The influence of extra-framework cations on the intrinsic negative thermal expansion (NTE) of calcined ultrastable and lanthanum-exchanged zeolites Y was analysed. High-temperature thermal behaviour, cationic migration and dealumination were examined by in situ high temperature X-ray powder diffraction and thermogravimetric (TG) analyses. We analysed protonated ultrastable zeolite Y and zeolite Y containing 13% \(\hbox {La}_{2}\hbox {O}_{3}\) (LaY), and investigated how the presence of \(\hbox {La}^{3+}\) influences thermal behaviour of zeolite Y. Uncalcined LaY was also analysed to observe the \(\hbox {La}^{3+}\) migration before calcination. Mass loss up to \(990{^{\circ }}\hbox {C}\) was accompanied by TG analyses. X-ray powder diffraction data were analysed by Rietveld method. Our data show that lanthanum migration from supercages to sodalitic cavities is not reversible. However, some \(\hbox {La}^{3+}\) migration occurs above \(400{^{\circ }}\hbox {C}\) and we observe emptying of site \(\hbox {I}{'}\), migration to site I and to some extent to site \(\hbox {II}{'}\). Furthermore, we examined the dealumination process as well. Both samples show two distinct thermal behaviours, positive or near-zero thermal expansion up to \(500{^{\circ }}\hbox {C}\) and NTE above this temperature. Together with intrinsic NTE in faujasite type zeolites, the dealumination process is largely responsible for NTE at high temperatures.
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