Chemistry Reference
In-Depth Information
2.4 The Opposite Way: From Olivine to Fluorite
Until here, we have dealt with the olivine
spinel transition path. Now we will
discuss the phases located on the upper row of Scheme
1
, i.e. the phases existing in
the olivine
!
fluorite path.
phases, i.e. III-(
!
C
mcm, olivine-related) (463 K), II-(
P
nma, olivine-like) (493 K)
and I-Na
2
SO
4
(
restrict our comments to the hexagonal phase I-Na
2
SO
4
whose Na
2
S subarray is
As stated above, the pressure-induced thenardite
P
!
spinel transition involves the
simultaneous TiSi
2
!
MgCu
2
-type transition in the cation arrays. This transforma-
tion clearly illuminates that the structure of thenardite is midway between olivine
exerted by oxygens is released, giving rise to the olivine-related structures of the III,
II and I phases, with the simultaneous TiSi
2
!
Ni
2
In transition of the Na
2
S
subarray. The exact coincidence of both the structure of I-Na
2
SO
4
and that of
In this context, one would expect that, at higher temperatures (equivalent to
lower pressures), I-Na
2
SO
4
could further transform into a
-K
2
SO
4
type (with the
Na
2
SO
4
, but the transformation occurs in the ternary sulphate KLiSO
4
above
expected to provide new insights about these transitions. We discuss it below in
Sect.
5
.
b
a
b
a
Na
c
b
Fig. 6 The structures of I-Na
2
SO
4
(a) and that of the HP-Na
2
S(b) projected on the (110) plane of
the hexagonal (P6
3
/mmc) cells, showing the identical arrangement of both Na
2
S arrays. The figure
emphasizes the Na
6
trigonal prisms which are filled by S atoms (
yellow spheres
)inNa
2
S(b) and
by (SO
4
) groups in Na
2
SO
4
(a), where the rotational disorder is made evident