18 research outputs found
BibliografĂa
Reaction of the anion-deficient,
cation-ordered perovskite phase
Ba<sub>2</sub>YFeO<sub>5</sub> with 80 atm of oxygen pressure at 410
°C results in the formation of the Fe<sup>4+</sup> phase Ba<sub>2</sub>YFeO<sub>5.5</sub>. The topochemical insertion of oxide ions
lifts the inversion symmetry of the centrosymmetric host phase, Ba<sub>2</sub>YFeO<sub>5</sub> (space group <i>P</i>2<sub>1</sub>/<i>n</i>), to yield a noncentrosymmetric (NCS) phase Ba<sub>2</sub>YFeO<sub>5.5</sub> (space group <i>Pb</i>2<sub>1</sub><i>m</i> (No. 26), <i>a</i> = 12.1320(2) Ă
, <i>b</i> = 6.0606(1) Ă
, <i>c</i> = 8.0956(1) Ă
, <i>V</i> = 595.257(2) Ă
<sup>3</sup>) confirmed by the observation
of second-harmonic generation. Dielectric and PUND ferroelectric measurements,
however, show no evidence for a switchable ferroelectric polarization,
limiting the material to pyroelectric behavior. Magnetization and
low-temperature neutron diffraction data indicate that Ba<sub>2</sub>YFeO<sub>5.5</sub> undergoes a magnetic transition at 20 K to adopt
a state which exhibits a combination of ferromagnetic and antiferromagnetic
order. The symmetry breaking from centrosymmetric to polar noncentrosymmetric,
which occurs during the topochemical oxidation process is discussed
on the basis of induced lattice strain and an electronic instability
and represents a new strategy for the preparation of NCS materials
that readily incorporate paramagnetic transition metal centers
Structure and Magnetism of Sr<sub>3</sub>Co<sub>2</sub>O<sub>4</sub>Cl<sub>2</sub>î¸An Electronically Driven Lattice Distortion in an Oxychloride Containing Square Planar Co<sup>II</sup> Centers
Topochemical reduction of Sr<sub>3</sub>Co<sub>2</sub>O<sub>5</sub>Cl<sub>2</sub> with NaH at 200 °C yields Sr<sub>3</sub>Co<sub>2</sub>O<sub>4</sub>Cl<sub>2</sub>, a phase consisting
of infinite
double sheets of corner-linked Co<sup>II</sup>O<sub>4</sub> square
planes stacked with SrCl rocksalt layers. At 298 K, the structure
of Sr<sub>3</sub>Co<sub>2</sub>O<sub>4</sub>Cl<sub>2</sub> is described
in the tetragonal space group <i>I</i>4/<i>mmm</i> [<i>a</i> = 4.007(1) Ă
, <i>c</i> = 22.282(1)
Ă
]; however, on cooling below 200 K, the structure undergoes
a lattice distortion to adopt a structure with orthorhombic symmetry
in space group <i>Immm</i> [<i>a</i> = 3.9757(5)
Ă
, <i>b</i> = 4.0294(5) Ă
, and <i>c</i> = 22.147(3) Ă
at 5 K]. The structural distortion can be considered
JahnâTeller-like as it lifts the orbital degeneracy of the
square planar, d<sup>7</sup>, Co<sup>II</sup> centers, demonstrating
a strong coupling between the electronic configuration and the structural
lattice of this oxychloride phase. On cooling below 50 K, Sr<sub>3</sub>Co<sub>2</sub>O<sub>4</sub>Cl<sub>2</sub> adopts a canted antiferromagnetically
ordered state. All magnetization data show that the local cobalt moment
is much greater than would be expected for a simple spin-only <i>S</i> = <sup>3</sup>/<sub>2</sub> center, indicating a strong
orbital contribution to the magnetic behavior
Directed Lifting of Inversion Symmetry in RuddlesdenâPopper OxideâFluorides: Toward Ferroelectric and Multiferroic Behavior
The
cooperative tilting distortions of <i>n</i> = 2 RuddlesdenâPopper
oxides can be utilized to break the inversion symmetry of the host
lattice and induce ferroelectric behavior. Unfortunately the desired
a<sup>â</sup>a<sup>â</sup>c<sup>+</sup>/a<sup>â</sup>a<sup>â</sup>c<sup>+</sup> structural deformation is only
stabilized in phases with extremely small structural tolerance factors,
limiting the chemical scope of this symmetry breaking approach. Here
we describe the influence of topochemical fluorination on the structural
distortions of <i>n</i> = 2 RuddlesdenâPopper oxides
and demonstrate that the conversion of La<sub>3</sub>Ni<sub>2</sub>O<sub>7</sub> to La<sub>3</sub>Ni<sub>2</sub>O<sub>5.5</sub>F<sub>3.5</sub> breaks the inversion symmetry of the perovskite double
layers which constitute the RuddlesdenâPopper framework, by
driving a change from an a<sup>â</sup>a<sup>â</sup>c<sup>0</sup>/a<sup>â</sup>a<sup>â</sup>c<sup>0</sup> distortion
in the parent phase to an a<sup>â</sup>a<sup>â</sup>c<sup>+</sup>/a<sup>â</sup>a<sup>â</sup>-(c<sup>+</sup>) distortion in the oxideâfluoride. In this instance, the
symmetry breaking distortions of adjacent acentric perovskite sheets
are antialigned, and as a result the inversion symmetry of the host
lattice is broken locally, but not globally, resulting in an antiferroelectric
structure. The breaking of local inversion symmetry in layered perovskite
phases, in the absence of second-order JahnâTeller active âdistortion
centersâ, is an important step toward the realization of ferroelectric
and multiferroic behavior in phases of this structure type
Diamagnetic Ru<sup>2+</sup> in Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>10â<i>x</i></sub> (0 < <i>x</i> < 2): A Series of Complex Oxides Prepared by Topochemical Reduction
Reaction of the <i>n</i> = 3 RuddlesdenâPopper phase Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>10</sub> with a 5% H<sub>2</sub>/95% N<sub>2</sub> atmosphere between 300 and 900 °C leads to the formation of
phases of composition Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>10â<i>x</i></sub> (0 < <i>x</i> <
2) via topochemical reduction. Magnetization data collected from Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>10â<i>x</i></sub> samples in the range 0 < <i>x</i> < 1 show
a rapid decline in susceptibility with increasing <i>x</i>, consistent with the conversion of S = 1, Ru<sup>4+</sup> centers
at <i>x</i> = 0 to S = 0, Ru<sup>2+</sup> centers at <i>x</i> = 1. We believe this is the first report of diamagnetic
Ru<sup>2+</sup> centers in an extended oxide phase. Further reduction
of Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>9</sub> leads
to the reduction of Ti<sup>4+</sup> to Ti<sup>3+</sup>; however, Na<sub>2</sub>La<sub>2</sub>Ti<sub>2</sub>RuO<sub>10â<i>x</i></sub> samples in the range 1 < <i>x</i> < 2 exhibit
only a very weak paramagnetic response. Given the highly insulating
nature of the phases, this suggests the electrons added on reduction
of titanium are paired within a local TiâTi bonding network
in a manner analogous to that observed for Ti<sub><i>n</i></sub>O<sub>2<i>n</i>â1</sub> phases
K<sub>4</sub>Fe<sub>3</sub>F<sub>12</sub>: An Fe<sup>2+</sup>/Fe<sup>3+</sup> Charge-Ordered, Ferrimagnetic Fluoride with a Cation-Deficient, Layered Perovskite Structure
A new mixed-valence iron (Fe<sup>2+</sup>/Fe<sup>3+</sup>) fluoride material with a layered perovskite-related
structure has been synthesized and characterized. The material, K<sub>4</sub>Fe<sub>3</sub>F<sub>12</sub> [K<sub>4</sub>(Fe<sup>2+</sup>)Â(Fe<sup>3+</sup>)<sub>2</sub>F<sub>12</sub>], was synthesized using
mild hydrothermal conditions. The material exhibits a layered perovskite
structure consisting of alternating sheets of apex-linked Fe<sup>2+</sup>F<sub>6</sub> and Fe<sup>3+</sup>F<sub>6</sub> octahedra; thus, each
layer of Fe<sup>2+</sup>F<sub>6</sub> centers is sandwiched between
two layers of Fe<sup>3+</sup>F<sub>6</sub> centers. Magnetization
and neutron powder diffraction data show that, upon cooling below
120 K, K<sub>4</sub>Fe<sub>3</sub>F<sub>12</sub> adopts a magnetically
ordered state in which the Fe<sup>3+</sup> and Fe<sup>2+</sup> spins
are aligned in an approximately antiparallel manner to each other
to yield a pseudoferrimagnetic structure with a net spontaneous moment
of 5.41 Îź<sub>B</sub> per formula unit at 10 K. Crystal data:
K<sub>4</sub>Fe<sub>3</sub>F<sub>12</sub>, trigonal space group <i>R</i>3Ě
<i>m</i> (No. 166), <i>a</i> = <i>b</i> = 5.7649(9) Ă
, <i>c</i> = 28.086(9)
Ă
, <i>V</i> = 808.36(3) Ă
<sup>3</sup>, <i>Z</i> = 3, <i>T</i> = 296(2) K
Synthesis and Selective Topochemical Fluorination of the Cation and Anion-Vacancy Ordered phases Ba<sub>2</sub>YCoO<sub>5</sub> and Ba<sub>3</sub>YCo<sub>2</sub>O<sub>7.5</sub>
The synthesis and characterization
of two cation-ordered, anion-vacancy ordered phases, Ba<sub>2</sub>YCoO<sub>5</sub> and Ba<sub>3</sub>YCo<sub>2</sub>O<sub>7.5</sub>, is described. Neutron powder diffraction data reveal both phases
adopt structures in which octahedral Y<sup>3+</sup> and tetrahedral
Co<sup>3+</sup> centers are ordered within a âcubicâ
perovskite lattice. The unusual ordered pattern adopted by the cations
can be attributed to the large concentration of anion vacancies within
each phase. Reaction of Ba<sub>2</sub>YCoO<sub>5</sub> with CuF<sub>2</sub> under flowing oxygen topochemically inserts fluorine into
the host material to form Ba<sub>2</sub>YCoO<sub>5</sub>F<sub>0.42(1)</sub>. In contrast Ba<sub>2</sub>YCoO<sub>5</sub> does not intercalate
oxygen, even under high oxygen pressure. The selective insertion of
fluorine, but not oxygen, into Ba<sub>2</sub>YCoO<sub>5</sub> is discussed
and rationalized on the basis of the lattice strain of the resulting
oxidized materials. Magnetization and neutron diffraction data reveal
Ba<sub>3</sub>YCo<sub>2</sub>O<sub>7.5</sub> and Ba<sub>2</sub>YCoO<sub>5</sub>F<sub>0.42</sub> adopt antiferromagnetically ordered states
at low-temperature, while in contrast Ba<sub>2</sub>YCoO<sub>5</sub> shows no sign of long-range magnetic order
Ca<sub>2</sub>MnO<sub>3</sub>X (X = Cl, Br) Oxyhalides with 1âDimensional Ferromagnetic Chains of Square-Planar S = 2 Mn<sup>3+</sup>
Mixed anion oxyhalides with the formula Ca2MnO3X (X = Cl, Br) are synthesized using solid-state reaction
methods.
These two materials crystallize in a novel structure type due to the
small ionic radius of Ca and the strong JahnâTeller effect
of Mn3+. The resulting structure (space group Cmcm) contains one-dimensional chains of MnO4 square planes,
with an angle of âź120° between neighboring planes. At
low temperatures, the two materials adopt magnetic arrangements, with
ferromagnetic chains coupled antiferromagnetically. On applying a
magnetic field, both materials experience spin-flop transitions
Coupled Electronic and Magnetic Phase Transition in the Infinite-Layer Phase LaSrNiRuO<sub>4</sub>
Topochemical reduction
of the ordered double perovskite LaSrNiRuO<sub>6</sub> with CaH<sub>2</sub> yields LaSrNiRuO<sub>4</sub>, an extended oxide phase containing
infinite sheets of apex-linked, square-planar Ni<sup>1+</sup>O<sub>4</sub> and Ru<sup>2+</sup>O<sub>4</sub> units ordered in a checkerboard
arrangement. At room temperature the localized Ni<sup>1+</sup> (d<sup>9</sup>, <i>S</i> = <sup>1</sup>/<sub>2</sub>) and Ru<sup>2+</sup> (d<sup>6</sup>, <i>S</i> = 1) centers behave paramagnetically.
However, on cooling below 250 K the system undergoes a cooperative
phase transition in which the nickel spins align ferromagnetically,
while the ruthenium cations appear to undergo a change in spin configuration
to a diamagnetic spin state. Features of the low-temperature crystal
structure suggest a symmetry lowering JahnâTeller distortion
could be responsible for the observed diamagnetism of the ruthenium
centers
Cation Exchange in a 3D Perovskiteî¸Synthesis of Ni<sub>0.5</sub>TaO<sub>3</sub>
Reaction of NiCl<sub>2</sub> with
NaTaO<sub>3</sub> leads the formation of the perovskite phase Ni<sub>0.5</sub>TaO<sub>3</sub>, via a topochemical nickel-for-sodium cation
exchange in which the framework of apex-linked TaO<sub>6</sub> octahedra
present in the parent phase is retained. Neutron powder diffraction
data indicate Ni<sub>0.5</sub>TaO<sub>3</sub> adopts a structure analogous
to the paraelectric phase of LiTaO<sub>3</sub>, with triclinic <i>P</i>1Ě
crystallographic symmetry. Although Ni<sub>0.5</sub>TaO<sub>3</sub> has features which make it a good candidate phase
for magnetoelectric multiferroic behavior, the phase remains paramagnetic
in the temperature range 15 < <i>T</i> (K) < 300,
and detailed crystallographic characterization and analysis of SHG
activity indicate it retains a centrosymmetric structure down to the
lowest temperatures measured (5 K). Topochemical cation exchange reactions
of 3D perovskite oxides offer the opportunity to prepare a wide range
of novel metastable phases in a rational manner with a high degree
of synthetic control
Structural Modification of the Cation-Ordered RuddlesdenâPopper Phase YSr<sub>2</sub>Mn<sub>2</sub>O<sub>7</sub> by Cation Exchange and Anion Insertion
Calcium-for-strontium
cation substitution of the a<sup>â</sup>b<sup>0</sup>c<sup>0</sup>/b<sup>0</sup>a<sup>â</sup>c<sup>0</sup>-distorted,
cation-ordered, <i>n</i> = 2 RuddlesdenâPopper phase,
YSr<sub>2</sub>Mn<sub>2</sub>O<sub>7</sub>, leads to separation into
two phases, which both retain an a<sup>â</sup>b<sup>0</sup>c<sup>0</sup>/b<sup>0</sup>a<sup>â</sup>c<sup>0</sup>-distorted
framework and have the same stoichiometry but exhibit different degrees
of Y/Sr/Ca cation order. Increasing the calcium concentration to form
YSr<sub>0.5</sub>Ca<sub>1.5</sub>Mn<sub>2</sub>O<sub>7</sub> leads
to a change in the cooperative tilting on the MnO<sub>6</sub> units
to a novel a<sup>â</sup>b<sup>â</sup>c<sup>â</sup>/b<sup>â</sup>a<sup>â</sup>c<sup>â</sup> arrangement
described in space group <i>P</i>2<sub>1</sub>/<i>n</i>11. Low-temperature, topochemical fluorination of YSr<sub>2</sub>Mn<sub>2</sub>O<sub>7</sub> yields YSr<sub>2</sub>Mn<sub>2</sub>O<sub>5.5</sub>F<sub>3.5</sub>. In contrast to many other fluorinated <i>n</i> = 2 RuddlesdenâPopper oxide phases, YSr<sub>2</sub>Mn<sub>2</sub>O<sub>5.5</sub>F<sub>3.5</sub> retains the a<sup>â</sup>b<sup>0</sup>c<sup>0</sup>/b<sup>0</sup>a<sup>â</sup>c<sup>0</sup> lattice distortion and <i>P</i>4<sub>2</sub>/<i>mnm</i> space group symmetry of the parent oxide phase. The
resilience of the a<sup>â</sup>b<sup>0</sup>c<sup>0</sup>/b<sup>0</sup>a<sup>â</sup>c<sup>0</sup>-distorted framework of YSr<sub>2</sub>Mn<sub>2</sub>O<sub>7</sub> to resist symmetry-changing deformations
upon both cation substitution and anion insertion/exchange is discussed
on the basis the A-site cation order of the lattice and the large
change in the ionic radius of manganese upon oxidation from Mn<sup>3+</sup> to Mn<sup>4+</sup>. The structure property relations observed
in the YâSrâCaâMnâOâF system provide
insight into assisting in the synthesis of <i>n</i> = 2
RuddlesdenâPopper phases, which adopt cooperative structural
distortions that break the inversion symmetry of the extended lattice
and therefore act as a route for the preparation of ferroelectric
and multiferroic materials