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Incommensurate crystal structure, thermal expansion study and magnetic properties of (dimethylimidazolium)2[Fe2Cl6(μ-O)]
Author(s) -
Fabio Scé,
Palmerina González-Izquierdo,
Israel Cano,
Garikoitz Beobide,
Óscar Fabelo,
Bruno J. C. Vieira,
João C. Waerenborgh,
Oriol Vallcorba,
Óscar Castillo,
Imanol de Pedro
Publication year - 2019
Publication title -
journal of physics materials
Language(s) - English
Resource type - Journals
ISSN - 2515-7639
DOI - 10.1088/2515-7639/ab423b
Subject(s) - thermal expansion , crystal structure , materials science , magnetic structure , condensed matter physics , crystallography , thermal , negative thermal expansion , chemistry , physics , thermodynamics , magnetization , metallurgy , magnetic field , quantum mechanics
A thorough characterization of the title compound, (dimim) 2 [Fe 2 Cl 6 ( μ -O)], consisting of a ( μ -oxido)-bridged binuclear iron(III) complex and 1,3-dimethylimiazolium (dimim) cation, has been performed using a wide range of techniques. The room temperature disordered crystal structure of this compound transits to an incommensurately modulated crystal structure at 100 K; to our knowledge, the first one found for an imidazolium halometallate complex. The crystal structure was solved in the superspace group P 1 ¯ (/ α / β / γ )0 with modulation vector q  = 0.1370(10)  0.0982(10)  0.326(2) at 100 K. Variable temperature synchrotron powder x-ray diffraction showed the presence of satellite peaks in addition to the main diffraction peaks up to 208 K. Furthermore, a thermal expansion study was performed with this technique from 100 to 383 K (near of its melting point) adressing questions about the nature and consequences of the ion self-assembly of this ( μ -oxido)-bridged binuclear iron(III) complex, as well as the molecular motion of the imidazolium cation within the crystalline structure as a response to the temperature effect. Finally, we present a deep magnetic study based on magnetic susceptibility, magnetization and Mössbauer measurements, where the strong antiferromagnetic exchange coupling detected is due to the occurrence of a μ -oxido bridge between the Fe(III), giving rise to an intra-dimeric antiferromagnetic exchange coupling of –308 cm −1 .

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