Journal of Applied Crystallography

Volume 30, Part 4 (August 1997)


research papers



J. Appl. Cryst. (1997). 30, 467-475    [ doi:10.1107/S0021889897001672 ]

The Quantification of Different Forms of Cristobalite in Devitrified Alumino-Silicate Ceramic Fibres

M. A. Butler and D. J. Dyson

Abstract: When heat treated, amorphous alumino-silicate fibres will devitrify into crystalline phases which on cooling become stable at room temperature. X-ray diffraction has been used to identify and quantify the phases present in such products; mullite and two distinct forms of cristobalite have been observed. One form of cristobalite has been identified as [alpha]-cristobalite, the second form has been designated as [alpha]'-cristobalite. An internal standard approach was used to enable calibration curves to be obtained for the three crystallite phases, including the [alpha]'- cristobalite for which no commercially available standard exists. The accuracy of the methods was estimated as ± 5 wt% for all three crystalline phases present. This was achieved by quantifying the proportion of [alpha]'-cristobalite in a standard alumino-silicate fibre after heat treatment for 48 h at 1773 K and then using this material as the `standard' for [alpha]'-cristobalite. This `standard' contained 32.9 wt% [alpha]'-cristobalite, 1.6 wt% [alpha]-cristobalite and 65.5 wt% mullite. The exact nature of the [alpha]'- cristobalite phase has also been examined using high-temperature X-ray diffraction and differential scanning calorimetry. It has been shown to be more similar in nature to [alpha]-cristobalite than [beta]-cristobalite since it undergoes an [alpha]' [rightwards arrow] [beta] phase transition on heating. Compared with [alpha]-cristobalite it has a different lattice size, and both the temperature and enthalpy of the [alpha]' [rightwards arrow] [beta] phase transition are lower than for the [alpha] [rightwards arrow] [beta] phase transition. It has been proposed that the [alpha]'-cristobalite observed is a defect form of [alpha]-cristobalite but with a constant amount of defects/substituted cations which gives it a well defined and consistent structure.

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