21 research outputs found

    PbMn(IV)TeO<sub>6</sub>: A New Noncentrosymmetric Layered Honeycomb Magnetic Oxide

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    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)

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    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

    No full text
    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

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    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)

    No full text
    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)

    No full text
    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

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    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

    No full text
    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

    No full text
    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

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    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
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