research communications
Synthesis, 1.64Zn1.64Fe1.36(PO4)3 with an alluaudite-like structure
determination of a novel phosphate AgaLaboratoire de Chimie Appliquée des Matériaux, Centre des Sciences des Matériaux, Faculty of Sciences, Mohammed V University in Rabat, Avenue Ibn Batouta, BP 1014, Rabat, Morocco
*Correspondence e-mail: j_khmiyas@yahoo.fr
Single crystals of Ag1.64Zn1.64Fe1.36(PO4)3 [silver zinc iron phosphate (1.64/1.64/1.36/3)] have been synthesized by a conventional solid-state reaction and structurally characterized by single-crystal X-ray diffraction. The title compound crystallizes with an alluaudite-like structure. All atoms of the structure are in general positions except for four, which reside on special positions of the C2/c. The Ag+ cations reside at full occupancy on inversion centre sites and at partial occupancy (64%) on a twofold rotation axis. In this structure, the unique Fe3+ ion with one of the two Zn2+ cations are substitutionally disordered on the same general position (Wyckoff site 8f), with a respective ratio of 0.68/0.32 (occupancies were fixed so as to ensure electrical neutrality for the whole structure). The remaining O and P atoms are located in general positions. The three-dimensional framework of this structure consists of kinked chains of edge-sharing octahedra stacked parallel to [10]. These chains are built up by a succession of [MO6] (M = Zn/Fe or Zn) units. Adjacent chains are connected by the PO4 anions, forming sheets oriented perpendicular to [010]. These interconnected sheets generate two types of channels parallel to the c axis, in which the Ag+ cations are located. The validity and adequacy of the proposed structural model of Ag1.64Zn1.64Fe1.36(PO4)3 was established by means of bond-valence-sum (BVS) and charge-distribution (CHARDI) analysis tools.
Keywords: orthophosphate; alluaudite-like structure; disorder; X-ray diffraction; crystal structure.
CCDC reference: 2024206
1. Chemical context
The first ) using a specimen of pegmatite from Buranga-Rwanda. The metallic monophosphates belonging to this large alluaudite family form an important class of materials whose numerous phases present rich chemistry and great structural originality. Moore (1971) proposed the following general formulation for alluaudites: A(2)A(1)M(1)M(2)2(PO4)3 with A and M being cationic sites classified in decreasing order of size (rM(2)<rM(1) <rA(1)<rA(2)). In this structure, the first site A(1) can host a mono- or divalent cation and a vacancy (□), while the second site, A(2) contains a vacancy (□) as well as a monovalent cation (Moore & Ito, 1979). The other sites, M(1) and M(2), display octahedral geometries, which may contain a distribution of di- and trivalent cations. The natural alluaudite studied by Moore exhibits the following chemical formula: Na2.5Li0.1Ca0.5Mn4.52+Mg0.2Fe7.93+(PO4)12 and crystallizes in the monoclinic system, C2/c. In the structure of this compound, the cations are distributed over the four types of site as follows: A(1): 2.5Na+ + 0.7Mn2+ + 0.5Ca2+ + 0.3□, A(2): 4□, M(1): 3.8Mn2+ + 0.1Mg2+ + 0.1Li+, M(2): 7.9Fe3+ + 0.1Mg2+. Later, Hatert et al. (2000) proposed a complex and more accurate general formula for the alluaudite structure in order to take into account the different cationic sites available within the channels in the structure.
of natural alluaudite was determined by Fisher (1955The main characteristic of the alluaudite structure is the remarkable flexibility of its anionic framework, which is amenable to various cationic substitutions in the A and M sites (Chaalia et al., 2012). As a result, a large number of alluaudite compounds with interesting physical properties have been synthesized and systematically characterized. Indeed, the existence of transition metals in the structure is often the origin of interesting properties viz. magnetic (Hatert et al., 2004), [e.g., the role of AgCaCdMg2(PO4)3 and AgCd2Mg2(PO4)3 in the conversion of butan-2-ol] (Kacimi et al., 2005), electronic conductivity and significant ionic mobility (Richardson, 2003).
Accordingly, our efforts have mainly focused on the development and characterization of new alluaudite-type phosphates in M2O–M′O–P2O5 systems (M = monovalent cation, M′ = divalent cation). The hydrothermal study of the pseudo-ternary system Na2O–MgO–P2O5 allowed the isolation of the alluaudite based on sodium and magnesium: NaMg3(PO4)(HPO4)2 (Ould Saleck et al., 2015). Similarly, the investigation of the two pseudo-quaternary systems Na2O–CoO–Fe2O3–P2O5 and Na2O–ZnO–Fe2O3–P2O5, made it possible to obtain two new phases: Na2Co2Fe(PO4)3 (Bouraima et al., 2015) and Na1.67Zn1.67Fe1.33(PO4)3 (Khmiyas et al., 2015), by a solid-state route. Herein we report the synthesis of the new phosphate Ag1.64Zn1.64Fe1.36(PO4)3 and its structural characterization by single crystal X-ray diffraction. The suggested structural model is supported by means of bond-valence-sum (BVS) (Altermatt & Brown, 1985) and charge-distribution (CHARDI) (Nespolo et al., 2001) validation methods.
2. Structural commentary
The isolated phosphate, Ag1.64Zn1.64Fe1.36(PO4)3, crystallizes in the alluaudite structure type. The fundamental building units of the are [Ag1O8] and [Ag2O8] polyhedra, [(Fe1/Zn1)O6] and [Zn2O6] octahedra and two PO4 tetrahedra, as shown in Fig. 1. In this structure, the 4e (twofold) is partially occupied by Ag1 with an occupancy of 64%, while the 4a () site is entirely occupied by Ag2. The remaining 4e (twofold) sites are completely filled by P2 and Zn2 atoms. The general position occupied by Fe1/Zn1 exhibits substitutional disorder with statistical distribution of Fe1/Zn1 = 0.68/0.32. The values of the occupancies of these sites were rounded and fixed after the last cycle to respect the electrical neutrality of the structure. The consists of extended kinked chains of two edge-sharing [(Fe1/Zn1)O6] octahedra, leading to the formation of [(Fe1/Zn1)2O10] dimers. These dimers are connected by a common edge to [Zn2O6] units, as depicted in Fig. 2. Adjacent chains are held together through common vertices with the PO4 tetrahedral groups, to form stacked sheets perpendicular to [010] (Fig. 3). The resulting three-dimensional framework delimits two types of channel that extend along the [001] direction, hosting Ag+ cations (Fig. 4). Although these cationic sites display the same coordination sphere (CN = 8), their morphologies are clearly different. Indeed, Ag1 adopts a gable disphenoid morphology while Ag2 occupies the centre of a deformed cube. The Ag1—O and Ag2—O interatomic distances are in the ranges of 2.495 (2)–2.916 (2) Å, and 2.387 (2)–2.946 (2) Å, respectively. A close examination of effective (ECoN) for [Ag1]/CN[Ag1] = 7.35/8 versus [Ag2]/CN[Ag1] = 6.47/8 ratios reveals a more pronounced distortion in the Ag2O8 than in the Ag1O8 polyhedra. The mixed-occupancy [Fe1/Zn1] site [occupancy ratio Fe1:Zn1 = 0.68:0.32], is closely surrounded by six oxygen atoms with Fe1/Zn1—O bond lengths ranging from 1.947 (2) Å to 2.246 (2) Å. The second zinc cation Zn2 exhibits a similar coordination sphere with interatomic distances varying between 2.091 (2) and 2.198 (2) Å. Both octahedral geometries are strongly deformed, with a notable axial compression in [Fe1/Zn1]O6 compared to Zn2O6. The P—O bond lengths within the regular PO4 tetrahedral units vary between 1.522 (2) and 1.553 (2) Å. Their mean distances <P1—O> = 1.540 Å and <P2—O> = 1.542 Å, are in a good agreement with the <P—O> length usually reported in orthophosphate groups (Baur, 1974).
3. Structural model validation
In order to support the current CHARDI2015 (Nespolo & Guillot, 2016) and EXPO2014 (Altomare et al., 2013) programs, respectively. The results are summarized in Tables 1 and 2. For the proposed structural model, BVS were calculated for all constituent atoms using the dual concept: bond lengths/bond strengths. This robust validation method estimates the oxidation states of atoms [valence: V(i)], evaluates effectively the quality of the elucidation and predicts the level of structural strains. In this model, all the nearest ion–counter ion distances less than 3 Å are considered as bonds and taken into account. The CHARDI method is a modern generalization of Pauling's concept of bond strength (Pauling, 1929). This approach introduces directly the inter-atomic bond distances in a self-consistent computation to assign a geometrically defined bond strength to each bond. This method adopts a Madelung-type approximation of the crystal structures by attributing point charges to the atoms (the formal charge is equal to the Eon & Nespolo, 2015). The CHARDI analysis also involves the distribution of computed ECoN of a central atom among all the neighbouring ligands (Hoppe, 1979). The determination of non-integer ECoN is directly interpreted in terms of atomic charge distribution in crystalline structures. For a well refined structure, the calculated valences V(i) and the Q(i) charges according to BVS and CHARDI concepts must converge towards the weighted q(i)·sof(i) of each atom [where q(i) = formal and sof(i) = site occupancy]. The resulting values from both conceptions confirm the expected formal ionic charges of Ag+, Zn2+, Fe3+, P5+ and O2−. In the thirteen independent atomic sites within the the cationic charges are located at seven sites, while in the remaining sites the oxygen atoms balance the charges. For all cations, the internal criterion q(i)/Q(i) ∼ 1, where Q(i) represents the computed charge, imply the correctness of the (Nespolo et al., 1999). In the structure, all oxygen atoms exhibit a lower over or under bonding (OUB) effect with the exception of atoms O2 and O5, which deviate slightly from the formal value of −2 (Table 1). To estimate the convergence of the (CHARDI) model, the mean absolute percentage deviation (MAPD) was computed. MAPD measures the agreement between the q(i) and Q(i) charges for the whole sets of PC (polyhedron-centring) atoms and of V (vertex) atoms (Nespolo, 2016),
determination, CHARDI (CHARge-DIstribution) and BVS (Bond-Valence-Sum) analyses were performed usingwhere N is the number of polyhedron-centring or vertex atoms in the Respecting this experimental distribution scheme, the resulting values of MAPD for the cationic and anion charges are only 1.1% and 2.4%, respectively. This result supports the applicability and adequacy of the current model.
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In order to prove the chemical plausibility of the GII; Salinas-Sanchez et al., 1992). The GII index
we have also calculated the Global Instability Index (estimates the coherence of the structure and measures the deviation of the bond-valence sums from the formal valence V(i) averaged over all N atoms of the In our case, we found a very good GII index of 0.087 v.u., indicating the stability and the rigidity of the proposed structural model.
4. Database survey
The 1.64Zn1.64Fe1.36 (PO4)3, confirms it to be isotypic with the alluaudite structure. The observed deviation of the chemical formulation from the stoichiometric composition is often encountered in phosphate materials of the alluaudite type viz. Na1.50Mn2.48Al0.85(PO4)3 (Hatert, 2006), Na1.25Mg1.10Fe1.90(PO4)3 (Hidouri et al., 2008), NaFe3.67(PO4)3 (Korzenski et al., 1998), Na1.79Mg1.79Fe1.21(PO4)3 (Hidouri et al., 2003), Na0.38Ca0.31MgFe2(PO4)3 (Zid et al., 2005), α-Na0.67FePO4 (Kim et al., 2013), Li0.5Na0.5MnFe2(PO4)3 (Trad et al., 2010), Na1.5Mn1.5Fe1.5(PO4)3 (Hatert, 2004), Na1.86Fe3(PO4)3 (Essehli et al., 2016), Na1.85Mg1.85In1.15(PO4)3&Ag1.69Mg1.69In1.31(PO4)3 (Ould Saleck et al., 2018), Ag1.655Co1.647Fe1.352(PO4)3 (Bouraima et al., 2017). Generally, in this structure the interconnected sheets produce two types of hexagonal channels parallel to the c-axis direction (Hatert, 2008): channel (1) at (½, 0, z) and (0, ½, z), while channel (2) is located at (0, 0, z) and (½, ½, z) (Leroux et al., 1995). Both channels host two kinds of site: A(1) and A(2)′. Although A(1) and A(2)′ are likely to display CN = 8 coordination, they adopt different geometries. For instance in the Ag1.64Zn1.64Fe1.36(PO4)3 structure, the Ag(2) and Ag(1) cations occupy the A(1) and A(2)′ sites respectively. However, the morphology of the A sites remains a controversial subject. Indeed, Antenucci et al. (1995), brought a restriction on certain cation–oxygen bonds: A(1)—O and A(2)′—O (A—O ∼ 3 Å). Thus the A sites can adopt the coordination CN = 6, which implies the passage towards an irregular octahedron and deformed trigonal prism for A(1) and A(2)′, respectively. The evolution from AO8 to AO6 polyhedra was also reported by Khorari et al. (1997) for a study on the alluaudite NaCaCdMg2(AsO4)3. On the other hand, according to Hatert et al. (2006), the A(1) site is distorted cubic, while A(2)′ would have a first coordination sphere of only four atoms.
of the new phosphate, Ag5. Synthesis and crystallization
Single crystals of Ag1.64Zn1.64Fe1.36(PO4)6 were synthesized by means of a classical solid-state reaction in air. Appropriate amounts of the starting reagents: AgNO3, Zn(NO3)2·6H2O, Fe(NO3)3·9H2O, H3PO4 (85%) were taken in the following molar ratios Ag:Zn:Fe:P = 2:2:1:3. The mixture was dissolved in concentrated nitric acid, stirred at room temperature for 24 h and subsequently evaporated to dryness. The obtained solid was carefully milled in an agate mortar, placed in a platinum crucible and heated up to the melting point of 1223 K. The molten product was maintained at this temperature for 1 h then cooled down slowly to 920 K at rate of 5 K h−1 and then rapidly to room temperature by turning off the oven. The title compound was isolated as yellow parallelepiped-shaped crystals.
6. Refinement
Crystal data, data collection and structure . The of all the variable parameters leads to well-defined displacement ellipsoids. In the final cycles, the mixed-occupancy (Fe1/Zn1) site was refined with fixed complementary occupancies of 0.68/0.32. This cationic distribution scheme satisfies the electrical neutrality requirement and leads to the corresponding non-stoichiometric compound. The highest peak and the deepest hole in the last difference Fourier map were 0.63 and 0.56 Å from Ag1 and P1, respectively.
details are summarized in Table 3Supporting information
CCDC reference: 2024206
https://doi.org/10.1107/S2056989020011408/pk2642sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989020011408/pk2642Isup2.hkl
Data collection: APEX3 (Bruker, 2016); cell
SAINT (Bruker, 2016); data reduction: SAINT (Bruker, 2016); program(s) used to solve structure: SHELXT2014/5 (Sheldrick, 2015a); program(s) used to refine structure: SHELXL2016/6 (Sheldrick, 2015b); molecular graphics: ORTEP-3 for Windows (Farrugia, 2012), DIAMOND (Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).Ag1.64Zn1.64Fe1.36(PO4)3 | F(000) = 1211 |
Mr = 644.97 | Dx = 4.882 Mg m−3 |
Monoclinic, C2/c | Mo Kα radiation, λ = 0.71073 Å |
a = 11.8151 (5) Å | Cell parameters from 1924 reflections |
b = 12.6367 (6) Å | θ = 2.5–35.0° |
c = 6.4056 (3) Å | µ = 10.84 mm−1 |
β = 113.431 (2)° | T = 296 K |
V = 877.52 (7) Å3 | Parallelepiped, yellow |
Z = 4 | 0.36 × 0.27 × 0.20 mm |
Bruker D8 VENTURE Super DUO diffractometer | 1924 independent reflections |
Radiation source: INCOATEC IµS micro-focus source | 1585 reflections with I > 2σ(I) |
HELIOS mirror optics monochromator | Rint = 0.060 |
Detector resolution: 10.4167 pixels mm-1 | θmax = 35.0°, θmin = 2.5° |
φ and ω scans | h = −19→19 |
Absorption correction: multi-scan (SADABS; Krause et al., 2015) | k = −20→20 |
Tmin = 0.638, Tmax = 0.746 | l = −10→10 |
25488 measured reflections |
Refinement on F2 | 0 restraints |
Least-squares matrix: full | w = 1/[σ2(Fo2) + (0.0142P)2 + 2.467P] where P = (Fo2 + 2Fc2)/3 |
R[F2 > 2σ(F2)] = 0.024 | (Δ/σ)max = 0.001 |
wR(F2) = 0.044 | Δρmax = 1.41 e Å−3 |
S = 1.07 | Δρmin = −0.90 e Å−3 |
1924 reflections | Extinction correction: SHELXL-2018/3 (Sheldrick 2018), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
95 parameters | Extinction coefficient: 0.00124 (7) |
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 | Occ. (<1) | |
Ag1 | 1.000000 | 0.49101 (4) | 0.750000 | 0.02841 (12) | 0.64 |
Ag2 | 0.500000 | 0.500000 | 0.000000 | 0.01591 (7) | |
Zn1 | 0.78254 (3) | 0.34690 (2) | 0.37235 (5) | 0.00670 (6) | 0.32 |
Fe1 | 0.78254 (3) | 0.34690 (2) | 0.37235 (5) | 0.00670 (6) | 0.68 |
Zn2 | 0.500000 | 0.73456 (3) | 0.250000 | 0.01000 (8) | |
P1 | 0.76144 (5) | 0.61144 (4) | 0.37475 (8) | 0.00534 (10) | |
P2 | 0.500000 | 0.28593 (6) | 0.250000 | 0.00479 (13) | |
O1 | 0.83549 (14) | 0.66439 (12) | 0.6084 (2) | 0.0081 (3) | |
O2 | 0.77834 (14) | 0.67712 (12) | 0.1861 (3) | 0.0096 (3) | |
O3 | 0.62482 (14) | 0.60856 (12) | 0.3287 (3) | 0.0092 (3) | |
O4 | 0.81553 (16) | 0.50008 (12) | 0.3824 (3) | 0.0135 (3) | |
O5 | 0.60368 (13) | 0.35972 (12) | 0.2534 (3) | 0.0084 (3) | |
O6 | 0.45827 (13) | 0.21643 (12) | 0.0329 (2) | 0.0073 (3) |
U11 | U22 | U33 | U12 | U13 | U23 | |
Ag1 | 0.01096 (18) | 0.0277 (3) | 0.0355 (3) | 0.000 | −0.00255 (17) | 0.000 |
Ag2 | 0.02498 (14) | 0.00877 (11) | 0.00979 (11) | 0.00478 (9) | 0.00245 (9) | 0.00065 (8) |
Zn1 | 0.00572 (12) | 0.00818 (13) | 0.00660 (12) | 0.00103 (10) | 0.00288 (9) | 0.00078 (10) |
Fe1 | 0.00572 (12) | 0.00818 (13) | 0.00660 (12) | 0.00103 (10) | 0.00288 (9) | 0.00078 (10) |
Zn2 | 0.01101 (17) | 0.00984 (17) | 0.01111 (17) | 0.000 | 0.00646 (14) | 0.000 |
P1 | 0.0065 (2) | 0.0055 (2) | 0.0040 (2) | −0.00099 (18) | 0.00202 (18) | −0.00037 (18) |
P2 | 0.0051 (3) | 0.0052 (3) | 0.0036 (3) | 0.000 | 0.0013 (2) | 0.000 |
O1 | 0.0102 (7) | 0.0082 (7) | 0.0054 (6) | −0.0012 (5) | 0.0024 (5) | −0.0016 (5) |
O2 | 0.0093 (7) | 0.0129 (7) | 0.0066 (7) | −0.0034 (6) | 0.0031 (5) | 0.0005 (5) |
O3 | 0.0067 (6) | 0.0108 (7) | 0.0106 (7) | −0.0015 (5) | 0.0039 (6) | −0.0003 (6) |
O4 | 0.0163 (8) | 0.0086 (7) | 0.0156 (8) | 0.0028 (6) | 0.0063 (6) | −0.0023 (6) |
O5 | 0.0062 (6) | 0.0079 (7) | 0.0101 (7) | −0.0005 (5) | 0.0021 (5) | 0.0023 (5) |
O6 | 0.0061 (6) | 0.0086 (7) | 0.0062 (6) | −0.0003 (5) | 0.0015 (5) | −0.0015 (5) |
Ag1—O4 | 2.4953 (17) | Zn1—O1vii | 2.0275 (15) |
Ag1—O4i | 2.4953 (17) | Zn1—O2iii | 2.0525 (15) |
Ag1—O4ii | 2.6368 (18) | Zn1—O6iv | 2.0762 (15) |
Ag1—O4iii | 2.6368 (18) | Zn1—O2ix | 2.2463 (16) |
Ag1—O1i | 2.8281 (16) | Zn2—O3 | 2.0911 (16) |
Ag1—O1 | 2.8282 (16) | Zn2—O3viii | 2.0911 (16) |
Ag1—O6iv | 2.9160 (15) | Zn2—O6iii | 2.1497 (15) |
Ag1—O6v | 2.9160 (15) | Zn2—O6vi | 2.1497 (15) |
Ag2—O5vi | 2.3866 (15) | Zn2—O1x | 2.1975 (15) |
Ag2—O5 | 2.3866 (15) | Zn2—O1xi | 2.1975 (15) |
Ag2—O3 | 2.4538 (15) | P1—O3 | 1.5217 (15) |
Ag2—O3vi | 2.4538 (15) | P1—O4 | 1.5382 (16) |
Ag2—O3vii | 2.5587 (15) | P1—O2 | 1.5431 (16) |
Ag2—O3viii | 2.5587 (15) | P1—O1 | 1.5532 (15) |
Ag2—O5vii | 2.9459 (16) | P2—O5 | 1.5328 (15) |
Ag2—O5viii | 2.9459 (16) | P2—O5viii | 1.5328 (15) |
Zn1—O5 | 1.9473 (15) | P2—O6 | 1.5502 (15) |
Zn1—O4 | 1.9706 (16) | P2—O6viii | 1.5503 (15) |
O4—Ag1—O4i | 174.74 (8) | O5—Zn1—O4 | 95.79 (7) |
O4—Ag1—O4ii | 102.59 (5) | O5—Zn1—O1vii | 109.03 (6) |
O4i—Ag1—O4ii | 77.17 (5) | O4—Zn1—O1vii | 88.50 (6) |
O4—Ag1—O4iii | 77.17 (5) | O5—Zn1—O2iii | 87.17 (6) |
O4i—Ag1—O4iii | 102.60 (5) | O4—Zn1—O2iii | 101.23 (7) |
O4ii—Ag1—O4iii | 175.11 (7) | O1vii—Zn1—O2iii | 160.33 (6) |
O4—Ag1—O1i | 119.87 (5) | O5—Zn1—O6iv | 160.35 (6) |
O4i—Ag1—O1i | 55.31 (5) | O4—Zn1—O6iv | 102.51 (6) |
O4ii—Ag1—O1i | 61.28 (5) | O1vii—Zn1—O6iv | 78.85 (6) |
O4iii—Ag1—O1i | 114.48 (5) | O2iii—Zn1—O6iv | 82.34 (6) |
O4—Ag1—O1 | 55.31 (5) | O5—Zn1—O2ix | 77.79 (6) |
O4i—Ag1—O1 | 119.87 (5) | O4—Zn1—O2ix | 171.76 (6) |
O4ii—Ag1—O1 | 114.48 (5) | O1vii—Zn1—O2ix | 88.76 (6) |
O4iii—Ag1—O1 | 61.28 (5) | O2iii—Zn1—O2ix | 83.75 (6) |
O1i—Ag1—O1 | 78.45 (6) | O6iv—Zn1—O2ix | 84.57 (6) |
O4—Ag1—O6iv | 70.89 (5) | O3—Zn2—O3viii | 80.82 (8) |
O4i—Ag1—O6iv | 114.20 (5) | O3—Zn2—O6iii | 113.09 (6) |
O4ii—Ag1—O6iv | 83.66 (5) | O3viii—Zn2—O6iii | 92.67 (6) |
O4iii—Ag1—O6iv | 100.79 (5) | O3—Zn2—O6vi | 92.67 (6) |
O1i—Ag1—O6iv | 144.45 (4) | O3viii—Zn2—O6vi | 113.09 (6) |
O1—Ag1—O6iv | 125.39 (4) | O6iii—Zn2—O6vi | 146.50 (8) |
O4—Ag1—O6v | 114.20 (5) | O3—Zn2—O1x | 85.40 (6) |
O4i—Ag1—O6v | 70.89 (5) | O3viii—Zn2—O1x | 164.84 (6) |
O4ii—Ag1—O6v | 100.79 (5) | O6iii—Zn2—O1x | 86.93 (6) |
O4iii—Ag1—O6v | 83.66 (5) | O6vi—Zn2—O1x | 73.66 (5) |
O1i—Ag1—O6v | 125.39 (4) | O3—Zn2—O1xi | 164.84 (6) |
O1—Ag1—O6v | 144.45 (4) | O3viii—Zn2—O1xi | 85.40 (6) |
O6iv—Ag1—O6v | 51.96 (6) | O6iii—Zn2—O1xi | 73.66 (5) |
O5vi—Ag2—O5 | 180.0 | O6vi—Zn2—O1xi | 86.93 (6) |
O5vi—Ag2—O3 | 98.00 (5) | O1x—Zn2—O1xi | 108.94 (8) |
O5—Ag2—O3 | 82.00 (5) | O3—Zn2—O5vi | 84.84 (5) |
O5vi—Ag2—O3vi | 82.00 (5) | O3viii—Zn2—O5vi | 61.40 (5) |
O5—Ag2—O3vi | 98.00 (5) | O6iii—Zn2—O5vi | 146.63 (5) |
O3—Ag2—O3vi | 180.0 | O6vi—Zn2—O5vi | 51.69 (5) |
O5vi—Ag2—O3vii | 109.52 (5) | O1x—Zn2—O5vi | 123.73 (5) |
O5—Ag2—O3vii | 70.48 (5) | O1xi—Zn2—O5vi | 83.04 (5) |
O3—Ag2—O3vii | 114.55 (6) | O3—Zn2—O5iii | 61.40 (5) |
O3vi—Ag2—O3vii | 65.45 (6) | O3viii—Zn2—O5iii | 84.84 (5) |
O5vi—Ag2—O3viii | 70.48 (5) | O6iii—Zn2—O5iii | 51.69 (5) |
O5—Ag2—O3viii | 109.52 (5) | O6vi—Zn2—O5iii | 146.63 (5) |
O3—Ag2—O3viii | 65.45 (6) | O1x—Zn2—O5iii | 83.04 (5) |
O3vi—Ag2—O3viii | 114.55 (6) | O1xi—Zn2—O5iii | 123.73 (5) |
O3vii—Ag2—O3viii | 180.0 | O5vi—Zn2—O5iii | 136.14 (5) |
O5vi—Ag2—O5vii | 53.05 (6) | O3—P1—O4 | 112.31 (9) |
O5—Ag2—O5vii | 126.95 (6) | O3—P1—O2 | 108.59 (9) |
O3—Ag2—O5vii | 83.55 (5) | O4—P1—O2 | 109.61 (9) |
O3vi—Ag2—O5vii | 96.45 (5) | O3—P1—O1 | 110.16 (9) |
O3vii—Ag2—O5vii | 70.07 (5) | O4—P1—O1 | 107.20 (9) |
O3viii—Ag2—O5vii | 109.93 (5) | O2—P1—O1 | 108.92 (9) |
O5vi—Ag2—O5viii | 126.95 (6) | O5—P2—O5viii | 105.07 (12) |
O5—Ag2—O5viii | 53.05 (6) | O5—P2—O6 | 108.94 (8) |
O3—Ag2—O5viii | 96.45 (5) | O5viii—P2—O6 | 111.39 (8) |
O3vi—Ag2—O5viii | 83.55 (5) | O5—P2—O6viii | 111.39 (8) |
O3vii—Ag2—O5viii | 109.93 (5) | O5viii—P2—O6viii | 108.94 (8) |
O3viii—Ag2—O5viii | 70.07 (5) | O6—P2—O6viii | 110.98 (12) |
O5vii—Ag2—O5viii | 180.0 |
Symmetry codes: (i) −x+2, y, −z+3/2; (ii) −x+2, −y+1, −z+1; (iii) x, −y+1, z+1/2; (iv) x+1/2, −y+1/2, z+1/2; (v) −x+3/2, −y+1/2, −z+1; (vi) −x+1, −y+1, −z; (vii) x, −y+1, z−1/2; (viii) −x+1, y, −z+1/2; (ix) −x+3/2, y−1/2, −z+1/2; (x) −x+3/2, −y+3/2, −z+1; (xi) x−1/2, −y+3/2, z−1/2. |
q(i) = formal oxidation number; sof(i) = site occupancy; CN(i) = classical coordination number; Q(i) = calculated charge; V(i) = calculated valence; ECoN(i) = effective coordination number. |
Cation | q(i)·sof(i) | CN(i) | ECoN(i) | V(i) | Q(i) | q(i)/Q(i) |
Ag1 | 0.41 | 8 | 6.92 | 0.82 | 0.63 | 1.01 |
Ag2 | 1 | 8 | 6.47 | 1.23 | 0.98 | 1.02 |
Fe1/Zn1 | 2.68 | 6 | 5.57 | 2.67 | 2.69 | 1.00 |
Zn2 | 2 | 6 | 5.91 | 1.83 | 2.00 | 1.00 |
P1 | 5 | 4 | 3.99 | 4.94 | 5.06 | 0.99 |
P2 | 5 | 4 | 4.00 | 4.91 | 4.89 | 1.02 |
Anion | q(i)·sof(i) | Q(i) | q(i)/Q(i) |
O1 | -2 | -2.00 | 1.00 |
O2 | -2 | -1.87 | 1.07 |
O3 | -2 | -2.01 | 1.00 |
O4 | -2 | -2.03 | 0.98 |
O5 | -2 | -2.10 | 0.95 |
O6 | -2 | -1.99 | 1.01 |
Acknowledgements
The authors thank the Unit of Support for Technical and Scientific Research (UATRS, CNRST) for the X-ray measurements and Mohammed V University, Rabat, Morocco, for financial support.
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