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Fig. 6 The Ni 2 In (BaF 2 -HP,
Pnma ) net and some related
structures of oxoacid salts:
Na 2 CO 3 ( C 2/ m ); b -Ca 2 SiO 4
(larnite) and isostructural
M 2 SiO 4 ,S 2 GeO 4
( P 2 1 / n );
Na 2 SO 4
and
isostructural
M 2 SO 4 ( Cmcm )
Table 4 Underlying nets in orthoborates
Underlying net
Orthoborate
Correspondence
BO 3
coordination type
T 6 ;T 33 ;T 42
pcu-b (NaCl)
MBO 3 (M ¼ Al, Ti, V, Cr, Fe,
Sc, In, Bi, La, Ce, Nd, Dy,
Sm, Eu, Yb, Lu)
Normal
T 33
nia (NiAs)
MBO 3 (M
¼
La, Ce, Nd)
Anti
T 6
cor (
a
-Al 2 O 3 ) 3 (BO 3 ) 2 (M
¼
Ca, Sr, Hg, Eu)
Anti
T 71
K 2 Te 3
M 3 (BO 3 ) 2 (M
¼
Mg, Mn, Ni, Cd)
Anti
T 9
gfy (UCl 3 )
Tl 3 BO 3
Anti
T (12)
sqc 908
Ag 3 BO 3
The low-temperature phase of Ag 2 CO 3 also has the 5,10-coordinated underlying net,
but of the MoSi 2 structure type.
3.1.2 Orthoborates
g ¼
1:1. This is the most numerous group of orthoborates that is topologically
closely related to carbonates. Since all these orthoborates are obtained at a high
temperature and/or pressure, it is not easy to determine which phase is the most
stable at ambient conditions [ 47 ] . However, the general trend is similar to carbo-
nates: smaller M 3+ cations provide the pcu-b cation array (Fig. 3 ) , while larger rare-
earth M 3+ cations give rise to a nia aragonite-like underlying net (Fig. 4 ; Table 4 ) .
 
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