Structural changes proceeding in gallium orthophosphate crystals under ther
mal treatment have been studied by means of thermoanalytical methods and X-
ray diffraction. The samples were characterized with respect to their water
content by means of IR absorption. The occurrence of structural changes ha
s been investigated as a function of thermal history, annealing temperature
, annealing duration, and cooling rate. Freshly crystallized material shows
always the low-quartz analogue modification, During the first heating a tr
ansformation into the high-cristobalite form proceeds at about 970 degrees
C. This structural change is connected with a weight loss and the emanation
of vapor phase species, both indicating the release of water from the samp
les. Cooling down the high-cristobalite form can lead either to the metasta
ble low-cristobalite or the thermodynamically stable low-quartz modificatio
n. The cooling rate is the deciding factor for the occurrence of one or the
other phase. The stability range of crystals originally in the low-cristob
alite form has been studied by various annealing procedures. It is conclude
d that the low-quartz structure is thermodynamically stable and can be deli
berately obtained between room temperature and about 930 degrees C, while t
he high-cristobalite modification is stable at higher temperatures. The low
-cristobalite form, observed at room temperature nearly without any excepti
on after a first high-temperature treatment, is only metastable. Its occurr
ence can be suppressed by proper thermal processing. (C) 2000 Academic Pres
s.