Westfälische Wilhelms-Universität
Münster
|
Sonderforschungsbereich 458 Ionenbewegung in Materialien mit ungeordneten Strukturen - vom Elementarschritt zum makroskopischen Transport - Schlossplatz 4/7 48149 Münster Sprecher: Prof. Dr. Klaus Funke |
Tel. (0251) 83-23402
Fax: (0251) 83-23403 e-mail: sfb458gs@uni-muenster.de www: http://www.uni-muenster.de/Chemie/PC/sfb |
|
Forschungsschwerpunkte 2001 - 2002 Sonderforschungsbereiche
|
||||
Struktur, Dynamik und Phasenübergänge anorganischer plastischer Kristalle
Phase
relations and
kinetics in the fast-ion conductor system
Na3PO4-Na2SO4
Analysis of in-situ XRD and neutron powder diffraction data for different
compositions in the
Na3PO4-Na2SO4 system established that
the solubility of
Na2SO4 in the low-temperature phase of
Na3PO4 is very
low. Samples of the Na3PO4-Na2SO4
solid solution
display a mixture of high and low-temperature phases. The transition temperature of the reaction
from high to
low-temperature phase decreases linearly with increasing Na2SO4
content.
Extrapolation implies that the low-temperature g phase should be
stabilized by
addition of ~23 % Na2SO4. Therefore, the experimentally
observed
stabilization of
g in the 10 % sample is a purely kinetic effect. There are
two
reasons for these
cumbersome kinetics. Firstly, there is a significant energy barrier associated with formation of
a within a matrix of g. This is not
surprising given the
large difference in unit cell volume for the two phases. Secondly, taking into account the low
solubility of
Na2SO4 in a, any ordering of the
PO4
tetrahedra requires either diffusion of S away from the nucleus or the pre-existence of a
Na3PO4 rich cluster.
Samples containing less than 10 % Na2SO4
in x-ray
diffraction
experiments display prominent a and g peaks with
additional peaks corresponding to the occurrence of two additional phases named bm and bt. The similarity in lattice parameters implies that b is more closely related to g than a. The transition g -> b is
first-order in character and kinetically favoured over the g ->
(a + g) transition on cooling. It is not,
therefore, a simple
displacive distortion of g and will involve diffusion of cations
and possibly anion
rotation.
Drittmittelgeber: Beteiligte Wissenschaftler: Veröffentlichungen: |
||||