2 research outputs found

    Charge Transfer Induced Multifunctional Transitions with Sensitive Pressure Manipulation in a Metalā€“Organic Framework

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    The metalā€“organic framework {[FeĀ­(2,2ā€²-bipyridine)Ā­(CN)<sub>4</sub>]<sub>2</sub>CoĀ­(4,4ā€²-bipyridine)}Ā·4H<sub>2</sub>O (Fe<sub>2</sub>Co-MOF) with single-chain magnetism undergoes an intermetallic charge transfer that converts the Fe<sub>2</sub>Co charge/spin configurations from Fe<sup>3+</sup><sub>LS</sub>ā€“Co<sup>2+</sup><sub>HS</sub>ā€“Fe<sup>3+</sup><sub>LS</sub> to Fe<sup>2+</sup><sub>LS</sub>ā€“Co<sup>3+</sup><sub>LS</sub>ā€“Fe<sup>3+</sup><sub>LS</sub> (LS = low spin, HS = high spin) around 220 K under ambient pressure. A series of coherent phase transitions in structure, magnetism, permittivity and ferroelectricity are found to take place accompanying with the charge transfer, making Fe<sub>2</sub>Co-MOF a unique ferroelectric single-chain magnet at low temperature. Moreover, our detailed measurements of magnetization, dielectric constant, and Raman scattering under high pressures illustrate that the charge transfer as well as the resulting multifunctional transitions can be readily induced to occur at room temperature by applying a tiny external pressure of about 0.5 kbar. The present study thus provides a pressure well-controllable multifunctional material with potential applications in a broad temperature region across room temperature

    Aā€‘Site and Bā€‘Site Charge Orderings in an <i>sā€“d</i> Level Controlled Perovskite Oxide PbCoO<sub>3</sub>

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    Perovskite PbCoO<sub>3</sub> synthesized at 12 GPa was found to have an unusual charge distribution of Pb<sup>2+</sup>Pb<sup>4+</sup><sub>3</sub>Co<sup>2+</sup><sub>2</sub>Co<sup>3+</sup><sub>2</sub>O<sub>12</sub> with charge orderings in both the A and B sites of perovskite ABO<sub>3</sub>. Comprehensive studies using density functional theory (DFT) calculation, electron diffraction (ED), synchrotron X-ray diffraction (SXRD), neutron powder diffraction (NPD), hard X-ray photoemission spectroscopy (HAXPES), soft X-ray absorption spectroscopy (XAS), and measurements of specific heat as well as magnetic and electrical properties provide evidence of lead ion and cobalt ion charge ordering leading to Pb<sup>2+</sup>Pb<sup>4+</sup><sub>3</sub>Co<sup>2+</sup><sub>2</sub>Co<sup>3+</sup><sub>2</sub>O<sub>12</sub> quadruple perovskite structure. It is shown that the average valence distribution of Pb<sup>3.5+</sup>Co<sup>2.5+</sup>O<sub>3</sub> between Pb<sup>3+</sup>Cr<sup>3+</sup>O<sub>3</sub> and Pb<sup>4+</sup>Ni<sup>2+</sup>O<sub>3</sub> can be stabilized by tuning the energy levels of Pb 6<i>s</i> and transition metal 3<i>d</i> orbitals
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