research papers
Ammonium bis(salicylaldehyde thiosemicarbazonato)ferrate(III), a supramolecular material containing low-spin FeIII
aSchool of Engineering and Applied Science, Chemical Engineering and Applied Chemistry, Aston University, Aston Triangle, Birmingham B4 7ET, West Midlands, UK, bAston Institute of Materials Research, Aston University, Birmingham B4 7ET, West Midlands, UK, cX-ray Center, Vienna University of Technology, Getreidemarkt 9, 1060 Vienna, Austria, and dInstitute of Applied Synthetic Chemistry, Vienna University of Technology, Getreidemarkt 9/163-01-3, 1060 Vienna, Austria
*Correspondence e-mail: p.vankoningsbruggen@aston.ac.uk
The synthesis and κ3O,N1,S]iron(III), NH4[Fe(C8H7N3OS)2], is reported. The consists of an octahedral [FeIII(thsa)2]− fragment, where thsa2− is salicylaldehyde thiosemicarbazonate(2−), and an NH4+ cation. Each thsa2− ligand binds via the thiolate S, the imine N and the phenolate O donor atoms, resulting in an FeIIIS2N2O2 chromophore. The ligands are orientated in two perpendicular planes, with the O and S atoms in cis and the N atoms in trans positions. The FeIII ion is in the low-spin state at 100 K. The belongs to a category I order–disorder (OD) family. It is a polytype of a maximum degree of order (MDO). Fragments of the second MDO polytype lead to systematic by pseudomerohedry.
(100 K) of the title compound, ammonium bis[salicylaldehyde thiosemicarbazonato(2−)-Keywords: ammonium; iron(III); crystal structure; low spin; order-disorder; maximum degree of disorder; MDO.
CCDC reference: 2003812
1. Introduction
The study of the coordination chemistry of thiosemicarbazones is an attractive research area. Thiosemicarbazones display a wide range of pharmacological uses based, for example, on their antineoplastic, antibacterial, antiviral and antifungal activities (Beraldo & Gambino, 2004; Yemeli Tido et al., 2010). This pharmacological action is often related to coordination of the thiosemicarbazone to metal ions (Farrell, 2002). On the other hand, the magnetic properties of iron(III) compounds of thiocarbazone derivatives have attracted attention, particularly as switching behaviour was displayed for iron(III) bound to particular salicylaldehyde thiosemicarbazone derivatives (van Koningsbruggen et al., 2004; Phonsri et al., 2017; Powell et al., 2014, 2015; Yemeli Tido, 2010; Zelentsov et al., 1973, Ryabova et al., 1978, 1981a,b, 1982; Floquet et al., 2003, 2006, 2009; Li et al., 2013).
This type of magnetic interconversion between the low-spin (S = ) and high-spin (S = ) state in FeIII (3d5) systems has now been found to be triggered by a change in temperature or pressure, or by light irradiation (Hayami et al., 2000, 2009; van Koningsbruggen et al., 2004) and may be used in a functional way in research and technology (Létard et al., 2004; Gütlich et al., 2004; Gütlich & Goodwin 2004; van Koningsbruggen et al., 2004; Nihei et al., 2007; Halcrow, 2013; Harding et al., 2016).
In recent years, particular interest has focused on FeIII complexes of substituted derivatives of R-salicylaldehyde 4R′-thiosemicarbazone (Powell et al., 2014, 2015; Yemeli Tido, 2010; Floquet et al., 2003, 2006, 2009; Li et al., 2013) for generating FeIII spin crossover. In solution, free R-salicylaldehyde 4R′-thiosemicarbazone (H2L) exists in two tautomeric forms, i.e. the thione and thiol forms, as illustrated in Scheme 1. The chemistry of the FeIII compounds is rather complicated as it is possible for the tridentate R-salicylaldehyde 4R′-thiosemicarbazone ligand (H2L) to exist in tautomeric forms; moreover, the ligand may also be present in its neutral, anionic or dianionic form. However, the formation of a particular type of FeIII complex unit, i.e. neutral, monocationic or monoanionic, can be achieved by tuning the degree of deprotonation of the ligand through pH variation of the reaction solution during the synthesis (Powell et al., 2014, 2015; Powell, 2016; Yemeli Tido, 2010; Floquet et al., 2009). We have been particularly skilled in preparing anionic FeIII complexes of the general formula (cation+)[Fe(L2−)2]·x(solvent), for which it became evident that the electronic state of the FeIII ion is dependent on the nature of the counter-ion, the nature and degree of solvation and the nature of the R,R′-substituted ligands (Powell et al., 2014, 2015; Powell, 2016; Yemeli Tido, 2010).
We report here a novel FeIII compound, ammonium bis[salicylaldehyde thiosemicarbazonato(2−)-κ3O,N1,S]iron(III), (I) (see Scheme 2), containing two dianionic tridentate ligands, i.e. salicylaldehyde thiosemicarbazonate(2−), abbreviated as thsa2−, whose structure was determined at 100 K. Ryabova et al. (1981a) reported the crystallographic data of the related compound Cs[Fe(thsa)2] at 103 and 298 K, which contains FeIII in the high-spin electronic state (S = ). The main difference between NH4[Fe(thsa)2] and Cs[Fe(thsa)2] is the associated outer-sphere cation. This article describes that the variation in the cation leads to a modification of the structure of the FeIII compound, also changing the crystal packing, and being responsible for the FeIII in the present NH4[Fe(thsa)2] compound exhibiting the low-spin electronic state (S = ).
Compound (I) systematically crystallizes as twins. The will be interpreted in the light of order–disorder (OD) theory (Dornberger-Schiff & Grell-Niemann, 1961). The OD theory was created in the 1950s to explain the common occurrence of and stacking faults. It has since been developed into a comprehensive theory of local/partial symmetry. According to OD theory, if a structure is composed of layers and the layers are related by that is not valid for the whole structure, then the stacking becomes ambiguous. This means that the layers can be arranged in different ways, which are nevertheless all locally equivalent. Owing to the short range of interatomic interactions, these different stacking arrangements are also energetically equivalent. Consequently, OD structures often feature stacking faults. In OD twins, such as the title compound, the stacking faults lead to domains with different spacial orientations and are sporadic, i.e. the resulting domains are macroscopic and do not diffract coherently.
2. Experimental
2.1. Spectroscopic measurements
Room-temperature IR spectra within the range 4000–400 cm−1 were recorded on a PerkinElmer FT–IR spectrometer Spectrum RXI using KBr pellets. Variable-temperature FT–IR spectra were measured with the attenuated total reflectance (ATR) technique using a PerkinElmer spectrum 400 with a Harrick diamond ATR equipped with a thermostatable temperature-control device. 1H and 13C{1H} NMR spectra were recorded on a Bruker 200 spectrometer with a broadband probe head. All NMR chemical shifts are reported in ppm; 1H and 13C shifts are established on the basis of the residual solvent resonance.
2.2. Synthesis and crystallization
The synthesis of H2thsa was carried out according to the general procedure described by Yemeli Tido (2010). Salicylaldehyde (49 mmol, 5.98 g) was dissolved in ethanol (80 ml) with constant stirring, and was added to a solution of thiosemicarbazide (49 mmol, 3.68 g) in ethanol (40 ml). The corresponding mixture was refluxed for 120 min. The resulting solution was cooled to room temperature and the solid isolated by filtration, washed with ether and dried in a vacuum for 2 d (yield: 7.75 g, 39.7 mmol, 81.0%; m.p. 491 K). H2thsa is soluble in methanol, acetone and dimethyl sulfoxide (DMSO). 1H NMR (200 MHz, DMSO-d6): δ (ppm) 11.39 (s, 1H, NH), 9.84 (s, 1H, OH), 8.40 (s, 1H, CH), 8.10 (s, 1H, o-ArCH), 7.87 (d, J = 8.8 Hz, 2H, NH2), 7.19 (t, J = 7.7 Hz, 1H, p-ArCH), 6.92–6.71 (m, 2H, m-ArCH). 13C NMR (50 MHz, DMSO-d6): δ (ppm) 177.76 (C=S), 156.52 (C—OH), 140.16 (C=N), 131.31 (ArCH), 126.99 (ArCH), 120.33 (ArCH), 119.48 (ArCH), 116.22 (ArCH). IR (cm−1, KBr): 3445 (νOH), 3175 (νNH), 3319 (νNH2), 1616 (νC=N), 1540–1603 (νC=C), 1266 (νC—N), 1111 (νC=S).
For the synthesis of NH4[Fe(thsa)2], (I), Fe(p-CH3C6H4SO3)3·6H2O (1.0 mmol, 0.68 g) was dissolved in methanol (5 ml). H2thsa (1.0 mmol, 0.20 g) was dissolved in methanol (25 ml) with the addition of NH4OH (20 ml, 35 wt% in water). To this mixture, the methanolic solution of the FeIII salt was added dropwise with constant stirring. The resulting dark-green solution was stirred and heated to 353 K for approximately 10 min. The solution was then allowed to stand at room temperature until crystals had formed. The dark-green microcrystals were isolated by filtration and dried (yield: 0.10 g, 0.22 mmol, 21.7%). Elemental analysis found/calculated (%) for C16H18FeN7O2S2: C, 41.47/41.47, H 3.90/3.94, N 20.99/21.30, O 8.05/6.95, S 13.87/13.93. IR (cm−1, KBr): 3472, 3240 (νNH), 3016 (νNH2), 1595 (νC=N), 1546–1509 (νC=C ring), 1278 (νC—O), 1203 (νN—N), 1027 (νC—N), 756 (νC—S).
2.3. Refinement
Crystal data, data collection and structure . The crystal was modelled as twinned by reflection at (100). The positions of the H atoms on the amine N atoms were located in difference Fourier maps and were refined with restrained N—H distances of 0.87 (2) Å. The NH4+ cation is disordered around a pseudo-twofold axis. The ammonium N atom was refined as disordered about two positions (N7 and N7′). The sum of the occupancy parameters was constrained to 1. The atomic displacement parameters (ADPs) were constrained to the same value, resulting in a significant decrease of the estimated on the occupancy parameters. Even though residual electron density in the difference Fourier maps could be attributed to the H atoms of the disordered ammonium positions, a reliable was not possible. The ammonium H atoms were therefore ultimately omitted from the Other H atoms were included in the in calculated positions and allowed to ride on their parent atoms.
details are summarized in Table 13. Results and discussion
3.1. Crystal structure
The structure of NH4[Fe(thsa)2], (I) (Fig. 1), was determined at 100 K and was found to crystallize in the monoclinic P21/n. The consists of one formula unit, i.e. NH4[Fe(thsa)2], with no atom on a special position. The FeIII cation is coordinated by two dianionic O,N,S-tridentate chelating thsa2− ligands, displaying a distorted octahedral FeIIIO2N2S2 geometry. Selected geometric parameters are listed in Table 2. The twofold deprotonated ligands are coordinated to the FeIII atom via the phenolate O, thiolate S and imine N atoms. These donor–FeIII bonds are located in two perpendicular planes, with the O and S atoms in cis positions, whereby the S1—Fe—S2 and O1—Fe—O2 angles are 92.07 (3) and 88.53 (12)°, respectively. In addition, the N atoms are situated in trans positions, which is evidenced by the N1—Fe—N4 bond angle of 176.71 (11)°. The FeO2N2S2 coordination core is distorted; the Fe–donor atom distances fall within the range expected for FeIII in the low-spin state (van Koningsbruggen et al., 2004).
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The incorporation of a monovalent NH4+ cation could be corroborated by variable-temperature FT–IR spectroscopy, which revealed the sharpening of the N—H stretching vibrational mode of the NH4+ cation at 3240 cm−1 upon cooling from ambient temperature to 173 K, which is in line with the freezing of the rotation of the NH4+ cation in the cavity.
The presence of the trivalent iron cation is supported by the coordination of two doubly deprotonated ligands to the FeIII ion. In addition, the presence of both dianionic ligands is confirmed by the C—S, C—N and N—N bond lengths (Table 2) obtained for NH4[Fe(thsa)2], which show characteristics of a bond order between single and double bonds. Ryabova et al. (1981a) reported the structure of the related high-spin compound Cs[Fe(thsa)2] at 103 and 298 K, which crystallizes in the Pna21 with an consisting of a Cs+ cation and an [Fe(thsa)2]− anionic unit. The C—S, C—N and N—N bond lengths [at 103 K: C—S = 1.749 (9) and 1.761 (9) Å; C—N = 1.314 (10) and 1.303 (11) Å; N—N = 1.371 (11) and 1.380 (11) Å; at 298 K: C—S = 1.743 (14) and 1.775 (17) Å; C—N = 1.281 (19) and 1.281 (19) Å; N—N = 1.393 (18) and 1.412 (18) Å] reported by Ryabova et al. (1981a) for Cs[Fe(thsa)2], correspond to the bond lengths for NH4[Fe(thsa)2], (I), at 100 K.
The hydrogen-bonding interactions of NH4[Fe(thsa)2] are listed in Table 3 and are displayed in Fig. 2. The terminal N atoms of the tridentate ligands (N3 and N6), form N6—HN62⋯O2i and N3—HN32⋯O1ii contacts with the phenolate donor atoms O1 and O2, respectively. In this manner, successive FeIII entities are linked in the c direction. The NH4+ cations are distributed in between the layers of the FeIII entities, with alternate separations of the N atoms of the NH4+ cation of 3.915 (7) [at (x + 1, y, z), denoted iii] and 4.547 (7) Å [at (x + , −y + , z + ), denoted iv] in the a direction. The FeIII⋯FeIII separations in the present compound are 8.4393 (8) Å for FeIII⋯FeIIIiii and 9.7134 (13) Å for FeIII⋯FeIIIv [symmetry code: (v) −x, −y + 1, −z + 1]. The FeIII units in NH4[Fe(thsa)2] are linked by hydrogen-bonding interactions between the corresponding phenolate O and amino N atoms of the FeIII units.
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The embedding of the NH4+ cation is, therefore, essentially different from that of the Cs+ cation in Cs[Fe(thsa)2] at 103 and 298 K, where the nearest-neighbour coordination sphere of the Cs+ cation is constituted by O, N and C atoms, which form a seven-pointed polyhedron with Cs–(ligand donor atom) separations between 3.06 and 3.82 Å (Ryabova et al., 1981a). This feature shows some similarity with the Cs+ cation in Cs[Fe(5-Br-thsa)2] (Powell et al., 2015) that is at the centre of an irregular seven-donor-atom polyhedron, the donor atoms of which originate from symmetry-related equivalents of both symmetry-independent 5-bromosalicylaldehyde thiosemicarbazonate(2−) (5-Br-thsa) ligands. Several donor atoms coordinated to the FeIII atom of Cs[Fe(5-Br-thsa)2] form interactions with the Cs+ cation in the second coordination sphere; this is likely to modulate the electron density of the Fe–(donor atom) bonds and hence influence the electronic state of the FeIII cation. The latter is also prone to be affected by the assembly of FeIII units in the The presence of the Br substituent on the salicylaldehyde group of the ligand in Cs[Fe(5-Br-thsa)2] is a factor in determining the crystal packing, as the Br substituent of one Cs[Fe(5-Br-thsa)2] unit provides a hydrogen-bonding interaction with an amino group of a neighbouring FeIII unit, creating ring systems.
Clearly, the variation in cation, ligand substituents and crystal packing is related to the spin state of FeIII being high-spin in Cs[Fe(thsa)2] at 103 and 298 K (Ryabova et al., 1981a), low-spin in Cs[Fe(5-Br-thsa)2] at 293 K (Powell et al., 2015) and low-spin in the present NH4[Fe(thsa)2] at 100 K. Variable-temperature measurements (10–300 K) confirm that the FeIII ion in NH4[Fe(thsa)2] remains in the low-spin state over this temperature range (Powell, 2016). In addition, within this family of cation(+) bis[R-salicylaldehyde 4R′-thiosemicarbazonato(2−)]ferrate(III) salts, the presence of particular solvent molecules may further affect the crystal packing, with the associated intermolecular effects influencing the electronic structure of FeIII, e.g. leading to a low-spin state of FeIII in Cs[Fe(L)2]·CH3OH [L = 3-ethoxysalicylaldehyde 4-methylthiosemicarbazonate(2−)] at 100 K (Powell et al., 2014). Our further studies of members of this FeIII family may shed more light on how the spin state of FeIII may be tuned in these systems.
3.2. Systematic and OD theory
Even though NH4[Fe(thsa)2] crystallizes in the monoclinic P21/n, the lattice is metrically virtually orthorhombic primitive [oP, β = 90.052 (4)°]. The crystals are systematically twinned by the additional symmetry of the lattice with respect to the 2/m of the crystal. Thus, the comprises the operations {2[100], m[100], 2[001], m[001]} and the twin (Nespolo, 2004) is 2′/m′2/m2′/m′. Since the reflections of both domains overlap nearly perfectly (twin index 1, ∼0), the can be classified as being by metric pseudomerohedry (Nespolo & Ferraris, 2000).
A higher ) was introduced in the 1950s to deal precisely with these kinds of structures.
of the lattice compared to the of the crystal is often associated with However, it is not a sufficient precondition for its existence. In fact, many polar structures do not form twins by inversion despite inversion being an intrinsic symmetry of any lattice. One common and often overlooked cause of is which may lead to a twin interface that is locally equivalent to the twin individuals. The order–disorder (OD) theory (Dornberger-Schiff & Grell-Niemann, 1961In the light of OD theory, the 4[Fe(thsa)2] can be decomposed into OD layers An (n being a sequential number) parallel to (010), which, in this case, also correspond to layers in the crystallochemical sense (Fig. 3). The crucial point of an is that operations relate individual layers, yet need not be valid for the whole structure. In the case of NH4[Fe(thsa)2], the An layers possess (idealized) P2(n)a symmetry (Fig. 4). In this layer-group notation, which is commonly used in the OD literature, the parentheses indicate the direction missing translational symmetry. The [Fe(thsa)2]− ions are located on the twofold axes of the An layers, whereas the ammonium ions are disordered about these axes.
of NHThe set of 4[Fe(thsa)2] is described by the OD family symbol (Dornberger-Schiff & Grell-Niemann, 1961).
operations of any possible stacking of NHP 2 (n) a
n2,r 22 2r–1
OD n2,r represents a glide reflection with the intrinsic translation b/2 + rc/2, whereby r is one of the metric parameters the OD family abstracts from.
families are the analogue of types in classical crystallography. They abstract from metric parameters and additionally of the particular stacking. The first line of the symbol indicates the layer symmetry, the second line one set of operations relating adjacent layers. Since the intrinsic translations are not limited to those found in space groups, a generalization of the Hermann-Mauguin notation is used. For example,Owing to the NFZ relationship (Ďurovič, 1997), which reads as Z = N/F = [Gn:Gn∩Gn+1]. Gn = P1(1)a is the group of operations of the An layer that do not invert An with respect to the stacking direction. Since the a-glide planes of adjacent layers do not overlap, Gn∩Gn+1 = P1(1)1. The possible layer arrangements are determined by decomposition of the latter in the former. In other words, given the An layer, the adjacent An+1 layer can be placed in Z = [P1(1)a:P1(1)1] = 2 ways, which are related by the a-glide reflection of the An layer.
layers can be arranged in different ways while keeping pairs of adjacent layers geometrically equivalent. These stacking possibilities can be enumerated using theOf the infinity of the thus obtained locally equivalent n-tuples of adjacent layers are equivalent (for a more rigorous definition, see Dornberger-Schiff, 1982). of the MDO type play a special role in OD theory, because all other can be decomposed into fragments of MDO Moreover, experience shows that ordered bulk are in most cases of the MDO type. The OD family of NH4[Fe(thsa)2] contains two MDO polytypes:
a finite number is especially simple in the sense that they cannot be decomposed into fragments of even simpler In these which are said to be of a maximum degree of order (MDO), not only pairs but also triples, quadruples and generallyMDO1: P2/b11, b = 2b0 + rc
MDO2: P21/n, b = 2b0
where b0 is the vector perpendicular to the layer lattices with the length of one layer width. Both MDO are shown schematically in Fig. 5. The twin individuals of NH4[Fe(thsa)2] correspond to the MDO2 polytype. A fragment of the MDO1 polytype is located at the twin interface.
Thus, the OD theory plausibly explains the formation of the observed twins, as the twin interface is geometrically and, if interactions over one layer width are ignored, also energetically equivalent to the twin individuals. Moreover, it explains the pseudo-oP metrics of the lattice. Such a metric pseudo-symmetry has often been considered as `accidental'. However, here it is clearly very much intrinsic to the structure family.
Finally, it should be noted that an OD description is usually based on a certain degree of idealization. Ordered ). Indeed, in the actual MDO2 of NH4[Fe(thsa)2], the symmetry of the An layers is reduced by an index of 2 from P2(n)a to P1(n)1. Accordingly, the of the [Fe(thsa)2]− ion is reduced from 2 to 1. Moreover, the unit-cell parameters deviate slightly from orthorhombic metrics [β = 90.052 (4)°, according to single-crystal diffraction]. Finally, the is also observed by a splitting of the single disordered ammonium position into two independent positions, which are now not forcibly disordered in a 1:1 manner. Indeed, the ratio of the occupancies of both positions refines to 52.7 (9):47.3 (9). However, collectively the deviations from the idealized are minute and the OD description can be considered as correct.
are desymmetrized with respect to the ideal description (Ďurovič, 1979Supporting information
CCDC reference: 2003812
https://doi.org/10.1107/S2053229620006452/ky3195sup1.cif
contains datablocks I, global. DOI:Structure factors: contains datablock I. DOI: https://doi.org/10.1107/S2053229620006452/ky3195Isup2.hkl
Data collection: APEX2 (Bruker, 2012); cell
APEX2 (Bruker, 2012); data reduction: SAINT-Plus (Bruker, 2012); program(s) used to solve structure: SUPERFLIP (Palatinus & Chapuis, 2007); program(s) used to refine structure: SHELXL2018 (Sheldrick, 2015); molecular graphics: ORTEP-3 (Farrugia, 2010); software used to prepare material for publication: SHELXL2018 (Sheldrick, 2015).C16H18FeN7O2S2 | F(000) = 948 |
Mr = 460.34 | Dx = 1.688 Mg m−3 |
Monoclinic, P21/n | Mo Kα radiation, λ = 0.71073 Å |
a = 8.4393 (8) Å | Cell parameters from 9753 reflections |
b = 18.2444 (17) Å | θ = 2.8–30.2° |
c = 11.7635 (11) Å | µ = 1.09 mm−1 |
β = 90.052 (4)° | T = 100 K |
V = 1811.2 (3) Å3 | Rhombic prism, green |
Z = 4 | 0.60 × 0.36 × 0.18 mm |
Bruker Kappa APEXII CCD diffractometer | 4839 reflections with I > 2σ(I) |
Graphite monochromator | Rint = 0.041 |
ω– and φ–scans | θmax = 30.2°, θmin = 1.1° |
Absorption correction: multi-scan (SADABS; Bruker, 2012) | h = −11→11 |
Tmin = 0.601, Tmax = 0.746 | k = −25→25 |
62618 measured reflections | l = −16→16 |
5355 independent reflections |
Refinement on F2 | 4 restraints |
Least-squares matrix: full | Hydrogen site location: mixed |
R[F2 > 2σ(F2)] = 0.042 | H atoms treated by a mixture of independent and constrained refinement |
wR(F2) = 0.110 | w = 1/[σ2(Fo2) + (0.0283P)2 + 5.6668P] where P = (Fo2 + 2Fc2)/3 |
S = 1.10 | (Δ/σ)max < 0.001 |
5355 reflections | Δρmax = 0.93 e Å−3 |
274 parameters | Δρmin = −0.74 e Å−3 |
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. Refined as a 2-component twin. Crystal data collection for NH4[Fe(thsa)2] was carried out after attaching a single crystal to a Kapton micro mount by using perfluorinated oil and mounted on a Bruker KAPPA APEX II diffractometer equipped with a CCD detector. Data were collected at 100 K in a dry stream of nitrogen with MoKα radiation (λ = 0.71073 Å). Data were reduced to intensity values using SAINT-Plus (Bruker, 2012) and absorption correction was applied using the multi-scan method implemented by SADABS (Bruker, 2012). The structure was solved using charge-flipping implemented by SUPERFLIP (Palatinus & Chapuis, 2007) and refined against F2 with SHELX (Sheldrick, 2014). |
x | y | z | Uiso*/Ueq | Occ. (<1) | |
Fe1 | −0.18454 (6) | 0.24824 (3) | 0.47816 (5) | 0.01283 (9) | |
S1 | −0.36955 (12) | 0.16316 (4) | 0.51161 (7) | 0.02015 (17) | |
S2 | −0.36760 (11) | 0.33417 (4) | 0.44372 (7) | 0.01932 (17) | |
O1 | −0.0177 (3) | 0.31944 (16) | 0.4514 (2) | 0.0256 (6) | |
O2 | −0.0210 (3) | 0.17473 (16) | 0.5062 (2) | 0.0269 (6) | |
N1 | −0.1906 (3) | 0.26809 (14) | 0.6398 (2) | 0.0151 (5) | |
N2 | −0.2879 (3) | 0.22705 (15) | 0.7119 (2) | 0.0155 (5) | |
N3 | −0.4684 (4) | 0.13350 (17) | 0.7206 (3) | 0.0202 (6) | |
N4 | −0.1913 (3) | 0.22967 (15) | 0.3155 (2) | 0.0135 (5) | |
N5 | −0.2879 (3) | 0.27192 (16) | 0.2434 (2) | 0.0164 (5) | |
N6 | −0.4642 (4) | 0.36688 (17) | 0.2347 (3) | 0.0201 (6) | |
N7 | 0.2779 (9) | 0.2599 (4) | 0.4588 (7) | 0.0181 (8) | 0.473 (9) |
N7' | 0.2763 (8) | 0.2370 (4) | 0.4976 (6) | 0.0181 (8) | 0.527 (9) |
C1 | −0.0056 (4) | 0.37125 (18) | 0.6414 (3) | 0.0168 (6) | |
C2 | 0.0357 (4) | 0.3690 (2) | 0.5250 (3) | 0.0197 (6) | |
C3 | 0.1472 (4) | 0.4205 (2) | 0.4859 (3) | 0.0260 (8) | |
H3 | 0.178472 | 0.419564 | 0.408318 | 0.031* | |
C4 | 0.2126 (4) | 0.47272 (19) | 0.5580 (3) | 0.0255 (8) | |
H4 | 0.286056 | 0.507260 | 0.528461 | 0.031* | |
C5 | 0.1725 (5) | 0.47535 (18) | 0.6724 (3) | 0.0227 (7) | |
H5A | 0.217916 | 0.510869 | 0.721708 | 0.027* | |
C6 | 0.0642 (4) | 0.42452 (19) | 0.7123 (3) | 0.0202 (7) | |
H6 | 0.035885 | 0.425576 | 0.790412 | 0.024* | |
C7 | −0.1138 (4) | 0.31973 (19) | 0.6915 (3) | 0.0178 (6) | |
H7 | −0.130724 | 0.324031 | 0.771063 | 0.021* | |
C8 | −0.3732 (4) | 0.17776 (17) | 0.6582 (3) | 0.0142 (6) | |
C9 | −0.0054 (4) | 0.12707 (18) | 0.3156 (3) | 0.0168 (6) | |
C10 | 0.0329 (4) | 0.12625 (19) | 0.4325 (3) | 0.0190 (6) | |
C11 | 0.1425 (4) | 0.0731 (2) | 0.4712 (3) | 0.0255 (7) | |
H11 | 0.168253 | 0.071316 | 0.549825 | 0.031* | |
C12 | 0.2123 (4) | 0.02419 (19) | 0.3988 (3) | 0.0244 (8) | |
H12 | 0.285668 | −0.010784 | 0.427276 | 0.029* | |
C13 | 0.1755 (5) | 0.02567 (18) | 0.2828 (3) | 0.0234 (7) | |
H13 | 0.224536 | −0.008008 | 0.232264 | 0.028* | |
C14 | 0.0679 (4) | 0.07619 (19) | 0.2421 (3) | 0.0210 (7) | |
H14 | 0.042748 | 0.076766 | 0.163369 | 0.025* | |
C15 | −0.1132 (4) | 0.17866 (18) | 0.2639 (3) | 0.0164 (6) | |
H15 | −0.128169 | 0.174734 | 0.184033 | 0.020* | |
C16 | −0.3709 (4) | 0.32150 (17) | 0.2965 (3) | 0.0162 (6) | |
HN31 | −0.496 (8) | 0.154 (3) | 0.785 (3) | 0.06 (2)* | |
HN32 | −0.534 (5) | 0.104 (2) | 0.684 (4) | 0.040 (15)* | |
HN61 | −0.523 (5) | 0.400 (2) | 0.264 (4) | 0.028 (12)* | |
HN62 | −0.484 (6) | 0.355 (2) | 0.164 (2) | 0.027 (12)* |
U11 | U22 | U33 | U12 | U13 | U23 | |
Fe1 | 0.01120 (16) | 0.01814 (17) | 0.00915 (15) | 0.00055 (17) | 0.00122 (18) | 0.00086 (13) |
S1 | 0.0290 (4) | 0.0192 (3) | 0.0123 (4) | −0.0058 (3) | 0.0039 (3) | −0.0012 (3) |
S2 | 0.0272 (4) | 0.0188 (3) | 0.0120 (4) | 0.0058 (3) | −0.0018 (3) | −0.0016 (3) |
O1 | 0.0215 (13) | 0.0417 (15) | 0.0136 (12) | −0.0145 (11) | 0.0028 (10) | −0.0018 (10) |
O2 | 0.0283 (14) | 0.0434 (15) | 0.0091 (11) | 0.0183 (12) | −0.0018 (10) | −0.0033 (10) |
N1 | 0.0121 (12) | 0.0176 (11) | 0.0156 (13) | −0.0010 (10) | 0.0009 (10) | 0.0042 (9) |
N2 | 0.0137 (14) | 0.0211 (12) | 0.0117 (11) | −0.0005 (10) | 0.0040 (9) | 0.0005 (9) |
N3 | 0.0254 (16) | 0.0178 (13) | 0.0175 (14) | −0.0029 (11) | 0.0060 (12) | 0.0008 (11) |
N4 | 0.0120 (11) | 0.0231 (12) | 0.0055 (11) | −0.0001 (10) | 0.0000 (9) | 0.0003 (9) |
N5 | 0.0149 (14) | 0.0206 (12) | 0.0137 (12) | 0.0020 (10) | −0.0006 (10) | 0.0021 (10) |
N6 | 0.0257 (16) | 0.0197 (14) | 0.0148 (14) | 0.0038 (11) | −0.0040 (12) | −0.0010 (11) |
N7 | 0.0184 (15) | 0.020 (2) | 0.016 (2) | −0.003 (2) | 0.003 (2) | −0.0010 (14) |
N7' | 0.0184 (15) | 0.020 (2) | 0.016 (2) | −0.003 (2) | 0.003 (2) | −0.0010 (14) |
C1 | 0.0156 (15) | 0.0206 (14) | 0.0142 (15) | −0.0007 (12) | 0.0013 (12) | 0.0008 (11) |
C2 | 0.0149 (14) | 0.0279 (16) | 0.0162 (15) | −0.0055 (12) | −0.0008 (12) | 0.0034 (13) |
C3 | 0.0241 (18) | 0.0355 (19) | 0.0186 (16) | −0.0105 (14) | 0.0018 (13) | 0.0035 (14) |
C4 | 0.0233 (19) | 0.0233 (15) | 0.0299 (19) | −0.0041 (13) | −0.0013 (14) | 0.0059 (14) |
C5 | 0.0225 (17) | 0.0168 (14) | 0.0289 (19) | −0.0001 (13) | 0.0001 (15) | −0.0041 (12) |
C6 | 0.0182 (15) | 0.0187 (15) | 0.0236 (17) | −0.0001 (12) | 0.0004 (13) | −0.0015 (13) |
C7 | 0.0133 (14) | 0.0260 (15) | 0.0141 (14) | 0.0000 (12) | 0.0015 (12) | 0.0013 (12) |
C8 | 0.0167 (13) | 0.0155 (13) | 0.0104 (14) | 0.0006 (11) | 0.0046 (12) | 0.0016 (10) |
C9 | 0.0122 (14) | 0.0203 (14) | 0.0180 (15) | −0.0011 (11) | 0.0027 (11) | 0.0006 (12) |
C10 | 0.0176 (15) | 0.0261 (16) | 0.0132 (15) | 0.0037 (12) | 0.0033 (12) | −0.0004 (12) |
C11 | 0.0219 (17) | 0.0359 (19) | 0.0188 (17) | 0.0124 (14) | 0.0024 (13) | 0.0041 (14) |
C12 | 0.0210 (19) | 0.0223 (15) | 0.030 (2) | 0.0049 (13) | 0.0035 (14) | 0.0038 (13) |
C13 | 0.0222 (17) | 0.0184 (14) | 0.0296 (19) | 0.0007 (14) | 0.0026 (16) | −0.0051 (12) |
C14 | 0.0213 (16) | 0.0204 (16) | 0.0214 (17) | −0.0011 (13) | 0.0019 (13) | −0.0048 (13) |
C15 | 0.0162 (14) | 0.0225 (15) | 0.0106 (13) | −0.0007 (12) | 0.0027 (12) | −0.0011 (11) |
C16 | 0.0159 (13) | 0.0158 (13) | 0.0168 (16) | −0.0024 (11) | −0.0022 (13) | 0.0010 (11) |
Fe1—N1 | 1.937 (3) | N5—C16 | 1.304 (4) |
Fe1—O1 | 1.941 (3) | N6—C16 | 1.354 (4) |
Fe1—N4 | 1.944 (3) | C1—C6 | 1.410 (5) |
Fe1—O2 | 1.952 (3) | C1—C2 | 1.413 (5) |
Fe1—S1 | 2.2369 (10) | C1—C7 | 1.438 (5) |
Fe1—S2 | 2.2377 (10) | C2—C3 | 1.408 (5) |
S1—C8 | 1.745 (3) | C3—C4 | 1.389 (5) |
S2—C16 | 1.747 (3) | C4—C5 | 1.389 (5) |
O1—C2 | 1.330 (4) | C5—C6 | 1.384 (5) |
O2—C10 | 1.320 (4) | C9—C14 | 1.412 (5) |
N1—C7 | 1.295 (4) | C9—C10 | 1.413 (5) |
N1—N2 | 1.398 (4) | C9—C15 | 1.443 (5) |
N2—C8 | 1.313 (4) | C10—C11 | 1.415 (5) |
N3—C8 | 1.355 (4) | C11—C12 | 1.367 (5) |
N4—C15 | 1.293 (4) | C12—C13 | 1.400 (5) |
N4—N5 | 1.406 (4) | C13—C14 | 1.380 (5) |
N1—Fe1—O1 | 93.08 (11) | C6—C1—C7 | 118.2 (3) |
N1—Fe1—N4 | 176.71 (11) | C2—C1—C7 | 122.4 (3) |
O1—Fe1—N4 | 88.73 (11) | O1—C2—C3 | 117.9 (3) |
N1—Fe1—O2 | 88.97 (11) | O1—C2—C1 | 124.5 (3) |
O1—Fe1—O2 | 88.53 (12) | C3—C2—C1 | 117.6 (3) |
N4—Fe1—O2 | 93.83 (11) | C4—C3—C2 | 121.6 (3) |
N1—Fe1—S1 | 86.44 (9) | C3—C4—C5 | 121.2 (3) |
O1—Fe1—S1 | 177.74 (10) | C6—C5—C4 | 117.8 (3) |
N4—Fe1—S1 | 91.85 (9) | C5—C6—C1 | 122.5 (3) |
O2—Fe1—S1 | 89.26 (10) | N1—C7—C1 | 126.9 (3) |
N1—Fe1—S2 | 91.60 (9) | N2—C8—N3 | 118.2 (3) |
O1—Fe1—S2 | 90.15 (9) | N2—C8—S1 | 124.7 (2) |
N4—Fe1—S2 | 85.65 (9) | N3—C8—S1 | 117.0 (2) |
O2—Fe1—S2 | 178.59 (10) | C14—C9—C10 | 119.3 (3) |
S1—Fe1—S2 | 92.07 (3) | C14—C9—C15 | 116.5 (3) |
C8—S1—Fe1 | 94.63 (11) | C10—C9—C15 | 124.2 (3) |
C16—S2—Fe1 | 95.57 (12) | O2—C10—C9 | 123.6 (3) |
C2—O1—Fe1 | 126.5 (2) | O2—C10—C11 | 118.3 (3) |
C10—O2—Fe1 | 126.4 (2) | C9—C10—C11 | 118.0 (3) |
C7—N1—N2 | 113.5 (3) | C12—C11—C10 | 121.9 (3) |
C7—N1—Fe1 | 125.7 (2) | C11—C12—C13 | 120.0 (3) |
N2—N1—Fe1 | 120.8 (2) | C14—C13—C12 | 119.8 (3) |
C8—N2—N1 | 113.4 (3) | C13—C14—C9 | 121.0 (3) |
C15—N4—N5 | 114.0 (3) | N4—C15—C9 | 126.4 (3) |
C15—N4—Fe1 | 125.0 (2) | N5—C16—N6 | 118.6 (3) |
N5—N4—Fe1 | 121.0 (2) | N5—C16—S2 | 124.0 (3) |
C16—N5—N4 | 113.7 (3) | N6—C16—S2 | 117.4 (3) |
C6—C1—C2 | 119.4 (3) |
D—H···A | D—H | H···A | D···A | D—H···A |
C11—H11···N6i | 0.95 | 2.69 | 3.409 (5) | 133 |
N3—HN31···O1ii | 0.87 (2) | 2.03 (3) | 2.879 (4) | 164 (6) |
N6—HN62···O2iii | 0.88 (2) | 1.96 (2) | 2.834 (4) | 178 (5) |
Symmetry codes: (i) x+1/2, −y+1/2, z+1/2; (ii) x−1/2, −y+1/2, z+1/2; (iii) x−1/2, −y+1/2, z−1/2. |
Acknowledgements
Elemental analysis was performed at the Microanalytical Laboratory, Vienna University. PW thanks the Distinguished Visitor Fund of Aston University enabling his research visits to Aston University. The Austrian Science Fund (FWF) is kindly acknowledged for financial support for PW. PvK thanks the TU Wien International Office for financial support for her research visits to the TU Wien.
Funding information
Funding for this research was provided by: Austrian Science Fund (project No. P 31076).
References
Beraldo, H. & Gambino, D. (2004). Med. Chem. 4, 31–39. Google Scholar
Bruker (2012). APEX2 and SAINT-Plus. Bruker AXS Inc., Madison, Wisconsin, USA. Google Scholar
Dornberger-Schiff, K. (1982). Acta Cryst. A38, 483–491. CrossRef CAS Web of Science IUCr Journals Google Scholar
Dornberger-Schiff, K. & Grell-Niemann, H. (1961). Acta Cryst. 14, 167–177. CrossRef IUCr Journals Web of Science Google Scholar
Ďurovič, S. (1979). Krist. Tech. 14, 1047–1053. Google Scholar
Ďurovič, S. (1997). EMU Notes in Mineralogy, Vol. 1, edited by S. Merlino, pp. 3–28. Jena, Germany: European Mineralogical Union. Google Scholar
Farrell, N. (2002). Coord. Chem. Rev. 232, 1–4. Web of Science CrossRef CAS Google Scholar
Farrugia, L. J. (2012). J. Appl. Cryst. 45, 849–854. Web of Science CrossRef CAS IUCr Journals Google Scholar
Floquet, S., Boillot, M. L., Rivière, E., Varret, F., Boukheddaden, K., Morineau, D. & Négrier, P. (2003). New J. Chem. 27, 341–348. Web of Science CrossRef CAS Google Scholar
Floquet, S., Guillou, N., Négrier, P., Rivière, E. & Boillot, M. L. (2006). New J. Chem. 30, 1621–1627. Web of Science CrossRef CAS Google Scholar
Floquet, S., Muñoz, M. C., Guillot, R., Rivière, E., Blain, G., Réal, J. A. & Boillot, M. L. (2009). Inorg. Chim. Acta, 362, 56–64. Web of Science CrossRef CAS Google Scholar
Gütlich, P. & Goodwin, H. A. (2004). Top. Curr. Chem. 233, 1–47. Google Scholar
Gütlich, P., van Koningsbruggen, P. J. & Renz, F. (2004). Struct. Bond. 107, 27–75. Google Scholar
Halcrow, M. A. (2013). In Spin-Crossover Materials: Properties and Applications, 1st ed. Chichester: John Wiley & Sons Ltd. Google Scholar
Harding, D. J., Harding, P. & Phonsri, W. (2016). Coord. Chem. Rev. 313, 38–61. Web of Science CrossRef CAS Google Scholar
Hayami, S., Gu, Z., Shiro, M., Einaga, Y., Fujishima, A. & Sato, O. (2000). J. Am. Chem. Soc. 122, 7126–7127. Web of Science CrossRef CAS Google Scholar
Hayami, S., Hiki, K., Kawahara, T., Maeda, Y., Urakami, D., Inoue, K., Ohama, M., Kawata, S. & Sato, O. (2009). Chem. Eur. J. 15, 3497–3508. Web of Science CrossRef PubMed CAS Google Scholar
Koningsbruggen, P. J. van, Maeda, Y. & Oshio, H. (2004). Top. Curr. Chem. 233, 259–324. Google Scholar
Létard, J. F., Guionneau, P. & Goux-Capes, L. (2004). Top. Curr. Chem. 235, 221–249. Google Scholar
Li, Z. Y., Dai, J. W., Shiota, Y., Yoshizawa, K., Kanegawa, S. & Sato, O. (2013). Chem. Eur. J. 19, 12948–12952. CrossRef CAS PubMed Google Scholar
Nespolo, M. (2004). Z. Kristallogr. 219, 57–71. Web of Science CrossRef CAS Google Scholar
Nespolo, M. & Ferraris, G. (2000). Z. Kristallogr. 215, 77–81. Web of Science CrossRef CAS Google Scholar
Nihei, M., Shiga, T., Maeda, Y. & Oshio, H. (2007). Coord. Chem. Rev. 251, 2606–2621. Web of Science CrossRef CAS Google Scholar
Palatinus, L. & Chapuis, G. (2007). J. Appl. Cryst. 40, 786–790. Web of Science CrossRef CAS IUCr Journals Google Scholar
Phonsri, W., Darveniza, L. C., Batten, S. R. & Murray, K. S. (2017). Inorganics, 5, 51. Google Scholar
Powell, R. E. (2016). PhD thesis, Aston University, Birmingham, UK. Google Scholar
Powell, R. E., Schwalbe, C. H., Tizzard, G. J. & van Koningsbruggen, P. J. (2014). Acta Cryst. C70, 595–598. Web of Science CrossRef IUCr Journals Google Scholar
Powell, R. E., Schwalbe, C. H., Tizzard, G. J. & van Koningsbruggen, P. J. (2015). Acta Cryst. C71, 169–174. Google Scholar
Ryabova, N. A., Ponomarev, V. I., Atovmyan, L. O., Zelentsov, V. V. & Shipilov, V. I. (1978). Koord. Khim. 4, 119–126. CAS Google Scholar
Ryabova, N. A., Ponomarev, V. I., Zelentsov, V. V. & Atovmyan, L. O. (1981a). Kristallografiya, 26, 101–108. Google Scholar
Ryabova, N. A., Ponomarev, V. I., Zelentsov, V. V. & Atovmyan, L. O. (1982). Kristallografiya, 27, 81–91. CAS Google Scholar
Ryabova, N. A., Ponomarev, V. I., Zelentsov, V. V., Shipilov, V. I. & Atovmyan, L. O. (1981b). J. Struct. Chem. 22, 234–238. Google Scholar
Sheldrick, G. M. (2015). Acta Cryst. C71, 3–8. Web of Science CrossRef IUCr Journals Google Scholar
Yemeli Tido, E. W. (2010). PhD thesis, University of Groningen, The Netherlands. Google Scholar
Yemeli Tido, E. W. Y., Faulmann, R., Roswanda, A., Meetsma, A. & van Koningsbruggen, P. J. (2010). Dalton Trans. 39, 1643–1651. Google Scholar
Zelentsov, V. V., Bogdanova, L. G., Ablov, A. V., Gerbeleu, N. V. & Dyatlova, C. V. (1973). Russ. J. Inorg. Chem. 18, 2654–2657. CAS Google Scholar
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