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inorganic compounds
Na3Co2(AsO4)(As2O7): a new sodium cobalt arsenate
aLaboratoire de Matériaux et Cristallochimie, Faculté des Sciences, El Manar II, 2092 Tunis, Tunisia, and bInstitut Préparatoire aux Etudes d'Ingénieurs d'El Manar, BP 244 El Manar II, 2092 Tunis, Tunisia
*Correspondence e-mail: abderrahmen.guesmi@ipeim.rnu.tn
In the title compound, trisodium dicobalt arsenate diarsenate, Na3Co2AsO4As2O7, the two Co atoms, one of the two As and three of the seven O atoms lie on special positions, with site symmetries 2 and m for the Co, m for the As, and 2 and twice m for the O atoms. The two Na atoms are disordered over two general and special positions [occupancies 0.72 (3):0.28 (3) and 0.940 (6):0.060 (6), respectively]. The main structural feature is the association of the CoO6 octahedra in the ab plane, forming Co4O20 units, which are corner- and edge-connected via AsO4 and As2O7 arsenate groups, giving rise to a complex polyhedral connectivity with small tunnels, such as those running along the b- and c-axis directions, in which the Na+ ions reside. The structural model is validated by both bond-valence-sum and charge-distribution methods, and the distortion of the coordination polyhedra is analyzed by means of the effective coordination number.
Related literature
For related structures, see: Ruiz-Valero et al. (1996); Ben Smail & Jouini (2005
); Guesmi & Driss (2002a
,b
). For bond-valence analysis, see: Brown (2002
); Adams (2003
). For the charge distribution method, see: Nespolo et al. (2001
); Nespolo (2001
); Guesmi et al. (2006
).
Experimental
Crystal data
|
Refinement
|
|
Data collection: CAD-4 EXPRESS (Enraf–Nonius, 1995); cell CAD-4 EXPRESS; data reduction: XCAD4 (Harms & Wocadlo, 1995
); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008
); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008
); molecular graphics: DIAMOND (Brandenburg, 2001
); software used to prepare material for publication: WinGX (Farrugia, 1999
) and publCIF (Westrip, 2010)
.
Supporting information
https://doi.org/10.1107/S1600536812027791/jj2142sup1.cif
contains datablocks I, global. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S1600536812027791/jj2142Isup2.hkl
Supporting information file. DOI: https://doi.org/10.1107/S1600536812027791/jj2142Isup3.cml
The investigated compound was synthesized by a solid state reaction from a mixture of Na2CO3 (0.46 g, Fluka, 99.0%), cobalt (II and III) oxides (0.1 g, Fluka, 99.0%, Co 71% min.) and As2O5 (0.33 g, Prolabo). The reaction mixture was heated at 673 K for 24 h and progressively at 923 K and kept at this temperature for three days. Finally, it was slowly cooled to room temperature. The obtained pink crystals were separated from the excess
by washing the product in boiling water.The non-equivalent sodium ions are inserted in the anionic framework first in two full-occupied general and special crystallographic sites. The Na1 atoms are better described by a split model with two independent general positions, refined with the same thermal paramaters. The highest Fourier peaks near the Na2A site suggests that the Na2A position deviates from the full occupancy and another partial-occupied position (Na2B) was introduced in the model, leading to a lowering of R values and residual electron density peaks.
The rich chemistry of the A–Co–P/As–O crystallographic systems (A is a monovalent cation), has been shown by the synthesis and crystal structures of several compounds with particular crystallographic properties such as: Na4Co3(PO4)2P2O7, a phosphate containing a three-dimensional system of large intersecting tunnels (Ruiz-Valero et al. 1996), AgCo3H2(PO4)3, an alluaudite-like phosphate structure (Guesmi & Driss, 2002a), K2CoP2O7, a layered tetrahedral phosphate with the mellilite structure (Guesmi & Driss, 2002b), etc.
For the case of arsenates, their main structural difference if compared to phosphates is that arsenic atoms can also adopt an octahedral coordination; it is the case for example of the oxygen-deficient layered sodium arsenate Na7As11O31 (Guesmi et al. 2006). Continuous investigations on the crystal chemistry of the arsenates are performed because arsenic is at the top of the priority of the most hazardous substances, but less is known about its crystal structures.
We are interested in the present work in the
of the new compound Na3Co2AsO4As2O7 (I). The of the isostructural Na3Ni2(As0.1P0.9)O4(As1.3P0.7)O7 compound and properties of its limiting arsenate has been studied (Ben Smail & Jouini, 2005). The chemical formula of (I) has been established as a result of the determination and the obtained structural model is validated by means of charge distribution (CD) (Nespolo et al. 2001, Nespolo, 2001) and bond valence sum methods (BVS) (Brown, 2002; Adams, 2003) as the formal charges (Q) and valences (V) agree well with the expected values (Table 1).The new compound (I) is an example of a mixed transition-metal arsenate, representing the first cobalt arsenate built up from mono- and diarsenate groups. In the asymetric unit, the
is built up from corner and edge-sharing between cobalt octahedra and arsenate groups (Fig. 1). The two crystallographically distinct cobalt atoms exhibit a slightly distorted octahedral coordination with effective coordination numbers ECoN(Co1)=5.97 and ECoN(Co2)=5.62 and weighted average distances dmed(Co1)=2.14 Å and dmed(Co2)=2.08 Å. The longest Co–O6 bond distances in the two octahedra correspond to the three-coordinated oxygen atom, related also to As1.The As1 tetrahedron, with a 2 + 2 coordination, shares its four corners with five octahedra. The As2 tetrahedron, a more precisely a trigonal pyramid (1 + 3 coordination), is more distorted with O5 as a bridging oxygen in the As(2)2O7 group (ECoN(As2)=3.89 and dmed(As2)=1.69 Å). The other six corners in the diarsenate group are common with four Co1 and two Co2 octahedra. It is worth noting that the Co2 and As1 polyhedra share a common edge which induces a strong repulsion between positive charges; this type of connection was also observed in the structure of Na4Co3(PO4)2P2O7 (Ruiz-Valero et al. 1996).
The cobalt octahedra are associated in the ab plane to form the original octahedral metallic units Co4O20 which are corner- and edge-connected via As(1)O4 and As(2)2O7 arsenate groups, giving rise to a complex polyhedral connectivity which produces small tunnels, such as those running along the b and c axis, where the sodium cations reside (Figs. 2–4).
The anionic framework can be decomposed in a succession of alternate layers in the ac plane, stacked along the crystallographic b-axis. They are built up of Co1 octahedra and As(2)2O7 groups in such a way that each octahedron is corner-shared to four diarsenate groups (Fig. 3). These layers are alternate by a chain type resulting from the connection between Co2 and As1 polyhedra and formed by the centrosymmetric cyclic units [Co2As2O14] (Fig. 4), each one of these units is connected to two neighbours by means of mixed Co–O–As bridges.
The Na1 ions are split into two independent positions near c/2, Na1B has the more distorted polyhedron and the ECoN(Na1B) is as low as 5.72. The Na2 ions are also disordered with the Na2B polyhedron sandwiched by Na2A ones which are off-centred around the Na2B positions. The motion of sodium cations within the framewok of (I) by means of theoretical studies and electrical measuremeents will be the subject of future works.
For related structures, see: Ruiz-Valero et al. (1996); Ben Smail & Jouini (2005); Guesmi & Driss (2002a,b). For bond-valence analysis, see Brown (2002); Adams (2003). For the charge distribution method, see Nespolo et al. (2001); Nespolo (2001); Guesmi et al. (2006).
Data collection: CAD-4 EXPRESS (Enraf–Nonius, 1995); cell
CAD-4 EXPRESS (Enraf–Nonius, 1995); data reduction: XCAD4 (Harms & Wocadlo, 1995); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: DIAMOND (Brandenburg, 2001); software used to prepare material for publication: WinGX (Farrugia, 1999) and publCIF (Westrip, 2010).Na3Co2(AsO4)(As2O7) | F(000) = 1096 |
Mr = 587.59 | Dx = 4.052 Mg m−3 |
Monoclinic, C2/m | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -C 2y | Cell parameters from 25 reflections |
a = 10.484 (3) Å | θ = 11.7–14.5° |
b = 16.309 (2) Å | µ = 13.87 mm−1 |
c = 6.531 (1) Å | T = 293 K |
β = 120.40 (2)° | Parallelepiped, pink |
V = 963.2 (3) Å3 | 0.20 × 0.10 × 0.10 mm |
Z = 4 |
Enraf–Nonius CAD-4 diffractometer | 998 reflections with I > 2σ(I) |
Radiation source: fine-focus sealed tube | Rint = 0.041 |
Graphite monochromator | θmax = 28.0°, θmin = 2.5° |
ω/2θ scans | h = −13→13 |
Absorption correction: ψ scan (North et al., 1968) | k = −1→21 |
Tmin = 0.168, Tmax = 0.338 | l = −8→3 |
1765 measured reflections | 2 standard reflections every 120 min |
1183 independent reflections | intensity decay: 1% |
Refinement on F2 | Primary atom site location: structure-invariant direct methods |
Least-squares matrix: full | Secondary atom site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.027 | w = 1/[σ2(Fo2) + (0.0261P)2] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.067 | (Δ/σ)max = 0.005 |
S = 1.01 | Δρmax = 0.72 e Å−3 |
1183 reflections | Δρmin = −0.80 e Å−3 |
103 parameters | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
0 restraints | Extinction coefficient: 0.00124 (17) |
Na3Co2(AsO4)(As2O7) | V = 963.2 (3) Å3 |
Mr = 587.59 | Z = 4 |
Monoclinic, C2/m | Mo Kα radiation |
a = 10.484 (3) Å | µ = 13.87 mm−1 |
b = 16.309 (2) Å | T = 293 K |
c = 6.531 (1) Å | 0.20 × 0.10 × 0.10 mm |
β = 120.40 (2)° |
Enraf–Nonius CAD-4 diffractometer | 998 reflections with I > 2σ(I) |
Absorption correction: ψ scan (North et al., 1968) | Rint = 0.041 |
Tmin = 0.168, Tmax = 0.338 | 2 standard reflections every 120 min |
1765 measured reflections | intensity decay: 1% |
1183 independent reflections |
R[F2 > 2σ(F2)] = 0.027 | 103 parameters |
wR(F2) = 0.067 | 0 restraints |
S = 1.01 | Δρmax = 0.72 e Å−3 |
1183 reflections | Δρmin = −0.80 e Å−3 |
Geometry. All e.s.d.'s (except the e.s.d. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell e.s.d.'s are taken into account individually in the estimation of e.s.d.'s in distances, angles and torsion angles; correlations between e.s.d.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell e.s.d.'s is used for estimating e.s.d.'s involving l.s. planes. |
Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2, conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > σ(F2) is used only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2 are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger. |
x | y | z | Uiso*/Ueq | Occ. (<1) | |
Co1 | 0.5000 | 0.32196 (5) | 1.0000 | 0.0091 (2) | |
Co2 | 0.29864 (9) | 0.5000 | 0.08408 (15) | 0.0090 (2) | |
As1 | 0.38970 (6) | 0.5000 | 0.67693 (11) | 0.00692 (16) | |
As2 | 0.11973 (5) | 0.33430 (3) | 0.76867 (8) | 0.00892 (14) | |
O1 | 0.5206 (4) | 0.2480 (2) | 0.7535 (6) | 0.0219 (8) | |
O2 | 0.2686 (3) | 0.3079 (2) | 0.7525 (6) | 0.0173 (7) | |
O3 | 0.2608 (5) | 0.5000 | 0.7550 (8) | 0.0097 (9) | |
O4 | 0.1460 (3) | 0.40124 (19) | 0.9821 (6) | 0.0136 (6) | |
O5 | 0.0000 | 0.3884 (3) | 0.5000 | 0.0133 (9) | |
O6 | 0.5077 (3) | 0.41858 (19) | 0.7766 (6) | 0.0126 (6) | |
O7 | 0.2869 (5) | 0.5000 | 0.3808 (8) | 0.0193 (11) | |
Na1A | 0.1740 (18) | 0.1692 (4) | 0.5940 (15) | 0.032 (2) | 0.72 (3) |
Na1B | 0.225 (3) | 0.1686 (13) | 0.617 (4) | 0.032 (2) | 0.28 (3) |
Na2A | 0.0488 (3) | 0.5000 | 0.2908 (8) | 0.0353 (11) | 0.940 (6) |
Na2B | −0.021 (6) | 0.5000 | −0.054 (13) | 0.0353 (11) | 0.060 (6) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Co1 | 0.0097 (4) | 0.0075 (4) | 0.0088 (4) | 0.000 | 0.0037 (3) | 0.000 |
Co2 | 0.0094 (4) | 0.0105 (4) | 0.0067 (4) | 0.000 | 0.0038 (3) | 0.000 |
As1 | 0.0077 (3) | 0.0073 (3) | 0.0047 (3) | 0.000 | 0.0023 (2) | 0.000 |
As2 | 0.0091 (2) | 0.0071 (2) | 0.0073 (2) | −0.00090 (15) | 0.00172 (18) | 0.00007 (17) |
O1 | 0.0297 (19) | 0.0157 (17) | 0.015 (2) | 0.0132 (15) | 0.0073 (16) | −0.0024 (15) |
O2 | 0.0091 (14) | 0.0211 (18) | 0.0157 (18) | 0.0020 (13) | 0.0018 (14) | −0.0030 (14) |
O3 | 0.0093 (19) | 0.015 (2) | 0.008 (2) | 0.000 | 0.0072 (18) | 0.000 |
O4 | 0.0163 (14) | 0.0152 (15) | 0.0089 (15) | −0.0044 (13) | 0.0061 (13) | −0.0053 (14) |
O5 | 0.0128 (19) | 0.011 (2) | 0.008 (2) | 0.000 | −0.0008 (18) | 0.000 |
O6 | 0.0114 (13) | 0.0098 (14) | 0.0158 (16) | 0.0014 (12) | 0.0064 (13) | 0.0017 (13) |
O7 | 0.014 (2) | 0.040 (3) | 0.004 (2) | 0.000 | 0.005 (2) | 0.000 |
Na1A | 0.047 (6) | 0.0192 (12) | 0.021 (2) | 0.012 (3) | 0.011 (4) | −0.0034 (12) |
Na1B | 0.047 (6) | 0.0192 (12) | 0.021 (2) | 0.012 (3) | 0.011 (4) | −0.0034 (12) |
Na2A | 0.0179 (15) | 0.0196 (17) | 0.059 (3) | 0.000 | 0.0126 (18) | 0.000 |
Na2B | 0.0179 (15) | 0.0196 (17) | 0.059 (3) | 0.000 | 0.0126 (18) | 0.000 |
Co1—O1 | 2.108 (3) | Na1A—O6viii | 2.621 (11) |
Co1—O1i | 2.108 (3) | Na1A—O2viii | 2.646 (11) |
Co1—O2 | 2.141 (3) | Na1A—O1vii | 2.682 (13) |
Co1—O2i | 2.141 (3) | Na1A—O4ix | 2.694 (10) |
Co1—O6 | 2.177 (3) | Na1A—O7viii | 2.782 (7) |
Co1—O6i | 2.177 (3) | Na1A—O6vii | 2.936 (13) |
Co2—O3ii | 1.978 (4) | Na1B—O2 | 2.39 (2) |
Co2—O7 | 2.003 (5) | Na1B—O2viii | 2.47 (2) |
Co2—O4ii | 2.126 (3) | Na1B—O4ix | 2.53 (2) |
Co2—O4iii | 2.126 (3) | Na1B—O7viii | 2.75 (2) |
Co2—O6iv | 2.201 (3) | Na1B—O1viii | 2.83 (2) |
Co2—O6v | 2.201 (3) | Na1B—O6viii | 2.87 (2) |
As1—O3 | 1.669 (4) | Na2A—O7 | 2.257 (5) |
As1—O7 | 1.671 (5) | Na2A—O5 | 2.480 (4) |
As1—O6vi | 1.704 (3) | Na2A—O5x | 2.480 (4) |
As1—O6 | 1.704 (3) | Na2A—O4xi | 2.501 (4) |
As2—O1vii | 1.670 (3) | Na2A—O4x | 2.501 (4) |
As2—O2 | 1.673 (3) | Na2B—O4xi | 2.27 (6) |
As2—O4 | 1.680 (3) | Na2B—O4x | 2.27 (6) |
As2—O5 | 1.790 (2) | Na2B—O4ii | 2.30 (5) |
Na1A—O2 | 2.475 (9) | Na2B—O4iii | 2.30 (5) |
Na1A—O1viii | 2.540 (12) | Na2B—O7xii | 2.51 (5) |
O1—Co1—O1i | 110.2 (2) | O3ii—Co2—O6iv | 94.87 (13) |
O1—Co1—O2 | 82.94 (14) | O7—Co2—O6iv | 95.48 (14) |
O1i—Co1—O2 | 90.01 (14) | O4ii—Co2—O6iv | 93.63 (12) |
O1—Co1—O2i | 90.01 (14) | O4iii—Co2—O6iv | 167.77 (12) |
O1i—Co1—O2i | 82.94 (14) | O3ii—Co2—O6v | 94.87 (13) |
O2—Co1—O2i | 167.7 (2) | O7—Co2—O6v | 95.48 (14) |
O1—Co1—O6 | 81.33 (13) | O4ii—Co2—O6v | 167.77 (12) |
O1i—Co1—O6 | 168.19 (14) | O4iii—Co2—O6v | 93.63 (12) |
O2—Co1—O6 | 89.07 (13) | O6iv—Co2—O6v | 74.22 (16) |
O2i—Co1—O6 | 99.88 (13) | O3—As1—O7 | 101.9 (2) |
O1—Co1—O6i | 168.19 (14) | O3—As1—O6vi | 115.27 (14) |
O1i—Co1—O6i | 81.33 (13) | O7—As1—O6vi | 111.14 (15) |
O2—Co1—O6i | 99.88 (13) | O3—As1—O6 | 115.27 (14) |
O2i—Co1—O6i | 89.07 (13) | O7—As1—O6 | 111.14 (14) |
O6—Co1—O6i | 87.23 (18) | O6vi—As1—O6 | 102.4 (2) |
O3ii—Co2—O7 | 167.01 (18) | O1vii—As2—O2 | 111.18 (19) |
O3ii—Co2—O4ii | 87.38 (12) | O1vii—As2—O4 | 114.04 (17) |
O7—Co2—O4ii | 84.15 (12) | O2—As2—O4 | 116.98 (16) |
O3ii—Co2—O4iii | 87.38 (12) | O1vii—As2—O5 | 103.39 (16) |
O7—Co2—O4iii | 84.15 (12) | O2—As2—O5 | 106.19 (13) |
O4ii—Co2—O4iii | 98.49 (17) | O4—As2—O5 | 103.43 (16) |
Symmetry codes: (i) −x+1, y, −z+2; (ii) x, y, z−1; (iii) x, −y+1, z−1; (iv) −x+1, y, −z+1; (v) −x+1, −y+1, −z+1; (vi) x, −y+1, z; (vii) x−1/2, −y+1/2, z; (viii) −x+1/2, −y+1/2, −z+1; (ix) −x+1/2, −y+1/2, −z+2; (x) −x, −y+1, −z+1; (xi) −x, y, −z+1; (xii) −x, −y+1, −z. |
Experimental details
Crystal data | |
Chemical formula | Na3Co2(AsO4)(As2O7) |
Mr | 587.59 |
Crystal system, space group | Monoclinic, C2/m |
Temperature (K) | 293 |
a, b, c (Å) | 10.484 (3), 16.309 (2), 6.531 (1) |
β (°) | 120.40 (2) |
V (Å3) | 963.2 (3) |
Z | 4 |
Radiation type | Mo Kα |
µ (mm−1) | 13.87 |
Crystal size (mm) | 0.20 × 0.10 × 0.10 |
Data collection | |
Diffractometer | Enraf–Nonius CAD-4 |
Absorption correction | ψ scan (North et al., 1968) |
Tmin, Tmax | 0.168, 0.338 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 1765, 1183, 998 |
Rint | 0.041 |
(sin θ/λ)max (Å−1) | 0.659 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.027, 0.067, 1.01 |
No. of reflections | 1183 |
No. of parameters | 103 |
Δρmax, Δρmin (e Å−3) | 0.72, −0.80 |
Computer programs: CAD-4 EXPRESS (Enraf–Nonius, 1995), XCAD4 (Harms & Wocadlo, 1995), SHELXS97 (Sheldrick, 2008), SHELXL97 (Sheldrick, 2008), DIAMOND (Brandenburg, 2001), WinGX (Farrugia, 1999) and publCIF (Westrip, 2010).
Cation | q(i).sof(i) | V(i) | Q(i) | CN(i) | ECoN(i) | dmoy(i) | dmed(i) |
Co1 | 2.00 | 1.87 | 2.01 | 6 | 5.97 | 2.14 | 2.14 |
Co2 | 2.00 | 2.05 | 2.03 | 6 | 5.62 | 2.11 | 2.08 |
As1 | 5.00 | 4.99 | 5.13 | 4 | 3.99 | 1.69 | 1.69 |
As2 | 5.00 | 4.93 | 4.94 | 4 | 3.89 | 1.70 | 1.69 |
Na1A | 0.72 | 0.65 | 0.72 | 8 | 7.33 | 2.67 | 2.63 |
Na1B | 0.28 | 0.25 | 0.27 | 8 | 5.72 | 2.74 | 2.58 |
Na2A | 0.94 | 1.02 | 0.92 | 7 | 5.52 | 2.58 | 2.45 |
Na2B | 0.06 | 0.07 | 0.06 | 6 | 4.78 | 2.45 | 2.31 |
q(i) = formal oxidation number; sof(i) = site occupation factor; dmoy(i) = arithmetic average distance; dmed(i) = weighted average distance; sodium CNs for d(Na–O)max = 3.10 Å; σcat = dispersion factor on cationic charges measuring the deviation of the computed charges (Q) with respect to the formal oxidation numbers; σcat = [Σi(qi-Qi)2/N-1]1/2 = 0.055. |
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The rich chemistry of the A–Co–P/As–O crystallographic systems (A is a monovalent cation), has been shown by the synthesis and crystal structures of several compounds with particular crystallographic properties such as: Na4Co3(PO4)2P2O7, a phosphate containing a three-dimensional system of large intersecting tunnels (Ruiz-Valero et al. 1996), AgCo3H2(PO4)3, an alluaudite-like phosphate structure (Guesmi & Driss, 2002a), K2CoP2O7, a layered tetrahedral phosphate with the mellilite structure (Guesmi & Driss, 2002b), etc.
For the case of arsenates, their main structural difference if compared to phosphates is that arsenic atoms can also adopt an octahedral coordination; it is the case for example of the oxygen-deficient layered sodium arsenate Na7As11O31 (Guesmi et al. 2006). Continuous investigations on the crystal chemistry of the arsenates are performed because arsenic is at the top of the priority of the most hazardous substances, but less is known about its crystal structures.
We are interested in the present work in the crystal structure of the new compound Na3Co2AsO4As2O7 (I). The crystal structure of the isostructural Na3Ni2(As0.1P0.9)O4(As1.3P0.7)O7 compound and ionic conductivity properties of its limiting arsenate has been studied (Ben Smail & Jouini, 2005). The chemical formula of (I) has been established as a result of the crystal structure determination and the obtained structural model is validated by means of charge distribution (CD) (Nespolo et al. 2001, Nespolo, 2001) and bond valence sum methods (BVS) (Brown, 2002; Adams, 2003) as the formal charges (Q) and valences (V) agree well with the expected values (Table 1).
The new compound (I) is an example of a mixed transition-metal arsenate, representing the first cobalt arsenate built up from mono- and diarsenate groups. In the asymetric unit, the crystal structure is built up from corner and edge-sharing between cobalt octahedra and arsenate groups (Fig. 1). The two crystallographically distinct cobalt atoms exhibit a slightly distorted octahedral coordination with effective coordination numbers ECoN(Co1)=5.97 and ECoN(Co2)=5.62 and weighted average distances dmed(Co1)=2.14 Å and dmed(Co2)=2.08 Å. The longest Co–O6 bond distances in the two octahedra correspond to the three-coordinated oxygen atom, related also to As1.
The As1 tetrahedron, with a 2 + 2 coordination, shares its four corners with five octahedra. The As2 tetrahedron, a more precisely a trigonal pyramid (1 + 3 coordination), is more distorted with O5 as a bridging oxygen in the As(2)2O7 group (ECoN(As2)=3.89 and dmed(As2)=1.69 Å). The other six corners in the diarsenate group are common with four Co1 and two Co2 octahedra. It is worth noting that the Co2 and As1 polyhedra share a common edge which induces a strong repulsion between positive charges; this type of connection was also observed in the structure of Na4Co3(PO4)2P2O7 (Ruiz-Valero et al. 1996).
The cobalt octahedra are associated in the ab plane to form the original octahedral metallic units Co4O20 which are corner- and edge-connected via As(1)O4 and As(2)2O7 arsenate groups, giving rise to a complex polyhedral connectivity which produces small tunnels, such as those running along the b and c axis, where the sodium cations reside (Figs. 2–4).
The anionic framework can be decomposed in a succession of alternate layers in the ac plane, stacked along the crystallographic b-axis. They are built up of Co1 octahedra and As(2)2O7 groups in such a way that each octahedron is corner-shared to four diarsenate groups (Fig. 3). These layers are alternate by a chain type resulting from the connection between Co2 and As1 polyhedra and formed by the centrosymmetric cyclic units [Co2As2O14] (Fig. 4), each one of these units is connected to two neighbours by means of mixed Co–O–As bridges.
The Na1 ions are split into two independent positions near c/2, Na1B has the more distorted polyhedron and the ECoN(Na1B) is as low as 5.72. The Na2 ions are also disordered with the Na2B polyhedron sandwiched by Na2A ones which are off-centred around the Na2B positions. The motion of sodium cations within the framewok of (I) by means of theoretical studies and electrical measuremeents will be the subject of future works.