research communications
Glycine zinc sulfate pentahydrate: redetermination at 10 K from time-of-flight neutron Laue diffraction
aISIS Facility, Rutherford Appleton Laboratory, Harwell Science and Innovation, Campus, Didcot, Oxfordshire OX11 0QX, England, and bDepartment of Earth Sciences, University College London, Gower Street, London, WC1E 6BT, England
*Correspondence e-mail: dominic.fortes@stfc.ac.uk
Single crystals of glycine zinc sulfate pentahydrate [systematic name: hexaaquazinc tetraaquadiglycinezinc bis(sulfate)], [Zn(H2O)6][Zn(C2H5NO2)2(H2O)4](SO4)2, have been grown by isothermal evaporation from aqueous solution at room temperature and characterized by single-crystal neutron diffraction. The contains two unique ZnO6 octahedra on sites of symmetry -1 and two SO4 tetrahedra with 1; the octahedra comprise one [tetraaqua-diglycine zinc]2+ ion (centred on one Zn atom) and one [hexaaquazinc]2+ ion (centred on the other Zn atom); the glycine zwitterion, NH3+CH2COO−, adopts a monodentate coordination to the first Zn atom. All other atoms sit on general positions of 1. Glycine forms centrosymmetric closed cyclic dimers due to N—H⋯O hydrogen bonds between the amine and carboxylate groups of adjacent and exhibits torsion angles varying from ideal planarity by no more than 1.2°, the smallest values for any known glycine zwitterion not otherwise constrained by a mirror plane. This work confirms the H-atom locations estimated in three earlier single-crystal X-ray diffraction studies with the addition of independently refined fractional coordinates and Uij parameters, which provide accurate internuclear X—H (X = N, O) bond lengths and consequently a more accurate and precise depiction of the hydrogen-bond framework.
Keywords: crystal structure; glycine; zinc sulfate; zwitterion; dimer; neutron diffraction.
CCDC reference: 1503478
1. Chemical context
Numerous coordination compounds of glycine (Glyc) with divalent metal sulfates are known. For the case of zinc, there is an anhydrous species, 2Glyc·ZnSO4 (Moldobaev & Nogoev, 1970) and two hydrates, Glyc·ZnSO4·3H2O and Glyc·ZnSO4·5H2O. The trihydrate is dimorphic, occurring either as an orthorhombic crystal (space group Pca21) or as a monoclinic crystal (P21/n) depending on the synthesis route (Fleck & Bohatý, 2004). The monoclinic form is isotypic with compounds of general formula Glyc·M(II)SO4·3H2O where M(II) = Mg, Co or Fe (Oguey et al., 2013a,b, 2014). Compounds with the general formula Glyc·M(II)SO4·5H2O are known only as isotypic triclinic crystals (P) for M(II) = Mg, Mn, Co, Fe and Zn (Lindqvist & Rosenstein, 1960; Elayaraja et al., 2007; Fleck & Bohatý, 2006; Tepavitcharova et al., 2012). Solubility data have been published for a purported Glyc·NiSO4·5H2O (Moldobaev et al., 1970; Alymkulova & Salyeva, 1987). We have collected as-yet unpublished X-ray powder-diffraction data from this species, showing that it is isotypic with the other known members of the series. The existence of Glyc·CuSO4·5H2O has been reported by Thilagavathi et al. (2012) but their work is in error, and quite unambiguously describes the well-known material CuSO4·5H2O.
We recently carried out the first neutron diffraction study of Glyc·MgSO4·3H2O and Glyc·MgSO4·5H2O using perdeuterated powder specimens (Howard et al., 2016). Glyc·MgSO4·5H2O tends to form masses of crystals that are both of poor quality and are too small for single-crystal neutron diffraction study; however, this is not the case for Glyc·MnSO4·5H2O and Glyc·ZnSO4·5H2O, where fine tabular to blocky single crystals with volumes substantially in excess of 10 mm3 are formed with ease (Fig. 1). The objective of this work was to carry out the first single-crystal neutron diffraction study of any Glyc·M(II)SO4·5H2O compound, specifically using a specimen with M(II) = Zn.
Optical and mechanical properties of the title compound were reported by Balakrishnan & Ramamurthy (2007), although they incorrectly give the composition as Glyc·ZnSO4·7H2O. The effect of doping Glyc·ZnSO4·5H2O with cobalt is described by El-Fadl & Abdulwahab (2010). Three prior structure refinements from single-crystal X-ray diffraction data have been reported (Balamurugan et al., 2011; Tepavitcharova et al., 2012; Oguey et al., 2013c); comparisons with this work are detailed in Section 2.
2. Structural commentary
Although the stoichiometry of the material is accurately reflected in its common name, glycine zinc sulfate pentahydrate, the presence of two symmetry-inequivalent Zn sites means that the crystallographically proper structural composition is the `double' formula [Gly·ZnSO4·5H2O]2, or more precisely [Zn(H2O)6][Zn(H2O)4(C2H5NO2)2](SO4)2; the contains one of these units.
The Zn1 coordination octahedron consists of tetraaqua-diglycine zinc(II) with the glycine zwitterion (NH3+CH2COO−) coordinating to Zn by one of the carboxylate oxygen atoms (Fig. 2); the inversion centre results in an all-trans configuration for these units. The Zn2 octahedron has the form hexaaquazinc(II); the sulfate tetrahedra are isolated, accepting hydrogen bonds primarily (but not exclusively) from Zn-coordinating water molecules (Fig. 3). The S—O bond lengths (Table 1) reflect the number of hydrogen bonds accepted by each apical oxygen atom with a statistical significance which was not apparent from the powder of Howard et al. (2016) but which are in excellent agreement with the single-crystal X-ray study of Tepavitcharova et al. (2012).
Bond lengths and angles of the glycine zwitterion agree very well with other determinations of related compounds made by X-ray single-crystal diffraction at higher temperatures and extremely well with the determinations in α-glycine at room temperature by neutron single-crystal diffraction (Jönsson & Kvick, 1972; Power et al., 1976), particularly in respect of their mean N—H bond lengths (1.039 Å) and mean C—H bond lengths (1.090 Å). The glycine zwitterion is remarkably planar, with torsion angles O7—C1—C2—N1 = −1.18 (3)° and O8—C1—C2—N1 = 179.23 (2)°, even by comparison with, for example, glycine nickel bromide tetrahydrate (Fleck & Bohatý, 2005), glycine lithium chromate monohydrate and glycine lithium molybdate (Fleck et al., 2006), where torsion angles are in the range 169–176°. Only in glycine magnesium chloride tetrahydrate, where the glycine zwitterion lies on a mirror plane, are values of 180° realized (Fleck & Bohatý, 2005). In α-glycine, the equivalent torsion angles are −19.60 (3) and 161.28 (2)°.
In respect of the heavy atoms, agreement in the interatomic distances and angles between the single-crystal X-ray and single-crystal neutron refinements (Table 1) is excellent, with some differences emerging in respect of the room-temperature by Balamurugan et al. (2011). However, the neutron data provide a substantial improvement in accuracy with respect to the X-ray data in the hydrogen atom's fractional coordinates and Uij parameters. This is not surprising since neutrons are sensitive to the nuclear positions and X-rays to the electron density; in the covalent X—H bond the centroid of the H-atom's electron-density distribution is displaced towards the heavy atom by 0.1 Å, yielding X—H distances from 10–15% shorter than the true internuclear separation (Coppens, 1997). Table 2 compares X—H bond lengths from a range of Gly·M(II)SO4·5H2O crystals obtained by single-crystal X-ray diffraction and by neutron powder diffraction. In the work of Elayaraja et al. (2007), methyl hydrogens were positioned geometrically and allowed to ride with Uiso(H) = 1.2Ueq(C); water hydrogen atoms were refined with restraints; the N—H bond lengths were all restrained to be equal. Balamurugan et al. (2011) placed the majority of their hydrogen atoms geometrically, although failed to identify the third amine hydrogen atom; water and the two amine H atoms were refined isotropically whereas the two methyl hydrogen atoms were riding on the C atom. Tepavitcharova et al. (2012) placed the hydrogen atoms in Gly·ZnSO4·5H2O geometrically and treated all of them as riding on their associated heavy atom during Oguey et al. (2013c) allowed all water hydrogen atoms to refine isotropically but fixed the methyl and amine hydrogens to ride on C and N, respectively. The coordinates of hydrogen atoms in this work were unrestrained and allowed to refine anisotropically.
|
Our values for the N—H and C—H bond lengths are in excellent agreement with other single-crystal neutron diffraction work, as noted in the preceding paragraph. Our values for the O—H bond lengths also agree well with those found in similar environments in hydrated M(II) coordination compounds, such as MgSO4·11H2O and MgCrO4·11H2O where the average O–H = 0.974 Å (Fortes et al., 2013), MgSeO4·9H2O, O—Hav = 0.972 Å (Fortes et al., 2015), and MgSeO4·7H2O, O—Hav = 0.974 Å (Fortes & Gutmann, 2014).
3. Supramolecular features
The overall three-dimensional framework is completed by a variety of hydrogen bonds with a range of strengths (Table 3). Fig. 4 shows the spatial relationship of the main structural elements. The majority of the hydrogen bonds are O—H⋯O contacts of medium strength (1.66 < H⋯O < 1.90 Å) and high linearity (∠ O—H⋯O > 157°), characteristic of two-centred interactions. As expected, the N—H⋯O hydrogen bonds are weaker (i.e., longer, 1.85 < H⋯O < 2.22 Å) and more strained (∠ N—H⋯O between approx. 140–160°). The methyl groups appear to participate in weak C—H⋯O hydrogen bonds (cf., Steiner & Desiraju, 1998). One C—H⋯O bond is evidently a two-centred interaction, being the shortest and most of linear contact of this kind, with H⋯O = 2.58 (1) Å and ∠ C—H⋯O = 167 (1)°. The other, involving C—H2A, is clearly a two-centred interaction (i.e., a bifurcated hydrogen bond) with `arms' of roughly equal length, H⋯O ≃ 2.7 Å and C—H⋯O angles of 119 and 128° involving O2 and O5, respectively.
|
3.1. Glycine dimers
A hitherto unrecognized aspect of the supramolecular structure of Glyc·M(II)SO4·5H2O compounds is the presence of glycine dimers (Fig. 5). These occur as closed cyclic structures formed by N—H⋯O hydrogen bonds between the amine group of one glycine zwitterion and the Zn-coordinating carboxylate oxygen (O7) of another zwitterion, related to the first by an inversion centre. A similar cyclic dimer occurs in the structure of α-glycine. A direct comparison between the dimers in Glyc·ZnSO4·5H2O and in α-glycine is shown in Fig. 6; clearly, the main difference between these two dimers is the orientation of the carboxylate group, which is presumably due to the influence of a divalent metal being coordinated by the O7 carboxylate oxygen. Experimental studies of aqueous solutions indicate that only glycine monomers exist in the liquid phase (Huang et al., 2008). However, there has been widespread disagreement on this matter from computational studies, which indicate either that there are no dimers (Hamad & Catlow, 2011), substantial quantities of closed zwitterionic dimers (Friant-Michel & Ruiz-López, 2010), or a small fraction of open dimers (Yani et al., 2012) present in saturated solutions. The presence or absence of glycine polymerization in coordination compounds such as these may be useful in understanding the association of glycine in saturated aqueous solutions during nucleation and the role of solvated metal ions in polymerizing amino acids in Earth's Hadean oceans (Kitadai et al., 2011, 2016) or in extraterrestrial oceans elsewhere in our solar system (Kimura & Kitadai, 2015).
4. Database survey
A search of the Cambridge Structural Database (Groom et al., 2016) identified the following directly relevant entries:
Glyc·M(II)SO4 pentahydrates: 672589 (Mg); 857075 (Mg); 1451396 (Mg); 296329 (Co); 857073 (Co); 806684 (Zn); 857076 (Zn); 936400 (Zn).
Glyc·M(II)SO4 trihydrates: 989590 (Mg); 1451397 (Mg); 857074 (Co); 936396 (Fe); 243588 (Zn, orthorhombic); 936394 (Zn, monoclinic).
Glyc·M(II)SO4 hexahydrates: 1285639 (Ni).
5. Vibrational spectroscopy
Laser-stimulated Raman spectra were measured using a portable B&WTek i-Raman Plus spectrometer equipped with a 532 nm laser (Pmax = 37 mW at the probe tip) that records spectra over the range 171–4002 cm−1 with an optimal resolution of 3 cm−1. Measurements were carried out on powdered specimens of α-glycine and Glyc·ZnSO4·5H2O. Samples were measured in thin-walled glass vials using the BC100 fibre-optic coupled Raman probe; the total integration time and laser power for each sample is provided with the tabulated results (see supplementary material).
The Raman spectrum of Glyc·ZnSO4·5H2O (Fig. 6) is virtually identical with that of Glyc·MgSO4·5H2O reported in Howard et al. (2016) and is in excellent agreement with the spectrum shown in Tepavitcharova et al. (2012). Numerical data of the Raman spectrum are provided as an electronic supplement; peak positions and vibrational mode assignments are given in Table 4. The main differences between the two divalent-metal-substituted compounds include the blue-shifting of octahedral deformation modes and blue-shifting of both symmetric and asymmetric COO− stretching modes. A large blue-shift of ν(A) and ν(S) COO− occurs when glycine coordinates to Mg2+ and the shift increases when glycine coordinates to Zn2+. Raman spectra of α-glycine and Glyc·ZnSO4·5H2O are shown in Fig. 7.
|
6. Synthesis and crystallization
Glyc·ZnSO4·5H2O was crystallized by evaporation at room temperature of an equimolar aqueous solution of α-glycine (Alfa Aesar A13816) and ZnSO4·7H2O (Sigma Aldrich Z4750) in deionized water (Alfa Aesar 36645). Unlike the MgSO4-bearing analogue, Glyc·ZnSO4·5H2O forms large well-faceted crystals that are both amenable to morphological study and suitably large for single-crystal neutron Fig. 1 shows photographs of a representative crystal viewed along its a axis and series of drawings with indexed crystal faces.
7. Data collection and refinement
Crystal data, data collection and structure . Data were collected from a pair of single crystals at a series of four discrete rotational positions about the vertical axis, each frame being counted for 5 h, equivalent to 800 µAhr of ISIS proton beam current per frame. The structure of Glyc(d5)·MgSO4·5D2O at 10 K reported by Howard et al. (2016) was used as a starting point for the A total of eleven peaks, with the largest σ(Fobs–Fcalc) values were omitted from the such outliers are fairly common in SXD measurement when peaks occur close to the edges of detectors. A mild restraint on the Uij parameters of the sulfur atom was imposed (SHELX ISOR command) in order to avoid a slightly non-positive-definite displacement ellipsoid. Since sulfur has the smallest neutron scattering of any atom in the structure, and since it is both comparatively heavy and the temperature is very low, it is not surprising that – within errors – the effective Uiso parameter should refine to a small negative value.
details are summarized in Table 5
|
Supporting information
CCDC reference: 1503478
https://doi.org/10.1107/S2056989016014304/wm5318sup1.cif
contains datablock I. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2056989016014304/wm5318Isup2.hkl
Raman spectrum of glycine zinc sulfate pentahydrate. Raman shift is in units of reciprocal centimetre and the intensity is in arbitrary units. DOI: https://doi.org/10.1107/S2056989016014304/wm5318sup3.txt
Data collection: SXD2001 (Gutmann, 2005); cell
SXD2001 (Gutmann, 2005); data reduction: SXD2001 (Gutmann, 2005); program(s) used to solve structure: SHELXT2014 (Sheldrick, 2015a; Gruene et al., 2014); program(s) used to refine structure: SHELXL2014 (Sheldrick, 2015b; Gruene et al., 2014); molecular graphics: DIAMOND (Putz & Brandenburg, 2006); software used to prepare material for publication: publCIF (Westrip, 2010).[Zn(H2O)6][Zn(C2H5NO2)2(H2O)4](SO4)2 | Z = 1 |
Mr = 653.20 | F(000) = 336 |
Triclinic, P1 | Dx = 2.086 Mg m−3 |
a = 5.9601 (15) Å | Neutron radiation, λ = 0.48-7.0 Å |
b = 6.7670 (17) Å | Cell parameters from 550 reflections |
c = 13.112 (4) Å | µ = 5.02 + 0.0182 * λ mm−1 |
α = 84.955 (18)° | T = 10 K |
β = 83.25 (2)° | Tabular, colourless |
γ = 83.042 (19)° | 4 × 2.5 × 1 mm |
V = 519.8 (2) Å3 |
SXD diffractometer | 8296 reflections with I > 2σ(I) |
Radiation source: ISIS neutron spallation source | Rint = 0.089 |
time–of–flight LAUE diffraction scans | θmax = 87.4°, θmin = 8.2° |
Absorption correction: numerical The is wavelength dependent and is calculated as: µ = 5.0165 + 0.0182 * λ [cm-1] as determined by Gaussian integration in SXD2001 (Gutmann, 2005) | h = −15→15 |
k = −18→16 | |
8296 measured reflections | l = −28→29 |
8296 independent reflections |
Refinement on F2 | Hydrogen site location: difference Fourier map |
Least-squares matrix: full | All H-atom parameters refined |
R[F2 > 2σ(F2)] = 0.089 | w = 1/[σ2(Fo2) + (0.1376P)2 + 36.2519P] where P = (Fo2 + 2Fc2)/3 |
wR(F2) = 0.246 | (Δ/σ)max < 0.001 |
S = 1.09 | Δρmax = 3.20 e Å−3 |
8296 reflections | Δρmin = −3.47 e Å−3 |
291 parameters | Extinction correction: SHELXL, Fc*=kFc[1+0.001xFc2λ3/sin(2θ)]-1/4 |
12 restraints | Extinction coefficient: 0.0386 (18) |
Experimental. For peak integration a local UB matrix refined for each frame, using approximately 50 reflections from each of the 11 detectors. Hence _cell_measurement_reflns_used 550 For final cell dimensions a weighted average of all local cells was calculated Because of the nature of the experiment, it is not possible to give values of theta_min and theta_max for the cell determination. The same applies for the wavelength used for the experiment. The range of wavelengths used was 0.48–7.0 Angstroms, BUT the bulk of the diffraction information is obtained from wavelengths in the range 0.7–2.5 Angstroms. The data collection procedures on the SXD instrument used for the single-crystal neutron data collection are most recently summarized in the Appendix to the following paper Wilson, C.C. (1997). J. Mol. Struct. 405, 207–217 |
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. |
Refinement. The variable wavelength nature of the data collection procedure means that sensible values of _diffrn_reflns_theta_min & _diffrn_reflns_theta_max cannot be given instead the following limits are given _diffrn_reflns_sin(theta)/lambda_min 0.06 _diffrn_reflns_sin(theta)/lambda_max 1.38 _refine_diff_density_max/min is given in Fermi per angstrom cubed not electons per angstrom cubed. Another way to consider the _refine_diff_density_ is as a percentage of the scattering density of a given atom: _refine_diff_density_max = 5.7 % of hydrogen _refine_diff_density_min = -6.1 % of hydrogen 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 | ||
S1 | 0.0141 (6) | 0.9128 (6) | 0.1847 (4) | 0.0008 (6) | |
O1 | 0.1809 (4) | 1.0196 (3) | 0.1159 (2) | 0.0036 (4) | |
O2 | −0.0249 (4) | 0.7303 (3) | 0.1375 (2) | 0.0037 (4) | |
O3 | −0.2027 (4) | 1.0416 (3) | 0.2010 (2) | 0.0040 (4) | |
O4 | 0.1050 (4) | 0.8522 (4) | 0.2845 (2) | 0.0038 (3) | |
Zn1 | 0.5000 | 0.0000 | 0.5000 | 0.0017 (4) | |
O5 | 0.1954 (4) | 0.1618 (4) | 0.5392 (2) | 0.0049 (4) | |
H5A | 0.0913 (11) | 0.1389 (11) | 0.6009 (6) | 0.0198 (11) | |
H5B | 0.0998 (10) | 0.2109 (9) | 0.4826 (6) | 0.0170 (10) | |
O6 | 0.4360 (4) | 0.0464 (4) | 0.3456 (2) | 0.0043 (4) | |
H6A | 0.5654 (10) | 0.0305 (9) | 0.2922 (5) | 0.0162 (10) | |
H6B | 0.3082 (10) | −0.0116 (10) | 0.3229 (6) | 0.0179 (11) | |
O7 | 0.6512 (4) | 0.2793 (4) | 0.4768 (2) | 0.0037 (3) | |
O8 | 0.9812 (4) | 0.3195 (4) | 0.3809 (2) | 0.0060 (4) | |
N1 | 0.3991 (2) | 0.5025 (2) | 0.34432 (14) | 0.0044 (2) | |
H1N | 0.3634 (11) | 0.5559 (12) | 0.4165 (6) | 0.0218 (13) | |
H2N | 0.3159 (12) | 0.6073 (10) | 0.2963 (7) | 0.0212 (12) | |
H3N | 0.3294 (11) | 0.3719 (9) | 0.3435 (6) | 0.0199 (12) | |
C1 | 0.7711 (3) | 0.3465 (3) | 0.39746 (19) | 0.0029 (3) | |
C2 | 0.6484 (3) | 0.4781 (3) | 0.3163 (2) | 0.0041 (3) | |
H2A | 0.7111 (11) | 0.6233 (9) | 0.3086 (7) | 0.0220 (13) | |
H2B | 0.6871 (11) | 0.4134 (12) | 0.2420 (6) | 0.0222 (13) | |
Zn2 | 0.5000 | 0.5000 | 0.0000 | 0.0008 (3) | |
O9 | 0.2958 (4) | 0.3897 (3) | 0.1320 (2) | 0.0045 (4) | |
H9A | 0.2434 (11) | 0.2593 (8) | 0.1279 (6) | 0.0175 (11) | |
H9B | 0.1606 (10) | 0.4824 (9) | 0.1443 (6) | 0.0190 (11) | |
O10 | 0.7911 (4) | 0.3443 (4) | 0.0509 (2) | 0.0048 (4) | |
H10A | 0.7828 (12) | 0.2322 (9) | 0.1030 (6) | 0.0180 (10) | |
H10B | 0.8989 (11) | 0.2959 (10) | −0.0061 (6) | 0.0197 (11) | |
O11 | 0.5434 (4) | 0.7298 (4) | 0.0881 (2) | 0.0054 (4) | |
H11A | 0.6938 (9) | 0.7484 (9) | 0.1036 (6) | 0.0182 (11) | |
H11B | 0.4422 (10) | 0.8523 (8) | 0.0915 (7) | 0.0200 (12) |
U11 | U22 | U33 | U12 | U13 | U23 | |
S1 | 0.0006 (10) | 0.0009 (11) | 0.0010 (18) | 0.0001 (8) | −0.0003 (9) | 0.0000 (11) |
O1 | 0.0027 (6) | 0.0037 (7) | 0.0038 (10) | −0.0006 (5) | 0.0016 (5) | 0.0001 (7) |
O2 | 0.0029 (6) | 0.0028 (6) | 0.0058 (11) | −0.0007 (5) | −0.0007 (6) | −0.0012 (7) |
O3 | 0.0017 (6) | 0.0040 (7) | 0.0053 (11) | 0.0018 (5) | 0.0010 (6) | 0.0000 (7) |
O4 | 0.0039 (6) | 0.0054 (7) | 0.0018 (10) | 0.0001 (5) | −0.0015 (6) | 0.0011 (7) |
Zn1 | 0.0015 (4) | 0.0017 (4) | 0.0017 (5) | −0.0001 (3) | −0.0001 (3) | 0.0000 (3) |
O5 | 0.0036 (7) | 0.0071 (8) | 0.0032 (11) | 0.0014 (5) | −0.0002 (6) | 0.0011 (7) |
H5A | 0.015 (2) | 0.028 (3) | 0.014 (3) | −0.0027 (18) | 0.0046 (18) | 0.002 (2) |
H5B | 0.015 (2) | 0.019 (2) | 0.016 (3) | 0.0017 (15) | −0.0065 (17) | 0.004 (2) |
O6 | 0.0041 (7) | 0.0064 (7) | 0.0021 (11) | −0.0005 (5) | −0.0004 (6) | 0.0002 (7) |
H6A | 0.0142 (18) | 0.021 (2) | 0.013 (3) | −0.0020 (15) | 0.0034 (16) | −0.005 (2) |
H6B | 0.017 (2) | 0.023 (2) | 0.017 (3) | −0.0076 (17) | −0.0052 (18) | −0.005 (2) |
O7 | 0.0042 (6) | 0.0041 (7) | 0.0026 (10) | −0.0011 (5) | −0.0004 (6) | 0.0014 (7) |
O8 | 0.0028 (7) | 0.0091 (9) | 0.0050 (12) | 0.0008 (5) | 0.0001 (6) | 0.0022 (8) |
N1 | 0.0030 (4) | 0.0057 (5) | 0.0041 (7) | 0.0012 (3) | −0.0013 (4) | 0.0004 (5) |
H1N | 0.017 (2) | 0.033 (3) | 0.015 (3) | 0.002 (2) | 0.0004 (19) | −0.009 (3) |
H2N | 0.019 (2) | 0.020 (2) | 0.025 (4) | 0.0015 (18) | −0.011 (2) | 0.006 (2) |
H3N | 0.018 (2) | 0.015 (2) | 0.027 (4) | −0.0066 (16) | −0.001 (2) | 0.001 (2) |
C1 | 0.0020 (5) | 0.0034 (6) | 0.0032 (9) | 0.0000 (4) | −0.0011 (5) | 0.0007 (6) |
C2 | 0.0042 (6) | 0.0047 (6) | 0.0030 (9) | −0.0002 (4) | −0.0004 (5) | 0.0017 (6) |
H2A | 0.020 (2) | 0.013 (2) | 0.033 (4) | −0.0078 (17) | −0.005 (2) | 0.007 (2) |
H2B | 0.018 (2) | 0.035 (3) | 0.013 (3) | 0.007 (2) | −0.0031 (19) | −0.006 (3) |
Zn2 | 0.0008 (4) | 0.0008 (4) | 0.0009 (5) | −0.0001 (3) | −0.0001 (3) | 0.0001 (3) |
O9 | 0.0045 (7) | 0.0035 (7) | 0.0050 (11) | −0.0005 (5) | 0.0005 (6) | 0.0004 (7) |
H9A | 0.021 (2) | 0.0115 (17) | 0.021 (3) | −0.0064 (15) | −0.001 (2) | −0.001 (2) |
H9B | 0.0135 (19) | 0.016 (2) | 0.024 (4) | 0.0064 (14) | 0.0009 (18) | −0.001 (2) |
O10 | 0.0039 (7) | 0.0047 (7) | 0.0050 (11) | 0.0019 (5) | −0.0012 (6) | 0.0010 (7) |
H10A | 0.024 (3) | 0.015 (2) | 0.013 (3) | 0.0011 (17) | 0.0002 (19) | 0.0054 (19) |
H10B | 0.020 (2) | 0.020 (2) | 0.016 (3) | 0.0065 (17) | 0.0040 (19) | −0.002 (2) |
O11 | 0.0033 (6) | 0.0048 (7) | 0.0086 (12) | 0.0002 (5) | −0.0015 (6) | −0.0033 (8) |
H11A | 0.0091 (16) | 0.022 (2) | 0.025 (3) | −0.0030 (15) | −0.0057 (17) | −0.004 (2) |
H11B | 0.017 (2) | 0.0118 (18) | 0.031 (4) | 0.0059 (14) | −0.003 (2) | −0.006 (2) |
S1—O3 | 1.473 (4) | N1—H1N | 1.033 (7) |
S1—O1 | 1.474 (5) | N1—C2 | 1.481 (2) |
S1—O4 | 1.480 (6) | C1—C2 | 1.523 (4) |
S1—O2 | 1.484 (4) | C2—H2A | 1.085 (6) |
Zn1—O5 | 2.039 (2) | C2—H2B | 1.091 (7) |
Zn1—O5i | 2.039 (2) | Zn2—O10 | 2.067 (3) |
Zn1—O6 | 2.093 (3) | Zn2—O10ii | 2.067 (3) |
Zn1—O6i | 2.094 (3) | Zn2—O11ii | 2.075 (2) |
Zn1—O7i | 2.173 (2) | Zn2—O11 | 2.075 (2) |
Zn1—O7 | 2.173 (2) | Zn2—O9 | 2.129 (3) |
O5—H5A | 0.973 (7) | Zn2—O9ii | 2.129 (3) |
O5—H5B | 0.997 (7) | O9—H9B | 0.966 (6) |
O6—H6A | 0.981 (6) | O9—H9A | 0.979 (5) |
O6—H6B | 0.985 (6) | O10—H10A | 0.977 (8) |
O7—C1 | 1.272 (4) | O10—H10B | 0.979 (6) |
O8—C1 | 1.240 (3) | O11—H11B | 0.966 (6) |
N1—H3N | 1.022 (6) | O11—H11A | 0.966 (6) |
N1—H2N | 1.027 (8) | ||
O3—S1—O1 | 110.2 (3) | O8—C1—O7 | 126.0 (3) |
O3—S1—O4 | 110.1 (3) | O8—C1—C2 | 116.2 (2) |
O1—S1—O4 | 109.5 (3) | O7—C1—C2 | 117.7 (2) |
O3—S1—O2 | 109.3 (3) | H2A—C2—H2B | 107.9 (7) |
O1—S1—O2 | 109.3 (3) | H2A—C2—N1 | 109.5 (4) |
O4—S1—O2 | 108.4 (3) | H2B—C2—N1 | 109.5 (4) |
O5—Zn1—O5i | 180.0 | H2A—C2—C1 | 108.5 (5) |
O5—Zn1—O6 | 88.59 (11) | H2B—C2—C1 | 109.7 (4) |
O5i—Zn1—O6 | 91.41 (11) | O10—Zn2—O10ii | 180.0 |
O5—Zn1—O6i | 91.41 (11) | O10—Zn2—O11ii | 91.57 (10) |
O5i—Zn1—O6i | 88.59 (11) | O10ii—Zn2—O11ii | 88.43 (10) |
O6—Zn1—O6i | 180.0 | O10—Zn2—O11 | 88.43 (10) |
O5—Zn1—O7i | 92.01 (9) | O10ii—Zn2—O11 | 91.57 (10) |
O5i—Zn1—O7i | 87.99 (9) | O11ii—Zn2—O11 | 180.0 |
O6—Zn1—O7i | 93.38 (10) | O10—Zn2—O9 | 91.52 (11) |
O6i—Zn1—O7i | 86.62 (10) | O10ii—Zn2—O9 | 88.48 (11) |
O5—Zn1—O7 | 87.99 (9) | O11ii—Zn2—O9 | 94.16 (10) |
O5i—Zn1—O7 | 92.01 (9) | O11—Zn2—O9 | 85.84 (10) |
O6—Zn1—O7 | 86.62 (10) | O10—Zn2—O9ii | 88.48 (11) |
O6i—Zn1—O7 | 93.38 (10) | O10ii—Zn2—O9ii | 91.52 (11) |
O7i—Zn1—O7 | 180.0 | O11ii—Zn2—O9ii | 85.84 (10) |
H5A—O5—H5B | 106.7 (6) | O11—Zn2—O9ii | 94.16 (10) |
H6A—O6—H6B | 108.1 (6) | O9—Zn2—O9ii | 180.00 (12) |
C1—O7—Zn1 | 128.26 (18) | H9B—O9—H9A | 106.2 (6) |
H3N—N1—H2N | 107.6 (6) | H10A—O10—H10B | 106.1 (6) |
H3N—N1—H1N | 109.8 (7) | H11B—O11—H11A | 111.4 (6) |
H2N—N1—H1N | 105.0 (6) |
Symmetry codes: (i) −x+1, −y, −z+1; (ii) −x+1, −y+1, −z. |
D—H···A | D—H | H···A | D···A | D—H···A |
O5—H5A···O4iii | 0.973 (7) | 1.793 (7) | 2.755 (4) | 169.0 (7) |
O5—H5B···O8iv | 0.997 (7) | 1.656 (8) | 2.642 (4) | 168.9 (6) |
O6—H6A···O3v | 0.981 (6) | 1.722 (6) | 2.696 (3) | 170.8 (5) |
O6—H6B···O4vi | 0.985 (6) | 1.751 (5) | 2.729 (3) | 171.8 (7) |
O9—H9A···O1vi | 0.979 (5) | 1.732 (5) | 2.707 (3) | 173.8 (6) |
O9—H9B···O2 | 0.966 (6) | 1.895 (6) | 2.811 (3) | 157.2 (6) |
O10—H10A···O3v | 0.977 (8) | 1.740 (8) | 2.713 (4) | 173.0 (7) |
O10—H10B···O2ii | 0.979 (6) | 1.811 (7) | 2.745 (4) | 158.5 (7) |
O11—H11A···O2vii | 0.966 (6) | 1.772 (6) | 2.726 (3) | 168.6 (6) |
O11—H11B···O1 | 0.966 (6) | 1.824 (6) | 2.750 (3) | 159.5 (7) |
C2—H2A···O2vii | 1.085 (6) | 2.682 (9) | 3.351 (4) | 119.4 (6) |
C2—H2A···O5viii | 1.085 (6) | 2.716 (8) | 3.489 (3) | 127.9 (6) |
C2—H2B···O10 | 1.091 (7) | 2.579 (8) | 3.649 (4) | 166.7 (7) |
N1—H1N···O7viii | 1.033 (7) | 1.853 (7) | 2.848 (3) | 160.8 (7) |
N1—H2N···O4 | 1.027 (8) | 1.961 (7) | 2.877 (3) | 147.0 (7) |
N1—H3N···O6 | 1.022 (6) | 2.216 (7) | 3.066 (3) | 139.5 (5) |
Symmetry codes: (ii) −x+1, −y+1, −z; (iii) −x, −y+1, −z+1; (iv) x−1, y, z; (v) x+1, y−1, z; (vi) x, y−1, z; (vii) x+1, y, z; (viii) −x+1, −y+1, −z+1. |
The distortion index and quadratic elongation are dimensionless, whereas the bond-angle variance is in units of degrees squared. |
This work | Balamurugan et al. (2011) | Tepavitcharova et al. (2012) | Oguey et al. (2013c) | |
Single-crystal neutron | Single-crystal X-ray | Single-crystal X-ray | Single-crystal X-ray | |
T = 10 K | T = 293 K | T = 150 K | T = 153 K | |
S—O1* | 1.474 (5) | 1.472 (2) | 1.472 (1) | 1.473 (2) |
S—O2 | 1.484 (4) | 1.478 (2) | 1.482 (1) | 1.485 (2) |
S—O3* | 1.473 (4) | 1.472 (2) | 1.477 (1) | 1.481 (2) |
S—O4 | 1.480 (5) | 1.481 (2) | 1.484 (1) | 1.479 (2) |
Mean S—O | 1.478 | 1.476 | 1.479 | 1.479 |
SO4 volume | 1.656 | 1.649 | 1.659 | 1.661 |
Distortion index | 0.0028 | 0.0025 | 0.0027 | 0.0022 |
Quadratic elongation | 1.000 | 1.000 | 1.000 | 1.000 |
Bond-angle variance | 0.410 | 0.268 | 0.320 | 0.420 |
Zn1—O5 | 2.039 (2) | 2.024 (3) | 2.032 (1) | 2.035 (2) |
Zn1—O6 | 2.093 (2) | 2.101 (3) | 2.098 (1) | 2.098 (2) |
Zn1—O7† | 2.173 (2) | 2.181 (3) | 2.177 (1) | 2.176 (2) |
Mean Zn1—O | 2.102 | 2.102 | 2.102 | 2.103 |
ZnO6 volume | 12.338 | 12.339 | 12.339 | 12.336 |
Distortion index | 0.0227 | 0.0251 | 0.0238 | 0.0232 |
Quadratic elongation | 1.003 | 1.003 | 1.003 | 1.003 |
Bond-angle variance | 6.308 | 4.815 | 5.975 | 6.292 |
Zn2—O9 | 2.129 (3) | 2.141 (3) | 2.133 (1) | 2.135 (2) |
Zn2—O10 | 2.067 (3) | 2.071 (3) | 2.070 (1) | 2.072 (2) |
Zn2—O11 | 2.075 (2) | 2.063 (3) | 2.065 (2) | 2.065 (2) |
Mean Zn2—O | 2.090 | 2.092 | 2.089 | 2.091 |
ZnO6 volume | 12.127 | 12.176 | 12.123 | 12.145 |
Distortion index | 0.0124 | 0.0156 | 0.0139 | 0.0142 |
Quadratic elongation | 1.003 | 1.002 | 1.002 | 1.002 |
Bond-angle variance | 7.982 | 5.942 | 6.617 | 6.541 |
C1—O7 | 1.272 (4) | 1.272 (5) | 1.274 (2) | 1.278 (3) |
C1—O8 | 1.240 (3) | 1.228 (5) | 1.236 (2) | 1.234 (3) |
C1—C2 | 1.523 (4) | 1.516 (5) | 1.525 (3) | 1.522 (3) |
C2—N1 | 1.481 (2) | 1.478 (5) | 1.480 (2) | 1.480 (3) |
*Denotes sulfate oxygens accepting two hydrogen bonds instead of three. †Denotes carboxylate oxygen ligand instead of water oxygen. |
Element symbols indicate the cation in each compound. `X-ray' denotes single-crystal X-ray diffraction; `NPD' denotes a neutron powder diffraction experiment on a deuterated analogue carried out at 10 K; `neutron' indicates single-crystal neutron diffraction on a protonated analogue carried out at 10 K. Note that the atom symbols employed in our work are the same as those used by Elayaraja et al. (2007) and by Howard et al. (2016). Although other authors have used different atom labels – and indeed use them inconsistently in their own reports – we list equivalent contacts in this table. |
Mg, X-ray(a) | Mg, NPD(b) | Co, X-ray(c) | Mg, X-ray(c) | Zn, X-ray(c) | Zn, X-ray(d) | Zn, X-ray(e) | Zn, neutron(f) | |
N—H1N | 0.87 (4) | 1.008 (4) | 0.847 (1) | 0.849 (1) | 0.881 (2) | 0.85 (2) | 0.910 (2) | 1.033 (7) |
N—H2N | 0.87 (4) | 0.982 (4) | 0.907 (1) | 0.898 (1) | 0.904 (1) | 0.83 (3) | 0.911 (2) | 1.028 (8) |
N—H3N | 0.87 (5) | 0.991 (5) | 0.904 (1) | 0.902 (1) | 0.946 (1) | absent | 0.910 (2) | 1.022 (6) |
Average N—H | 0.87 | 0.995 | 0.877 | 0.874 | 0.892 | 0.84 | 0.911 | 1.030 |
C—H2A | 0.970 (4) | 1.077 (4) | 0.961 (1) | 0.960 (1) | 0.967 (2) | 0.970 (3) | 0.990 (2) | 1.085 (6) |
C—H2B | 0.970 (3) | 1.083 (4) | 0.901 (1) | 1.014 (1) | 1.050 (2) | 0.970 (3) | 0.990 (2) | 1.091 (7) |
Average C—H | 0.970 | 1.080 | 0.931 | 0.987 | 1.009 | 0.970 | 0.990 | 1.088 |
O5—H5A | 0.84 (3) | 0.975 (5) | 0.880 (1) | 0.789 (1) | 0.879 (2) | 0.85 (2) | 0.83 (3) | 0.973 (7) |
O5—H5B | 0.85 (3) | 0.946 (5) | 0.914 (1) | 0.930 (1) | 0.838 (1) | 0.85 (3) | 0.85 (3) | 0.997 (7) |
O6—H6A | 0.84 (2) | 0.987 (5) | 0.964 (1) | 0.875 (1) | 0.864 (1) | 0.83 (3) | 0.86 (3) | 0.981 (6) |
O6—H6B | 0.83 (3) | 0.988 (5) | 0.906 (1) | 0.897 (1) | 0.886 (1) | 0.84 (3) | 0.85 (2) | 0.985 (6) |
O9—H9A | 0.83 (2) | 0.977 (5) | 0.864 (1) | 0.871 (1) | 0.881 (2) | 0.87 (3) | 0.86 (2) | 0.979 (5) |
O9—H9b | 0.84 (2) | 0.984 (4) | 0.884 (1) | 0.901 (1) | 0.964 (1) | 0.87 (2) | 0.87 (3) | 0.966 (6) |
O10—H10A | 0.84 (4) | 0.954 (5) | 0.972 (1) | 0.911 (1) | 0.887 (1) | 0.82 (2) | 0.87 (2) | 0.977 (8) |
O10—H10B | 0.84 (3) | 0.972 (5) | 0.855 (1) | 0.821 (1) | 0.913 (1) | 0.84 (2) | 0.85 (2) | 0.978 (6) |
O11—H11A | 0.84 (3) | 1.002 (5) | 0.822 (1) | 0.884 (1) | 0.808 (1) | 0.83 (3) | 0.86 (2) | 0.966 (6) |
O11—H11B | 0.83 (3) | 0.965 (5) | 0.906 (1) | 0.859 (1) | 0.900 (1) | 0.84 (2) | 0.84 (2) | 0.966 (6) |
Average O—H | 0.84 | 0.975 | 0.897 | 0.874 | 0.882 | 0.85 | 0.85 | 0.977 |
(a) Elayaraja et al. (2007); (b) Howard et al. (2016); (c) Tepavitcharova et al. (2012); (d) Balamurugan et al. (2011); (e) Oguey et al. (2013c); (f) this work. |
Meaning of symbols: ν = stretch; δ = deformation; ρ = rock; ω = wag; Γ = twist; (A) = asymmetric; (S) = symmetric. |
α-Glycinea | Glyc·MgSO4·5H2Oa | Glyc·ZnSO4·5H2O | |
Vibrational mode | 180 s, 18 mW | 1400 s, 18 mW | 540 s, 18 mW |
δ M2+—O (?) | – | 208 | 203 |
– | 236 | 220 | |
δ CCN+ | 356 | 361 | 382 |
ρ COO- | |||
δ(S) SO42- | – | 453 | 451 |
ρ COO- | 497 | 522 | 527 |
ω COO- | 601 | 597 | 582 |
599 | |||
δ(A) SO42- | 623 | 626 | |
645 | 644 | ||
δ COO- | 696 | – | – |
unknown | – | 794 | – |
ν C—C+ | 893 | 890 | 890 |
ν C—N | 905 | 906 | |
ν C—O | |||
ρ CH2 | 922 | – | – |
ν(S) SO42- | – | 983.8 | 983.2 |
ν C—N | 1036 | 1020 | 1021 |
ν(A) SO42- | – | 1077 | 1078 |
1100 | 1101 | ||
ρ NH3+ | 1108 | 1139 | 1141 |
1140 | |||
ω CH2 | 1325 | 1305 | 1306 |
Γ CH2 | 1328 | 1327 | |
ν(S) COO- | 1410 | 1395 | 1391 |
δ(S) CH2 | 1441 | 1434 | 1433 |
1457 | |||
δ(A) NH3+ | 1502 | ||
δ(S) NH3+ | 1516 | 1488 | 1488 |
1569 | |||
ν C—C+ | 1634 | 1597 | 1590 |
ω CH2 | |||
ν(A) COO- | 1670 | 1631 | 1614 |
ν(S) CH2 | 2972 | 2997 | 2996 |
ν(A) CH2 | 3009 | 3038 | 3037 |
ν(S) NH3+ | 3143 | – | – |
ν(S) H2O | – | 3248 | 3204 |
3233 | |||
ν(A) H2O | – | 3384 | 3331 |
3405 |
aHoward et al. (2016). |
Acknowledgements
The authors thank the STFC ISIS facility for beam-time access. IGW acknowledges a grant from STFC, No. ST/K000934/1; CMH is similarly supported by a postgraduate studentship from STFC.
References
Alymkulova, K. & Salyeva, N. V. (1987). Koordinatsionnye Soedinenija Metallov s Bioligandami, Institut Neorganicheskoj i Fizicheskoj Khimii pp. 77–79. Kyrgyz SSR Ilimder Akademijasy. (In Russian). Google Scholar
Balakrishnan, T. & Ramamurthy, K. (2007). Spectrochim. Acta A, 68, 360–363. Web of Science CrossRef CAS Google Scholar
Balamurugan, M. S., Subramanian, P. & Rao, P. S. (2011). Private communication ( Deposition number CCDC 8606684). CCDC, Cambridge, England. DOI: 10.5517/ccw2f2f. Google Scholar
Coppens, P. (1997). X-ray Charge Density and Chemical Bonding. Oxford University Press, Oxford, England. Google Scholar
Elayaraja, K., Parthiban, S. P., Ramalingom, S., Bocelli, G. & Kalkura, S. N. (2007). Acta Cryst. E63, m2901–m2902. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
El-Fadl, A. A. & Abdulwahab, A. M. (2010). Physica B, 405, 3421–3426. Google Scholar
Fleck, M. & Bohatý, L. (2004). Acta Cryst. C60, m291–m295. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
Fleck, M. & Bohatý, L. (2005). Acta Cryst. C61, m412–m416. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
Fleck, M. & Bohatý, L. (2006). Acta Cryst. C62, m22–m26. Web of Science CSD CrossRef CAS IUCr Journals Google Scholar
Fortes, A. D., Alfè, D., Hernández, E. R. & Gutmann, M. J. (2015). Acta Cryst. B71, 313–327. Web of Science CSD CrossRef IUCr Journals Google Scholar
Fortes, A. D. & Gutmann, M. J. (2014). Acta Cryst. E70, 134–137. CSD CrossRef IUCr Journals Google Scholar
Fortes, A. D., Wood, I. G. & Gutmann, M. J. (2013). Acta Cryst. C69, 324–329. Web of Science CrossRef CAS IUCr Journals Google Scholar
Friant-Michel, P. & Ruiz-López, M. F. (2010). ChemPhysChem, 11, 3499–3504. Web of Science CAS PubMed Google Scholar
Groom, C. R., Bruno, I. J., Lightfoot, M. P. & Ward, S. C. (2016). Acta Cryst. B72, 171–179. Web of Science CSD CrossRef IUCr Journals Google Scholar
Gruene, T., Hahn, H. W., Luebben, A. V., Meilleur, F. & Sheldrick, G. M. (2014). J. Appl. Cryst. 47, 462–466. Web of Science CrossRef CAS IUCr Journals Google Scholar
Gutmann, M. J. (2005). SXD2001. ISIS Facility, Rutherford Appleton Laboratory, Oxfordshire, England. Google Scholar
Hamad, S. & Catlow, C. R. A. (2011). CrystEngComm, 13, 4391–4399. Web of Science CrossRef CAS Google Scholar
Howard, C., Wood, I. G., Knight, K. S. & Fortes, A. D. (2016). Acta Cryst. C72, 203–216. Web of Science CSD CrossRef IUCr Journals Google Scholar
Huang, J., Stringfellow, T. C. & Yu, L. (2008). J. Am. Chem. Soc. 130, 13973–13980. Web of Science CrossRef PubMed CAS Google Scholar
Jönsson, P.-G. & Kvick, Å. (1972). Acta Cryst. B28, 1827–1833. CSD CrossRef IUCr Journals Web of Science Google Scholar
Kaminsky, W. (2005). J. Appl. Cryst. 38, 566–567. Web of Science CrossRef CAS IUCr Journals Google Scholar
Kaminsky, W. (2007). J. Appl. Cryst. 40, 382–385. Web of Science CrossRef CAS IUCr Journals Google Scholar
Kimura, J. & Kitadai, N. (2015). Astrobiology, 15, 430–441. Web of Science CrossRef CAS PubMed Google Scholar
Kitadai, N. (2016). Orig. Life Evol. Biosph. 10, 1007s11084-016-9510-5. Google Scholar
Kitadai, N., Yokoyama, T. & Nakashima, S. (2011). Geochim. Cosmochim. Acta, 75, 6285–6299. Web of Science CrossRef CAS Google Scholar
Lindqvist, I. & Rosenstein, R. (1960). Acta Chem. Scand. 14, 1228–1229. CrossRef CAS Web of Science Google Scholar
Moldobaev, S. & Nogoev, K. (1970). Materialy Nauchnoi Konferentsii Posvyashchennoy 100-letiyu Periodicheskogo Zakona D. I. Mendeleeva, C-29. (In Russian). Google Scholar
Moldobaev, S., Nogoev, K. & Ismailov, T. (1970). Materialy Nauchnoi Konferentsii Posvyashchennoy 100-letiyu Periodicheskogo Zakona D. I. Mendeleeva, C-120. (In Russian). Google Scholar
Oguey, S., Jacquier, Y., Neels, A. & Stoeckli-Evans, H. (2013a). Private communication (deposit number CCDC 936393). CCDC, Cambridge, England. DOI: 10.5517/cc10fd72 Google Scholar
Oguey, S., Jacquier, Y., Neels, A. & Stoeckli-Evans, H. (2013b). Private communication (deposit number CCDC 936394. CCDC, Union Road, Cambridge, England. DOI: 10.5517/cc10fd83 Google Scholar
Oguey, S., Jacquier, Y., Neels, A. & Stoeckli-Evans, H. (2013c). Private communication (deposit number CCDC 936400). CCDC, Cambridge, England. DOI: 10.5517/cc10fdg9 Google Scholar
Oguey, S., Jacquier, Y., Sereda, O., Neels, A. & Stoeckli-Evans, H. (2014). Private communication (deposit number CCDC 989590). CCDC, Cambridge, England. DOI: 10.5517/cc126r89 Google Scholar
Power, L. F., Turner, K. E. & Moore, F. H. (1976). Acta Cryst. B32, 11–16. CSD CrossRef CAS IUCr Journals Web of Science Google Scholar
Putz, H. & Brandenburg, K. (2006). DIAMOND. Crystal Impact GbR, Bonn, Germany. Google Scholar
Robinson, K., Gibbs, G. V. & Ribbe, P. H. (1971). Science, 172, 567–570. CrossRef PubMed CAS Web of Science Google Scholar
Rosado, M. T., Duarte, M. L. T. S. & Fausto, R. (1998). Vib. Spectrosc. 16, 35–54. Web of Science CrossRef CAS Google Scholar
Sheldrick, G. M. (2015a). Acta Cryst. A71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Sheldrick, G. M. (2015b). Acta Cryst. C71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Steiner, T. & Desiraju, G. R. (1998). Chem. Commun. pp. 891–892. Web of Science CrossRef Google Scholar
Stenbäck, H. (1976). J. Raman Spectrosc. 5, 49–55. Google Scholar
Tepavitcharova, S., Rabadjieva, D., Havlíček, D., Němec, I., Vojtíšek, P., Plocek, J. & Koleva, Z. (2012). J. Mol. Struct. 1018, 113–121. Web of Science CSD CrossRef CAS Google Scholar
Thilagavathi, R., Selvarajan, P. & Kumari, V. V. (2012). Int. J. Adv. Sci. Tech. Res, 2, 164–183. Google Scholar
Westrip, S. P. (2010). J. Appl. Cryst. 43, 920–925. Web of Science CrossRef CAS IUCr Journals Google Scholar
Yang, X., Lu, J., Wang, X. & Ching, C. B. (2008). J. Raman Spectrosc. 39, 1433–1439. Web of Science CrossRef CAS Google Scholar
Yani, Y., Chow, P. S. & Tan, R. B. H. (2012). Cryst. Growth Des. 12, 4771–4778. Web of Science CrossRef CAS Google Scholar
This is an open-access article distributed under the terms of the Creative Commons Attribution (CC-BY) Licence, which permits unrestricted use, distribution, and reproduction in any medium, provided the original authors and source are cited.