inorganic compounds
Silver indium diphosphate, AgInP2O7
aLaboratoire de Chimie du Solide Appliquée, Faculté des Sciences, Université Mohammed V-Agdal, Avenue Ibn Batouta, BP 1014, Rabat, Morocco, and bCentre National pour la Recherche Scientifique et Technique, Division UATRS, Angle Allal AlFassi et Avenue des FAR, Hay Ryad, BP 8027, Rabat, Morocco
*Correspondence e-mail: zouihri@cnrst.ma
Polycrystalline material of the title compound, AgInP2O7, was synthesized by traditional high-temperature solid-state methods and single crystals were grown from the melt of a mixture of AgInP2O7 and B2O3 as in a platinium crucible. The structure consists of InO6 octahedra, which are corner-shared to PO4 tetrahedra into a three-dimensional network with hexagonal channels running parallel to the c axis. The silver cation, located in the channel, is bonded to seven O atoms of the [InP2O7] framework with Ag–O distances ranging from 2.370 (2) to 3.015 (2) Å. The P2O7 diphosphate anion is characterized by a P—O—P angle of 137.27 (9) and a nearly eclipsed conformation. AgInP2O7 is isotypic with the MIFeP2O7 (MI = Na, K, Rb, Cs and Ag) diphosphate family.
Related literature
For properties of MIFeP2O7 (MI = Na, K, Rb, Cs and Ag) diphosphates, see: Terebilenko et al. (2010); Hizhnyi et al. (2008); Whangbo et al. (2004); Vitins et al. (2000). For isotypic structures, see: Belkouch et al. (1995); Gabelica-Robert et al. (1982); Moya-Pizarro et al. (1984); Mercader et al. (1990).
Experimental
Crystal data
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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); software used to prepare material for publication: WinGX (Farrugia, 1999).
Supporting information
https://doi.org/10.1107/S1600536810052451/br2154sup1.cif
contains datablocks I, global. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S1600536810052451/br2154Isup2.hkl
AgInP2O7 in the form of single crystals was prepared by stoichiometric reaction of AgNO3, (NH4)2HPO4 and In2O3 in B2O3
The mixture was heated at 773 K under ambiante atmosphere for 6 h and 973 K for 2 h with intermediate grindings to ensure complete reaction. Subsequent melting at 1323 K followed by slow cooling to room temperature at a rate of 12°K h-1 resulted in colourless crystals of the title compound.The highest and deepest hole residual peak in the final difference Fourier map are located at 0.49 Å and 0.58 Å, respectively from Ag1 atom. The not significants bonds and angles were removed from the
file.The diphosphates AIMIIIP2O7 (AI = Li, Na, K, Rb, Cs and Ag; MIII = Al, Ga, Cr, Fe, In, Y) are extensively studied for their electrical and optical properties and for its perspective application as magnetic materials (Terebilenko et al. (2010); Hizhnyi et al. (2008); Whangbo et al. (2004); Vitins et al. (2000)). The crystal structures of most of these compounds are known except a few cases in which the crystal growth is difficult. In this context, the present paper reports on the determination of AgInP2O7
from X-ray diffraction single-crystal data.The structure of this phosphate is characterized by a three-dimensional network built up from indum octahedra linked to diphosphate groups by a corner-sharing. Each InO6 octahedra is surrounded by six PO4 tetrahedra belonging to five different P2O7 groups (see Fig.1 and Fig.2). As a result of these blocks, assemblage three-dimensional-framework is formed with hexagonal channels, where silver cations reside. Although, the coordination sphere of Ag+ cations is composed of seven O2- anions in an irregular geometry, located at Ag–O distances between 2.370 (2) and 3.015 (2) Å (see Fig.2). Furthermore, the diphosphate group contains two distorted PO4 tetrahedra sharing one corner and display a nearly eclipsed conformation. The P–O bond-lengths range between 1.492 (2) Å for terminal P1–O1 and 1.606 (2) Å for the bridging P2–O7 bond. Therefore, a P1–O7–P2 angle of 137.27 (9) ° is wider than 133.6 (3)° and 132.9 (3) ° reported for both AgFeP2O7 and NaFeP2O7 respectively (Belkouch et al. (1995); Gabelica-Robert et al. (1982); Moya-Pizarro et al. (1984); Mercader et al. (1990)).
Silver indium diphosphate (pyrophosphate) is isostructural to AIFeP2O7 (AI = Na, K, Rb, Cs and Ag) diphosphates family and is categorized as a dichromate type.
For properties of MIFeP2O7 (MI = Na, K, Rb, Cs and Ag) diphosphates, see: Terebilenko et al. (2010); Hizhnyi et al. (2008); Whangbo et al. (2004); Vitins et al. (2000). For isotypic structures, see: Belkouch et al. (1995); Gabelica-Robert et al. (1982); Moya-Pizarro et al. (1984); Mercader et al. (1990).
Data collection: APEX2 (Bruker, 2005); cell
SAINT (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); software used to prepare material for publication: WinGX (Farrugia, 1999).AgInP2O7 | F(000) = 728 |
Mr = 396.63 | Dx = 4.670 Mg m−3 |
Monoclinic, P21/c | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -P 2ybc | Cell parameters from 317 reflections |
a = 7.4867 (3) Å | θ = 2.5–30.2° |
b = 8.2620 (3) Å | µ = 8.11 mm−1 |
c = 9.8383 (5) Å | T = 296 K |
β = 112.038 (2)° | Block, colourless |
V = 564.09 (4) Å3 | 0.08 × 0.06 × 0.05 mm |
Z = 4 |
Bruker X8 APEXII CCD area-detector diffractometer | 3730 independent reflections |
Radiation source: fine-focus sealed tube | 3245 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.035 |
ω and φ scans | θmax = 41.0°, θmin = 2.9° |
Absorption correction: multi-scan (SADABS; Sheldrick, 1999) | h = −13→13 |
Tmin = 0.563, Tmax = 0.667 | k = −15→15 |
21692 measured reflections | l = −18→18 |
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)] = 0.021 | w = 1/[σ2(Fo2) + (0.017P)2 + 0.9979P] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.048 | (Δ/σ)max = 0.001 |
S = 1.03 | Δρmax = 1.62 e Å−3 |
3730 reflections | Δρmin = −2.04 e Å−3 |
101 parameters | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
0 restraints | Extinction coefficient: 0.0171 (4) |
AgInP2O7 | V = 564.09 (4) Å3 |
Mr = 396.63 | Z = 4 |
Monoclinic, P21/c | Mo Kα radiation |
a = 7.4867 (3) Å | µ = 8.11 mm−1 |
b = 8.2620 (3) Å | T = 296 K |
c = 9.8383 (5) Å | 0.08 × 0.06 × 0.05 mm |
β = 112.038 (2)° |
Bruker X8 APEXII CCD area-detector diffractometer | 3730 independent reflections |
Absorption correction: multi-scan (SADABS; Sheldrick, 1999) | 3245 reflections with I > 2σ(I) |
Tmin = 0.563, Tmax = 0.667 | Rint = 0.035 |
21692 measured reflections |
R[F2 > 2σ(F2)] = 0.021 | 101 parameters |
wR(F2) = 0.048 | 0 restraints |
S = 1.03 | Δρmax = 1.62 e Å−3 |
3730 reflections | Δρmin = −2.04 e Å−3 |
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 | ||
In1 | 0.242354 (15) | 0.495357 (12) | 0.247622 (11) | 0.00618 (3) | |
Ag1 | −0.20911 (3) | 0.52697 (2) | 0.30478 (2) | 0.02442 (4) | |
P1 | 0.57689 (6) | 0.74758 (5) | 0.46083 (4) | 0.00600 (6) | |
P2 | 0.17589 (6) | 0.78735 (5) | 0.45174 (4) | 0.00656 (6) | |
O1 | 0.6810 (2) | 0.86792 (17) | 0.40464 (15) | 0.0141 (2) | |
O2 | 0.6836 (2) | 0.71622 (16) | 0.62241 (14) | 0.0136 (2) | |
O3 | 0.52473 (17) | 0.59259 (15) | 0.36935 (14) | 0.01027 (19) | |
O4 | 0.04427 (18) | 0.91166 (17) | 0.35059 (15) | 0.0123 (2) | |
O5 | 0.1917 (2) | 0.79561 (16) | 0.60976 (14) | 0.0126 (2) | |
O6 | 0.13231 (18) | 0.61348 (15) | 0.39564 (14) | 0.01054 (19) | |
O7 | 0.37868 (18) | 0.83601 (16) | 0.44239 (16) | 0.0128 (2) |
U11 | U22 | U33 | U12 | U13 | U23 | |
In1 | 0.00656 (4) | 0.00614 (4) | 0.00593 (4) | −0.00024 (3) | 0.00244 (3) | −0.00045 (3) |
Ag1 | 0.01913 (7) | 0.02720 (8) | 0.03341 (9) | −0.00235 (6) | 0.01725 (7) | −0.01071 (7) |
P1 | 0.00574 (14) | 0.00643 (14) | 0.00582 (14) | −0.00025 (11) | 0.00217 (11) | 0.00044 (11) |
P2 | 0.00588 (14) | 0.00706 (14) | 0.00644 (14) | 0.00073 (11) | 0.00195 (11) | −0.00090 (12) |
O1 | 0.0185 (6) | 0.0141 (5) | 0.0133 (5) | −0.0053 (4) | 0.0104 (5) | 0.0012 (4) |
O2 | 0.0195 (6) | 0.0098 (5) | 0.0070 (4) | −0.0006 (4) | −0.0001 (4) | 0.0018 (4) |
O3 | 0.0072 (4) | 0.0099 (5) | 0.0130 (5) | −0.0012 (3) | 0.0030 (4) | −0.0040 (4) |
O4 | 0.0084 (5) | 0.0135 (5) | 0.0135 (5) | 0.0034 (4) | 0.0023 (4) | 0.0041 (4) |
O5 | 0.0211 (6) | 0.0099 (5) | 0.0072 (4) | −0.0009 (4) | 0.0058 (4) | −0.0023 (4) |
O6 | 0.0116 (5) | 0.0097 (5) | 0.0123 (5) | −0.0019 (4) | 0.0067 (4) | −0.0039 (4) |
O7 | 0.0078 (5) | 0.0100 (5) | 0.0217 (6) | 0.0010 (4) | 0.0069 (4) | −0.0020 (4) |
In1—O1i | 2.0799 (13) | Ag1—O5vii | 2.7829 (14) |
In1—O4ii | 2.1120 (12) | Ag1—O6vii | 3.0153 (14) |
In1—O2iii | 2.1133 (13) | P1—O1 | 1.4919 (13) |
In1—O5iv | 2.1401 (13) | P1—O2 | 1.5097 (13) |
In1—O3 | 2.1562 (12) | P1—O3 | 1.5292 (13) |
In1—O6 | 2.1569 (12) | P1—O7 | 1.6021 (13) |
Ag1—O3v | 2.3703 (12) | P2—O4 | 1.5101 (13) |
Ag1—O6 | 2.4757 (13) | P2—O5 | 1.5158 (13) |
Ag1—O4ii | 2.4865 (14) | P2—O6 | 1.5295 (13) |
Ag1—O2vi | 2.6991 (14) | P2—O7 | 1.6062 (13) |
Ag1—O7ii | 2.7744 (15) | ||
O1i—In1—O4ii | 90.70 (6) | O3v—Ag1—O5vii | 94.99 (4) |
O1i—In1—O2iii | 86.35 (6) | O6—Ag1—O5vii | 104.03 (4) |
O4ii—In1—O2iii | 89.82 (6) | O4ii—Ag1—O5vii | 80.85 (4) |
O1i—In1—O5iv | 89.04 (5) | O2vi—Ag1—O5vii | 157.25 (4) |
O4ii—In1—O5iv | 93.79 (5) | O7ii—Ag1—O5vii | 71.00 (4) |
O2iii—In1—O5iv | 174.18 (6) | O3v—Ag1—O6vii | 72.37 (4) |
O1i—In1—O3 | 96.36 (5) | O6—Ag1—O6vii | 88.04 (4) |
O4ii—In1—O3 | 172.86 (5) | O4ii—Ag1—O6vii | 119.79 (4) |
O2iii—In1—O3 | 89.55 (5) | O2vi—Ag1—O6vii | 148.46 (4) |
O5iv—In1—O3 | 87.43 (5) | O7ii—Ag1—O6vii | 119.64 (4) |
O1i—In1—O6 | 173.56 (5) | O5vii—Ag1—O6vii | 50.65 (4) |
O4ii—In1—O6 | 82.94 (5) | O1—P1—O2 | 111.17 (8) |
O2iii—In1—O6 | 92.62 (5) | O1—P1—O3 | 113.17 (8) |
O5iv—In1—O6 | 92.35 (5) | O2—P1—O3 | 113.16 (8) |
O3—In1—O6 | 89.98 (5) | O1—P1—O7 | 104.17 (8) |
O3v—Ag1—O6 | 134.04 (4) | O2—P1—O7 | 107.40 (8) |
O3v—Ag1—O4ii | 155.99 (4) | O3—P1—O7 | 107.10 (7) |
O6—Ag1—O4ii | 69.47 (4) | O4—P2—O5 | 115.20 (8) |
O3v—Ag1—O2vi | 85.86 (5) | O4—P2—O6 | 113.76 (8) |
O6—Ag1—O2vi | 91.29 (4) | O5—P2—O6 | 109.65 (8) |
O4ii—Ag1—O2vi | 89.15 (5) | O4—P2—O7 | 100.90 (8) |
O3v—Ag1—O7ii | 102.17 (4) | O5—P2—O7 | 109.63 (8) |
O6—Ag1—O7ii | 123.47 (4) | O6—P2—O7 | 107.01 (7) |
O4ii—Ag1—O7ii | 54.04 (4) | P1—O7—P2 | 137.27 (9) |
O2vi—Ag1—O7ii | 86.57 (4) |
Symmetry codes: (i) −x+1, y−1/2, −z+1/2; (ii) −x, y−1/2, −z+1/2; (iii) −x+1, −y+1, −z+1; (iv) x, −y+3/2, z−1/2; (v) x−1, y, z; (vi) x−1, −y+3/2, z−1/2; (vii) −x, −y+1, −z+1. |
Experimental details
Crystal data | |
Chemical formula | AgInP2O7 |
Mr | 396.63 |
Crystal system, space group | Monoclinic, P21/c |
Temperature (K) | 296 |
a, b, c (Å) | 7.4867 (3), 8.2620 (3), 9.8383 (5) |
β (°) | 112.038 (2) |
V (Å3) | 564.09 (4) |
Z | 4 |
Radiation type | Mo Kα |
µ (mm−1) | 8.11 |
Crystal size (mm) | 0.08 × 0.06 × 0.05 |
Data collection | |
Diffractometer | Bruker X8 APEXII CCD area-detector |
Absorption correction | Multi-scan (SADABS; Sheldrick, 1999) |
Tmin, Tmax | 0.563, 0.667 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 21692, 3730, 3245 |
Rint | 0.035 |
(sin θ/λ)max (Å−1) | 0.923 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.021, 0.048, 1.03 |
No. of reflections | 3730 |
No. of parameters | 101 |
Δρmax, Δρmin (e Å−3) | 1.62, −2.04 |
Computer programs: APEX2 (Bruker, 2005), SAINT (Bruker, 2005), SHELXS97 (Sheldrick, 2008), SHELXL97 (Sheldrick, 2008), ORTEP-3 for Windows (Farrugia, 1997), WinGX (Farrugia, 1999).
Footnotes
‡Permanent address: Centre National pour la Recherche Scientifique et Technique, Division UATRS, Angle Allal AlFassi et Avenue des FAR, Hay Ryad, BP 8027, Rabat, Morocco.
Acknowledgements
The authors thank the Unit of Support for Technical and Scientific Research (UATRS, CNRST) for the X-ray data collection.
References
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The diphosphates AIMIIIP2O7 (AI = Li, Na, K, Rb, Cs and Ag; MIII = Al, Ga, Cr, Fe, In, Y) are extensively studied for their electrical and optical properties and for its perspective application as magnetic materials (Terebilenko et al. (2010); Hizhnyi et al. (2008); Whangbo et al. (2004); Vitins et al. (2000)). The crystal structures of most of these compounds are known except a few cases in which the crystal growth is difficult. In this context, the present paper reports on the determination of AgInP2O7 crystal structure from X-ray diffraction single-crystal data.
The structure of this phosphate is characterized by a three-dimensional network built up from indum octahedra linked to diphosphate groups by a corner-sharing. Each InO6 octahedra is surrounded by six PO4 tetrahedra belonging to five different P2O7 groups (see Fig.1 and Fig.2). As a result of these blocks, assemblage three-dimensional-framework is formed with hexagonal channels, where silver cations reside. Although, the coordination sphere of Ag+ cations is composed of seven O2- anions in an irregular geometry, located at Ag–O distances between 2.370 (2) and 3.015 (2) Å (see Fig.2). Furthermore, the diphosphate group contains two distorted PO4 tetrahedra sharing one corner and display a nearly eclipsed conformation. The P–O bond-lengths range between 1.492 (2) Å for terminal P1–O1 and 1.606 (2) Å for the bridging P2–O7 bond. Therefore, a P1–O7–P2 angle of 137.27 (9) ° is wider than 133.6 (3)° and 132.9 (3) ° reported for both AgFeP2O7 and NaFeP2O7 respectively (Belkouch et al. (1995); Gabelica-Robert et al. (1982); Moya-Pizarro et al. (1984); Mercader et al. (1990)).
Silver indium diphosphate (pyrophosphate) is isostructural to AIFeP2O7 (AI = Na, K, Rb, Cs and Ag) diphosphates family and is categorized as a dichromate type.