79 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
Discrete Element Simulation of GasâSolid and GasâLiquidâSolid Flows
Multiphase flow (i.e., gasâsolid flow and gasâliquidâsolid
flow) extensively exists in industries, yet the strong coupling between
different phases poses challenges in the discrete element method (DEM)-based
model establishment. This work developed a fully coupled framework
by combining computational fluid dynamics (CFD) with DEM, with the
further extension to incorporate volume-of-fluid (VOF) to study multiphase
flow systems. A smoothing method is implemented to allow the grid
size to be close to or smaller than the diameter of the particles,
benefiting the subsequent interphase and interfacial interactions
calculation. Iso-Advector, an advanced VOF-based surface-capturing
method, is further introduced to describe interface evolution and
interfacial interactions effectively. The integrated model is verified
in three benchmark cases, i.e., a quasi-two-dimensional spouted bed,
a fully three-dimensional spout-fluid bed, and a dam-break flow. The
numerical results agree well with experimental measurements, confirming
the modelâs reliability in simulating multiphase flow systems
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
The phylogenetic tree based on 16S rDNA of strain Q3 and those of herbicide-degrading species.
<p>Q3 and other two quinclorac degrading bacteria, such as <i>Burkholderia cepacia</i> and <i>Bordetella petrii</i> are in different branches of the tree.</p
Effect of pH on degradation of quinclorac and growth of Q3.
<p>Both growth and quinclorac degradation of Q3 reached peak values at pH of 8.</p
Effect of initial quinclorac concentration on Q3 growth and degradation of quinclorac.
<p>Both growth and quinclorac degradation of Q3 reached peak values when initial quinclorac concentration was 20 mg/L.</p
Possible F4 quinclorac degradation products and pathways.
<p>Possible F4 quinclorac degradation products and pathways.</p
Morphological characteristics of strain Q3.
<p>Colony morphology on LB plate (left) and cell morphology under electron microscope (right).</p
Mass spectrum of quinclorac degradation products of Q3.
<p>The molecular formula of quinclorac and three degradation products are labeled.</p
Growth curve and degradation curve of F4 and <i>E coli</i> Top10 (control) after different culture timed durations.
<p>Growth curve and degradation curve of F4 and <i>E coli</i> Top10 (control) after different culture timed durations.</p
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