Chemical stabilization of beta-cristobalite has been achieved using tw
o methods: (1) incorporating ''stuffing'' cations Na, Ca, Cu, and Sr i
nto the cavities in the tectosilicate framework, as previously reporte
d, and (2) without ''stuffing'' cations, by substituting AlPO4 into th
e framework. XRD, TEM, FTIR, DSC, and solid-state variable-temperature
Si-29 NMR confirm that stabilization occurs by both methods. Dynamic
disorder, characteristic of the beta-cristobalite structure above the
alpha <-- --> beta phase transition, was observed via TEM in the NaAlO
2-, CaAl2O4-, and CuAl2O4-stabilized cristobalites at room temperature
. For AlPO4-stabilized material intergrowths of AlPO4 regions with a t
ridymite-type structure suppress the beta- --> alpha-cristobalite phas
e transition.