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omitted. Note that this topology differs from other 5,10-coordinated nets (alb and
Zn
2
SiO
4
-II, has a 4,8-coordinated
sqc
1964 underlying net that we saw in chlorates
g
¼
4:3. Bi
4
(SiO
4
)
3
(eulitite) and isostructural Bi
4
(GeO
4
)
3
have a Th
3
P
4
-like
3.3.2 Orthophosphates and Orthoarsenates
g
¼
1:1. In this group of oxoacid salts, the pcu-b and nia underlying nets are again
observed (Table
10
). Orthophosphates and orthoarsenates with small trivalent
well-known relations between these groups of compounds [
68
].
Orthophosphates and orthoarsenates with tetrahedrally coordinated M
3+
cations
represent a large group of silica-like structures most of which are microporous
Table 10 Underlying nets in orthophosphates and orthoarsenates
Underlying net
Orthophosphate/orthoarsenate
Correspondence XO
4
coordination
type
K
42
pcu-b (NaCl)
BiPO
4
-HT
Normal
K
6
nia (NiAs)
MPO
4
(M
¼
Al, In, Ti, V, Cr, Fe,
Tl); MAsO
4
(M
Normal
¼
Cr, Mn)
K
8
lsz
MPO
4
(M
¼
Yb, Lu); MAsO
4
Normal
(M
¼
Bi, Sm)
K
61
,K
52
bcu-7-
P
2
1
/
c
(RhSi)
MPO
4
(M
Bi, La, Ce, Pr, Nd,
Sm, Eu, Gd); MAsO
4
(M
¼
Normal
¼
Bi,
La, Ce, Nd) (monazite type)
K
42
msw
MPO
4
(M
Sc, Y, Tb, Dy, Ho, Er,
Tm, Lu); MAsO
4
(M
¼
Sc, Y,
Sm, Eu, Tb, Dy, Ho, Yb, Lu)
¼
K
42
sma
MPO
4
(M
¼
La, Ce, Nd)
K
5
nia-5,5-
P
2
1
/
c
FeXO
4
(X
¼
P, As)
K
4
dia-b (ZnS, sphalerite) MPO
4
(M
¼
Al, Ga); AlAsO
4
Normal
K
4
qtz (
a
-HgS)
MPO
4
(M
¼
Al, Fe, Ga); MAsO
4
Normal
(M
¼
Al, Ga)
K
4
lon (ZnS, wurtzite)
AlPO
4
Normal
K
4
alw (Rh
2
O
3
-HP)
Sb
2
(PO
4
)
3
Normal
K
4
cor (
a
-Al
2
O
3
)
Nb
2
(PO
4
)
3
Normal
K
61
XEBHOB
M
3
(PO
4
)
2
(M
¼
Mg, Co, Zn);
Zn
3
(AsO
4
)
2
K
(12)
Cu
3
Sb
Li
3
XO
4
(X
¼
P, As)
Normal
K
(12)
ith (Cr
3
Si)
Ag
3
XO
4
(X
¼
P, As)
Normal
K
68
wzz
K
3
AsO
4