

Supporting information
![]() | Crystallographic Information File (CIF) https://doi.org/10.1107/S1600536812014870/wm2609sup1.cif |
![]() | Structure factor file (CIF format) https://doi.org/10.1107/S1600536812014870/wm2609Isup2.hkl |
Key indicators
- Single-crystal X-ray study
- T = 296 K
- Mean
(P-O) = 0.003 Å
- R factor = 0.016
- wR factor = 0.039
- Data-to-parameter ratio = 18.6
checkCIF/PLATON results
No syntax errors found
Alert level A PLAT772_ALERT_2_A Suspect O-H Bond in CIF: O7 -- H8B .. 1.65 Ang. PLAT900_ALERT_1_A No Matching Reflection File Found .............. !
Alert level C PLAT416_ALERT_2_C Short Intra D-H..H-D H7 .. H8B .. 1.96 Ang. PLAT790_ALERT_4_C Centre of Gravity not Within Unit Cell: Resd. # 1 Co2 H4 O10 P2 Pb PLAT924_ALERT_1_C The Reported and Calculated Rho(min) Differ by . 1.49 eA-3 PLAT925_ALERT_1_C The Reported and Calculated Rho(max) Differ by . 1.76 eA-3
Alert level G PLAT004_ALERT_5_G Info: Polymeric Structure Found with Dimension . 3 PLAT005_ALERT_5_G No _iucr_refine_instructions_details in CIF .... ? PLAT007_ALERT_5_G Note: Number of Unrefined D-H Atoms ............ 4 PLAT153_ALERT_1_G The su's on the Cell Axes are Equal .......... 0.00010 Ang. PLAT232_ALERT_2_G Hirshfeld Test Diff (M-X) Pb1 -- O3 .. 8.6 su
2 ALERT level A = Most likely a serious problem - resolve or explain 0 ALERT level B = A potentially serious problem, consider carefully 4 ALERT level C = Check. Ensure it is not caused by an omission or oversight 5 ALERT level G = General information/check it is not something unexpected 4 ALERT type 1 CIF construction/syntax error, inconsistent or missing data 3 ALERT type 2 Indicator that the structure model may be wrong or deficient 0 ALERT type 3 Indicator that the structure quality may be low 1 ALERT type 4 Improvement, methodology, query or suggestion 3 ALERT type 5 Informative message, check
The title compound, Co2Pb(HPO4)(PO4)OH.H2O, was obtained from the hydrothermal treatment of a reaction mixture of Pb(NO3)2, metallic cobalt and 85wt% phosphoric acid in the molar ratio Pb:Co:P = 1:3:3. The hydrothermal reaction was conducted in a 23 ml Teflon-lined autoclave under autogeneous pressure at 473 K for three days. The product was filtered off, washed with deionized water and air dried. The resulting product consists of pink crystals besides some pink powder.
The O-bound 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). The highest remaining positive and negative electron densities observed in the final Fourier map are 0.76 Å and 0.78 Å, respectively, from Pb1.
Metal based phosphates are of great interest owing to either their remarkable diversity of structures or their properties and applications in catalysis, as ion-exchangers (Cheetham et al., 1999; Clearfield, 1988) or as positive electrode materials in lithium- and sodium-containing batteries (Trad et al., 2010)). Mainly, our focus of investigation is focused on orthophosphates with (mixed) divalent metals with general formula (M,M')3(PO4)2.nH2O (Assani et al., 2010). It has been pointed out that the structural diversity of this family of compounds depends on the size difference of the divalent cations (Effenberger, 1999) and on the degree of hydratation (Yakubovich et al., 2001; Lee et al., 2008. The highest water content known up to date is realised for Mg3(PO4)2.22H2O (Britvin et al., 2002). In this work, a new dicobalt lead phosphate(V)] with formula Co2Pb(HPO4)(PO4)OH.H2O, was hydrothermally synthesized and structurally characterized.
A search in the ICSD (Belsky et al., 2002) reveals that the crystal structure of this phosphate represents a new structure type. A plot of the crystal structure illustrating the most important coordination polyhedra and their mutual connections is represented in Fig. 1. All atoms are in special positions, except two oxygen atoms (O3,O6) in general position of the P21/m space group. The crystal structure is built up from three different types of polyhedra more or less distorted, viz. two PbO8 polyhedra (m symmetry), PO4 and PO3(OH) tetrahedra (both with m symmetry) and two CoO6 octahedra (both with 1 symmetry). The CoO6 octahedra share edges and form 1∞[Co(1)O2/1(H2O)2/2O2/2] and 1∞[Co(2)O2/1(OH)2/2O2/2] chains running parallel to [010], as shown in Fig. 2. Adjacent chains are connected by PO4 and HPO4 tetrahedra via vertices, leading to the formation of layers parallel to (100). These layers are in turn linked by sheets of distorted PbO8 polyhedra as also shown in Fig.2.
Bond valence sum calculations (Brown & Altermatt, 1985) for Pb12+, Co12+, Co22+, P15+ and P25+ ions are as expected, viz. 1.92, 2.03, 1.93, 5.05 and 5.05 valence units, respectively. The values of the bond valence sums calculated for the oxygen atoms show low values for O2, O7 and O8 when the contribution of H atoms are not considered (i.e. 1.23, 0.88 and 0.75 valence units, respectively). Hence these O atoms are associated with protons and are involved in O—H···O hydrogen bonding (Table 1). H atoms of the water molecule form very strong hydrogen bonds, especially O8–H8B···O7 with an D···A distance less than 2.5 Å. The H atom of the OH- group (O7) and the hydrogenphosphate group (O2) form weak bifurcated (O2) and trifurcated (O7) hydrogen bonds (Fig. 2, Table 1).
For catalytic properties of phosphates, see: Cheetham et al. (1999); Clearfield (1988); Trad et al. (2010). For compounds with related structures, see: Yakubovich et al. (2001); Lee et al. (2008); Effenberger (1999); Britvin et al. (2002); Assani et al. (2010). For bond-valence analysis, see: Brown & Altermatt (1985). For background to the Inorganic Crystal Structure Database (ICSD), see: Belsky et al. (2002).
Data collection: APEX2 (Bruker, 2005); cell refinement: 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) and DIAMOND (Brandenburg, 2006); software used to prepare material for publication: PLATON (Spek, 2009) and publCIF (Westrip, 2010).
Co2Pb(HPO4)(PO4)OH·H2O | F(000) = 500 |
Mr = 551.02 | Dx = 4.807 Mg m−3 |
Monoclinic, P21/m | Mo Kα radiation, λ = 0.71073 Å |
Hall symbol: -P 2yb | Cell parameters from 1601 reflections |
a = 7.4299 (1) Å | θ = 2.5–33.5° |
b = 6.2949 (1) Å | µ = 26.83 mm−1 |
c = 8.9057 (1) Å | T = 296 K |
β = 113.936 (1)° | Prism, pink |
V = 380.70 (1) Å3 | 0.18 × 0.12 × 0.08 mm |
Z = 2 |
Bruker X8 APEXII diffractometer | 1601 independent reflections |
Radiation source: fine-focus sealed tube | 1558 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.027 |
φ and ω scans | θmax = 33.5°, θmin = 2.5° |
Absorption correction: multi-scan (SADABS; Sheldrick, 1999) | h = −9→11 |
Tmin = 0.029, Tmax = 0.117 | k = −9→9 |
8321 measured reflections | l = −13→13 |
Refinement on F2 | Secondary atom site location: difference Fourier map |
Least-squares matrix: full | Hydrogen site location: difference Fourier map |
R[F2 > 2σ(F2)] = 0.016 | H-atom parameters constrained |
wR(F2) = 0.039 | w = 1/[σ2(Fo2) + (0.0153P)2 + 0.885P] where P = (Fo2 + 2Fc2)/3 |
S = 1.11 | (Δ/σ)max = 0.001 |
1601 reflections | Δρmax = 1.76 e Å−3 |
86 parameters | Δρmin = −1.49 e Å−3 |
0 restraints | Extinction correction: SHELXL97 (Sheldrick, 2008), Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
Primary atom site location: structure-invariant direct methods | Extinction coefficient: 0.0061 (3) |
Co2Pb(HPO4)(PO4)OH·H2O | V = 380.70 (1) Å3 |
Mr = 551.02 | Z = 2 |
Monoclinic, P21/m | Mo Kα radiation |
a = 7.4299 (1) Å | µ = 26.83 mm−1 |
b = 6.2949 (1) Å | T = 296 K |
c = 8.9057 (1) Å | 0.18 × 0.12 × 0.08 mm |
β = 113.936 (1)° |
Bruker X8 APEXII diffractometer | 1601 independent reflections |
Absorption correction: multi-scan (SADABS; Sheldrick, 1999) | 1558 reflections with I > 2σ(I) |
Tmin = 0.029, Tmax = 0.117 | Rint = 0.027 |
8321 measured reflections |
R[F2 > 2σ(F2)] = 0.016 | 0 restraints |
wR(F2) = 0.039 | H-atom parameters constrained |
S = 1.11 | Δρmax = 1.76 e Å−3 |
1601 reflections | Δρmin = −1.49 e Å−3 |
86 parameters |
Geometry. All e.s.d.'s (except the e.s.d. in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell e.s.d.'s are taken into account individually in the estimation of e.s.d.'s in distances, angles and torsion angles; correlations between e.s.d.'s in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell e.s.d.'s is used for estimating e.s.d.'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 > 2σ(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 | ||
Pb1 | 0.006473 (17) | 0.2500 | 0.232477 (15) | 0.01414 (5) | |
Co1 | −0.5000 | 0.0000 | 0.0000 | 0.00717 (8) | |
Co2 | 0.5000 | 0.5000 | 0.5000 | 0.00859 (8) | |
P1 | −0.22391 (12) | −0.2500 | 0.32517 (9) | 0.00646 (13) | |
P2 | −0.21025 (11) | 0.2500 | −0.16270 (9) | 0.00642 (13) | |
O1 | −0.3205 (3) | −0.2500 | 0.4478 (3) | 0.0088 (4) | |
O2 | 0.0058 (4) | −0.2500 | 0.4403 (3) | 0.0145 (5) | |
H2 | 0.0642 | −0.2500 | 0.3744 | 0.017* | |
O3 | −0.2656 (2) | −0.0469 (3) | 0.2228 (2) | 0.0102 (3) | |
O4 | 0.0041 (4) | 0.2500 | −0.0355 (3) | 0.0160 (5) | |
O5 | −0.3411 (3) | 0.2500 | −0.0638 (3) | 0.0096 (4) | |
O6 | −0.2489 (3) | 0.0525 (3) | −0.2742 (2) | 0.0135 (3) | |
O7 | −0.4341 (4) | 0.2500 | 0.3936 (3) | 0.0100 (4) | |
H7 | −0.3197 | 0.2500 | 0.3910 | 0.012* | |
O8 | −0.6059 (3) | 0.2500 | 0.0885 (3) | 0.0086 (4) | |
H8A | −0.7322 | 0.2500 | 0.0522 | 0.010* | |
H8B | −0.5660 | 0.2500 | 0.1937 | 0.010* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Pb1 | 0.01157 (7) | 0.02066 (8) | 0.01059 (7) | 0.000 | 0.00492 (4) | 0.000 |
Co1 | 0.00890 (17) | 0.00553 (19) | 0.00703 (16) | 0.00041 (14) | 0.00319 (14) | 0.00011 (13) |
Co2 | 0.01066 (18) | 0.0070 (2) | 0.00765 (16) | −0.00114 (14) | 0.00323 (14) | −0.00053 (13) |
P1 | 0.0091 (3) | 0.0062 (3) | 0.0048 (3) | 0.000 | 0.0035 (3) | 0.000 |
P2 | 0.0068 (3) | 0.0075 (3) | 0.0052 (3) | 0.000 | 0.0028 (2) | 0.000 |
O1 | 0.0122 (10) | 0.0082 (10) | 0.0084 (9) | 0.000 | 0.0067 (8) | 0.000 |
O2 | 0.0080 (10) | 0.0233 (14) | 0.0106 (10) | 0.000 | 0.0022 (8) | 0.000 |
O3 | 0.0119 (7) | 0.0090 (7) | 0.0083 (6) | −0.0011 (6) | 0.0027 (5) | 0.0010 (6) |
O4 | 0.0073 (10) | 0.0287 (15) | 0.0101 (10) | 0.000 | 0.0016 (8) | 0.000 |
O5 | 0.0110 (10) | 0.0101 (10) | 0.0105 (9) | 0.000 | 0.0071 (8) | 0.000 |
O6 | 0.0156 (8) | 0.0124 (8) | 0.0088 (6) | 0.0056 (7) | 0.0010 (6) | −0.0041 (6) |
O7 | 0.0113 (10) | 0.0130 (11) | 0.0074 (9) | 0.000 | 0.0055 (8) | 0.000 |
O8 | 0.0097 (9) | 0.0100 (10) | 0.0072 (9) | 0.000 | 0.0047 (8) | 0.000 |
Pb1—O4 | 2.380 (3) | P1—O1 | 1.531 (2) |
Pb1—O6i | 2.5429 (18) | P1—O2 | 1.595 (3) |
Pb1—O6ii | 2.5429 (18) | P2—O4 | 1.535 (3) |
Pb1—O3 | 2.7284 (17) | P2—O6 | 1.5432 (18) |
Pb1—O3iii | 2.7284 (17) | P2—O6iii | 1.5432 (18) |
Pb1—O5 | 2.846 (2) | P2—O5 | 1.554 (2) |
Pb1—O1iv | 2.857 (2) | O1—Co2xi | 2.2302 (16) |
Pb1—O2iv | 2.952 (3) | O1—Co2xii | 2.2302 (16) |
Co1—O8 | 2.0544 (14) | O1—Pb1iv | 2.857 (2) |
Co1—O8v | 2.0544 (14) | O2—Pb1iv | 2.952 (3) |
Co1—O3v | 2.0624 (16) | O2—H2 | 0.8600 |
Co1—O3 | 2.0624 (16) | O5—Co1xiii | 2.1766 (15) |
Co1—O5 | 2.1766 (15) | O6—Co2xiv | 2.1426 (17) |
Co1—O5v | 2.1766 (15) | O6—Pb1ii | 2.5429 (18) |
Co2—O7vi | 1.9978 (14) | O7—Co2xv | 1.9978 (14) |
Co2—O7vii | 1.9978 (14) | O7—Co2xii | 1.9978 (14) |
Co2—O6i | 2.1426 (17) | O7—H7 | 0.8600 |
Co2—O6viii | 2.1426 (17) | O7—H8B | 1.6474 |
Co2—O1ix | 2.2302 (16) | O8—Co1xiii | 2.0544 (14) |
Co2—O1iv | 2.2302 (16) | O8—H8A | 0.8600 |
P1—O3x | 1.5274 (18) | O8—H8B | 0.8600 |
P1—O3 | 1.5274 (18) | ||
O4—Pb1—O6i | 82.12 (5) | O3v—Co1—O5 | 88.92 (8) |
O4—Pb1—O6ii | 82.12 (5) | O3—Co1—O5 | 91.08 (8) |
O6i—Pb1—O6ii | 97.00 (9) | O8—Co1—O5v | 96.95 (6) |
O4—Pb1—O3 | 105.34 (5) | O8v—Co1—O5v | 83.05 (6) |
O6i—Pb1—O3 | 171.63 (5) | O3v—Co1—O5v | 91.08 (8) |
O6ii—Pb1—O3 | 87.90 (7) | O3—Co1—O5v | 88.92 (8) |
O4—Pb1—O3iii | 105.34 (5) | O5—Co1—O5v | 180.00 (12) |
O6i—Pb1—O3iii | 87.90 (7) | O7vi—Co2—O7vii | 180.0 |
O6ii—Pb1—O3iii | 171.63 (5) | O7vi—Co2—O6i | 87.93 (9) |
O3—Pb1—O3iii | 86.46 (8) | O7vii—Co2—O6i | 92.07 (9) |
O4—Pb1—O5 | 55.64 (7) | O7vi—Co2—O6viii | 92.07 (9) |
O6i—Pb1—O5 | 117.25 (4) | O7vii—Co2—O6viii | 87.93 (9) |
O6ii—Pb1—O5 | 117.25 (4) | O6i—Co2—O6viii | 180.0 |
O3—Pb1—O5 | 65.72 (4) | O7vi—Co2—O1ix | 100.06 (7) |
O3iii—Pb1—O5 | 65.72 (4) | O7vii—Co2—O1ix | 79.94 (7) |
O4—Pb1—O1iv | 132.09 (7) | O6i—Co2—O1ix | 93.55 (8) |
O6i—Pb1—O1iv | 67.09 (5) | O6viii—Co2—O1ix | 86.45 (8) |
O6ii—Pb1—O1iv | 67.09 (5) | O7vi—Co2—O1iv | 79.94 (7) |
O3—Pb1—O1iv | 109.06 (5) | O7vii—Co2—O1iv | 100.06 (7) |
O3iii—Pb1—O1iv | 109.06 (5) | O6i—Co2—O1iv | 86.45 (8) |
O5—Pb1—O1iv | 172.27 (6) | O6viii—Co2—O1iv | 93.55 (8) |
O4—Pb1—O2iv | 178.00 (7) | O1ix—Co2—O1iv | 180.0 |
O6i—Pb1—O2iv | 99.18 (5) | O3x—P1—O3 | 113.68 (14) |
O6ii—Pb1—O2iv | 99.18 (5) | O3x—P1—O1 | 112.68 (8) |
O3—Pb1—O2iv | 73.26 (5) | O3—P1—O1 | 112.68 (8) |
O3iii—Pb1—O2iv | 73.26 (5) | O3x—P1—O2 | 106.78 (8) |
O5—Pb1—O2iv | 122.36 (7) | O3—P1—O2 | 106.78 (8) |
O1iv—Pb1—O2iv | 49.91 (6) | O1—P1—O2 | 103.32 (13) |
O8—Co1—O8v | 180.00 (11) | O4—P2—O6 | 109.94 (9) |
O8—Co1—O3v | 87.37 (8) | O4—P2—O6iii | 109.94 (9) |
O8v—Co1—O3v | 92.63 (8) | O6—P2—O6iii | 107.30 (15) |
O8—Co1—O3 | 92.63 (8) | O4—P2—O5 | 106.40 (14) |
O8v—Co1—O3 | 87.37 (8) | O6—P2—O5 | 111.63 (9) |
O3v—Co1—O3 | 180.00 (13) | O6iii—P2—O5 | 111.63 (9) |
O8—Co1—O5 | 83.05 (6) | H8A—O8—H8B | 104.5 |
O8v—Co1—O5 | 96.95 (6) |
Symmetry codes: (i) −x, y+1/2, −z; (ii) −x, −y, −z; (iii) x, −y+1/2, z; (iv) −x, −y, −z+1; (v) −x−1, −y, −z; (vi) x+1, y, z; (vii) −x, −y+1, −z+1; (viii) x+1, −y+1/2, z+1; (ix) x+1, y+1, z; (x) x, −y−1/2, z; (xi) x−1, y−1, z; (xii) −x, y−1/2, −z+1; (xiii) −x−1, y+1/2, −z; (xiv) −x, y−1/2, −z; (xv) x−1, y, z. |
D—H···A | D—H | H···A | D···A | D—H···A |
O2—H2···O6ii | 0.86 | 2.28 | 3.027 (3) | 145 |
O2—H2···O6xiv | 0.86 | 2.28 | 3.027 (3) | 145 |
O7—H7···O2iv | 0.86 | 2.20 | 2.915 (3) | 140 |
O7—H7···O3 | 0.86 | 2.53 | 2.986 (2) | 114 |
O7—H7···O3iii | 0.86 | 2.53 | 2.986 (2) | 114 |
O8—H8A···O4xv | 0.86 | 1.79 | 2.649 (3) | 177 |
O8—H8B···O7 | 0.86 | 1.65 | 2.489 (3) | 165 |
Symmetry codes: (ii) −x, −y, −z; (iii) x, −y+1/2, z; (iv) −x, −y, −z+1; (xiv) −x, y−1/2, −z; (xv) x−1, y, z. |
Experimental details
Crystal data | |
Chemical formula | Co2Pb(HPO4)(PO4)OH·H2O |
Mr | 551.02 |
Crystal system, space group | Monoclinic, P21/m |
Temperature (K) | 296 |
a, b, c (Å) | 7.4299 (1), 6.2949 (1), 8.9057 (1) |
β (°) | 113.936 (1) |
V (Å3) | 380.70 (1) |
Z | 2 |
Radiation type | Mo Kα |
µ (mm−1) | 26.83 |
Crystal size (mm) | 0.18 × 0.12 × 0.08 |
Data collection | |
Diffractometer | Bruker X8 APEXII |
Absorption correction | Multi-scan (SADABS; Sheldrick, 1999) |
Tmin, Tmax | 0.029, 0.117 |
No. of measured, independent and observed [I > 2σ(I)] reflections | 8321, 1601, 1558 |
Rint | 0.027 |
(sin θ/λ)max (Å−1) | 0.777 |
Refinement | |
R[F2 > 2σ(F2)], wR(F2), S | 0.016, 0.039, 1.11 |
No. of reflections | 1601 |
No. of parameters | 86 |
H-atom treatment | H-atom parameters constrained |
Δρmax, Δρmin (e Å−3) | 1.76, −1.49 |
Computer programs: APEX2 (Bruker, 2005), SAINT (Bruker, 2005), SHELXS97 (Sheldrick, 2008), SHELXL97 (Sheldrick, 2008), ORTEP-3 for Windows (Farrugia,1997) and DIAMOND (Brandenburg, 2006), PLATON (Spek, 2009) and publCIF (Westrip, 2010).
D—H···A | D—H | H···A | D···A | D—H···A |
O2—H2···O6i | 0.86 | 2.28 | 3.027 (3) | 144.7 |
O2—H2···O6ii | 0.86 | 2.28 | 3.027 (3) | 144.7 |
O7—H7···O2iii | 0.86 | 2.20 | 2.915 (3) | 140.0 |
O7—H7···O3 | 0.86 | 2.53 | 2.986 (2) | 114.4 |
O7—H7···O3iv | 0.86 | 2.53 | 2.986 (2) | 114.4 |
O8—H8A···O4v | 0.86 | 1.79 | 2.649 (3) | 176.6 |
O8—H8B···O7 | 0.86 | 1.65 | 2.489 (3) | 165.4 |
Symmetry codes: (i) −x, −y, −z; (ii) −x, y−1/2, −z; (iii) −x, −y, −z+1; (iv) x, −y+1/2, z; (v) x−1, y, z. |
Metal based phosphates are of great interest owing to either their remarkable diversity of structures or their properties and applications in catalysis, as ion-exchangers (Cheetham et al., 1999; Clearfield, 1988) or as positive electrode materials in lithium- and sodium-containing batteries (Trad et al., 2010)). Mainly, our focus of investigation is focused on orthophosphates with (mixed) divalent metals with general formula (M,M')3(PO4)2.nH2O (Assani et al., 2010). It has been pointed out that the structural diversity of this family of compounds depends on the size difference of the divalent cations (Effenberger, 1999) and on the degree of hydratation (Yakubovich et al., 2001; Lee et al., 2008. The highest water content known up to date is realised for Mg3(PO4)2.22H2O (Britvin et al., 2002). In this work, a new dicobalt lead phosphate(V)] with formula Co2Pb(HPO4)(PO4)OH.H2O, was hydrothermally synthesized and structurally characterized.
A search in the ICSD (Belsky et al., 2002) reveals that the crystal structure of this phosphate represents a new structure type. A plot of the crystal structure illustrating the most important coordination polyhedra and their mutual connections is represented in Fig. 1. All atoms are in special positions, except two oxygen atoms (O3,O6) in general position of the P21/m space group. The crystal structure is built up from three different types of polyhedra more or less distorted, viz. two PbO8 polyhedra (m symmetry), PO4 and PO3(OH) tetrahedra (both with m symmetry) and two CoO6 octahedra (both with 1 symmetry). The CoO6 octahedra share edges and form 1∞[Co(1)O2/1(H2O)2/2O2/2] and 1∞[Co(2)O2/1(OH)2/2O2/2] chains running parallel to [010], as shown in Fig. 2. Adjacent chains are connected by PO4 and HPO4 tetrahedra via vertices, leading to the formation of layers parallel to (100). These layers are in turn linked by sheets of distorted PbO8 polyhedra as also shown in Fig.2.
Bond valence sum calculations (Brown & Altermatt, 1985) for Pb12+, Co12+, Co22+, P15+ and P25+ ions are as expected, viz. 1.92, 2.03, 1.93, 5.05 and 5.05 valence units, respectively. The values of the bond valence sums calculated for the oxygen atoms show low values for O2, O7 and O8 when the contribution of H atoms are not considered (i.e. 1.23, 0.88 and 0.75 valence units, respectively). Hence these O atoms are associated with protons and are involved in O—H···O hydrogen bonding (Table 1). H atoms of the water molecule form very strong hydrogen bonds, especially O8–H8B···O7 with an D···A distance less than 2.5 Å. The H atom of the OH- group (O7) and the hydrogenphosphate group (O2) form weak bifurcated (O2) and trifurcated (O7) hydrogen bonds (Fig. 2, Table 1).