Literature DB >> 30225131

Na1.85Mg1.85In1.15(PO4)3 and Ag1.69Mg1.69In1.31(PO4)3 with alluaudite-type structures.

Ahmed Ould Saleck1, Abderrazzak Assani1, Mohamed Saadi1, Cyrille Mercier2, Claudine Follet2, Lahcen El Ammari1.   

Abstract

Single crystals of two new phosphates, sodium magnesium indium(III) tris-(orthophosphate) and silver magnesium indium(III) tris-(orthophosphate), were obtained from solid-state reactions. The two phosphates are isotypic and exhibit alluaudite-type structures. They are characterized by a cationic disorder of the Mg and In sites and a partial occupation of the Na and Ag sites, respectively. The structure of both phosphates is made up of chains of edge-sharing [(Mg,In)O6] octa-hedra extending parallel to [10]. Adjacent chains are linked by PO4 tetra-hedra to form a three-dimensional framework delimiting two types of channels parallel to [001] in which the monovalent cations are situated. The coordination numbers of the Na+ cations are 6 and 8, and for both Ag+ cations 6. The corresponding coordination spheres are considerably distorted.

Entities:  

Keywords:  alluaudite; crystal structure; disorder; mixed-metal phosphate; solid-state reaction

Year:  2018        PMID: 30225131      PMCID: PMC6127713          DOI: 10.1107/S2056989018011799

Source DB:  PubMed          Journal:  Acta Crystallogr E Crystallogr Commun


Chemical context

The crystal structure of the mineral alluaudite was determined by Moore (1971 ▸). Since then, many new members of this structure type, including phosphates, arsenates, molybdates, sulfates and, more recently, vanadates have been synthesized and structurally characterized. The growing inter­est in these kinds of materials is related to their inter­esting physical properties, in particular in electrochemistry and battery research. For example, the phosphate Na2Ni2Fe(PO4)3 (Essehli et al., 2015 ▸) is a promising cathode in sodium batteries since its electrochemical behaviour is comparable to that of LiFePO4. In this context, alluaudite-type phosphates such as Na1.67Zn1.67Fe1.33(PO4)3 (Khmiyas et al., 2015 ▸), Ag1.655Co1.647Fe1.352(PO4)3 (Bouraima et al., 2017 ▸) and the vanadate (Na0.7)(Na0.70, Mn0.30) (Fe3+, Fe2+)2Fe2+(VO4)3 (Benhsina et al., 2016 ▸) have been investigated by our group. In the present work, the synthesis and structure determination of two new magnesium-based alluaudite-type phosphates with composition Na1.85Mg1.85In1.15(PO4)3 (I) and Ag1.69Mg1.69In1.31(PO4)3 (II) are reported.

Structural commentary

In the crystal structures of the two isotypic phosphates (I) and (II), site Na1 (Ag1) shows full occupancy and is located on an inversion centre (Wyckoff position 4b), and one mixed-occupied (Mg/In)2 site [occupancy ratio Mg:In = 0.51:0.49 for (I) and 0.314:0.686 for (II)], the second partially occupied Na2 (Ag2) site [occupancy 0.848 (9) for (I) and 0.6988 for (II)] and the P1 site are located on twofold rotation axes (4e) of space group type C2/c. There is another mixed-occupancy (Mg,In)1 site in a general position (8f) with occupancy ratios Mg:In = 0.68:0.32 for (I) and 0.687 (2):0.314 (2) for (II). This kind of cationic disorder is a characteristic feature of alluaudite-type structures. The principal building units in the crystal structures of (I) and (II) are [(Mg/In)1O6] and [(Mg,In)2O6] octa­hedra and two PO4 tetra­hedra (Figs. 1 ▸ and 2 ▸). Two [(Mg/In)1O6] octa­hedra are linked together by a common edge into an [(Mg/In)1)2O10] dimer. These dimers are connected through edge-sharing with [(Mg/In)2O6] octa­hedra into undulating chains extending parallel to [10] (Fig. 3 ▸). Adjacent chains are linked together by P1O4 and P2O4 tetra­hedra into (010) sheets, as shown in Fig. 4 ▸. Neighbouring sheets are finally fused into a three-dimensional framework structure by P1O4 tetra­hedra. This framework delimits two types of hexa­gonal channels oriented parallel to [001], in which the Na+ (for (I) or Ag+ (for (II) cations are located (Fig. 5 ▸). The Na—O distances fall in the range 2.307 (2)–2.960 (2) Å with coordination numbers of six for Na1 and eight for Na2, while those for Ag—O vary between 2.345 (2) and 2.963 (2) Å, with coordination numbers of six for both Ag+ cations.
Figure 1

The principal building units in the structure of Na1.85Mg1.85In1.15(PO4)3, (I). Displacement ellipsoids are drawn at the 50% probability level. [Symmetry codes: (i) −x + , y + , −z + ; (ii) −x + , −y + , −z + 1; (iii) −x + 1, −y + 1, −z; (iv) −x + , −y + , −z; (v) −x + 1, y, −z + ; (vi) x − , −y + , z − ; (vii) x, −y + 1, z + ; (viii) x, −y + 1, z − ; (ix) −x + 2, y, −z + ; (x) −x + 2, −y + 1, −z + 1; (xi) x + , −y + , z + ; (xii) −x + , −y + , −z + 1.]

Figure 2

The principal building units in the structure of Ag1.69Mg1.69In1.31(PO4)3, (II). Displacement ellipsoids are drawn at the 50% probability level. Symmetry codes are as in Fig. 1 ▸.

Figure 3

Edge-sharing [(Mg/In)2O6] octa­hedra and [(Mg/In)1)2O10] dimers forming an infinite chain extending parallel to [00]. Data taken from (I).

Figure 4

[(Mg/In)O6] octa­hedra and PO4 tetra­hedra forming a sheet extending parallel to (010). Data taken from (I).

Figure 5

Polyhedral representation of the crystal structure of (I) showing Na+ cations situated in the two types of channels parallel to [001].

Database Survey

The presence of disordered alkali metal or other cations in the channels of alluaudite-type structures is a concomitant feature of the cationic disorder at the octa­hedral sites, as observed for example in Cu1.35Fe3(PO4)3 (Warner et al., 1993 ▸), (Na0.38,Ca0.31)MgFe2(PO4)3 (Zid et al., 2005 ▸), K0.53Mn2.37Fe1.24(PO4)3 (Hidouri & Ben Amara, 2011 ▸), NaFe3.67(PO4)3 (Korzenski et al., 1998 ▸), Na1.25Mg1.10Fe1.90(PO4)3 (Hidouri et al., 2008 ▸), Na1.50Mn2.48Al0.85(PO4)3 (Hatert, 2006 ▸), Na1.79Mg1.79Fe1.21(PO4)3 (Hidouri et al., 2003 ▸), Na1.67Zn1.67Fe1.33(PO4)3 (Khmiyas et al., 2015 ▸) or Ag1.655Co1.647Fe1.352(PO4)3 (Bouraima et al., 2017 ▸).

Synthesis and crystallization

Single crystals of (I) and (II) were grown by solid-state reactions. The starting mixtures comprising of Mg(NO3)2·6H2O (Sigma–Aldrich, 97%), InI3 (Ventron, 99%), NH4H2PO4 (Alfa Aesar, 98%), ANO3 (A = Na or Ag) (NaNO3: Acros Organics, 99%; AgNO3: Sigma–Aldrich, 99%) were weighted in molar ratios A:Zn:In:P = 2:2:1:3 and placed in a platinum cruicible. After inter­mediate grinding and temperature treatments at 573, 673, 773 and 873 K in a platinum crucible, both mixtures were heated at 1373 K above the melting temperatures. The cruicibles were then cooled slowly to 1093 K at a rate of 5 K h−1, followed by cooling to room temperature after switching off the furnace. Transparent, colourless crystals with a blocky form were isolated from the two final products. The bulk products were not checked for phase purity.

Refinement

Crystal data, data collection and structure refinement details are summarized in Table 1 ▸. In the initial stages of the refinements the occupancies of the disordered sodium (Na2) or silver (Ag2) sites were refined freely and the mixed-occupancy (Mg/In) sites were refined under consideration of full occupancy for each of these sites. The obtained occupancy rates of Mg:In were rounded and subsequently fixed for charge-neutrality of the compounds. The maximum and minimum electron densities are located 0.55 Å from Mg2 and 0.38 Å from P1 for (I) and 0.78 and 0.59 Å, respectively, from Ag2 for (II).
Table 1

Experimental details

 (I)(II)
Crystal data
Chemical formulaNa1.85Mg1.85In1.15(PO4)3 Ag1.69Mg1.69In1.31(PO4)3
M r 504.46658.40
Crystal system, space groupMonoclinic, C2/c Monoclinic, C2/c
Temperature (K)296296
a, b, c (Å)11.9796 (13), 12.6935 (13), 6.5239 (7)12.0273 (3), 12.8120 (3), 6.5061 (2)
β (°)114.555 (3)114.519 (1)
V3)902.33 (17)912.14 (4)
Z 44
Radiation typeMo KαMo Kα
μ (mm−1)3.827.59
Crystal size (mm)0.31 × 0.24 × 0.200.30 × 0.27 × 0.23
 
Data collection
DiffractometerBruker X8 APEXIIBruker X8 APEXII
Absorption correctionMulti-scan (SADABS; Krause et al., 2015)Multi-scan (SADABS; Krause et al., 2015)
T min, T max 0.596, 0.7480.404, 0.748
No. of measured, independent and observed [I > 2σ(I)] reflections21364, 2076, 201213615, 1827, 1818
R int 0.0260.027
(sin θ/λ)max−1)0.8190.781
 
Refinement
R[F 2 > 2σ(F 2)], wR(F 2), S 0.024, 0.058, 1.290.022, 0.053, 1.25
No. of reflections20761827
No. of parameters9797
Δρmax, Δρmin (e Å−3)0.64, −0.882.32, −1.36

Computer programs: APEX2 and SAINT (Bruker, 2014 ▸), SHELXS2016 (Sheldrick, 2015a ▸), SHELXL2016 (Sheldrick, 2015b ▸), ORTEP-3 for Windows (Farrugia, 2012 ▸), DIAMOND (Brandenburg, 2006 ▸) and publCIF (Westrip, 2010 ▸).

Crystal structure: contains datablock(s) I, II, global. DOI: 10.1107/S2056989018011799/wm5457sup1.cif Structure factors: contains datablock(s) I. DOI: 10.1107/S2056989018011799/wm5457Isup2.hkl Structure factors: contains datablock(s) II. DOI: 10.1107/S2056989018011799/wm5457IIsup3.hkl CCDC references: 1862981, 1862980 Additional supporting information: crystallographic information; 3D view; checkCIF report
Na1.85Mg1.85In1.15(PO4)3F(000) = 960
Mr = 504.46Dx = 3.713 Mg m3
Monoclinic, C2/cMo Kα radiation, λ = 0.71073 Å
a = 11.9796 (13) ÅCell parameters from 2076 reflections
b = 12.6935 (13) Åθ = 2.5–35.6°
c = 6.5239 (7) ŵ = 3.82 mm1
β = 114.555 (3)°T = 296 K
V = 902.33 (17) Å3Block, colourless
Z = 40.31 × 0.24 × 0.20 mm
Bruker X8 APEXII diffractometer2076 independent reflections
Radiation source: fine-focus sealed tube2012 reflections with I > 2σ(I)
Graphite monochromatorRint = 0.026
φ and ω scansθmax = 35.6°, θmin = 2.5°
Absorption correction: multi-scan (SADABS; Krause et al., 2015)h = −19→19
Tmin = 0.596, Tmax = 0.748k = −20→20
21364 measured reflectionsl = −10→4
Refinement on F297 parameters
Least-squares matrix: full0 restraints
R[F2 > 2σ(F2)] = 0.024w = 1/[σ2(Fo2) + (0.0082P)2 + 5.6344P] where P = (Fo2 + 2Fc2)/3
wR(F2) = 0.058(Δ/σ)max = 0.001
S = 1.29Δρmax = 0.64 e Å3
2076 reflectionsΔρmin = −0.88 e Å3
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.
xyzUiso*/UeqOcc. (<1)
Mg10.71903 (3)0.84384 (2)0.13247 (5)0.00578 (6)0.68
In10.71903 (3)0.84384 (2)0.13247 (5)0.00578 (6)0.32
In20.5000000.73266 (2)0.2500000.00619 (6)0.51
Mg20.5000000.73266 (2)0.2500000.00619 (6)0.49
P10.76657 (4)0.60997 (4)0.37446 (8)0.00665 (8)
P20.5000000.29168 (6)0.2500000.00702 (11)
Na10.5000000.5000000.0000000.0261 (4)
Na21.0000000.4813 (2)0.7500000.0369 (8)0.848 (9)
O10.77790 (14)0.67695 (12)0.1877 (2)0.0092 (2)
O20.83997 (14)0.66480 (12)0.6061 (2)0.0096 (2)
O30.82556 (15)0.50207 (12)0.3858 (3)0.0126 (3)
O40.62982 (14)0.60255 (13)0.3291 (3)0.0128 (3)
O50.59943 (14)0.36515 (12)0.2450 (3)0.0124 (3)
O60.45840 (13)0.22035 (12)0.0372 (2)0.0099 (2)
U11U22U33U12U13U23
Mg10.00607 (11)0.00594 (11)0.00620 (11)−0.00056 (8)0.00342 (8)−0.00092 (8)
In10.00607 (11)0.00594 (11)0.00620 (11)−0.00056 (8)0.00342 (8)−0.00092 (8)
In20.00700 (12)0.00580 (11)0.00657 (11)0.0000.00360 (9)0.000
Mg20.00700 (12)0.00580 (11)0.00657 (11)0.0000.00360 (9)0.000
P10.00876 (19)0.00636 (18)0.00521 (17)−0.00120 (14)0.00328 (15)−0.00039 (14)
P20.0072 (3)0.0077 (3)0.0054 (2)0.0000.0018 (2)0.000
Na10.0375 (9)0.0121 (6)0.0156 (6)0.0017 (6)−0.0020 (6)0.0029 (5)
Na20.0228 (11)0.0569 (17)0.0235 (11)0.0000.0020 (8)0.000
O10.0121 (6)0.0098 (6)0.0062 (5)−0.0004 (5)0.0044 (5)0.0014 (4)
O20.0136 (6)0.0099 (6)0.0053 (5)−0.0027 (5)0.0039 (5)−0.0017 (4)
O30.0189 (7)0.0062 (5)0.0135 (6)0.0003 (5)0.0077 (5)−0.0009 (5)
O40.0109 (6)0.0136 (6)0.0156 (7)−0.0035 (5)0.0072 (5)−0.0016 (5)
O50.0090 (6)0.0111 (6)0.0155 (7)−0.0012 (5)0.0036 (5)0.0053 (5)
O60.0083 (5)0.0131 (6)0.0076 (5)0.0007 (5)0.0026 (4)−0.0026 (5)
Mg1—O5i1.9992 (16)P2—O6v1.5558 (15)
Mg1—O3i2.0690 (16)P2—O61.5558 (15)
Mg1—O2ii2.1030 (15)Na1—O5iii2.3068 (15)
Mg1—O6iii2.1099 (15)Na1—O52.3068 (15)
Mg1—O1iv2.1207 (14)Na1—O42.4387 (16)
Mg1—O12.2144 (15)Na1—O4iii2.4388 (16)
In2—O4v2.1783 (17)Na1—O4viii2.6072 (15)
In2—O42.1784 (17)Na1—O4v2.6072 (15)
In2—O2ii2.1807 (15)Na1—O5viii2.9603 (17)
In2—O2vi2.1807 (15)Na1—O5v2.9603 (17)
In2—O6vii2.2115 (15)Na2—O32.4401 (17)
In2—O6iii2.2115 (15)Na2—O3ix2.4401 (17)
P1—O31.5287 (16)Na2—O3x2.5955 (17)
P1—O11.5373 (15)Na2—O3vii2.5955 (17)
P1—O41.5419 (16)Na2—O6xi2.856 (3)
P1—O21.5609 (15)Na2—O6xii2.856 (3)
P2—O51.5238 (16)Na2—O22.913 (3)
P2—O5v1.5238 (16)Na2—O2ix2.913 (3)
O5i—Mg1—O3i95.94 (6)O5—Na1—O4viii72.41 (6)
O5i—Mg1—O2ii111.05 (6)O4—Na1—O4viii111.56 (7)
O3i—Mg1—O2ii86.09 (6)O4iii—Na1—O4viii68.44 (7)
O5i—Mg1—O6iii162.43 (6)O5iii—Na1—O4v72.41 (6)
O3i—Mg1—O6iii99.50 (6)O5—Na1—O4v107.59 (6)
O2ii—Mg1—O6iii78.50 (6)O4—Na1—O4v68.44 (7)
O5i—Mg1—O1iv87.10 (6)O4iii—Na1—O4v111.56 (7)
O3i—Mg1—O1iv100.00 (6)O4viii—Na1—O4v180.0
O2ii—Mg1—O1iv160.31 (6)O5iii—Na1—O5viii52.70 (6)
O6iii—Mg1—O1iv82.03 (6)O5—Na1—O5viii127.30 (6)
O5i—Mg1—O181.05 (6)O4—Na1—O5viii85.86 (5)
O3i—Mg1—O1174.39 (6)O4iii—Na1—O5viii94.14 (5)
O2ii—Mg1—O190.57 (6)O4viii—Na1—O5viii66.27 (5)
O6iii—Mg1—O184.22 (6)O4v—Na1—O5viii113.73 (5)
O1iv—Mg1—O184.63 (6)O5iii—Na1—O5v127.30 (6)
O4v—In2—O481.40 (8)O5—Na1—O5v52.70 (6)
O4v—In2—O2ii165.44 (6)O4—Na1—O5v94.14 (5)
O4—In2—O2ii86.40 (6)O4iii—Na1—O5v85.86 (5)
O4v—In2—O2vi86.40 (6)O4viii—Na1—O5v113.73 (5)
O4—In2—O2vi165.44 (6)O4v—Na1—O5v66.27 (5)
O2ii—In2—O2vi106.70 (8)O5viii—Na1—O5v180.0
O4v—In2—O6vii90.87 (6)O3—Na2—O3ix167.61 (15)
O4—In2—O6vii113.19 (6)O3—Na2—O3x98.29 (5)
O2ii—In2—O6vii86.65 (5)O3ix—Na2—O3x80.70 (5)
O2vi—In2—O6vii74.72 (5)O3—Na2—O3vii80.70 (5)
O4v—In2—O6iii113.19 (6)O3ix—Na2—O3vii98.29 (5)
O4—In2—O6iii90.87 (6)O3x—Na2—O3vii170.69 (14)
O2ii—In2—O6iii74.72 (5)O3—Na2—O6xi73.60 (6)
O2vi—In2—O6iii86.65 (5)O3ix—Na2—O6xi118.42 (10)
O6vii—In2—O6iii148.70 (8)O3x—Na2—O6xi84.80 (7)
O3—P1—O1110.04 (9)O3vii—Na2—O6xi103.66 (8)
O3—P1—O4112.79 (9)O3—Na2—O6xii118.42 (10)
O1—P1—O4108.57 (9)O3ix—Na2—O6xii73.60 (6)
O3—P1—O2106.82 (9)O3x—Na2—O6xii103.66 (8)
O1—P1—O2108.72 (8)O3vii—Na2—O6xii84.80 (7)
O4—P1—O2109.83 (9)O6xi—Na2—O6xii52.60 (8)
O5—P2—O5v104.53 (13)O3—Na2—O254.35 (6)
O5—P2—O6v114.33 (8)O3ix—Na2—O2114.22 (10)
O5v—P2—O6v107.48 (9)O3x—Na2—O2109.91 (9)
O5—P2—O6107.48 (9)O3vii—Na2—O261.95 (6)
O5v—P2—O6114.33 (8)O6xi—Na2—O2126.98 (4)
O6v—P2—O6108.82 (12)O6xii—Na2—O2146.30 (5)
O5iii—Na1—O5180.0O3—Na2—O2ix114.22 (10)
O5iii—Na1—O499.83 (6)O3ix—Na2—O2ix54.35 (6)
O5—Na1—O480.17 (6)O3x—Na2—O2ix61.95 (6)
O5iii—Na1—O4iii80.17 (6)O3vii—Na2—O2ix109.91 (9)
O5—Na1—O4iii99.83 (6)O6xi—Na2—O2ix146.30 (5)
O4—Na1—O4iii180.0O6xii—Na2—O2ix126.98 (4)
O5iii—Na1—O4viii107.59 (6)O2—Na2—O2ix73.83 (9)
Ag1.69Mg1.69In1.31(PO4)3F(000) = 1219
Mr = 658.40Dx = 4.794 Mg m3
Monoclinic, C2/cMo Kα radiation, λ = 0.71073 Å
a = 12.0273 (3) ÅCell parameters from 1827 reflections
b = 12.8120 (3) Åθ = 2.5–33.7°
c = 6.5061 (2) ŵ = 7.59 mm1
β = 114.519 (1)°T = 296 K
V = 912.14 (4) Å3Block, colourless
Z = 40.30 × 0.27 × 0.23 mm
Bruker X8 APEXII diffractometer1827 independent reflections
Radiation source: fine-focus sealed tube1818 reflections with I > 2σ(I)
Graphite monochromatorRint = 0.027
φ and ω scansθmax = 33.7°, θmin = 2.5°
Absorption correction: multi-scan (SADABS; Krause et al., 2015)h = −18→18
Tmin = 0.404, Tmax = 0.748k = −20→20
13615 measured reflectionsl = −10→7
Refinement on F20 restraints
Least-squares matrix: fullw = 1/[σ2(Fo2) + (0.0071P)2 + 8.2996P] where P = (Fo2 + 2Fc2)/3
R[F2 > 2σ(F2)] = 0.022(Δ/σ)max = 0.001
wR(F2) = 0.053Δρmax = 2.32 e Å3
S = 1.25Δρmin = −1.36 e Å3
1827 reflectionsExtinction correction: SHELXL2016 (Sheldrick, 2015b), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4
97 parametersExtinction coefficient: 0.00143 (15)
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.
xyzUiso*/UeqOcc. (<1)
In10.71633 (3)0.84600 (3)0.12503 (6)0.0061 (2)0.314 (2)
Mg10.71633 (3)0.84600 (3)0.12503 (6)0.0061 (2)0.687 (2)
Mg20.5000000.73554 (2)0.2500000.00583 (9)0.314 (2)
In20.5000000.73554 (2)0.2500000.00583 (9)0.686 (2)
Ag10.5000000.5000000.0000000.02109 (10)
Ag21.0000000.48627 (5)0.7500000.03258 (15)0.6988
P10.76583 (5)0.61258 (4)0.37509 (9)0.00362 (10)
P20.5000000.29241 (6)0.2500000.00404 (13)
O10.77898 (15)0.67881 (13)0.1901 (3)0.0064 (3)
O20.84069 (15)0.66448 (13)0.6096 (3)0.0065 (3)
O30.81775 (16)0.50301 (13)0.3825 (3)0.0096 (3)
O40.62999 (15)0.60993 (13)0.3340 (3)0.0080 (3)
O50.60107 (15)0.36446 (13)0.2501 (3)0.0094 (3)
O60.45894 (15)0.22207 (13)0.0360 (3)0.0062 (3)
U11U22U33U12U13U23
In10.00587 (16)0.00690 (16)0.00638 (17)−0.00070 (10)0.00336 (11)−0.00109 (10)
Mg10.00587 (16)0.00690 (16)0.00638 (17)−0.00070 (10)0.00336 (11)−0.00109 (10)
Mg20.00560 (13)0.00642 (13)0.00604 (13)0.0000.00297 (9)0.000
In20.00560 (13)0.00642 (13)0.00604 (13)0.0000.00297 (9)0.000
Ag10.03303 (18)0.00978 (13)0.01314 (14)0.00397 (10)0.00229 (11)0.00201 (9)
Ag20.0127 (2)0.0291 (3)0.0406 (3)0.000−0.00429 (19)0.000
P10.0037 (2)0.0038 (2)0.0036 (2)−0.00040 (15)0.00170 (17)−0.00038 (15)
P20.0035 (3)0.0051 (3)0.0031 (3)0.0000.0010 (2)0.000
O10.0069 (6)0.0084 (6)0.0043 (6)−0.0004 (5)0.0027 (5)0.0011 (5)
O20.0084 (6)0.0072 (6)0.0034 (6)−0.0025 (5)0.0020 (5)−0.0018 (5)
O30.0106 (7)0.0043 (6)0.0142 (8)0.0006 (5)0.0055 (6)−0.0022 (5)
O40.0052 (6)0.0078 (6)0.0120 (7)0.0002 (5)0.0045 (6)0.0009 (5)
O50.0055 (6)0.0091 (7)0.0129 (8)−0.0018 (5)0.0032 (6)0.0031 (6)
O60.0052 (6)0.0091 (6)0.0043 (6)−0.0006 (5)0.0019 (5)−0.0014 (5)
In1—O5i2.0146 (17)Ag1—O5viii2.9625 (19)
In1—O3i2.0495 (17)Ag1—O5v2.9625 (19)
In1—O1ii2.0985 (16)Ag2—O32.4934 (19)
In1—O2iii2.1098 (17)Ag2—O3ix2.4934 (19)
In1—O6iv2.1140 (16)Ag2—O3x2.6713 (18)
In1—O12.2518 (17)Ag2—O3vii2.6713 (18)
Mg2—O42.1502 (17)Ag2—O2ix2.8751 (18)
Mg2—O4v2.1503 (17)Ag2—O22.8751 (18)
Mg2—O2iii2.1665 (16)Ag2—O6xi2.9558 (18)
Mg2—O2vi2.1665 (16)Ag2—O6xii2.9558 (18)
Mg2—O6vii2.1827 (16)P1—O31.5290 (17)
Mg2—O6iv2.1827 (16)P1—O11.5335 (17)
Ag1—O52.3450 (17)P1—O41.5425 (17)
Ag1—O5iv2.3451 (17)P1—O21.5624 (17)
Ag1—O4iv2.5162 (17)P2—O5v1.5261 (17)
Ag1—O42.5162 (17)P2—O51.5261 (17)
Ag1—O4viii2.6449 (17)P2—O61.5569 (17)
Ag1—O4v2.6449 (17)P2—O6v1.5569 (17)
O5i—In1—O3i93.91 (7)O4viii—Ag1—O5viii68.99 (5)
O5i—In1—O1ii86.84 (7)O4v—Ag1—O5viii111.01 (5)
O3i—In1—O1ii102.20 (7)O5—Ag1—O5v52.97 (7)
O5i—In1—O2iii110.35 (7)O5iv—Ag1—O5v127.03 (7)
O3i—In1—O2iii87.27 (7)O4iv—Ag1—O5v84.06 (5)
O1ii—In1—O2iii159.96 (6)O4—Ag1—O5v95.94 (5)
O5i—In1—O6iv160.79 (7)O4viii—Ag1—O5v111.01 (5)
O3i—In1—O6iv104.16 (7)O4v—Ag1—O5v68.99 (5)
O1ii—In1—O6iv83.05 (6)O5viii—Ag1—O5v180.0
O2iii—In1—O6iv77.49 (6)O3—Ag2—O3ix170.14 (8)
O5i—In1—O179.17 (7)O3—Ag2—O3x101.46 (5)
O3i—In1—O1170.47 (7)O3ix—Ag2—O3x78.02 (5)
O1ii—In1—O184.09 (6)O3—Ag2—O3vii78.02 (5)
O2iii—In1—O189.01 (6)O3ix—Ag2—O3vii101.46 (5)
O6iv—In1—O183.56 (6)O3x—Ag2—O3vii174.11 (7)
O4—Mg2—O4v83.10 (9)O3—Ag2—O2ix116.17 (5)
O4—Mg2—O2iii85.00 (6)O3ix—Ag2—O2ix54.71 (5)
O4v—Mg2—O2iii166.46 (6)O3x—Ag2—O2ix62.21 (5)
O4—Mg2—O2vi166.46 (6)O3vii—Ag2—O2ix112.62 (5)
O4v—Mg2—O2vi84.99 (6)O3—Ag2—O254.71 (5)
O2iii—Mg2—O2vi107.51 (9)O3ix—Ag2—O2116.17 (5)
O4—Mg2—O6vii111.55 (6)O3x—Ag2—O2112.62 (5)
O4v—Mg2—O6vii90.29 (6)O3vii—Ag2—O262.21 (5)
O2iii—Mg2—O6vii88.11 (6)O2ix—Ag2—O274.85 (7)
O2vi—Mg2—O6vii74.86 (6)O3—Ag2—O6xi73.59 (5)
O4—Mg2—O6iv90.29 (6)O3ix—Ag2—O6xi115.97 (5)
O4v—Mg2—O6iv111.55 (6)O3x—Ag2—O6xi83.88 (5)
O2iii—Mg2—O6iv74.86 (6)O3vii—Ag2—O6xi101.50 (5)
O2vi—Mg2—O6iv88.11 (6)O2ix—Ag2—O6xi145.67 (5)
O6vii—Mg2—O6iv151.18 (9)O2—Ag2—O6xi127.48 (4)
O4—Mg2—O5iv83.64 (6)O3—Ag2—O6xii115.97 (5)
O5—Ag1—O5iv180.0O3ix—Ag2—O6xii73.59 (5)
O5—Ag1—O4iv98.18 (6)O3x—Ag2—O6xii101.50 (5)
O5iv—Ag1—O4iv81.82 (6)O3vii—Ag2—O6xii83.88 (5)
O5—Ag1—O481.82 (6)O2ix—Ag2—O6xii127.48 (4)
O5iv—Ag1—O498.17 (6)O2—Ag2—O6xii145.67 (5)
O4iv—Ag1—O4180.0O6xi—Ag2—O6xii50.87 (6)
O5—Ag1—O4viii70.42 (6)O3—P1—O1111.04 (10)
O5iv—Ag1—O4viii109.58 (6)O3—P1—O4112.00 (10)
O4iv—Ag1—O4viii67.05 (7)O1—P1—O4108.85 (9)
O4—Ag1—O4viii112.95 (7)O3—P1—O2107.32 (10)
O5—Ag1—O4v109.58 (6)O1—P1—O2109.01 (9)
O5iv—Ag1—O4v70.42 (6)O4—P1—O2108.55 (10)
O4iv—Ag1—O4v112.95 (7)O5v—P2—O5105.56 (14)
O4—Ag1—O4v67.05 (7)O5v—P2—O6113.12 (9)
O4viii—Ag1—O4v180.00 (5)O5—P2—O6107.91 (9)
O5—Ag1—O5viii127.03 (7)O5v—P2—O6v107.91 (9)
O5iv—Ag1—O5viii52.97 (7)O5—P2—O6v113.12 (9)
O4iv—Ag1—O5viii95.94 (5)O6—P2—O6v109.26 (13)
O4—Ag1—O5viii84.06 (5)
  6 in total

1.  Na(1.50)Mn(2.48)Al(0.85)(PO4)3, a new synthetic alluaudite-type compound.

Authors:  Frédéric Hatert
Journal:  Acta Crystallogr C       Date:  2005-12-10       Impact factor: 1.172

2.  Alluaudite Na2Co2Fe(PO4)3 as an electroactive material for sodium ion batteries.

Authors:  R Essehli; I Belharouak; H Ben Yahia; K Maher; A Abouimrane; B Orayech; S Calder; X L Zhou; Z Zhou; Y-K Sun
Journal:  Dalton Trans       Date:  2015-05-07       Impact factor: 4.390

3.  K(0.53)Mn(2.37)Fe(1.24)(PO(4))(3).

Authors:  Mourad Hidouri; Mongi Ben Amara
Journal:  Acta Crystallogr Sect E Struct Rep Online       Date:  2010-12-11

4.  Comparison of silver and molybdenum microfocus X-ray sources for single-crystal structure determination.

Authors:  Lennard Krause; Regine Herbst-Irmer; George M Sheldrick; Dietmar Stalke
Journal:  J Appl Crystallogr       Date:  2015-01-30       Impact factor: 3.304

5.  SHELXT - integrated space-group and crystal-structure determination.

Authors:  George M Sheldrick
Journal:  Acta Crystallogr A Found Adv       Date:  2015-01-01       Impact factor: 2.290

6.  Crystal structure refinement with SHELXL.

Authors:  George M Sheldrick
Journal:  Acta Crystallogr C Struct Chem       Date:  2015-01-01       Impact factor: 1.172

  6 in total

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