Crystal structure of poly[[di-aqua-tetra-μ2-cyanido-iron(II)platinum(II)] acetone disolvate].

In the title polymeric complex, {[FePt(CN)4(H2O)2]·2C3H6O} n , the FeII cation has an octa-hedral [FeN4O2] geometry being coordinated by two water mol-ecules and four cyanide anions. The Pt cation is located on an inversion centre and has a square-planar coordination environment formed by four cyanide groups. The tetra-cyano-platinate anions bridge the FeII cations to form infinite two-dimensional layers that propagate in the bc plane. Two guest mol-ecules of acetone per FeII are located between the layers. These guest acetone mol-ecules inter-act with the coordinated water mol-ecules by O-H⋯O hydrogen bonds. © Kuzevanova et al. 2019.

Chemical context

Hofmann clathrates and their analogues form one the most famous families of compounds that are able to incorporate guest mol­ecules. The first clathrate was obtained by Hofmann and Küspert in 1897 (Hofmann & Küspert, 1897 ▸) and was of composition [Ni(NH3)2Ni(CN)4]·2C6H6. It was a 2D coord­in­ation compound formed by infinite cyano­metallic layers that propagate along the ab plane. The 2D system was supported by ammine axial ligands, and guest mol­ecules of benzene were trapped between the layers.

Later, by slight modifications of the chemical composition, several analogous compounds were obtained, leading to the creation of a new class of coordination materials. The first modification was the substitution of nickel with other transition metals, as well as the introduction of other small aromatic guest mol­ecules that resulted in the creation of compounds with the general formula [M(NH3)2 M′(CN)4]·2G (where M = Mn, Fe, Co, Ni, Cu, Zn, Cd, M′ = Ni, Pd, Pt and G = benzene, pyrrole, thio­phene, aniline, biphenyl, etc.; Iwamoto, 1996 ▸). The second modification of the Hofmann clathrate was the substitution of square-planar {M′(CN)4}2− anions with tetra­hedral ({M′(CN)4}2−, M′ = Cd, Hg; Arcís-Castillo et al., 2013 ▸), linear ({M′(CN)2}−, M′ = Cu, Ag, Au; Gural’skiy, Golub et al., 2016 ▸; Gural’skiy, Shylin et al., 2016 ▸), octa­hedral ({M′(CN)6}3−, M′ = Co, Cr; Dommann et al., 1990 ▸) and even dodeca­hedral ({M′(CN)8}4−, M′ = W, Nb; Ohkoshi et al., 2013 ▸) fragments. Additionally, a very important modification was made by the introduction of other organic ligands instead of ammonia. For example, by the introduction of pyridine, the first FeII-based clathrate [Fe(py)2{Pt(CN)4}] exhibiting spin-crossover (SCO) behaviour was obtained by Kitazawa et al. (1996 ▸). At the same time, the introduction of various bidentate ligands such as pyrazine (Niel et al., 2001 ▸; Gural’skiy, Shylin et al., 2016 ▸), pyrimidine (Agustí et al., 2008 ▸), bis­(4-pyrid­yl)acetyl­ene (Agustí et al., 2008 ▸) and others allowed the formation of 3D SCO networks.

Additionally, the characteristics of spin transition in coordination compounds are known to be extremely sensitive to any changes in the chemical environment. As Hofmann clathrate analogues are very easy to modulate, numerous SCO complexes with very different temperatures, abruptnesses and hystereses of SCO were obtained. Moreover, the ability of Hofmann clathrate analogues to incorporate guest mol­ecules provided SCO-based chemical sensors (Ohba et al., 2009 ▸).

Herein we present a new Fe–Pt Hofmann clathrate analogue [Fe(H2O)2{Pt(CN)4}]·2(CH3)2CO.

Structural commentary

The title compound crystallizes in the P4/mmm space group. The FeII cation has a [FeN4O2] coordination environment (Fig. 1 ▸) comprising four CN− anions in the equatorial positions [Fe1—N1 = 2.158 (5) Å] and two water mol­ecules in the axial positions [Fe1—O1 = 2.130 (6) Å]. The Fe—O bonds are slightly shorter than the Fe–N bonds, thus leading to a compressed octa­hedral geometry. Judging by the bond length, the FeII cation is in a high-spin state at the experimental temperature (180 K). This is corroborated by the presence of H2O mol­ecules in the coordination sphere of FeII. The cyanide anions connect the FeII and PtII cations into infinite two-dimensional layers. The PtII cation is located at a fourfold rotation axis and possesses a square-planar geometry [Pt1—C1 = 1.993 (6) Å, C1—Pt–C1 = 90°]. Thanks to the tetra­gonal symmetry of the crystalline compound, no deviation from an ideal octa­hedron is observed for FeII, Σ|90 – θ| = 0°, where θ is the N—Fe—N or O—Fe—N angles. Additionally, the compound incorporates two guest mol­ecules of acetone per FeII centers.

Figure 1

A fragment of the mol­ecular structure of the title compound showing the atom-labelling scheme. Displacement ellipsoids are drawn at the 50% probability level [symmetry codes: (i) x, −y, 1 − z; (ii) −x, −y, z; (iii) x, −y, z; (iv) −x, y, z; (v) −1 + x, −y, z; (vi) −1 + x, −y, −z; (vii) 1 − x, y, 1 + z; (viii) 1 − x, y, 1 − z].

Supra­molecular features

The crystalline structure is connected by bridging tetra­cyano­platinate moieties, which form a two-dimensional grid that propagates along the ab plane (Fig. 2 ▸). As imposed by symmetry, no deviation from linearity for the Fe—N—C—Pt linkages is observed [Fe—N—C = 180°, N—C—Pt = 180°, C—Pt—C = 180°]. The distance between parallel cyano­metallic layers is 7.973 (6) Å. The guest acetone mol­ecules are located between the cyano­metallic layers. Each oxygen atom of the coordinated water mol­ecules inter­acts with acetone by O—H⋯O hydrogen bonds (Fig. 3 ▸, Table 1 ▸), creating a three-dimensional supramolecular framewor. The size of the available voids between the cyano­metallic layers allows the acetone mol­ecules to rotate freely, thus leading to disorder of the acetone mol­ecules over four positions.

Figure 2

View of the crystal structure of the title compound in the bc plane showing the two-dimensional cyano­metallic layers. Hydrogen bonds are shown as dashed lines. Acetone H atoms are omitted for clarity.

Figure 3

View of the structure of the title compound in the ab plane showing the distortion of the acetone guest mol­ecules. Hydrogen bonds are shown as dashed lines. Acetone H atoms are omitted for clarity.

Table 1

Hydrogen-bond geometry (Å, °)

D—H⋯A	D—H	H⋯A	D⋯A	D—H⋯A
O1—H1A⋯O2i	0.84	2.03	2.775 (11)	147
O1—H1A⋯O2ii	0.84	2.03	2.775 (11)	148
O1—H1B⋯O2iii	0.85	2.04	2.775 (11)	144
O1—H1B⋯O2iv	0.85	2.14	2.775 (11)	131

Symmetry codes: (i) ; (ii) ; (iii) ; (iv) .

Database survey

A survey of the Cambridge Structural Database (Version 5.38; Groom et al., 2016 ▸) confirmed that the title compound has never been published before. It revealed 51 cyano­metallic structures of the general formula [TM(H2O)2{TM(CN)4}], where TM = any transition metal. There were also 19 hits for structures containing [Fe{Pt(CN)4}] fragments: refcodes: OVILEM, OVIRUI, OVIRUI01, OVIRUI02 and OVIRUI03 (Sciortino et al., 2017 ▸), AMIJOX (Kucheriv et al., 2016 ▸), BEDWEO and BEDWIS (Sciortino et al., 2012 ▸), CEMYUQ (Mũnoz-Lara et al., 2013 ▸), MUHMEI, MUHNAF, MUHNAF01, MUHNAF02, MUHPAH and MUHPAH01 (Martínez et al., 2009 ▸), QADDUX (Sakaida et al., 2016 ▸), QOJWIW and QOJWIW01 (Cobo et al., 2008 ▸) and TURXIP (Ohtani et al., 2013 ▸).

Synthesis and crystallization

Crystals of the title compound were obtained by slow diffusion (three layers) in a 3 ml tube. The first layer contained 19 mg (0.05 mmol) of K2[Pt(CN)4] in 0.5 ml of water. The middle layer contained 1.5 ml of a water:acetone (1:1) solution. The third layer contained 25 mg (0.05 mmol) of Fe(OTs)2·6H2O in 0.4 ml of acetone and 0.1 ml of water. The colourless crystals grew in the middle layer within three weeks and were kept in the mother solution prior to measurements.

Refinement

Crystal data, data collection and structure refinement details are summarized in Table 2 ▸. All hydrogen atoms were fixed at calculated positions and refined as riding with C—H = 0.96 Å and O–H = 0.84 Å, U iso(H) = 1.5U iso(C,O). The OH group and the idealized methyl group were refined as rotating.

Table 2

Experimental details

Crystal data
Chemical formula	[FePt(CN)4(H2O)2]·2C3H6O
M r	507.21
Crystal system, space group	Tetragonal, P4/m m m
Temperature (K)	180
a, c (Å)	7.4802 (4), 7.9725 (11)
V (Å3)	446.09 (8)
Z	1
Radiation type	Mo Kα
μ (mm−1)	8.66
Crystal size (mm)	0.05 × 0.05 × 0.02
Data collection
Diffractometer	Rigaku Oxford Diffraction Xcalibur, Eos
Absorption correction	Multi-scan (CrysAlis PRO; Rigaku OD, 2015 ▸)
T min, T max	0.699, 1.000
No. of measured, independent and observed [I > 2σ(I)] reflections	1126, 361, 359
R int	0.037
(sin θ/λ)max (Å−1)	0.682
Refinement
R[F 2 > 2σ(F 2)], wR(F 2), S	0.025, 0.046, 1.04
No. of reflections	361
No. of parameters	34
H-atom treatment	H-atom parameters constrained
Δρmax, Δρmin (e Å−3)	1.25, −1.06

Computer programs: CrysAlis PRO (Rigaku OD, 2015 ▸), SHELXT (Sheldrick, 2015a ▸), SHELXL (Sheldrick, 2015b ▸) and OLEX2 (Dolomanov et al., 2009 ▸).

Crystal structure: contains datablock(s) I. DOI: 10.1107/S2056989019012945/tx2013sup1.cif

Additional supporting information: crystallographic information; 3D view; checkCIF report

[FePt(CN)4(H2O)2]·2C3H6O	Dx = 1.888 Mg m−3
Mr = 507.21	Mo Kα radiation, λ = 0.71073 Å
Tetragonal, P4/mmm	Cell parameters from 664 reflections
a = 7.4802 (4) Å	θ = 2.5–28.5°
c = 7.9725 (11) Å	µ = 8.66 mm−1
V = 446.09 (8) Å3	T = 180 K
Z = 1	Plate, clear colourless
F(000) = 240	0.05 × 0.05 × 0.02 mm

Rigaku Oxford Diffraction Xcalibur, Eos diffractometer	361 independent reflections
Radiation source: fine-focus sealed X-ray tube, Enhance (Mo) X-ray Source	359 reflections with I > 2σ(I)
Graphite monochromator	Rint = 0.037
Detector resolution: 8.0797 pixels mm-1	θmax = 29.0°, θmin = 2.6°
ω scans	h = −5→10
Absorption correction: multi-scan (CrysAlisPro; Rigaku OD, 2015)	k = −10→5
Tmin = 0.699, Tmax = 1.000	l = −10→5
1126 measured reflections

Refinement on F2	Primary atom site location: dual
Least-squares matrix: full	Hydrogen site location: mixed
R[F2 > 2σ(F2)] = 0.025	H-atom parameters constrained
wR(F2) = 0.046	w = 1/[σ2(Fo2) + (0.0197P)2] where P = (Fo2 + 2Fc2)/3
S = 1.03	(Δ/σ)max < 0.001
361 reflections	Δρmax = 1.25 e Å−3
34 parameters	Δρmin = −1.06 e Å−3
0 restraints

Geometry. All esds (except the esd in the dihedral angle between two l.s. planes) are estimated using the full covariance matrix. The cell esds are taken into account individually in the estimation of esds in distances, angles and torsion angles; correlations between esds in cell parameters are only used when they are defined by crystal symmetry. An approximate (isotropic) treatment of cell esds is used for estimating esds involving l.s. planes.

	x	y	z	Uiso*/Ueq	Occ. (<1)
Pt1	0.500000	0.500000	0.500000	0.01400 (17)
Fe1	0.000000	0.000000	0.500000	0.0104 (4)
O1	0.000000	0.000000	0.2329 (8)	0.0276 (16)
H1A	0.105309	0.000432	0.196819	0.041*	0.25
H1B	−0.043425	0.098216	0.196839	0.041*	0.125
C1	0.3116 (6)	0.3116 (6)	0.500000	0.0186 (15)
N1	0.2040 (5)	0.2040 (5)	0.500000	0.0210 (13)
C3	0.475 (9)	0.036 (8)	0.1546 (18)	0.08 (2)	0.25
H3A	0.473348	0.162844	0.175407	0.114*	0.25
H3B	0.531096	−0.023709	0.246770	0.114*	0.25
H3C	0.354004	−0.005924	0.142949	0.114*	0.25
O2	0.7276 (18)	0.043 (3)	0.000000	0.055 (5)	0.25
C2	0.574 (2)	0.000000	0.000000	0.055 (5)	0.5

	U11	U22	U33	U12	U13	U23
Pt1	0.00585 (17)	0.00585 (17)	0.0303 (3)	0.000	0.000	0.000
Fe1	0.0068 (5)	0.0068 (5)	0.0177 (10)	0.000	0.000	0.000
O1	0.030 (2)	0.030 (2)	0.023 (4)	0.000	0.000	0.000
C1	0.0092 (18)	0.0092 (18)	0.037 (4)	0.003 (2)	0.000	0.000
N1	0.0121 (16)	0.0121 (16)	0.039 (4)	−0.005 (2)	0.000	0.000
C3	0.04 (4)	0.13 (5)	0.056 (9)	−0.03 (2)	0.013 (14)	−0.05 (2)
O2	0.019 (4)	0.109 (15)	0.036 (6)	−0.005 (10)	0.000	0.000
C2	0.019 (4)	0.109 (15)	0.036 (6)	−0.005 (10)	0.000	0.000

Pt1—C1i	1.993 (6)	Fe1—N1v	2.158 (5)
Pt1—C1	1.993 (6)	Fe1—N1vi	2.158 (5)
Pt1—C1ii	1.993 (6)	Fe1—N1	2.158 (5)
Pt1—C1iii	1.993 (6)	C1—N1	1.138 (8)
Fe1—O1iv	2.130 (6)	C3—C2	1.46 (4)
Fe1—O1	2.130 (6)	O2—O2vii	0.64 (5)
Fe1—N1iv	2.158 (5)	O2—C2	1.19 (2)
C1i—Pt1—C1ii	90.0	O1iv—Fe1—N1vi	90.0
C1ii—Pt1—C1	90.0	N1iv—Fe1—N1vi	90.0
C1i—Pt1—C1	180.0	N1—Fe1—N1vi	90.0
C1i—Pt1—C1iii	90.0	N1iv—Fe1—N1v	90.0
C1iii—Pt1—C1	90.0	N1—Fe1—N1iv	180.0
C1ii—Pt1—C1iii	180.0	N1—Fe1—N1v	90.0
O1—Fe1—O1iv	180.0	N1vi—Fe1—N1v	180.0
O1—Fe1—N1	90.0	N1—C1—Pt1	180.0
O1—Fe1—N1vi	90.0	C1—N1—Fe1	180.0
O1iv—Fe1—N1v	90.0	O2vii—O2—C2	74.4 (12)
O1iv—Fe1—N1	90.0	O2vii—C2—C3	123 (2)
O1—Fe1—N1v	90.0	O2—C2—C3	116 (2)
O1—Fe1—N1iv	90.0	O2—C2—O2vii	31 (2)
O1iv—Fe1—N1iv	90.0

D—H···A	D—H	H···A	D···A	D—H···A
O1—H1A···O2viii	0.84	2.03	2.775 (11)	147
O1—H1A···O2ix	0.84	2.03	2.775 (11)	148
O1—H1B···O2x	0.85	2.04	2.775 (11)	144
O1—H1B···O2xi	0.85	2.14	2.775 (11)	131