2 research outputs found
Charge Transfer Induced Multifunctional Transitions with Sensitive Pressure Manipulation in a MetalāOrganic Framework
The
metalāorganic framework {[FeĀ(2,2ā²-bipyridine)Ā(CN)<sub>4</sub>]<sub>2</sub>CoĀ(4,4ā²-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>āCo<sup>2+</sup><sub>HS</sub>āFe<sup>3+</sup><sub>LS</sub> to Fe<sup>2+</sup><sub>LS</sub>āCo<sup>3+</sup><sub>LS</sub>āFe<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
AāSite and BāSite Charge Orderings in an <i>sād</i> Level Controlled Perovskite Oxide PbCoO<sub>3</sub>
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