Chemistry Reference
In-Depth Information
Fig. 13 The TiO 2 (rutile) net
( P 4 2 / mnm ) and some related
structures of oxoacid salts:
Ti(SeO 3 ) 2 ;
-Cu(IO 3 ) 2 and
isotypic M(IO 3 ) 2 ( P 2 1 )
a
Table 8 Underlying nets in chlorates, bromates, and iodates
Underlying
net
Chlorate/bromate/iodate
Correspondence LO 3
coordination
type
T 33 ,T 6 ,T 42
pcu-b
(NaCl)
MClO 3 ; MBrO 3 (M
¼
Na, K, Rb, Tl); MIO 3
Normal
(M
¼
K, Tl)
T 6
nia (NiAs)
MIO 3 (M
¼
Li, Na)
Normal
T 4
crb (CrB 4 )
b
-LiIO 3
Normal
T 5
nia-5,5-
Pna 2 1
g
-LiIO 3
T 6
FEQWOO
NaIO 3
T 6
Tl 2 S 2
AgClO 3
Normal
T 331 ,T 61 ,
T 52
kwh
CsBrO 3 ; MIO 3 (M
¼
K, Rb)
T 331
bcu-7- Pnnm CsIO 3
T 3
rtl (TiO 2 ,
rutile)
M(IO 3 ) 2 (M
¼
Mg, Mn, Co, Cu)
Normal
T 31
scu (BaTe 2 )
Ba(LO 3 ) 2 (L ¼ Br, I)
Normal
T 31 ,T 4
sqc 1964
M(ClO 3 ) 2 (M ¼ Sr, Ba, Pb); Ba(BrO 3 ) 2
B 2
acs (WC)
M(IO 3 ) 3 (M ¼ Al, Fe, Ga, In)
Normal
Table 7 ); they emerge in
modifications of Sn(SeO 3 ) 2 , respectively. The
pyrite cation array was also revealed for the M(NO 3 ) 2 compounds (Fig. 11 ; Table 6 );
the relation between
a
and
b
b
-Sn(SeO 3 ) 2 and M(NO 3 ) 2 was reported in [ 59 ] .
3.2.2 Chlorates, Bromates, and Iodates
The relations of chlorates, bromates, and iodates to binodal nets are quite similar to
sulfites and selenites owing to the like geometry and coordination capability of their
oxoanions; the differences are mainly caused by a smaller charge of the chlorate-,
bromate, or iodate oxoanions compared to sulfite or selenite ones and, hence, other
possible g ratios (Table 8 ) .
g ¼
1:1. The general trend in the cation array topology follows the features
described in the previous part. Large alkali cations promote the pcu-b underlying
net, while smaller ones tend to form the NiAs-like underlying net. In both cases, the
underlying nets are geometrically distorted in comparison with the ideal pcu-b and
 
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