5 research outputs found
Three Oxidation States of Manganese in the Barium Hexaferrite BaFe<sub>12â<i>x</i></sub>Mn<sub><i>x</i></sub>O<sub>19</sub>
The coexistence of three
valence states of Mn ions, namely, +2, +3, and +4, in substituted
magnetoplumbite-type BaFe<sub>12â<i>x</i></sub>Mn<sub><i>x</i></sub>O<sub>19</sub> was observed by soft X-ray
absorption spectroscopy at the Mn-L<sub>2,3</sub> edge. We infer that
the occurrence of multiple valence states of Mn situated in the pristine
purely ironÂ(III) compound BaFe<sub>12</sub>O<sub>19</sub> is made
possible by the fact that the charge disproportionation of Mn<sup>3+</sup> into Mn<sup>2+</sup> and Mn<sup>4+</sup> requires less energy
than that of Fe<sup>3+</sup> into Fe<sup>2+</sup> and Fe<sup>4+</sup>, related to the smaller effective Coulomb interaction of Mn<sup>3+</sup> (d<sup>4</sup>) compared to Fe<sup>3+</sup> (d<sup>5</sup>). The different chemical environments determine the location of
the differently charged ions: with Mn<sup>3+</sup> occupying positions
with (distorted) octahedral local symmetry, Mn<sup>4+</sup> ions prefer
octahedrally coordinated sites in order to optimize their covalent
bonding. Larger and more ionic bonded Mn<sup>2+</sup> ions with a
spherical charge distribution accumulate at tetrahedrally coordinated
sites. Simulations of the experimental Mn-L<sub>2,3</sub> XAS spectra
of two different samples with <i>x</i> = 1.5 and <i>x</i> = 1.7 led to Mn<sup>2+</sup>:Mn<sup>3+</sup>:Mn<sup>4+</sup> atomic ratios of 0.16:0.51:0.33 and 0.19:0.57:0.24
Intermediate-Valence Ytterbium Compound Yb<sub>4</sub>Ga<sub>24</sub>Pt<sub>9</sub>: Synthesis, Crystal Structure, and Physical Properties
The
title compound was synthesized by a reaction of the elemental educts
in a corundum crucible at 1200 °C under an Ar atmosphere. The
excess of Ga used in the initial mixture served as a flux for the
subsequent crystal growth at 600 °C. The crystal structure of
Yb<sub>4</sub>Ga<sub>24</sub>Pt<sub>9</sub> was determined from single-crystal
X-ray diffraction data: new prototype of crystal structure, space
group <i>C</i>2<i>/m</i>, Pearson symbol <i>mS</i>74, <i>a</i> = 7.4809(1) Ă
, <i>b</i> = 12.9546(2) Ă
, <i>c</i> = 13.2479(2) Ă
, β
= 100.879(1)°, <i>V</i> = 1260.82(6) Ă
<sup>3</sup>, <i>R</i><sub><i>F</i></sub> = 0.039 for 1781
observed reflections and 107 variable parameters. The structure is
described as an <i>ABABB</i> stacking of two slabs with
trigonal symmetry and compositions Yb<sub>4</sub>Ga<sub>6</sub> (<i>A</i>) and Ga<sub>12</sub>Pt<sub>6</sub> (<i>B</i>). The hard X-ray photoelectron spectrum (HAXPES) of Yb<sub>4</sub>Ga<sub>24</sub>Pt<sub>9</sub> shows both Yb<sup>2+</sup> and Yb<sup>3+</sup> contributions as evidence of an intermediate valence state
of ytterbium. The evaluated Yb valence of âź2.5 is in good agreement
with the results obtained from the magnetic susceptibility measurements.
The compound is a bad metallic conductor
Canted Antiferromagnetism on Rectangular Layers of Fe<sup>2+</sup> in Polymorphic CaFeSeO
From stoichiometric
amounts of CaO, Fe, and Se, pure powders and single crystals of quaternary Ca[FeSe2/2O2/2]â2 can be obtained by solid-state reaction and self-flux growth, respectively.
The as-synthesized compound exhibits a polymorphic crystal structure,
where the two modifications have different stacking sequences of [FeSe2/2O2/2]2ââ2 layers. The two polymorphs have similar unit cells
but different crystal symmetries (<i>Cmc</i>2<sub>1</sub> and <i>Pnma</i>), of which the former is non-centrosymmetric.
Fe is divalent (d<sup>6</sup>) and high-spin, as proven by X-ray spectroscopy,
MoĚssbauer spectroscopy, and powder neutron diffraction data.
The latter two, in combination with magnetic susceptibility and specific
heat data, reveal a long-range antiferromagnetic spin order (<i>T</i><sub>N</sub> = 160 K) with a minor spin canting. CaFeSeO
is an electronic insulator, as confirmed by resistivity measurements
and density functional theory calculations. The latter also suggest
a relatively small energy difference between the two polymorphs, explaining
their intimate intergrowth
Heteroepitaxy of Fe<sub>3</sub>O<sub>4</sub>/Muscovite: A New Perspective for Flexible Spintronics
Spintronics
has captured a lot of attention since it was proposed. It has been
triggering numerous research groups to make their efforts on pursuing
spin-related electronic devices. Recently, flexible and wearable devices
are in a high demand due to their outstanding potential in practical
applications. In order to introduce spintronics into the realm of
flexible devices, we demonstrate that it is feasible to grow epitaxial
Fe<sub>3</sub>O<sub>4</sub> film, a promising candidate for realizing
spintronic devices based on tunneling magnetoresistance, on flexible
muscovite. In this study, the heteroepitaxy of Fe<sub>3</sub>O<sub>4</sub>/muscovite is characterized by X-ray diffraction, high-resolution
transmission electron microscopy, and Raman spectroscopy. The chemical
composition and magnetic feature are investigated by a combination
of X-ray photoelectron spectroscopy and X-ray magnetic circular dichroism.
The electrical and magnetic properties are examined to show the preservation
of the primitive properties of Fe<sub>3</sub>O<sub>4</sub>. Furthermore,
various bending tests are performed to show the tunability of functionalities
and to confirm that the heterostructures retain the physical properties
under repeated cycles. These results illustrate that the Fe<sub>3</sub>O<sub>4</sub>/muscovite heterostructure can be a potential candidate
for the applications in flexible spintronics
A Complete High-to-Low spin state Transition of Trivalent Cobalt Ion in Octahedral Symmetry in SrCo<sub>0.5</sub>Ru<sub>0.5</sub>O<sub>3âδ</sub>
The complex metal oxide SrCo<sub>0.5</sub>Ru<sub>0.5</sub>O<sub>3âδ</sub> possesses a
slightly distorted perovskite
crystal structure. Its insulating nature infers a well-defined charge
distribution, and the six-fold coordinated transition metals have
the oxidation states +5 for ruthenium and +3 for cobalt as observed
by X-ray spectroscopy. We have discovered that Co<sup>3+</sup> ion
is purely high-spin at room temperature, which is unique for a Co<sup>3+</sup> in an octahedral oxygen surrounding. We attribute this to
the crystal field interaction being weaker than the Hundâs-rule
exchange due to a relatively large mean CoâO distances of 1.98(2)
Ă
, as obtained by EXAFS and X-ray diffraction experiments. A
gradual high-to-low spin state transition is completed by applying
high hydrostatic pressure of up to 40 GPa. Across this spin state
transition, the Co Kβ emission spectra can be fully explained
by a weighted sum of the high-spin and low-spin spectra. Thereby is
the much debated intermediate spin state of Co<sup>3+</sup> absent
in this material. These results allow us to draw an energy diagram
depicting relative stabilities of the high-, intermediate-, and low-spin
states as functions of the metalâoxygen bond length for a Co<sup>3+</sup> ion in an octahedral coordination