Crystal and magnetic structure of the (trimim)[FeBr4] molten salt: a temperature dependence study
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González Izquierdo, Palmerina; Fabelo Rosa, Óscar; Cañadillas-Delgado, Laura; Beobide Pacheco, Garikoitz; Cano, Israel; Vallcorba, Oriol; Rodríguez Fernández, Jesús

Fecha
2021-06-01Derechos
© 2021. This manuscript version is made available under the CC-BY-NC-ND 4.0 license
Publicado en
Journal of Molecular Liquids, Volume 331, 1 June 2021, article 115716
Editorial
Elsevier Science
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Palabras clave
Crystal and magnetic structure
Halometallate molten salt
Magneto-structural correlations
Three-dimensional magnetic ordering
Resumen/Abstract
A new imidazolium-based halometallate complex with formula (trimim)[FeBr4] (trimim: 1,2,3-
trimethylimidazolium) has been synthesized and characterized as a function of the temperature. The structural
phase transitions, magnetic properties and magnetic structure of this compound have been thoroughly studied.
The crystal structure evolution from 1.8 to 400 K has been investigated by a combination of synchrotron X-ray
and neutron powder diffraction, as well as single crystal X-ray and neutron diffraction. Four different phases
were found: phase I, from 400 to 350 K, with the orthorhombic Cmc21 space group; phase II, from 350 to
160 K,whichwasmodelledwith themonoclinic P21/mspace group; and phase III, stable down to 13 K and showing the monoclinic Cm space group. The transition from phase III to II involves the appearance of disorder in the organic cations.Magnetometry measurements indicate a long-range magnetic order below13 K, whichwas confirmed by single crystal and powder neutron X-ray diffraction analyses. The occurrence of new reflections that were not possible to index with the phase III unit cell suggests a symmetry breaking, giving rise to the phase IV. A joint refinement (single-crystal and powder data) revealed that the latter phase exhibits the magnetic Shubnikov Ccc space group. Thismodel consists of a strictly antiferromagnetic structure with ferromagnetic interactions within the unit cell, which is compatible with the magnetometry results.
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