research communications
Synthesis and 2Fe(PO4)3
of calcium dizinc iron(III) tris(orthophosphate), CaZnaLaboratoire de Chimie du Solide Appliquée, Faculty of Sciences, Mohammed V University in Rabat, Avenue Ibn Battouta, BP 1014, Rabat, Morocco
*Correspondence e-mail: j_khmiyas@yahoo.fr
Single crystals of the title compound, CaZn2Fe(PO4)3, were synthesized by conventional solid-state reaction. In the all atoms are located in fully occupied general positions of the P21/c The zinc atoms are located on two crystallographically independent sites with tetrahedral and distorted triangular-based bipyramidal geometries. Two edge-sharing triangular bipyramidal ZnO5 units form a dimer, which is linked to slightly deformed FeO6 octahedra via a common edge. The resulting chains are interconnected through PO4 tetrahedra to form a layer perpendicular to the b axis. Moreover, the remaining PO4 and ZnO4 tetrahedra are linked together through common vertices to form tapes parallel to the c axis and surrounding a chain of Ca2+ cations to build a sheet, also perpendicular to the b axis. The stacking of the two layers along the b axis leads to the resulting three-dimensional framework, which defines channels in which the Ca2+ cations are located, each cation being coordinated by seven oxygen atoms.
Keywords: crystal structure; CaZn2Fe(PO4)3; transition metal phosphate; solid-state reaction synthesis.
CCDC reference: 1497218
1. Chemical context
Microporous compounds with an open anionic framework containing transition metals have been widely studied during recent years, especially iron phosphates, because of their potential applications in several fields such as gas sensing (Abdurahman et al., 2014), catalysis (Ai, 1999), as cathode materials for rechargeable lithium batteries (Masquelier et al., 1998), biocompatibility of glass fibres for tissue engineering (Ahmed et al., 2004), and immobilization of spent (Mesko & Day, 1999). Metal phosphates with an open framework can exhibit different architectures such as linear-chain, layered and three-dimensional structures with channels or cavities where a variety of cations with different sizes, ratio and charges are accommodated. The occupancy of the allowed sites by cations can provide different properties such as remarkable flexibility, fast ionic conduction and low mainly observed in the compounds belonging to the NASICON family with the general formula MM′2P3O12 (where M = alkali metal, alkaline-earth metal or a vacant site and M′ = Zr, Ti, Hf, etc.; Senbhagaraman et al., 1993). In our previous hydrothermal investigations, a variety of compounds have been synthesized and characterized with different ratios of alkaline earth metal:P, viz. Sr2Mn3(HPO4)2(PO4)2 (Khmiyas et al., 2013), BaMnII2MnIII(PO4)3 (Assani et al., 2013), Mg7(PO4)2(HPO4)4 (Assani et al., 2011). In this context, our interest is focused on the synthesis of new iron orthophosphates with an open-framework structure. Accordingly, we have succeeded in synthesizing and structurally characterizing a new calcium, zinc and iron-based open-framework phosphate, namely CaZn2Fe(PO4)3.
2. Structural commentary
All atoms in P21/c The of this model was very easy and lead to an ordered structure in which the zinc cations occupy two sites with different environments. The coordination numbers of all cations were confirmed by bond-valence-sum calculations (Brown & Altermatt, 1985). The obtained values for CaII+, ZnII+, FeIII+ and PV+ are as expected, viz. Ca1 (1.93), Zn1 (2.00), Zn2 (1.91), Fe1 (3.04), P1 (5.11), P2 (4.97) and P3 (4.94). The is build up from PO4 and Zn1O4 tetrahedra, distorted triangular-based bipyramidal Zn2O5 and FeO6 octahedra, as shown in Fig. 1. The FeO6 octahedra are slightly deformed with Fe—O distances varying from 1.8908 (8) to 2.1318 (8) Å and share a common edge with the highly distorted [(Zn2)2O8] dimer resulting from the edge-sharing of two triangular-based bipyramidal Zn2O5 units. Sequences of these polyhedra build chains interconnected by PO4 tetrahedra, forming a layer perpendicular to the b axis, as shown in Fig. 2. The remaining Zn1O4 tetrahedra are linked to irregular PO4 groups via common corners, forming tapes parallel to the c axis, which are linked together by Ca2+ cations in sheets perpendicular to the b axis (see Fig. 3). The obtained three-dimensional framework shows one type of channel running along the [001] direction in which the Ca2+ cations are located, each being coordinated by seven oxygen atoms (Fig. 4).
of the title compound occupy general positions of the3. Database Survey
The formula of the title compound, CaZn2Fe(PO4)3, is similar to some compounds with alluaudite structures, C2/c or the α-CrPO4 structure, Imma. However, its structure is different and to our knowledge there is no known isotypic structure. Crystals of CaM2Fe(PO4)3 (M = Mg, Co, Ni, Cu) compounds, which are predicted to have the same structures or isotypes are in preparation, while the structures of SrM2Fe(PO4)3 (M = Co, Ni) compounds are isotypic with α-CrPO4 (Bouraima et al., 2016; Ouaatta et al., 2015). Mention may also be made of other similar compounds, for example the phosphates Na2Co2Fe(PO4)3, NaCr2Zn(PO4)3 and Na1.66Zn1.66Fe1.34(PO4)3 (Bouraima et al., 2015; Souiwa et al., 2015; Khmiyas et al., 2015) adopting the alluaudite structure type. In conclusion, we can say that the structure of this phosphate is similar to the alluaudite structure but with lower symmetry.
4. Synthesis and crystallization
Single crystals of CaZn2Fe(PO4)3 were synthesized by a conventional solid-state method. Appropriate amounts of metal nitrate reagents, in the presence of H3PO4 85 wt%, were first dissolved in deionized water in the molar ratio Ca:Zn:Fe:P = 2:2:1:3 for 24 h. Then, the resulting solution was evaporated to dryness. The powder residue was ground in an agate mortar and progressively heated in a platinum crucible at a heating rate of 141 K h−1 until melting occurred at 1283 K. The melted product was cooled down at a rate of 5 K h−1. As result of the reaction, we obtained transparent crystals corresponding to the title compound CaZn2Fe(PO4)3.
5. Refinement
Crystal data, data collection and structure . The reflections (202) and (330) probably affected by the beam-stop were omitted from the The maximum and minimum electron densities in the final Fourier map are at 0.56 and 0.44 Å from Ca1 and Zn2, respectively.
details are summarized in Table 1Supporting information
CCDC reference: 1497218
https://doi.org/10.1107/S2056989016012421/pj2033sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989016012421/pj2033Isup2.hkl
Data collection: APEX2 (Bruker, 2009); cell
SAINT (Bruker, 2009); data reduction: SAINT (Bruker, 2009); program(s) used to solve structure: SHELXT (Sheldrick, 2015a); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015b); molecular graphics: ORTEP-3 for Windows (Farrugia, 2012) and DIAMOND (Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).CaZn2Fe(PO4)3 | F(000) = 988 |
Mr = 511.58 | Dx = 3.618 Mg m−3 |
Monoclinic, P21/c | Mo Kα radiation, λ = 0.71073 Å |
a = 8.5619 (3) Å | Cell parameters from 4985 reflections |
b = 15.2699 (5) Å | θ = 2.7–37.6° |
c = 8.1190 (3) Å | µ = 7.72 mm−1 |
β = 117.788 (2)° | T = 296 K |
V = 939.06 (6) Å3 | Block, black |
Z = 4 | 0.30 × 0.26 × 0.18 mm |
Bruker X8 APEX diffractometer | 4985 independent reflections |
Radiation source: fine-focus sealed tube | 4493 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.033 |
φ and ω scans | θmax = 37.6°, θmin = 2.7° |
Absorption correction: multi-scan (SADABS; Krause et al., 2015) | h = −14→14 |
Tmin = 0.600, Tmax = 0.747 | k = −26→26 |
54053 measured reflections | l = −10→13 |
Refinement on F2 | 172 parameters |
Least-squares matrix: full | 0 restraints |
R[F2 > 2σ(F2)] = 0.017 | w = 1/[σ2(Fo2) + (0.0174P)2 + 0.7655P] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.041 | (Δ/σ)max = 0.003 |
S = 1.04 | Δρmax = 1.07 e Å−3 |
4985 reflections | Δρmin = −0.78 e Å−3 |
Geometry. All esds (except the esd in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell esds are taken into account individually in the estimation of esds in distances, angles and torsion angles; correlations between esds in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell esds is used for estimating esds involving l.s. planes. |
x | y | z | Uiso*/Ueq | ||
Zn1 | 0.81685 (2) | 0.73588 (2) | 0.30142 (2) | 0.00740 (3) | |
Zn2 | 0.88412 (2) | 0.52265 (2) | 0.59417 (2) | 0.01026 (3) | |
Fe1 | 0.67075 (2) | 0.49009 (2) | 0.83003 (2) | 0.00500 (3) | |
Ca1 | 0.27619 (3) | 0.75762 (2) | 0.47919 (3) | 0.01070 (4) | |
P1 | 0.29665 (3) | 0.58370 (2) | 0.77261 (4) | 0.00503 (4) | |
P2 | 0.96807 (3) | 0.62244 (2) | 0.09438 (4) | 0.00499 (4) | |
P3 | 0.60325 (3) | 0.64096 (2) | 0.49014 (4) | 0.00491 (4) | |
O1 | 0.29942 (13) | 0.67932 (6) | 0.72349 (13) | 0.01271 (15) | |
O2 | 0.30273 (12) | 0.58596 (6) | 0.96463 (12) | 0.01006 (14) | |
O3 | 0.12207 (10) | 0.54161 (6) | 0.62684 (12) | 0.01114 (15) | |
O4 | 0.43948 (11) | 0.52893 (6) | 0.76475 (14) | 0.01312 (16) | |
O5 | 0.77926 (10) | 0.58832 (5) | 0.00379 (12) | 0.00895 (13) | |
O6 | 1.00136 (11) | 0.67493 (6) | −0.04745 (13) | 0.01045 (14) | |
O7 | 1.00262 (11) | 0.68143 (6) | 0.26134 (13) | 0.01055 (14) | |
O8 | 1.09932 (10) | 0.54481 (5) | 0.17408 (12) | 0.00724 (13) | |
O9 | 0.75426 (11) | 0.65280 (6) | 0.43941 (13) | 0.01160 (15) | |
O10 | 0.59377 (10) | 0.71947 (6) | 0.60355 (12) | 0.00974 (14) | |
O11 | 0.66602 (11) | 0.55677 (5) | 0.61102 (12) | 0.00822 (13) | |
O12 | 0.41993 (10) | 0.62799 (6) | 0.32620 (12) | 0.01012 (14) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Zn1 | 0.00645 (5) | 0.00817 (5) | 0.00801 (6) | 0.00013 (4) | 0.00374 (4) | 0.00104 (4) |
Zn2 | 0.00760 (5) | 0.01471 (6) | 0.01073 (6) | 0.00042 (4) | 0.00616 (4) | −0.00080 (5) |
Fe1 | 0.00454 (5) | 0.00602 (6) | 0.00488 (6) | 0.00044 (4) | 0.00256 (4) | 0.00061 (4) |
Ca1 | 0.01029 (8) | 0.01095 (9) | 0.01178 (10) | 0.00175 (6) | 0.00591 (7) | 0.00601 (7) |
P1 | 0.00467 (9) | 0.00607 (10) | 0.00452 (10) | 0.00011 (7) | 0.00229 (8) | −0.00022 (8) |
P2 | 0.00441 (9) | 0.00482 (10) | 0.00581 (11) | 0.00038 (7) | 0.00243 (8) | −0.00009 (8) |
P3 | 0.00448 (9) | 0.00500 (10) | 0.00483 (10) | 0.00004 (7) | 0.00182 (8) | 0.00031 (8) |
O1 | 0.0222 (4) | 0.0076 (3) | 0.0109 (4) | −0.0001 (3) | 0.0098 (3) | 0.0019 (3) |
O2 | 0.0169 (3) | 0.0093 (3) | 0.0063 (3) | 0.0009 (3) | 0.0073 (3) | 0.0011 (3) |
O3 | 0.0051 (3) | 0.0176 (4) | 0.0102 (4) | −0.0030 (3) | 0.0030 (3) | −0.0063 (3) |
O4 | 0.0065 (3) | 0.0172 (4) | 0.0157 (4) | 0.0026 (3) | 0.0052 (3) | −0.0045 (3) |
O5 | 0.0056 (3) | 0.0100 (3) | 0.0101 (3) | −0.0016 (2) | 0.0028 (2) | −0.0034 (3) |
O6 | 0.0097 (3) | 0.0107 (3) | 0.0132 (4) | 0.0029 (3) | 0.0072 (3) | 0.0061 (3) |
O7 | 0.0079 (3) | 0.0122 (3) | 0.0115 (4) | −0.0005 (2) | 0.0045 (3) | −0.0062 (3) |
O8 | 0.0065 (3) | 0.0073 (3) | 0.0088 (3) | 0.0026 (2) | 0.0043 (2) | 0.0020 (2) |
O9 | 0.0111 (3) | 0.0118 (3) | 0.0161 (4) | 0.0008 (3) | 0.0098 (3) | 0.0042 (3) |
O10 | 0.0076 (3) | 0.0091 (3) | 0.0103 (3) | 0.0006 (2) | 0.0024 (3) | −0.0040 (3) |
O11 | 0.0100 (3) | 0.0080 (3) | 0.0082 (3) | 0.0028 (2) | 0.0055 (3) | 0.0039 (3) |
O12 | 0.0068 (3) | 0.0086 (3) | 0.0097 (3) | −0.0002 (2) | −0.0006 (3) | −0.0020 (3) |
Zn1—O9 | 1.9266 (9) | Ca1—O2i | 2.4075 (9) |
Zn1—O7 | 1.9518 (8) | Ca1—O7viii | 2.4709 (9) |
Zn1—O10i | 1.9578 (8) | Ca1—O6ix | 2.4840 (9) |
Zn1—O6ii | 2.0120 (8) | Ca1—O10 | 2.4885 (8) |
Zn2—O3iii | 1.9496 (8) | Ca1—O12 | 2.8984 (9) |
Zn2—O11 | 2.0038 (8) | P1—O4 | 1.5073 (9) |
Zn2—O3iv | 2.0241 (9) | P1—O1 | 1.5166 (9) |
Zn2—O8v | 2.0911 (8) | P1—O2 | 1.5358 (9) |
Zn2—O9 | 2.3371 (9) | P1—O3 | 1.5487 (8) |
Fe1—O4 | 1.8908 (8) | P2—O5 | 1.5222 (8) |
Fe1—O2vi | 1.9561 (9) | P2—O6 | 1.5348 (9) |
Fe1—O5vii | 1.9700 (8) | P2—O7 | 1.5371 (9) |
Fe1—O11 | 2.0330 (8) | P2—O8 | 1.5519 (8) |
Fe1—O8v | 2.0547 (8) | P3—O12 | 1.5253 (8) |
Fe1—O12iv | 2.1318 (8) | P3—O10 | 1.5365 (9) |
Ca1—O1 | 2.2439 (9) | P3—O9 | 1.5396 (9) |
Ca1—O1i | 2.3795 (10) | P3—O11 | 1.5534 (8) |
O9—Zn1—O7 | 106.60 (4) | O2i—Ca1—O6ix | 72.04 (3) |
O9—Zn1—O10i | 106.09 (4) | O7viii—Ca1—O6ix | 65.76 (3) |
O7—Zn1—O10i | 124.80 (4) | O1—Ca1—O10 | 83.50 (3) |
O9—Zn1—O6ii | 116.31 (4) | O1i—Ca1—O10 | 85.92 (3) |
O7—Zn1—O6ii | 85.46 (3) | O2i—Ca1—O10 | 98.16 (3) |
O10i—Zn1—O6ii | 116.93 (4) | O7viii—Ca1—O10 | 132.22 (3) |
O3iii—Zn2—O11 | 154.16 (4) | O6ix—Ca1—O10 | 160.73 (3) |
O3iii—Zn2—O3iv | 77.67 (4) | O1—Ca1—O12 | 97.73 (3) |
O11—Zn2—O3iv | 123.13 (3) | O1i—Ca1—O12 | 71.19 (3) |
O3iii—Zn2—O8v | 108.82 (4) | O2i—Ca1—O12 | 126.00 (3) |
O11—Zn2—O8v | 75.00 (3) | O7viii—Ca1—O12 | 79.74 (3) |
O3iv—Zn2—O8v | 121.44 (4) | O6ix—Ca1—O12 | 145.10 (3) |
O3iii—Zn2—O9 | 98.73 (4) | O10—Ca1—O12 | 53.99 (3) |
O11—Zn2—O9 | 65.84 (3) | O1—Ca1—O12ii | 69.93 (3) |
O3iv—Zn2—O9 | 97.26 (4) | O1i—Ca1—O12ii | 114.39 (3) |
O8v—Zn2—O9 | 135.92 (3) | O2i—Ca1—O12ii | 57.96 (3) |
O4—Fe1—O2vi | 96.63 (4) | O7viii—Ca1—O12ii | 140.52 (3) |
O4—Fe1—O5vii | 92.55 (4) | O6ix—Ca1—O12ii | 78.49 (3) |
O2vi—Fe1—O5vii | 90.75 (4) | O10—Ca1—O12ii | 82.24 (3) |
O4—Fe1—O11 | 90.37 (4) | O12—Ca1—O12ii | 135.98 (3) |
O2vi—Fe1—O11 | 171.82 (3) | O4—P1—O1 | 114.24 (6) |
O5vii—Fe1—O11 | 93.18 (4) | O4—P1—O2 | 114.28 (5) |
O4—Fe1—O8v | 164.34 (4) | O1—P1—O2 | 104.36 (5) |
O2vi—Fe1—O8v | 97.38 (3) | O4—P1—O3 | 104.50 (5) |
O5vii—Fe1—O8v | 94.22 (3) | O1—P1—O3 | 109.05 (5) |
O11—Fe1—O8v | 75.18 (3) | O2—P1—O3 | 110.42 (5) |
O4—Fe1—O12iv | 93.16 (4) | O5—P2—O6 | 110.07 (5) |
O2vi—Fe1—O12iv | 82.55 (4) | O5—P2—O7 | 110.55 (5) |
O5vii—Fe1—O12iv | 171.65 (3) | O6—P2—O7 | 109.20 (5) |
O11—Fe1—O12iv | 92.86 (4) | O5—P2—O8 | 109.84 (5) |
O8v—Fe1—O12iv | 81.77 (3) | O6—P2—O8 | 111.11 (5) |
O1—Ca1—O1i | 167.91 (4) | O7—P2—O8 | 106.00 (5) |
O1—Ca1—O2i | 126.91 (3) | O12—P3—O10 | 107.69 (5) |
O1i—Ca1—O2i | 60.49 (3) | O12—P3—O9 | 115.63 (5) |
O1—Ca1—O7viii | 92.62 (3) | O10—P3—O9 | 110.75 (5) |
O1i—Ca1—O7viii | 90.17 (3) | O12—P3—O11 | 110.86 (5) |
O2i—Ca1—O7viii | 120.77 (3) | O10—P3—O11 | 111.50 (5) |
O1—Ca1—O6ix | 89.31 (3) | O9—P3—O11 | 100.36 (5) |
O1i—Ca1—O6ix | 102.55 (3) |
Symmetry codes: (i) x, −y+3/2, z−1/2; (ii) x, −y+3/2, z+1/2; (iii) x+1, y, z; (iv) −x+1, −y+1, −z+1; (v) −x+2, −y+1, −z+1; (vi) −x+1, −y+1, −z+2; (vii) x, y, z+1; (viii) x−1, y, z; (ix) x−1, −y+3/2, z+1/2. |
Acknowledgements
The authors thank the Unit of Support for Technical and Scientific Research (UATRS, CNRST) for the X-ray measurements and Mohammed V University in Rabat, Morocco, for financial support.
References
Abdurahman, A., Nizamidin, P. & Yimit, A. (2014). Mater. Sci. Semicond. Process. 22, 21–27. Web of Science CrossRef CAS Google Scholar
Ahmed, I., Collins, C. A., Lewis, M. P., Olsen, I. & Knowles, J. C. (2004). Biomaterials, 25, 3223–3232. Web of Science CrossRef PubMed CAS Google Scholar
Ai, M. (1999). Catal. Today, 52, 65–69. Web of Science CrossRef CAS Google Scholar
Assani, A., Saadi, M., Alhakmi, G., Houmadi, E. & El Ammari, L. (2013). Acta Cryst. E69, i60. CrossRef IUCr Journals Google Scholar
Assani, A., Saadi, M., Zriouil, M. & El Ammari, L. (2011). Acta Cryst. E67, i52. Web of Science CrossRef IUCr Journals Google Scholar
Bouraima, A., Assani, A., Saadi, M., Makani, T. & El Ammari, L. (2015). Acta Cryst. E71, 558–560. Web of Science CSD CrossRef IUCr Journals Google Scholar
Bouraima, A., Makani, T., Assani, A., Saadi, M. & El Ammari, L. (2016). Acta Cryst. E72, 1143–1146. Web of Science CSD CrossRef IUCr Journals Google Scholar
Brandenburg, K. (2006). DIAMOND. Crystal Impact GbR, Bonn, Germany. Google Scholar
Brown, I. D. & Altermatt, D. (1985). Acta Cryst. B41, 244–247. CrossRef CAS Web of Science IUCr Journals Google Scholar
Bruker (2009). APEX2 and SAINT. Bruker AXS Inc., Madison, Wisconsin, USA. Google Scholar
Farrugia, L. J. (2012). J. Appl. Cryst. 45, 849–854. Web of Science CrossRef CAS IUCr Journals Google Scholar
Khmiyas, J., Assani, A., Saadi, M. & El Ammari, L. (2013). Acta Cryst. E69, i50. CrossRef IUCr Journals Google Scholar
Khmiyas, J., Assani, A., Saadi, M. & El Ammari, L. (2015). Acta Cryst. E71, 690–692. Web of Science CSD CrossRef IUCr Journals Google Scholar
Krause, L., Herbst-Irmer, R., Sheldrick, G. M. & Stalke, D. (2015). J. Appl. Cryst. 48, 3–10. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
Masquelier, C., Padhi, A. K., Nanjundaswamy, K. S. & Goodenough, J. B. (1998). J. Solid State Chem. 135, 228–234. Web of Science CrossRef CAS Google Scholar
Mesko, M. G. & Day, D. E. (1999). J. Nucl. Mater. 273, 27–36. Web of Science CrossRef CAS Google Scholar
Ouaatta, S., Assani, A., Saadi, M. & El Ammari, L. (2015). Acta Cryst. E71, 1255–1258. Web of Science CSD CrossRef IUCr Journals Google Scholar
Senbhagaraman, S., Guru Rowb, T. N. & Umarji, A. M. (1993). J. Mater. Chem. 3, 309–314. CrossRef CAS Web of Science Google Scholar
Sheldrick, G. M. (2015a). Acta Cryst. A71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Sheldrick, G. M. (2015b). Acta Cryst. C71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Souiwa, K., Hidouri, M., Toulemonde, O., Duttine, M. & Ben Amara, M. (2015). J. Alloys Compd, 627, 153–160. Web of Science CrossRef CAS Google Scholar
Westrip, S. P. (2010). J. Appl. Cryst. 43, 920–925. Web of Science CrossRef CAS IUCr Journals Google Scholar
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