Supporting information
Crystallographic Information File (CIF) https://doi.org/10.1107/S1600536805030552/cv6566sup1.cif | |
Rietveld powder data file (CIF format) https://doi.org/10.1107/S1600536805030552/cv6566Isup2.rtv | |
Structure factor file (CIF format) https://doi.org/10.1107/S1600536805030552/cv6566Isup3.hkl |
CCDC reference: 287536
Key indicators
- Powder synchrotron study
- T = 298 K
- Mean (C-C) = 0.001 Å
- R factor = 0.000
- wR factor = 0.000
- Data-to-parameter ratio = 0.0
checkCIF/PLATON results
No syntax errors found
Alert level A PLAT080_ALERT_2_A Maximum Shift/Error ............................ 2.25
Author Response: For structure solutions out of powder data this shift lies, due to correlations, within the expected area. |
Alert level C PLAT040_ALERT_1_C No H-atoms in this Carbon Containing Compound .. ? PLAT042_ALERT_1_C Calc. and Rep. MoietyFormula Strings Differ .... ? PLAT125_ALERT_4_C No _symmetry_space_group_name_Hall Given ....... ? PLAT141_ALERT_4_C su on a - Axis Small or Missing (x 100000) ..... 5 Ang. PLAT142_ALERT_4_C su on b - Axis Small or Missing (x 100000) ..... 6 Ang. PLAT143_ALERT_4_C su on c - Axis Small or Missing (x 100000) ..... 3 Ang. PLAT430_ALERT_2_C Short Inter D...A Contact O5 .. O5 .. 2.89 Ang.
1 ALERT level A = In general: serious problem 0 ALERT level B = Potentially serious problem 7 ALERT level C = Check and explain 0 ALERT level G = General alerts; check 2 ALERT type 1 CIF construction/syntax error, inconsistent or missing data 2 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 4 ALERT type 4 Improvement, methodology, query or suggestion
Disodium rhodizonate (97%, Aldrich) was dried in vacuo at 423 K over P4O10 for 3 d.
Powder diffraction data were collected at the high-resolution powder diffractometer at beamline ID31 at the European Synchrotron Radiation Facility (ESRF). An Si 111 reflection was used to select an X-ray energy of 30.99 keV. The size of the beam was adjusted to 2 × 0.6 mm2 using slits. The wavelength was determined to 0.40009 (5) Å from a silicon standard. The sample of (I) was contained in a 0.7 mm lithium borate glass (glass No. 50) capillary. The sample was rotated around θ in order to improve randomization of the crystallites. The diffracted beam was analyzed with a nine-crystal analyzer stage [nine Ge(111) crystals separated by 2° intervals] and detected with nine Na(Tl)I scintillation counters simultaneously. The incoming beam was monitored by an ion-chamber for normalization of the decay of the primary beam. 15 min scans were taken at T = 298 K in continuous mode for 1 h each, and later normalized and converted to step-scan data from −11.0 to 32.92° 2θ in steps of 0.002°. To minimize the effect of decomposition due to radiation damage, only identical scans were summed. Data reduction of the powder diffraction pattern of (I) was performed using the GUFI program (Dinnebier & Finger, 1998). Indexing using ITO (Visser, 1969) led to an orthorhombic unit cell. The space group assignment of Fddd was made according to the extinction rules, which could later be confirmed by Rietveld refinements (Rietveld, 1969). The number of formula units per unit cell (Z = 8) followed directly from volume increments. The peak profiles and precise lattice parameters were determined by Le Bail fits (Le Bail et al., 1988) using the program GSAS (Larson & Von Dreele, 1994). The background was modelled manually using GUFI. The peak profile was described by a pseudo-Voigt function (Thompson et al., 1987) in combination with a special function that accounts for the asymmetry due to axial divergence (Finger et al., 1994). The powder pattern of (I) exhibits some anisotropic peak broadening caused by lattice strain. The phenomenological strain model of Stephens (1999), as implemented in GSAS, was used to model the anisotropy of the full width at half maximum. Starting values for the unconstrained Rietveld refinement were taken from the isostructural compound 2 K+·C6O62− (Cowan & Howard, 2004). The background and starting values for the peak profile were taken from the corresponding LeBail fit. The Rietveld refinement converged satisfactorily (Fig. 5).
Data collection: Please complete; cell refinement: GSAS (Larson & Von Dreele, 1994); data reduction: GUFI (Dinnebier & Finger, 1998); program(s) used to solve structure: GSAS; program(s) used to refine structure: GSAS; molecular graphics: ATOMS (Dowty, 2002); software used to prepare material for publication: GSAS.
2Na+·C6O62− | F(000) = 848 |
Mr = 214.04 | Dx = 2.182 Mg m−3 |
Orthorhombic, Fddd | ? radiation, λ = 0.400094 Å |
a = 11.48349 (5) Å | µ = 0.0 mm−1 |
b = 14.32080 (6) Å | T = 298 K |
c = 7.92477 (3) Å | Particle morphology: block |
V = 1303.25 (2) Å3 | colourless |
Z = 8 | cylinder, 2 × 0.3 mm |
ID31 at ESRF diffractometer | Scan method: continuous |
Specimen mounting: 0.7 mm lithium borate glass capillary | 2θmin = 2°, 2θmax = 26°, 2θstep = 0.001° |
Data collection mode: transmission |
Refinement on Inet | Profile function: pseudo-Voigt |
Least-squares matrix: full | 28 parameters |
Rp = 0.058 | 0 restraints |
Rwp = 0.078 | 0 constraints |
Rexp = 0.060 | Weighting scheme based on measured s.u.'s |
R(F2) = 0.08970 | (Δ/σ)max = 2.25 |
χ2 = 1.690 | Background function: GSAS Background function number 2 with 4 terms. Cosine Fourier series 1: 0.00000 2: 0.00000 3: 0.00000 4: 0.00000 |
24000 data points | Preferred orientation correction: none |
2Na+·C6O62− | V = 1303.25 (2) Å3 |
Mr = 214.04 | Z = 8 |
Orthorhombic, Fddd | ? radiation, λ = 0.400094 Å |
a = 11.48349 (5) Å | µ = 0.0 mm−1 |
b = 14.32080 (6) Å | T = 298 K |
c = 7.92477 (3) Å | cylinder, 2 × 0.3 mm |
ID31 at ESRF diffractometer | Scan method: continuous |
Specimen mounting: 0.7 mm lithium borate glass capillary | 2θmin = 2°, 2θmax = 26°, 2θstep = 0.001° |
Data collection mode: transmission |
Rp = 0.058 | 24000 data points |
Rwp = 0.078 | 28 parameters |
Rexp = 0.060 | 0 restraints |
R(F2) = 0.08970 | (Δ/σ)max = 2.25 |
χ2 = 1.690 |
Refinement. CW Profile function number 4 with 18 terms has been used in the refinement. Pseudo-Voigt profile coefficients as parameterized in Thompson, Cox & Hastings (1987), asymmetry correction of Finger, Cox & Jephcoat (1994). Microstrain broadening by Stephens (1999). #1(GU) = 0.000 #2(GV) = 0.000 #3(GW) = 0.000 #4(GP) = 0.000 #5(LX) = 0.016 #6(ptec) = 0.00 #7(trns) = 0.00 #8(shft) = 0.0000 #9(sfec) = 0.00 #10(S/L) = 0.0013 #11(H/L) = 0.0020 #12(eta) = 0.8260 #13(S400) = 9.4E-03 #14(S040) = 3.8E-04 #15(S004) = 1.0E-02 #16(S220) = 2.2E-02 #17(S202) = 1.1E-02 #18(S022) = 3.4E-03 Peak tails are ignored where the intensity is below 0.0020 times the peak Aniso. broadening axis 0.0 0.0 1.0 |
x | y | z | Uiso*/Ueq | ||
Na1 | 0.47634 (6) | 0.125 | 0.125 | 0.0268 (3)* | |
C2 | 0.125 | 0.22737 (11) | 0.125 | 0.0181 (6)* | |
C3 | 0.12995 (16) | 0.17552 (8) | 0.28431 (12) | 0.0214 (4)* | |
O4 | 0.125 | −0.06472 (8) | 0.125 | 0.0270 (4)* | |
O5 | 0.14364 (7) | 0.03213 (5) | −0.17135 (9) | 0.0274 (3)* |
C2—C3 | 1.4658 (11) | C2—O4i | 1.2509 (17) |
C3—C3i | 1.451 (2) | C3—O5ii | 1.2537 (11) |
C3iii—C2—C3 | 119.13 (16) | C3i—C3—O5ii | 119.48 (7) |
C2—C3—C3i | 120.13 (8) | C2—C3—O5ii | 120.39 (11) |
C3—C2—O4i | 120.44 (8) |
Symmetry codes: (i) −x+1/4, −y+1/4, z; (ii) x, −y+1/4, −z+1/4; (iii) −x+1/4, y, −z+1/4. |
Experimental details
Crystal data | |
Chemical formula | 2Na+·C6O62− |
Mr | 214.04 |
Crystal system, space group | Orthorhombic, Fddd |
Temperature (K) | 298 |
a, b, c (Å) | 11.48349 (5), 14.32080 (6), 7.92477 (3) |
V (Å3) | 1303.25 (2) |
Z | 8 |
Radiation type | ?, λ = 0.400094 Å |
µ (mm−1) | 0.0 |
Specimen shape, size (mm) | Cylinder, 2 × 0.3 |
Data collection | |
Data collection method | ID31 at ESRF |
Specimen mounting | 0.7 mm lithium borate glass capillary |
Data collection mode | Transmission |
Scan method | Continuous |
2θ values (°) | 2θmin = 2 2θmax = 26 2θstep = 0.001 |
Refinement | |
R factors and goodness of fit | Rp = 0.058, Rwp = 0.078, Rexp = 0.060, R(F2) = 0.08970, χ2 = 1.690 |
No. of data points | 24000 |
No. of parameters | 28 |
(Δ/σ)max | 2.25 |
Computer programs: Please complete, GSAS (Larson & Von Dreele, 1994), GUFI (Dinnebier & Finger, 1998), GSAS, ATOMS (Dowty, 2002).
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Rhodizonic acid and its salts, especially the sodium and potassium salts, have been used, among others, in combination with tartaric acid as a determining reagent for gunpowder, the so called `rhodizonate staining technique' in forensic medicine (Marty et al., 2002; Bartsch et al., 1996). Academic interest has raised the question of whether oxocarbon dianions, CnOn2−, with their prototype C6O62− (rhodizonate), are aromatic or not (West, 1980; Braga et al., 2001). Recent studies of the solid-state structure of the rhodizonate dianion have showed that planar (2Rb+·C6O62−; Braga et al., 2001) as well as twisted boat-like (2 K+·C6O62−; Cowan & Howard, 2004) conformations are possible. Here, we report the crystal structure determination of the homologue 2Na+·C6O62−, (I), from synchrotron powder diffraction data.
Disodium rhodizonate (Fig. 1) is isostructural with dipotassium rhodizonate (Cowan & Howard, 2004). Layers of hexagonally packed cations alternate with layers of equally packed anions, as shown in Fig. 2, where the cations lie a/4 above the anions. The C—O bond lengths [1.250 (2) and 1.253 (1) Å] are similar to those of the higher homologues [K: 1.254 (5) and 1.255 (3) Å; Rb: 1.252 (9) and 1.255 (3) Å], whereas the C—C bond lengths [1.451 (2) and 1.466 (1) Å] are closer to those observed in the rubidium salt [1.468 (6) and 1.469 (6) Å] rather than those in the potassium salt [1.480 (5) and 1.479 (3) Å].
Fig. 3 shows the environment of the alkali metal. Like K2C6O6, the alkali metal in (I) is coordinated by eight O atoms from four different rhodizonate dianions, leading to a distorted quadratic antiprismatic coordination. Fig. 4 displays the slightly twisted conformation of the C6O62− anion (r.m.s. deviation from the mean plane is 0.113 Å).