inorganic compounds
Heptamagnesium bis(phosphate) tetrakis(hydrogen phosphate) with strong hydrogen bonds: Mg7(PO4)2(HPO4)4
aLaboratoire de Chimie du Solide Appliquée, Faculté des Sciences, Université Mohammed V-Agdal, Avenue Ibn Battouta, BP. 1014, Rabat, Morocco
*Correspondence e-mail: abder_assani@yahoo.fr
The title compound, Mg7(PO4)2(HPO4)4, was synthesized by the hydrothermal method. The structure is based on a framework of edge- and corner-sharing MgO6 and MgO4(OH)2 octahedra, an MgO5 polyhedron, PO4 and PO3(OH) tetrahedra. All atoms are in general positions except for one Mg atom, which is located on a crystallographic inversion centre. The OH groups, bridging Mg–(OH)–P, are involved in strong hydrogen bonds. Compounds with the general formula M7(PO4)2(HPO4)4 (M = Mg, Mn, Fe and Co) are all isostructural with their homologue arsenate Mg7(AsO4)2(HAsO4)4.
Related literature
For background to metal phosphates, see: Viter & Nagornyi (2009); Clearfield (1988); Trad et al. (2010). For the hydrothermal method, see: Assani et al. (2010, 2011a,b). For isostructural compounds, see: Zhou et al. (2002); Riou et al. (1987); Rojo et al. (2002); Lightfoot & Cheetham (1988); Kolitsch & Bartu (2004).
Experimental
Crystal data
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Refinement
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Data collection: APEX2 (Bruker, 2005); cell SAINT (Bruker, 2005); data reduction: SAINT; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: ORTEP-3 for Windows (Farrugia, 1997) and DIAMOND (Brandenburg, 2006); software used to prepare material for publication: WinGX publication routines (Farrugia, 1999).
Supporting information
https://doi.org/10.1107/S1600536811036361/bt5638sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S1600536811036361/bt5638Isup2.hkl
Supporting information file. DOI: https://doi.org/10.1107/S1600536811036361/bt5638Isup3.cml
The crystals of the title compound is isolated from the hydrothermal treatment of the reaction mixture of magnesium oxide (MgO) and 85%wt phosphoric acid (H3PO4) in the nominal proportion corresponding to the molar ratio Mg: P = 7:6. The hydrothermal reaction was conducted in a 23 ml Teflon-lined autoclave, filled to 50% with distilled water and under autogenously pressure at 468 K for two days. After being filtered off, washed with deionized water and air dried, the reaction product consists of a white powder and colourless parallelepipedic crystals corresponding to the title compound.
The H atoms were initially located in a difference map and refined with O—H distance restraints of 0.86 (1). In a the last cycle they were refined in the riding model approximation with Uiso(H) set to 1.2Ueq(O).
Widespread studies are devoted to the metal phosphate owing to their impressive structural diversity and to their prospective applications in catalysis (Viter & Nagornyi, 2009), ion-exchangers (Clearfield, 1988)) and in batteries performance (Trad et al., (2010)). Mainly, our most attention has been paid to the hydrothermal synthesis of new metal based phosphate. Accordingly, we have recently succeed to obtain new phosphates, such as Ni2Sr(PO4)2 2H2O (Assani et al. (2010)), AgMg3(PO4)(HPO4)2 (Assani et al. (2011b)) and Ag2Ni3(HPO4)(PO4)2 (Assani et al. (2011a)).
Besides, the investigation of the MO—P2O5 systems (M=divalent cations) has allowed to isolate a new member of the metal phosphates, with a general formula M7(PO4)2(HPO4)4. The present paper aims to develop the hydrothermal synthesis and the structural characterization of the Mg7(PO4)2(HPO4)4 which is isostructural with Fe7(PO4)2(HPO4)4 (Zhou et al. (2002)), Mn7(PO4)2(HPO4)4 (Riou et al. (1987) and (Rojo et al. (2002)), Co7(PO4)2(HPO4)4 (Lightfoot & Cheetham, (1988)) and with their homologue arsenate Mg7(AsO4)2(HAsO4)4 (Kolitsch & Bartu, (2004)).
The
of Mg7(PO4)2(HPO4)4 is built up from MgO6, MgO4(OH)2 octahedra, MgO5 polyhedron, PO4 and PO3(OH) tetrahedra, sharing corners and edges to form a three-dimensional framework as shown in Fig.1 and Fig.2. In the all atoms are in general positions except for atom Mg2, which is located at a crystallographic inversion centre (0, 0, 0). Each OH group is bonded to an Mg and an P atom. Atom Mg2 is located at the centre of an Mg2O6 octahedron with significant bond-length distortion as shown in Table 1. In contrast, Mg1O6 and Mg3O4(OH)2 represent less distorted octahedra, and atom Mg4 is surrounded by five O ligands, forming a distorted Mg4O5 trigonal bipyramid. In this structure, each Mg1O6 and Mg3O6 octahedron shares an edge with its symmetrical to form a dimer. Both dimers, Mg1O10 and Mg3O10 are bound by Mg4O5 by sharing two edges to form a zigzag chaine. The Mg2O6 octahedron and PO4 tetrahedra are linked to neighboring polyhedra by vertices. The three crystallographically independent P atoms show tetrahedral coordination. The PO4 groups are relatively regular, although the two protonated groups, centred by P1 and P3, show a stronger angular and bond-length distortion in comparison with the unprotonated P2O4 tetrahedron as shown in Table 1. Moreover the OH groups, bridging Mg–(OH)–P, are involved in strong hydrogen bonds (Table 2).For rmetal phosphates, see: Viter & Nagornyi (2009); Clearfield (1988); Trad et al. (2010). For the hydrothermal method, see: Assani et al. (2010, 2011a,b). For isostructural compounds, see: Zhou et al. (2002); Riou et al. (1987); Rojo et al. (2002); Lightfoot & Cheetham (1988); Kolitsch & Bartu (2004).
Data collection: APEX2 (Bruker, 2005); cell
APEX2 (Bruker, 2005); data reduction: SAINT (Bruker, 2005); program(s) used to solve structure: SHELXS97 (Sheldrick, 2008); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008); molecular graphics: ORTEP-3 for Windows (Farrugia,1997) and DIAMOND (Brandenburg, 2006); software used to prepare material for publication: WinGX publication routines (Farrugia, 1999).Mg7(PO4)2(HPO4)4 | Z = 1 |
Mr = 744.02 | F(000) = 370 |
Triclinic, P1 | Dx = 2.965 Mg m−3 |
Hall symbol: -P 1 | Mo Kα radiation, λ = 0.71073 Å |
a = 6.4204 (5) Å | Cell parameters from 1923 reflections |
b = 7.8489 (4) Å | θ = 2.4–27.6° |
c = 9.4315 (5) Å | µ = 1.06 mm−1 |
α = 104.442 (3)° | T = 296 K |
β = 108.505 (5)° | Parallelepipedic, colourless |
γ = 101.189 (8)° | 0.16 × 0.10 × 0.07 mm |
V = 416.70 (4) Å3 |
Bruker X8 APEX Diffractometer | 1923 independent reflections |
Radiation source: fine-focus sealed tube | 1715 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.036 |
φ and ω scans | θmax = 27.6°, θmin = 2.4° |
Absorption correction: multi-scan (SADABS; Bruker, 2005) | h = −8→8 |
Tmin = 0.881, Tmax = 0.929 | k = −10→10 |
9421 measured reflections | l = −11→12 |
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)] = 0.026 | Hydrogen site location: difference Fourier map |
wR(F2) = 0.072 | H-atom parameters constrained |
S = 1.07 | w = 1/[σ2(Fo2) + (0.0325P)2 + 0.6237P] where P = (Fo2 + 2Fc2)/3 |
1923 reflections | (Δ/σ)max < 0.001 |
169 parameters | Δρmax = 0.43 e Å−3 |
0 restraints | Δρmin = −0.42 e Å−3 |
Mg7(PO4)2(HPO4)4 | γ = 101.189 (8)° |
Mr = 744.02 | V = 416.70 (4) Å3 |
Triclinic, P1 | Z = 1 |
a = 6.4204 (5) Å | Mo Kα radiation |
b = 7.8489 (4) Å | µ = 1.06 mm−1 |
c = 9.4315 (5) Å | T = 296 K |
α = 104.442 (3)° | 0.16 × 0.10 × 0.07 mm |
β = 108.505 (5)° |
Bruker X8 APEX Diffractometer | 1923 independent reflections |
Absorption correction: multi-scan (SADABS; Bruker, 2005) | 1715 reflections with I > 2σ(I) |
Tmin = 0.881, Tmax = 0.929 | Rint = 0.036 |
9421 measured reflections |
R[F2 > 2σ(F2)] = 0.026 | 0 restraints |
wR(F2) = 0.072 | H-atom parameters constrained |
S = 1.07 | Δρmax = 0.43 e Å−3 |
1923 reflections | Δρmin = −0.42 e Å−3 |
169 parameters |
Geometry. All s.u.'s (except the s.u. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell s.u.'s are taken into account individually in the estimation of s.u.'s in distances, angles and torsion angles; correlations between s.u.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell s.u.'s is used for estimating s.u.'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 | ||
Mg1 | −0.38348 (12) | 0.54390 (10) | −0.10950 (8) | 0.00639 (17) | |
Mg2 | 0.0000 | 0.0000 | 0.0000 | 0.0094 (2) | |
Mg3 | −0.05324 (13) | 0.28758 (10) | −0.51536 (9) | 0.00821 (17) | |
Mg4 | −0.27778 (13) | 0.19081 (11) | −0.28530 (9) | 0.00902 (17) | |
P1 | 0.22691 (9) | 0.14512 (8) | −0.22413 (6) | 0.00561 (13) | |
P2 | 0.08899 (9) | 0.58025 (7) | −0.17255 (6) | 0.00465 (13) | |
P3 | −0.59090 (9) | 0.23141 (8) | −0.62865 (7) | 0.00658 (14) | |
O1 | 0.0189 (3) | 0.1762 (2) | −0.33779 (18) | 0.0081 (3) | |
O2 | 0.2208 (3) | 0.1877 (2) | −0.05694 (18) | 0.0074 (3) | |
O3 | 0.4517 (3) | 0.2446 (2) | −0.22968 (18) | 0.0077 (3) | |
O4 | 0.2013 (3) | −0.0667 (2) | −0.27972 (18) | 0.0091 (3) | |
H4 | 0.1828 | −0.1148 | −0.2104 | 0.011* | |
O5 | 0.3069 (3) | 0.5385 (2) | −0.08555 (18) | 0.0068 (3) | |
O6 | 0.0589 (3) | 0.5452 (2) | −0.34643 (18) | 0.0073 (3) | |
O7 | 0.1098 (3) | 0.7857 (2) | −0.09645 (19) | 0.0094 (3) | |
O8 | −0.1240 (3) | 0.4602 (2) | −0.16487 (18) | 0.0070 (3) | |
O9 | −0.3803 (3) | 0.2112 (2) | −0.50853 (19) | 0.0104 (3) | |
O10 | −0.5267 (3) | 0.3827 (2) | −0.69363 (19) | 0.0106 (3) | |
O11 | −0.7360 (3) | 0.0488 (2) | −0.76029 (19) | 0.0097 (3) | |
O12 | −0.7344 (3) | 0.2950 (2) | −0.52719 (19) | 0.0111 (3) | |
H12 | −0.6495 | 0.3935 | −0.4485 | 0.013* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Mg1 | 0.0064 (4) | 0.0077 (4) | 0.0058 (4) | 0.0022 (3) | 0.0028 (3) | 0.0028 (3) |
Mg2 | 0.0120 (5) | 0.0086 (5) | 0.0095 (5) | 0.0035 (4) | 0.0061 (4) | 0.0034 (4) |
Mg3 | 0.0091 (4) | 0.0083 (4) | 0.0076 (4) | 0.0021 (3) | 0.0037 (3) | 0.0029 (3) |
Mg4 | 0.0093 (4) | 0.0082 (4) | 0.0104 (4) | 0.0027 (3) | 0.0047 (3) | 0.0031 (3) |
P1 | 0.0055 (3) | 0.0055 (3) | 0.0056 (3) | 0.0011 (2) | 0.0024 (2) | 0.0016 (2) |
P2 | 0.0045 (3) | 0.0052 (3) | 0.0047 (3) | 0.0017 (2) | 0.0019 (2) | 0.0020 (2) |
P3 | 0.0058 (3) | 0.0073 (3) | 0.0067 (3) | 0.0019 (2) | 0.0023 (2) | 0.0025 (2) |
O1 | 0.0056 (7) | 0.0103 (8) | 0.0084 (8) | 0.0024 (6) | 0.0019 (6) | 0.0041 (6) |
O2 | 0.0086 (7) | 0.0070 (7) | 0.0056 (7) | 0.0010 (6) | 0.0031 (6) | 0.0008 (6) |
O3 | 0.0056 (7) | 0.0078 (7) | 0.0088 (7) | −0.0002 (6) | 0.0037 (6) | 0.0019 (6) |
O4 | 0.0133 (8) | 0.0067 (7) | 0.0085 (8) | 0.0025 (6) | 0.0057 (6) | 0.0030 (6) |
O5 | 0.0053 (7) | 0.0094 (7) | 0.0068 (7) | 0.0034 (6) | 0.0024 (6) | 0.0034 (6) |
O6 | 0.0097 (7) | 0.0081 (7) | 0.0053 (7) | 0.0036 (6) | 0.0035 (6) | 0.0030 (6) |
O7 | 0.0119 (8) | 0.0060 (7) | 0.0109 (8) | 0.0038 (6) | 0.0050 (6) | 0.0021 (6) |
O8 | 0.0049 (7) | 0.0071 (7) | 0.0091 (7) | 0.0010 (6) | 0.0037 (6) | 0.0020 (6) |
O9 | 0.0085 (8) | 0.0157 (8) | 0.0086 (8) | 0.0059 (6) | 0.0030 (6) | 0.0052 (6) |
O10 | 0.0117 (8) | 0.0093 (8) | 0.0087 (8) | −0.0002 (6) | 0.0018 (6) | 0.0048 (6) |
O11 | 0.0098 (7) | 0.0073 (7) | 0.0102 (8) | 0.0014 (6) | 0.0025 (6) | 0.0025 (6) |
O12 | 0.0084 (8) | 0.0137 (8) | 0.0099 (8) | 0.0037 (6) | 0.0042 (6) | 0.0010 (6) |
Mg1—O10i | 2.0235 (17) | P1—O2 | 1.5431 (16) |
Mg1—O5ii | 2.0462 (17) | P1—O4 | 1.5718 (16) |
Mg1—O5iii | 2.0643 (17) | P2—O5 | 1.5237 (16) |
Mg1—O8 | 2.0698 (17) | P2—O6 | 1.5350 (16) |
Mg1—O2ii | 2.1093 (17) | P2—O8 | 1.5362 (16) |
Mg1—O3iii | 2.2065 (17) | P2—O7 | 1.5533 (16) |
Mg2—O7iv | 2.0630 (16) | P3—O10 | 1.5131 (16) |
Mg2—O7ii | 2.0630 (16) | P3—O11 | 1.5245 (17) |
Mg2—O2 | 2.1296 (15) | P3—O9 | 1.5287 (16) |
Mg2—O2v | 2.1296 (15) | P3—O12 | 1.5853 (17) |
Mg2—O11vi | 2.2395 (16) | O2—Mg1ii | 2.1093 (17) |
Mg2—O11vii | 2.2395 (16) | O3—Mg4x | 2.0549 (17) |
Mg3—O4viii | 2.0415 (17) | O3—Mg1x | 2.2065 (17) |
Mg3—O1 | 2.0443 (17) | O4—Mg3viii | 2.0415 (17) |
Mg3—O6 | 2.0606 (17) | O4—H4 | 0.8601 |
Mg3—O6ix | 2.0649 (17) | O5—Mg1ii | 2.0462 (17) |
Mg3—O12x | 2.0759 (17) | O5—Mg1x | 2.0643 (17) |
Mg3—O9 | 2.0954 (17) | O6—Mg3ix | 2.0649 (17) |
Mg4—O8 | 2.0041 (17) | O7—Mg2xi | 2.0630 (16) |
Mg4—O11vi | 2.0426 (18) | O10—Mg1i | 2.0235 (17) |
Mg4—O9 | 2.0544 (17) | O11—Mg4vi | 2.0426 (18) |
Mg4—O3iii | 2.0549 (17) | O11—Mg2xii | 2.2395 (16) |
Mg4—O1 | 2.1312 (17) | O12—Mg3iii | 2.0759 (17) |
P1—O3 | 1.5252 (16) | O12—H12 | 0.8600 |
P1—O1 | 1.5297 (16) | ||
O10i—Mg1—O5ii | 177.45 (7) | O1—Mg3—O12x | 90.91 (7) |
O10i—Mg1—O5iii | 93.60 (7) | O6—Mg3—O12x | 95.01 (7) |
O5ii—Mg1—O5iii | 84.54 (7) | O6ix—Mg3—O12x | 82.93 (7) |
O10i—Mg1—O8 | 89.62 (7) | O4viii—Mg3—O9 | 82.41 (7) |
O5ii—Mg1—O8 | 91.62 (7) | O1—Mg3—O9 | 80.21 (7) |
O5iii—Mg1—O8 | 161.77 (7) | O6—Mg3—O9 | 96.14 (7) |
O10i—Mg1—O2ii | 97.16 (7) | O6ix—Mg3—O9 | 108.15 (7) |
O5ii—Mg1—O2ii | 84.67 (7) | O12x—Mg3—O9 | 165.63 (8) |
O5iii—Mg1—O2ii | 92.32 (7) | O8—Mg4—O11vi | 135.86 (7) |
O8—Mg1—O2ii | 105.09 (7) | O8—Mg4—O9 | 97.00 (7) |
O10i—Mg1—O3iii | 96.93 (7) | O11vi—Mg4—O9 | 124.27 (7) |
O5ii—Mg1—O3iii | 81.15 (6) | O8—Mg4—O3iii | 83.43 (7) |
O5iii—Mg1—O3iii | 83.53 (6) | O11vi—Mg4—O3iii | 102.94 (7) |
O8—Mg1—O3iii | 78.27 (6) | O9—Mg4—O3iii | 98.66 (7) |
O2ii—Mg1—O3iii | 165.53 (7) | O8—Mg4—O1 | 88.96 (7) |
O7iv—Mg2—O7ii | 180.00 (7) | O11vi—Mg4—O1 | 84.69 (7) |
O7iv—Mg2—O2 | 91.18 (6) | O9—Mg4—O1 | 79.14 (7) |
O7ii—Mg2—O2 | 88.82 (6) | O3iii—Mg4—O1 | 171.78 (7) |
O7iv—Mg2—O2v | 88.82 (6) | O3—P1—O1 | 111.79 (9) |
O7ii—Mg2—O2v | 91.18 (6) | O3—P1—O2 | 114.92 (9) |
O2—Mg2—O2v | 180.00 (7) | O1—P1—O2 | 110.31 (9) |
O7iv—Mg2—O11vi | 90.17 (6) | O3—P1—O4 | 106.96 (9) |
O7ii—Mg2—O11vi | 89.83 (6) | O1—P1—O4 | 107.87 (9) |
O2—Mg2—O11vi | 85.85 (6) | O2—P1—O4 | 104.43 (9) |
O2v—Mg2—O11vi | 94.15 (6) | O5—P2—O6 | 109.03 (9) |
O7iv—Mg2—O11vii | 89.83 (6) | O5—P2—O8 | 111.40 (9) |
O7ii—Mg2—O11vii | 90.17 (6) | O6—P2—O8 | 109.62 (9) |
O2—Mg2—O11vii | 94.15 (6) | O5—P2—O7 | 109.95 (9) |
O2v—Mg2—O11vii | 85.85 (6) | O6—P2—O7 | 108.49 (9) |
O11vi—Mg2—O11vii | 180.00 (8) | O8—P2—O7 | 108.30 (9) |
O4viii—Mg3—O1 | 104.92 (7) | O10—P3—O11 | 112.06 (9) |
O4viii—Mg3—O6 | 165.27 (8) | O10—P3—O9 | 112.08 (9) |
O1—Mg3—O6 | 89.19 (7) | O11—P3—O9 | 111.85 (9) |
O4viii—Mg3—O6ix | 87.80 (7) | O10—P3—O12 | 107.28 (9) |
O1—Mg3—O6ix | 165.83 (8) | O11—P3—O12 | 109.21 (9) |
O6—Mg3—O6ix | 78.70 (7) | O9—P3—O12 | 103.90 (9) |
O4viii—Mg3—O12x | 89.06 (7) |
Symmetry codes: (i) −x−1, −y+1, −z−1; (ii) −x, −y+1, −z; (iii) x−1, y, z; (iv) x, y−1, z; (v) −x, −y, −z; (vi) −x−1, −y, −z−1; (vii) x+1, y, z+1; (viii) −x, −y, −z−1; (ix) −x, −y+1, −z−1; (x) x+1, y, z; (xi) x, y+1, z; (xii) x−1, y, z−1. |
D—H···A | D—H | H···A | D···A | D—H···A |
O4—H4···O7iv | 0.86 | 1.61 | 2.460 (2) | 172 |
O12—H12···O10i | 0.86 | 1.80 | 2.656 (2) | 171 |
Symmetry codes: (i) −x−1, −y+1, −z−1; (iv) x, y−1, z. |
Experimental details
Crystal data | |
Chemical formula | Mg7(PO4)2(HPO4)4 |
Mr | 744.02 |
Crystal system, space group | Triclinic, P1 |
Temperature (K) | 296 |
a, b, c (Å) | 6.4204 (5), 7.8489 (4), 9.4315 (5) |
α, β, γ (°) | 104.442 (3), 108.505 (5), 101.189 (8) |
V (Å3) | 416.70 (4) |
Z | 1 |
Radiation type | Mo Kα |
µ (mm−1) | 1.06 |
Crystal size (mm) | 0.16 × 0.10 × 0.07 |
Data collection | |
Diffractometer | Bruker X8 APEX Diffractometer |
Absorption correction | Multi-scan (SADABS; Bruker, 2005) |
Tmin, Tmax | 0.881, 0.929 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 9421, 1923, 1715 |
Rint | 0.036 |
(sin θ/λ)max (Å−1) | 0.651 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.026, 0.072, 1.07 |
No. of reflections | 1923 |
No. of parameters | 169 |
H-atom treatment | H-atom parameters constrained |
Δρmax, Δρmin (e Å−3) | 0.43, −0.42 |
Computer programs: APEX2 (Bruker, 2005), SAINT (Bruker, 2005), SHELXS97 (Sheldrick, 2008), SHELXL97 (Sheldrick, 2008), ORTEP-3 for Windows (Farrugia,1997) and DIAMOND (Brandenburg, 2006), WinGX publication routines (Farrugia, 1999).
D—H···A | D—H | H···A | D···A | D—H···A |
O4—H4···O7i | 0.86 | 1.61 | 2.460 (2) | 171.8 |
O12—H12···O10ii | 0.86 | 1.80 | 2.656 (2) | 171.1 |
Symmetry codes: (i) x, y−1, z; (ii) −x−1, −y+1, −z−1. |
Acknowledgements
The authors thank the Unit of Support for Technical and Scientific Research (UATRS, CNRST) for the X-ray measurements.
References
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Widespread studies are devoted to the metal phosphate owing to their impressive structural diversity and to their prospective applications in catalysis (Viter & Nagornyi, 2009), ion-exchangers (Clearfield, 1988)) and in batteries performance (Trad et al., (2010)). Mainly, our most attention has been paid to the hydrothermal synthesis of new metal based phosphate. Accordingly, we have recently succeed to obtain new phosphates, such as Ni2Sr(PO4)2 2H2O (Assani et al. (2010)), AgMg3(PO4)(HPO4)2 (Assani et al. (2011b)) and Ag2Ni3(HPO4)(PO4)2 (Assani et al. (2011a)).
Besides, the investigation of the MO—P2O5 systems (M=divalent cations) has allowed to isolate a new member of the metal phosphates, with a general formula M7(PO4)2(HPO4)4. The present paper aims to develop the hydrothermal synthesis and the structural characterization of the Mg7(PO4)2(HPO4)4 which is isostructural with Fe7(PO4)2(HPO4)4 (Zhou et al. (2002)), Mn7(PO4)2(HPO4)4 (Riou et al. (1987) and (Rojo et al. (2002)), Co7(PO4)2(HPO4)4 (Lightfoot & Cheetham, (1988)) and with their homologue arsenate Mg7(AsO4)2(HAsO4)4 (Kolitsch & Bartu, (2004)).
The crystal structure of Mg7(PO4)2(HPO4)4 is built up from MgO6, MgO4(OH)2 octahedra, MgO5 polyhedron, PO4 and PO3(OH) tetrahedra, sharing corners and edges to form a three-dimensional framework as shown in Fig.1 and Fig.2. In the asymmetric unit, all atoms are in general positions except for atom Mg2, which is located at a crystallographic inversion centre (0, 0, 0). Each OH group is bonded to an Mg and an P atom. Atom Mg2 is located at the centre of an Mg2O6 octahedron with significant bond-length distortion as shown in Table 1. In contrast, Mg1O6 and Mg3O4(OH)2 represent less distorted octahedra, and atom Mg4 is surrounded by five O ligands, forming a distorted Mg4O5 trigonal bipyramid. In this structure, each Mg1O6 and Mg3O6 octahedron shares an edge with its symmetrical to form a dimer. Both dimers, Mg1O10 and Mg3O10 are bound by Mg4O5 by sharing two edges to form a zigzag chaine. The Mg2O6 octahedron and PO4 tetrahedra are linked to neighboring polyhedra by vertices. The three crystallographically independent P atoms show tetrahedral coordination. The PO4 groups are relatively regular, although the two protonated groups, centred by P1 and P3, show a stronger angular and bond-length distortion in comparison with the unprotonated P2O4 tetrahedron as shown in Table 1. Moreover the OH groups, bridging Mg–(OH)–P, are involved in strong hydrogen bonds (Table 2).