Chemistry Reference
In-Depth Information
The conclusion is that in both Ca
2
SnO
4
and Mn
2
GeO
4
, the insertion of an
additional Ca (Mn) atom into a hypothetical CaSn (MnGe) subarray stabilizes the
TiSi (FeB type) structures of their respective CaSn and MnGe moieties.
9 The Structure of Ba
2
SnO
4
Ba
2
SnO
4
and the isostructural Ca
2
GeO
4
compounds are the final step in the long
4/mmm) and
(Sect.
9.2
)
.
The classical description of this structure consists of an intergrowth of perov-
skite-like blocks of composition BaSnO
3
and fragments of BaO (NaCl type). Both
fragment is outlined in a unit cell of the rocksalt BaO structure in Fig.
27c
. These
The other component of the structure, the BaSnO
3
-blocks, are formed by slightly
distorted cubes of Ba atoms (4.14
I
3.88
˚
), centred by the Sn atoms. The
O atoms form octahedra around the Sn atoms. This is, in fact, a distortion of the
4.14
Fig. 27 (a) The structure of Ba
2
SnO
4
(I4/mmm), viewed along the
a
axis, showing the perovskite-
like blocks of composition BaSnO
3
alternating, along c, with fragments of the BaO (rocksalt)
structure. The atoms are Ba (
green
), Sn (
grey
) and O (
red
). (b) A view of the two fragments. The
upper side
shows a BaSnO
3
perovskite-like fragment. The
lower part
is a fragment of the BaO
represented in (c). (c) A unit cell of the rocksalt BaO structure. The
blue lines
remark the structural
fragments forming part of Ba
2
SnO
4
. The Ba-Ba distances in the BaO fragment are 4
4.14 and
4.02
˚
(mean 4.08
˚
)
4