4 research outputs found
Mo<sup>6+</sup> Cation Enrichment of the Structure Chemistry of Iodates: Syntheses, Structures, and Calculations of Ba(MoO<sub>2</sub>)<sub>2</sub>(IO<sub>3</sub>)<sub>4</sub>O, Ba<sub>3</sub>[(MoO<sub>2</sub>)<sub>2</sub>(IO<sub>3</sub>)<sub>4</sub>O(OH)<sub>4</sub>]Ā·2H<sub>2</sub>O, and Sr[(MoO<sub>2</sub>)<sub>6</sub>(IO<sub>4</sub>)<sub>2</sub>O<sub>4</sub>]Ā·H<sub>2</sub>O
The three metal iodates BaĀ(MoO<sub>2</sub>)<sub>2</sub>(IO<sub>3</sub>)<sub>4</sub>O (<b>1</b>), Ba<sub>3</sub>[(MoO<sub>2</sub>)<sub>2</sub>(IO<sub>3</sub>)<sub>4</sub>OĀ(OH)<sub>4</sub>]Ā·2H<sub>2</sub>O (<b>2</b>),
and SrĀ[(MoO<sub>2</sub>)<sub>6</sub>(IO<sub>4</sub>)<sub>2</sub>O<sub>4</sub>]Ā·H<sub>2</sub>O (<b>3</b>) have been successfully
synthesized by introducing second-order
JahnāTeller distorted Mo<sup>6+</sup> cations by a mild hydrothermal
method. Single-crystal X-ray diffraction (XRD) was used to determine
the structures of the three title compounds. In compound <b>1</b>, the [Mo<sub>2</sub>O<sub>11</sub>]<sup>10ā</sup> dimers
connect with the [IO<sub>3</sub>]<sup>ā</sup> units by sharing
oxygen atoms to form two-dimensional (2D) layers that are separated
by the Ba<sup>2+</sup> cations. For comparison, the [Mo<sub>2</sub>O<sub>11</sub>]<sup>10ā</sup> dimers and the [IO<sub>3</sub>]<sup>ā</sup> units are isolated in compound <b>2</b>, and they are connected by the [BaO<sub>11</sub>]<sup>20ā</sup> polyhedra forming a 3D network. For compound <b>3</b>, the
[MoO<sub>6</sub>]<sup>6ā</sup> polyhedra link with each other
by corner and edge sharing to build 2D corrugated layers with tunnels
containing isolated [IO<sub>4</sub>]<sup>3ā</sup> units. The
[SrO<sub>9</sub>]<sup>16ā</sup> polyhedra link the 2D corrugated
layers to form a 3D network. The infrared (IR) spectra, the ultravioletāvisibleānear-infrared
(UVāvisāNIR) diffuse reflectance spectra, and thermal
stabilities of compounds <b>1</b> and <b>2</b> are presented.
In addition, the theoretical calculations are also carried out to
evaluate their band gaps and density of states
Expanding Frontiers of Ultraviolet Nonlinear Optical Materials with Fluorophosphates
If
a bucket is to hold more water, its shortest plank must be made
longer. This guideline also applies to the exploration of ultraviolet
(UV) and deep-UV (DUV) nonlinear optical (NLO) materials that are
limited by multiple criteria. Phosphates are one kind of promising
candidate for new NLO materials. Unfortunately, the small birefringence,
as the shortest plank, severely restricts the phase-matching of second
harmonic generation (SHG) in the UV/DUV region. In this work, fluorophosphates
are rationally proposed as substitutes for phosphates to break down
the limitation of birefringence and simultaneously enhance SHG response
and retain wide UV transmittance. The (PO<sub>3</sub>F)<sup>2ā</sup> and (PO<sub>2</sub>F<sub>2</sub>)<sup>ā</sup> groups are
confirmed as superior material genomes to achieve the discussed combination
properties. Accordingly, (NH<sub>4</sub>)<sub>2</sub>PO<sub>3</sub>F was screened out by density functional theory calculation, and
single crystals with centimeter size have been grown. It possesses
a powder SHG efficiency of 1 Ć KH<sub>2</sub>PO<sub>4</sub> (KDP)
and is phase-matchable with output of SHG wavelength at 266 nm. To
the best of our knowledge, it is the first time that fluorophosphates
are identified and developed as new and ideal candidates to new UV/DUV
NLO materials by combining theories and experiments
Expanding Frontiers of Ultraviolet Nonlinear Optical Materials with Fluorophosphates
If
a bucket is to hold more water, its shortest plank must be made
longer. This guideline also applies to the exploration of ultraviolet
(UV) and deep-UV (DUV) nonlinear optical (NLO) materials that are
limited by multiple criteria. Phosphates are one kind of promising
candidate for new NLO materials. Unfortunately, the small birefringence,
as the shortest plank, severely restricts the phase-matching of second
harmonic generation (SHG) in the UV/DUV region. In this work, fluorophosphates
are rationally proposed as substitutes for phosphates to break down
the limitation of birefringence and simultaneously enhance SHG response
and retain wide UV transmittance. The (PO<sub>3</sub>F)<sup>2ā</sup> and (PO<sub>2</sub>F<sub>2</sub>)<sup>ā</sup> groups are
confirmed as superior material genomes to achieve the discussed combination
properties. Accordingly, (NH<sub>4</sub>)<sub>2</sub>PO<sub>3</sub>F was screened out by density functional theory calculation, and
single crystals with centimeter size have been grown. It possesses
a powder SHG efficiency of 1 Ć KH<sub>2</sub>PO<sub>4</sub> (KDP)
and is phase-matchable with output of SHG wavelength at 266 nm. To
the best of our knowledge, it is the first time that fluorophosphates
are identified and developed as new and ideal candidates to new UV/DUV
NLO materials by combining theories and experiments
Control of Ionic Conductivity by Lithium Distribution in Cubic Oxide Argyrodites Li<sub>6+<i>x</i></sub>P<sub>1ā<i>x</i></sub>Si<sub><i>x</i></sub>O<sub>5</sub>Cl
Argyrodite is a key structure type for ion-transporting
materials.
Oxide argyrodites are largely unexplored despite sulfide argyrodites
being a leading family of solid-state lithium-ion conductors, in which
the control of lithium distribution over a wide range of available
sites strongly influences the conductivity. We present a new cubic
Li-rich (>6 Li+ per formula unit) oxide argyrodite Li7SiO5Cl that crystallizes with an ordered cubic
(P213) structure at room temperature,
undergoing a transition at 473 K to a Li+ site disordered F4Ģ
3m structure, consistent with
the symmetry adopted by superionic sulfide argyrodites. Four different
Li+ sites are occupied in Li7SiO5Cl (T5, T5a, T3, and T4), the combination of which is previously
unreported for Li-containing argyrodites. The disordered F4Ģ
3m structure is stabilized to room temperature
via substitution of Si4+ with P5+ in Li6+xP1āxSixO5Cl (0.3 x < 0.85) solid solution. The resulting delocalization
of Li+ sites leads to a maximum ionic conductivity of 1.82(1)
Ć 10ā6 S cmā1 at x = 0.75, which is 3 orders of magnitude higher than the
conductivities reported previously for oxide argyrodites. The variation
of ionic conductivity with composition in Li6+xP1āxSixO5Cl is directly connected to structural changes
occurring within the Li+ sublattice. These materials present
superior atmospheric stability over analogous sulfide argyrodites
and are stable against Li metal. The ability to control the ionic
conductivity through structure and composition emphasizes the advances
that can be made with further research in the open field of oxide
argyrodites