High-pressure X-ray diffraction study of potassium chromate: pressure-induced orientational disorder and its implications for amorphization in A(2)BX(4) compounds
Cm. Edwards et al., High-pressure X-ray diffraction study of potassium chromate: pressure-induced orientational disorder and its implications for amorphization in A(2)BX(4) compounds, J PHYS CH S, 60(4), 1999, pp. 529-538
The high-pressure behaviour of potassium chromate, K2CTO4, has been investi
gated by angle-dispersive X-ray diffraction in a diamond-anvil cell. K2CrO4
, a pseudoscheelite salt, was found to be highly compressible with a bulk m
odulus B-0 = 26(2) GPa, with B-0(1) = 6.0(5) GPa; however, no pressure-indu
ced phase transition was observed up to 52 GPa. The pressure dependences of
the cell constant ratios, a/b and (a + b)/c, were found to be the reverse
of those for AX(2) compounds under compression, due to the differences in t
he nature of the constituent ions. A gradual decrease in the relative inten
sities of several diffraction peaks was observed, beginning above 16 GPa. O
n comparison with calculated diffraction patterns, the decrease in intensit
y under compression was shown to be consistent with the disordering of the
chromate ion tetrahedra. Since the tetrahedra are small compared with the c
avity in which they are located, pressure-induced orientational disordering
can occur initially without disruption of the metal sub-lattice. Pressure-
induced disordering of the BX4 tetrahedra is the first step in the amorphiz
ation of A(2)BX(4) compounds. (C) 1999 Elsevier Science Ltd. All rights res
erved.