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Fluorite-related one-dimensional units in natural bismuth oxysulfates: the crystal structures of Bi 14 O 16 (SO 4 ) 5 and Bi 30 O 33 (SO 4 ) 9 (AsO 4 ) 2
The crystal structures of two new natural Bi oxysulfates with the formula Bi
14
O
16
(SO
4
)
5
[labelled
new phase I
; monoclinic, space group
C
2,
a
= 21.658 (4),
b
= 5.6648 (9),
c
= 15.092 (3) Å, β = 119.433 (11)° and
Z
= 2] and Bi
30
O
33
(SO
4
)
9
(AsO
4
)
2
[labelled
new phase II
; triclinic, space group
P
1,
a
= 5.670 (3),
b
= 13.9408 (9),
c
= 22.7908 (18) Å, α = 80.903 (5), β = 82.854 (14), γ = 78.27 (2)° and
Z
= 1] from the high-temperature fumarole deposit of the La Fossa crater at Vulcano (Aeolian Islands, Italy) are reported. The structures are built up by a combination of fluorite-related Bi—O units and isolated (SO
4
)
2−
tetrahedra (
new phase I
) or both (SO
4
)
2−
and (AsO
4
)
3−
tetrahedra (
new phase II
). Owing to the effect of stereoactive lone pairs of Bi
3+
, Bi—O units in both the structures can be suitably described in terms of oxo-centered OBi
4
tetrahedra. The structure of Bi
14
O
16
(SO
4
)
5
is based upon one-dimensional [O
16
Bi
14
]
10+
ribbons formed by six chains of edge-sharing OBi
4
tetrahedra extending along [010]. In the structure of Bi
30
O
33
(SO
4
)
9
(AsO
4
)
2
the same ribbon type coexists with another one-dimensional ribbon formed by seven chains of edge-sharing OBi
4
tetrahedra and with the composition [O
17
Bi
16
]
14+
. Ribbons of the same type are joined by (SO
4
)
2−
and (AsO
4
)
3−
tetrahedra along [010] – if a reduced triclinic unit-cell setting is considered – so forming two different (001) slabs which alternate to each other along [001] and are joined by additional (SO
4
)
2−
tetrahedra.
New phase I
represents the natural analogues of synthetic Bi
14
O
16
(SO
4
)
5
, but with an ordered structure model.