Synthesis, crystal structures and magnetic properties of trinuclear oxo-centered homo- and mixed-valence manganese pivalate complexes with imidazole (Im) and 1-methylimidazole (1-MeIm): and

Two new μ₃-oxo-centered trinuclear manganese complexes, one of them a homo-valence (1) pivalate complex and the other a mixed-valence (2) pivalate complex (where Im = imidazole, 1-MeIm = 1-methylimidazole), have been synthesized and characterized by IR spectroscopy, thermogravimetric analysis, X-ray crystallography and magnetochemistry. Complexes 1 and 2 are μ₃-oxo-trinuclear compounds with the three manganese atoms bridged by six pivalate groups. At each axial position there is an Im (1) or 1-MeIm (2) molecule. In both compounds, the manganese coordination geometry is slightly distorted octahedral, consisting of the oxygen of the central triangle, four oxygen atoms from bridging pivalate ligands, and a terminal Im or 1-MeIm nitrogen atom. The crystal packing of 1 involves hydrogen bonding between complex cations [Mn₃O(Piv)₆(Im)₃]⁺ and outersphere pivalate ions, whereas in compound 2 interactions of the C–Hπ type, formed by both the aromatic and methyl C–H groups of 1-MeIm molecules, are present. Magnetic studies reveal that both compounds represent antiferromagnetically coupled, spin-frustrated triangular systems exhibiting weak to moderate exchange coupling constants.     

Two new two-dimensional organically templated phosphite compounds: (C6H16N2)0.5[M(HPO3)F], M=Fe(II) and Co(II): Solvothermal synthesis, crystal structures, thermal, spectroscopic, and magnetic properties

The organically templated (C₆H₁₆N₂)_0.5[M(HPO₃)F] [M(II)=Fe (1) and Co (2)] compounds have been synthesized by using mild hydrothermal conditions under autogeneous pressure. The crystal structures have been determined from X-ray single-crystal diffraction data. The compounds are isostructural and crystallize in the C2/c monoclinic space group. The unit-cell parameters are a=5.607(1), b=21.276(4), , β=93.74(1)° for the iron phase and a=5.5822(7), b=21.325(3), , β=93.464(9)° for the cobalt compound with Z=4. The crystal structure of these compounds consists of [M(HPO₃)F]⁻ anionic sheets. The layers are constructed from chains which contain [M₂O₆F₃] dimeric units linked by fluoride ions. The trans-1,4-diaminocyclohexane cations are placed in the interlayer space. The IR and Raman spectra show the bands corresponding to the phosphite oxoanion and organic dication. The Dq and Racah (B and C) parameters have been calculated from the diffuse reflectance spectra in the visible region. Dq parameter is 790 cm⁻¹ for compound (1). For phase (2) the Dq value is 725 cm⁻¹ and B and C are 930 and 4100 cm⁻¹, respectively. The thermal evolution of the molar magnetic susceptibilities of these compounds show maxima at 20.0 and 6.0 K for the iron(II) and cobalt(II) phases, respectively. These results indicate the existence of antiferromagnetic interactions in both compounds.     

A new layered organically templated iron(II) phosphite, (C2H10N2)[Fe3(HPO3)4]. Hydrothermal synthesis, crystal structure and spectroscopic and magnetic properties

The (C₂H₁₀N₂)[Fe₃(HPO₃)₄] compound has been synthesized by using mild hydrothermal conditions under autogeneous pressure and the ethylenediamine molecule as templating agent. The compound crystallizes in the triclinic space group with unit-cell parameters a=5.416(1), b=5.416(1), c=13.977(2) Å, α=80.64(2), β=85.25(1), γ=60.03(1)° and Z=1. The final R-factors were R₁=0.053 [wR₂=0.092]. The crystal structure is constructed of layers stacked along the c-axis. The sheets contain FeO₆ octahedra linked by (HPO₃)²⁻ phosphite oxoanions to give rise to Fe₃O₁₂ trimeric units sharing faces. The IR spectrum shows the characteristic bands of the phosphite and ethylenediammonium ions. From the diffuse reflectance spectrum, the Dq parameter of 805 cm⁻¹ has been calculated for the iron(II) cation in slightly distorted octahedral geometry. The Mössbauer spectrum exhibits two doublets characteristic of two crystallographically independent iron(II) ions in octahedral symmetry. Magnetic measurements indicate the existence of antiferromagnetic interactions.     

A new organically templated gallium(III)-doped chromium(III) fluorophosphite, (C2H10N2)[Ga0.98Cr0.02(HPO3)F3] hydrothermal synthesis, crystal structure and spectroscopic properties

A new organically templated fluoro-phosphite gallium(III)-doped chromium(III) with formula (C₂H₁₀N₂)[Ga_0.98Cr_0.02(HPO₃)F₃] has been synthesized by using mild hydrothermal conditions under autogeneous pressure. The crystal structure has been solved from X-ray single-crystal data. The compound crystallizes in the P2₁2₁2₁ orthorhombic space group, with the unit-cell parameters a=12.9417(7) Å, b=9.4027(6) Å, c=6.3502(4) Å and Z=4. The final R factors were R1=0.022 (all data) and wR2=0.050. The crystal structure consists of [Ga_0.98Cr_0.02(HPO₃)F₃]²⁻ anionic chains extended along the c-axis, with the ethylenediammonium cations placed in the cavities of the structure delimited by three different chains. The IR and Raman spectra show the characteristic bands of the phosphite oxoanion. The diffuse reflectance spectroscopy allowed us to calculate the Dq and Racah parameters of the Cr(III) cations in octahedral environment. The values are Dq=1375 cm⁻¹, B=780 cm⁻¹ and C=3420 cm⁻¹. The polycrystalline ESR spectra performed at X and Q-bands show the signals belonging to the diluted Cr(III) cation in this phase. From the fit of the X-band ESR spectrum at 4.2 K, the calculated values of the axial (D) and rhombic (E) distortion parameters are 0.075 and 0.042 cm⁻¹, respectively, the components of the g-tensor being g_x=1.98, g_y=1.99 and g_z=1.90.     

Mild hydrothermal synthesis, crystal structure, thermal behaviour, spectroscopic and magnetic properties of (NH4)0.80Li0.20[Fe(AsO4)F]

The (NH₄)_0.80Li_0.20[Fe(AsO₄)F] compound has been synthesized under mild hydrothermal conditions. The compound crystallize in the orthorhombic Pna2₁ space group, with cell parameters a=13.352(9), b=6.7049(9), c=10.943(2) Å and Z=8. The compound belongs to the KTiO(PO₄) structure type, with chains alternating FeO₄F₂ octahedra and AsO₄ tetrahedra, respectively, running along the “a” and “b” crystallographic axes. The diffuse reflectance spectrum in the visible region shows the forbidden electronic transitions characteristic of the Fe(III) d⁵-high spin cation in slightly distorted octahedral geometry. The Mössbauer spectrum at room temperature is characteristic of iron (III) cations. The ESR spectra, carried out from room temperature to 200 K, remain isotropic with variation in temperature; the g-value being 1.99(1). Magnetic measurements indicate the predominance of strong antiferromagnetic interactions.     

Ln2Sr2PtO7+δ (Ln=La, Pr, and Nd): Three new Pt-containing [AnBn−1O3n]-type hexagonal perovskites

Polycrystalline samples of Ln₂Sr₂PtO_7+δ (Ln=La, Pr, Nd) were prepared by conventional solid state synthesis. The three compounds are new examples for n=2 members of the [A_nB_n−1O_3n] family of hexagonal perovskites containing platinum as the B-type cation. XRD Rietveld refinements show the platinates to crystallize in space group and, in the case of Pr and Nd, revealed a complete ordering of Ln/Sr on the two distinct A-type positions, while for La a partial disorder was observed. By XANES investigations at the Pt-L_III threshold the oxidation state +4 for platinum was found. Thermogravimetry revealed a small oxygen excess for Ln=La and Pr (δ=0.13 and 0.07), pointing to the presence of peroxide ions as already observed for isostructural Ru- and Ir-based compounds. UV–Vis measurements were done for the yellow lanthanum and the green neodymium compound. They revealed two optical band gaps of 2.52 and 3.05 eV, respectively. Magnetic measurements showed La₂Sr₂PtO_7+δ to be diamagnetic as expected for Pt⁴⁺ with low-spin configuration. For Ln=Pr and Nd the observed strong paramagnetism can be explained solely by the magnetic moments of the rare earths.