diffraction [(sin theta/lambda
)(max) = 1.4 Angstrom(-1)]. It is shown that cation exchange severely disto
rts the skeleton, especially around the O2 atom. The high-resolution synchr
otron data reveal that this latter O atom is disordered and lies out of the
mirror plane it occupies in other A-type zeolites. This feature is related
to that observed for Ca2+ cations.