21 research outputs found
PbMn(IV)TeO<sub>6</sub>: A New Noncentrosymmetric Layered Honeycomb Magnetic Oxide
PbMnTeO<sub>6</sub>, a new noncentrosymmetric
layered magnetic oxide was synthesized and characterized. The crystal
structure is hexagonal, with space group <i>P</i>6̅2<i>m</i> (No. 189), and consists of edge-sharing (Mn<sup>4+</sup>/Te<sup>6+</sup>)O<sub>6</sub> trigonal prisms that form honeycomb-like
two-dimensional layers with Pb<sup>2+</sup> ions between the layers.
The structural difference between PbMnTeO<sub>6</sub>, with disordered/trigonal
prisms of Mn<sup>4+</sup>/Te<sup>6+</sup>, versus the similar chiral
SrGeTeO<sub>6</sub> (space group <i>P</i>312), with long-range
order of Ge<sup>4+</sup> and Te<sup>6+</sup> in octahedral coordination,
is attributed to a difference in the electronic effects of Ge<sup>4+</sup> and Mn<sup>4+</sup>. Temperature-dependent second harmonic
generation by PbMnTeO<sub>6</sub> confirmed the noncentrosymmetric
character between 12 and 873 K. Magnetic measurements indicated antiferromagnetic
order at <i>T</i><sub>N</sub> ≈ 20 K and a frustration
parameter (|θ|/<i>T</i><sub>N</sub>) of ∼2.16
Structure and Magnetic Behavior of Layered Honeycomb Tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn, Fe)
New
layered honeycomb tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn,
Fe) were synthesized and characterized. BiM(III)TeO<sub>6</sub> (M
= Cr, Fe) species crystallize in a trigonal space group, <i>P</i>3̅1<i>c</i> (No. 163), of edge-sharing M<sup>3+</sup>/Te<sup>6+</sup>O<sub>6</sub> octahedra, which form honeycomb-like
double layers in the <i>ab</i> plane with Bi<sup>3+</sup> cations located between the layers. Interestingly, the structure
of BiMnTeO<sub>6</sub> is similar to those of the Cr/Fe analogues,
but with monoclinic space group, <i>P</i>2<sub>1</sub>/<i>c</i> (No. 14), attributed to the strong Jahn–Teller
distortion of Mn<sup>3+</sup> cations. The crystal structure of BiM(III)TeO<sub>6</sub> is a superstructure of PbSb<sub>2</sub>O<sub>6</sub>-related
materials (ABB′O<sub>6</sub>). The Cr<sup>3+</sup> and Fe<sup>3+</sup> cations are ordered 80% and 90%, respectively, while the
Mn<sup>3+</sup> ions are completely ordered on the B-site of the ABB′O<sub>6</sub> structure. BiCrTeO<sub>6</sub> shows a broad antiferromagnetic
transition (AFM) at ∼17 K with a Weiss temperature (θ)
of −59.85 K, while BiFeTeO<sub>6</sub> and BiMnTeO<sub>6</sub> show sharp AFM transitions at ∼11 K with θ of −27.56
K and at ∼9.5 K with θ of −17.57 K, respectively.
These differences in the magnetic behavior are ascribed to the different
concentration of magnetic nearest versus next-nearest neighbor interactions
of magnetic cations due to the relative differences in the extent
of M/Te ordering
PbMn(IV)TeO<sub>6</sub>: A New Noncentrosymmetric Layered Honeycomb Magnetic Oxide
PbMnTeO<sub>6</sub>, a new noncentrosymmetric
layered magnetic oxide was synthesized and characterized. The crystal
structure is hexagonal, with space group <i>P</i>6̅2<i>m</i> (No. 189), and consists of edge-sharing (Mn<sup>4+</sup>/Te<sup>6+</sup>)O<sub>6</sub> trigonal prisms that form honeycomb-like
two-dimensional layers with Pb<sup>2+</sup> ions between the layers.
The structural difference between PbMnTeO<sub>6</sub>, with disordered/trigonal
prisms of Mn<sup>4+</sup>/Te<sup>6+</sup>, versus the similar chiral
SrGeTeO<sub>6</sub> (space group <i>P</i>312), with long-range
order of Ge<sup>4+</sup> and Te<sup>6+</sup> in octahedral coordination,
is attributed to a difference in the electronic effects of Ge<sup>4+</sup> and Mn<sup>4+</sup>. Temperature-dependent second harmonic
generation by PbMnTeO<sub>6</sub> confirmed the noncentrosymmetric
character between 12 and 873 K. Magnetic measurements indicated antiferromagnetic
order at <i>T</i><sub>N</sub> ≈ 20 K and a frustration
parameter (|θ|/<i>T</i><sub>N</sub>) of ∼2.16
Low-Temperature Vaterite-Type LuBO<sub>3</sub>, a Vacancy-Stabilized Phase Synthesized at High Temperature
Low-temperature
vaterite-type LuBO<sub>3</sub> (π-LBO) was prepared by a solid-state
reaction method at high temperature. The reasoning of the existence
of vacancy-stabilized π-LBO was investigated for the first time
using neutron diffraction patterns, Fourier transform infrared (FT-IR)
spectra, and high-resolution transmission electron microscopy. The
results clearly demonstrated that the B and O vacancies in π-LBO
came into being during the heating process. The existence of an open
B<sub>3</sub>O<sub>9</sub> ring consisting of BO<sub>3</sub> and BO<sub>4</sub> units in π-LBO due to the B and O vacancies was demonstrated
by FT-IR. The vacuum ultraviolet–ultraviolet spectroscopic
properties of π-LBO were studied in detail. In addition, the
luminescence mechanism of Ce<sup>3+</sup> in π-LBO was put forward
and discussed with that of calcite-type LuBO<sub>3</sub> (β-LBO)
Structure and Magnetic Behavior of Layered Honeycomb Tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn, Fe)
New
layered honeycomb tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn,
Fe) were synthesized and characterized. BiM(III)TeO<sub>6</sub> (M
= Cr, Fe) species crystallize in a trigonal space group, <i>P</i>3̅1<i>c</i> (No. 163), of edge-sharing M<sup>3+</sup>/Te<sup>6+</sup>O<sub>6</sub> octahedra, which form honeycomb-like
double layers in the <i>ab</i> plane with Bi<sup>3+</sup> cations located between the layers. Interestingly, the structure
of BiMnTeO<sub>6</sub> is similar to those of the Cr/Fe analogues,
but with monoclinic space group, <i>P</i>2<sub>1</sub>/<i>c</i> (No. 14), attributed to the strong Jahn–Teller
distortion of Mn<sup>3+</sup> cations. The crystal structure of BiM(III)TeO<sub>6</sub> is a superstructure of PbSb<sub>2</sub>O<sub>6</sub>-related
materials (ABB′O<sub>6</sub>). The Cr<sup>3+</sup> and Fe<sup>3+</sup> cations are ordered 80% and 90%, respectively, while the
Mn<sup>3+</sup> ions are completely ordered on the B-site of the ABB′O<sub>6</sub> structure. BiCrTeO<sub>6</sub> shows a broad antiferromagnetic
transition (AFM) at ∼17 K with a Weiss temperature (θ)
of −59.85 K, while BiFeTeO<sub>6</sub> and BiMnTeO<sub>6</sub> show sharp AFM transitions at ∼11 K with θ of −27.56
K and at ∼9.5 K with θ of −17.57 K, respectively.
These differences in the magnetic behavior are ascribed to the different
concentration of magnetic nearest versus next-nearest neighbor interactions
of magnetic cations due to the relative differences in the extent
of M/Te ordering
Structure and Magnetic Behavior of Layered Honeycomb Tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn, Fe)
New
layered honeycomb tellurates, BiM(III)TeO<sub>6</sub> (M = Cr, Mn,
Fe) were synthesized and characterized. BiM(III)TeO<sub>6</sub> (M
= Cr, Fe) species crystallize in a trigonal space group, <i>P</i>3̅1<i>c</i> (No. 163), of edge-sharing M<sup>3+</sup>/Te<sup>6+</sup>O<sub>6</sub> octahedra, which form honeycomb-like
double layers in the <i>ab</i> plane with Bi<sup>3+</sup> cations located between the layers. Interestingly, the structure
of BiMnTeO<sub>6</sub> is similar to those of the Cr/Fe analogues,
but with monoclinic space group, <i>P</i>2<sub>1</sub>/<i>c</i> (No. 14), attributed to the strong Jahn–Teller
distortion of Mn<sup>3+</sup> cations. The crystal structure of BiM(III)TeO<sub>6</sub> is a superstructure of PbSb<sub>2</sub>O<sub>6</sub>-related
materials (ABB′O<sub>6</sub>). The Cr<sup>3+</sup> and Fe<sup>3+</sup> cations are ordered 80% and 90%, respectively, while the
Mn<sup>3+</sup> ions are completely ordered on the B-site of the ABB′O<sub>6</sub> structure. BiCrTeO<sub>6</sub> shows a broad antiferromagnetic
transition (AFM) at ∼17 K with a Weiss temperature (θ)
of −59.85 K, while BiFeTeO<sub>6</sub> and BiMnTeO<sub>6</sub> show sharp AFM transitions at ∼11 K with θ of −27.56
K and at ∼9.5 K with θ of −17.57 K, respectively.
These differences in the magnetic behavior are ascribed to the different
concentration of magnetic nearest versus next-nearest neighbor interactions
of magnetic cations due to the relative differences in the extent
of M/Te ordering
Metastable γ‑Li<sub>2</sub>TiTeO<sub>6</sub>: Negative Chemical Pressure Interception and Polymorph Tuning of SHG
Intercepting
metastable phases by chemical approaches is an important
solution to explore structural varieties of functional materials under
positive/negative pressure, as paradigmatically exemplified by the
polymorph modification in Li2TiTeO6. Here, we
stabilized a novel metastable Li2TiTeO6 (denoted
as γ-phase) in the ordered-ilmenite-type R3 via facile topotactic reaction from Na2TiTeO6, which was found to crystallize in R3 instead
of the reported R3̅ structure. The calculated
equilibrium volume of γ-Li2TiTeO6 is larger than that of the ground-state Pnn2-Li2TiTeO6 (denoted as α-phase), indicating that γ-Li2TiTeO6 can only be stabilized under “negative pressure”
quantified to be around −6 GPa. The γ-phase irreversibly transforms into the α-phase
around 560 °C under ambient pressure, accompanied by a steep
increase (∼500 times) of the second harmonic generation (SHG),
indicating a potential application of γ-Li2TiTeO6 as an optical thermometer. These findings
elegantly show that chemical pressure as well as physical pressure
is powerful to tune the polymorphs for metastable phases and exotic
properties as paradigmatically exemplified by Li2TiTeO6, which undergoes consecutive polymorph tuning of γ (−6 GPa), α (0 GPa), β (6 GPa, R3-Ni3TeO6 type), and δ (40 GPa, predicted P21/n double perovskite) phases with densified atomic packing
Metastable γ‑Li<sub>2</sub>TiTeO<sub>6</sub>: Negative Chemical Pressure Interception and Polymorph Tuning of SHG
Intercepting
metastable phases by chemical approaches is an important
solution to explore structural varieties of functional materials under
positive/negative pressure, as paradigmatically exemplified by the
polymorph modification in Li2TiTeO6. Here, we
stabilized a novel metastable Li2TiTeO6 (denoted
as γ-phase) in the ordered-ilmenite-type R3 via facile topotactic reaction from Na2TiTeO6, which was found to crystallize in R3 instead
of the reported R3̅ structure. The calculated
equilibrium volume of γ-Li2TiTeO6 is larger than that of the ground-state Pnn2-Li2TiTeO6 (denoted as α-phase), indicating that γ-Li2TiTeO6 can only be stabilized under “negative pressure”
quantified to be around −6 GPa. The γ-phase irreversibly transforms into the α-phase
around 560 °C under ambient pressure, accompanied by a steep
increase (∼500 times) of the second harmonic generation (SHG),
indicating a potential application of γ-Li2TiTeO6 as an optical thermometer. These findings
elegantly show that chemical pressure as well as physical pressure
is powerful to tune the polymorphs for metastable phases and exotic
properties as paradigmatically exemplified by Li2TiTeO6, which undergoes consecutive polymorph tuning of γ (−6 GPa), α (0 GPa), β (6 GPa, R3-Ni3TeO6 type), and δ (40 GPa, predicted P21/n double perovskite) phases with densified atomic packing
Metastable γ‑Li<sub>2</sub>TiTeO<sub>6</sub>: Negative Chemical Pressure Interception and Polymorph Tuning of SHG
Intercepting
metastable phases by chemical approaches is an important
solution to explore structural varieties of functional materials under
positive/negative pressure, as paradigmatically exemplified by the
polymorph modification in Li2TiTeO6. Here, we
stabilized a novel metastable Li2TiTeO6 (denoted
as γ-phase) in the ordered-ilmenite-type R3 via facile topotactic reaction from Na2TiTeO6, which was found to crystallize in R3 instead
of the reported R3̅ structure. The calculated
equilibrium volume of γ-Li2TiTeO6 is larger than that of the ground-state Pnn2-Li2TiTeO6 (denoted as α-phase), indicating that γ-Li2TiTeO6 can only be stabilized under “negative pressure”
quantified to be around −6 GPa. The γ-phase irreversibly transforms into the α-phase
around 560 °C under ambient pressure, accompanied by a steep
increase (∼500 times) of the second harmonic generation (SHG),
indicating a potential application of γ-Li2TiTeO6 as an optical thermometer. These findings
elegantly show that chemical pressure as well as physical pressure
is powerful to tune the polymorphs for metastable phases and exotic
properties as paradigmatically exemplified by Li2TiTeO6, which undergoes consecutive polymorph tuning of γ (−6 GPa), α (0 GPa), β (6 GPa, R3-Ni3TeO6 type), and δ (40 GPa, predicted P21/n double perovskite) phases with densified atomic packing
Designing Polar and Magnetic Oxides: Zn<sub>2</sub>FeTaO<sub>6</sub> - in Search of Multiferroics
Polar oxides are technically of great
interest but difficult to
prepare. Our recent discoveries predicted that polar oxides can be
synthesized in the corundum-derivative A<sub>2</sub>BB′O<sub>6</sub> family with unusually small cations at the A-site and a d<sup>0</sup> electron configuration ion at B′-site. When magnetic
transition-metal ions are incorporated more interesting polar magnetic
oxides can form. In this work we experimentally verified this prediction
and prepared LiNbO<sub>3</sub> (LN)-type polar magnetic Zn<sub>2</sub>FeTaO<sub>6</sub> via high pressure and temperature synthesis. The
crystal structure analysis indicates highly distorted ZnO<sub>6</sub> and (Fe/Ta)O<sub>6</sub> octahedra, and an estimated spontaneous
polarization (<i>P</i><sub>S</sub>) of ∼50 μC/cm<sup>2</sup> along the <i>c</i>-axis was obtained from point
charge model calculations. Zn<sub>2</sub>Fe<sup>3+</sup>Ta<sup>5+</sup>O<sub>6</sub> has a lower magnetic transition temperature (<i>T</i><sub><i>N</i></sub> ∼ 22 K) than the Mn<sub>2</sub>FeTaO<sub>6</sub> analogue but is less conductive. The dielectric
and polarization measurements indicate a potentially switchable component