H. Graetsch, CHARACTERIZATION OF THE HIGH-TEMPERATURE MODIFICATIONS OF INCOMMENSURATE TRIDYMITE L3-T-O(MX-1) FROM 25-DEGREES-C TO 250-DEGREES-C, The American mineralogist, 83(7-8), 1998, pp. 872-880
Incommensurate tridymite L3-T-o(MX-1) shows a cascade of five phase tr
ansitions at 65, 110, 150, 200, and 380 degrees C upon heating. The X-
ray diffraction patterns were investigated with a Buerger precession c
amera revealing a sequence of four incommensurate phases in the range
from room temperature to 200 degrees C. The phases formed between 65 a
nd 110 degrees C and between 110 and 150 degrees C are new modificatio
ns of tridymite. At 65 degrees C the monoclinic tridymite L3-T-o(MX-1)
phase undergoes a first-order transformation to an orthorhombic phase
. The incommensurate structural modulation of the room-temperature pha
se with the wavevector q(1) = 0.663 a -0.498 c* flips to q(2) = 0.042
a -0.388 c*. Simultaneously, a commensurate modulation with tripled
b lattice parameter is formed. The wavelengths of both modulations do
not depend appreciably on the temperature. The incommensurate modulati
on discontinuously disappears near 110 degrees C whereas the commensur
ate modulation along the b axis becomes non-integral with a temperatur
e-dependent wavelength varying between 115 and 100 Angstrom. At 150 de
grees C the symmetry is reduced to monoclinic again with gamma = 90.4
degrees. Between 150 and 200 degrees C the monoclinic angle gradually
decreases to 90 degrees and the wavelength of the modulation from abou
t 90 to 65 Angstrom. At higher temperatures, the satellite reflections
fade into weak streaks and the normal orthorhombic high-temperature m
odification of tridymite is formed. The phase transitions are reversib
le upon cooling except for the first transformation that is partly irr
eversible for single crystals and reversible but incomplete for pulver
ized material at room temperature.