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Figure 3
Comparison of the observed (crosses) and calculated (solid line) powder diffraction patterns of high-temperature AlPO4 tridymite (a) at 473 K and (b) at 463 K. The arrows in (b) point to weak satellite reflections. The difference patterns are shown below. The short bars indicate the positions of the reflections of corundum (first row) and tridymite (second row).

Journal logoSTRUCTURAL
CHEMISTRY
ISSN: 2053-2296
Volume 58| Part 1| December 2002| Pages i18-i20
doi:10.1107/S0108270101015773
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