11 research outputs found
Metastable (Bi, M)<sub>2</sub>(Fe, Mn, Bi)<sub>2</sub>O<sub>6+<i>x</i></sub> (M = Na or K) Pyrochlores from Hydrothermal Synthesis
The hydrothermal
syntheses, structures, and magnetism of two new pyrochlore oxides
of compositions (Na<sub>0.60</sub>Bi<sub>1.40</sub>)Ā(Fe<sub>1.06</sub>Mn<sub>0.17</sub>Bi<sub>0.77</sub>)ĀO<sub>6.87</sub> and
(K<sub>0.24</sub>Bi<sub>1.51</sub>)Ā(Fe<sub>1.07</sub>Mn<sub>0.15</sub>Bi<sub>0.78</sub>)ĀO<sub>6.86</sub> are described. With
preparation at 200 Ā°C for 6 h in solutions of sodium or potassium
hydroxide, the alkali metals introduced from these mineralizers are
essential to the synthesis of the phases. The average long-range order
of the pyrochlore structure, with space group <i>Fd</i>3Ģ
<i>m</i>, was investigated and refined against X-ray and neutron
diffraction data, and it was shown that disorder is present in both
the metal and coordinating oxygen positions, along with metal-mixing
across both the A and B sites of the structure. XANES analysis confirms
the presence of Mn<sup>4+</sup>, mixed valence Bi<sup>3+</sup> and
Bi<sup>5+</sup>, and Fe<sup>3+</sup>, the last also verified by <sup>57</sup>Fe MoĢssbauer spectroscopy. Magnetic measurements show
a lack of long-range magnetic ordering that is typical of geometrically
frustrated pyrochlores. The observed glasslike interactions occur
at low temperatures, with the onset temperature depending upon the
magnitude of the applied external field. Variable temperature X-ray
diffraction shows that these pyrochlores are metastable and collapse
on heating at ca. 395 Ā°C, which suggests that their formation
by conventional solid-state synthesis would be impossible
Nanocomposite PyriteāGreigite Reactivity toward Se(IV)/Se(VI)
A nanopyrite/greigite composite was synthesized by reacting
FeCl<sub>3</sub> and NaHS in a ratio of 1:2 (Wei et al. 1996). Following
this
procedure, the obtained solid phases consisted of 30ā50 nm
sized particles containing 28% of greigite (Fe<sup>2+</sup>Fe<sup>3+</sup><sub>2</sub>S<sub>4</sub>) and 72% pyrite (FeS<sub>2</sub>). Batch reactor experiments were performed with selenite or selenate
by equilibrating suspensions containing the nanosized pyriteāgreigite
solid phase at different pH-values and with or without the addition
of extra Fe<sup>2+</sup>. XANES-EXAFS spectroscopic techniques revealed,
for the first time, the formation of ferroselite (FeSe<sub>2</sub>) as the predominant reaction product, along with elemental Se. In
the present experimental conditions, at pH 6 and in equilibrium with
Se<sup>0</sup>, the solution is oversaturated with respect to ferrosilite.
Furthermore, thermodynamic computations show that reaction kinetics
likely played a significant role in our experimental system
Systematic Study of Exchange Coupling in CoreāShell Fe<sub>3āĪ“</sub>O<sub>4</sub>@CoO Nanoparticles
Although single magnetic domain nanoparticles
are very promising
for many applications, size reduction usually results in low magnetic
anisotropy and unblocked domain at room temperature, e.g., superparamagnetism.
An alternative approach is coreāshell nanoparticles featured
by exchange bias coupling between ferroĀ(i)Āmagnetic [FĀ(i)ĀM] and antiferromagnetic
(AFM) phases. Although exchange bias coupling has been reported for
very diverse coreāshell nanoparticles, it is difficult to compare
these studies to rationalize the effect of many structural parameters
on the magnetic properties. Herein, we report on a systematic study
which consists of the modulation of the shell structure and its influence
on the exchange bias coupling. A series of Fe<sub>3āĪ“</sub>O<sub>4</sub>@CoO coreāshell nanoparticles has been synthesized
by seed-mediated growth based on the thermal decomposition technique.
The variation of Co reactant concentration resulted in the modulation
of the shell structure for which thickness, crystallinity, and interface
with the iron oxide core strongly affect the magnetic properties.
The thickest CoO shell and the largest FĀ(i)ĀM/AFM interface led to
the largest exchange bias coupling. Very high values of coercive field
(19āÆ000 Oe) and <i>M</i><sub>R</sub>/<i>M</i><sub>S</sub> ratio (0.86) were obtained. The most stricking results
consist of the increase of the coercive field while exchange field
vanishes when the CoO thickness decreases: it is ascribed to the diffusion
of Co species in the surface layer of iron oxide which generates to
some extent cobalt ferrite and induces hard/soft exchange coupling
between ferrimagnetic phases
Evidence of New Fluorinated Coordination Compounds in the Composition Space Diagram of FeF<sub>3</sub>/ZnF<sub>2</sub>āH<i>amtetraz</i>-HF<sub>aq</sub> System
The
exploration of the composition space diagram of the FeF<sub>3</sub>/ZnF<sub>2</sub>āH<i>amtetraz</i>-HF<sub>aq</sub> system (H<i>amtetraz</i> = 5-aminotetrazole) by solvothermal
synthesis at 160 Ā°C for 72 h in dimethylformamide (DMF) has evidenced
five new hybrid fluorides (<b>1</b>ā<b>5</b>);
the structures are characterized from single crystal X-ray diffraction
data. [H<i>dma</i>]ĀĀ·(ZnFe<sup>III</sup>(H<sub>2</sub>O)<sub>4</sub>F<sub>6</sub>) (<b>1</b>) and [H<i>dma</i>]ĀĀ·[H<i>gua</i>]<sub>2</sub>ĀĀ·(Fe<sup>III</sup>F<sub>6</sub>) (<b>2</b>) contain anionic inorganic
chains (<b>1</b>) or isolated octahedra (<b>2</b>) weakly
hydrogen bonded (Class I hybrids) to dimethylammonium (H<i>dma</i>) and/or guanidinium (H<i>gua</i>) cations which are produced
from the tetrazole ligand and solvent decomposition. [H<i>dma</i>]<sub>2</sub>ĀĀ·[H<i>gua</i>]ĀĀ·[NH<sub>4</sub>]ĀĀ·[ZnFe<sup>III</sup>F<sub>5</sub>(<i>amtetraz</i>)<sub>2</sub>]<sub>2</sub> (<b>3</b>), [H<i>dma</i>]<sub>2</sub>ĀĀ·[Zn<sub>1.6</sub>Fe<sup>II</sup><sub>0.4</sub>Fe<sup>III</sup>F<sub>6</sub>Ā(<i>amtetraz</i>)<sub>3</sub>] (<b>4</b>), and [H<i>dma</i>]ĀĀ·[Zn<sub>4</sub>F<sub>5</sub>(<i>amtetraz</i>)<sub>4</sub>] (<b>5</b>) are considered as Class II hybrids in which the (<i>amtetraz</i>)<sup>ā</sup> anions are strongly linked
to divalent metal cations via NāM bonds. In <b>3</b>, <sub>ā</sub>{[NH<sub>4</sub>]ĀĀ·[ZnFe<sup>III</sup>F<sub>5</sub>Ā(<i>amtetraz</i>)<sub>2</sub>]<sub>2</sub>} layers are separated by [H<i>dma</i>]<sup>+</sup> and
[H<i>gua</i>]<sup>+</sup> cations. <b>4</b> and <b>5</b> exhibit three-dimensional (3D) hybrid networks that contain
small cavities where [H<i>dma</i>]<sup>+</sup> cations are
inserted. A porous 3D metalāorganic framework intermediate
is evidenced from the thermogravimetric analysis and X-ray thermodiffraction
of <b>5</b>
Bioinspired Iron Sulfide Nanoparticles for Cheap and Long-Lived Electrocatalytic Molecular Hydrogen Evolution in Neutral Water
Alternative
materials to platinum-based catalysts are required
to produce molecular hydrogen from water at low overpotentials. Transition-metal
chalcogenide catalysts have attracted significant interest over the
past few years because of their activity toward proton reduction and
their relative abundance compared with platinum. We report the synthesis
and characterization of a new type of iron sulfide (FeS, pyrrhotite)
nanoparticles prepared via a solvothermal route. This material can
achieve electrocatalysis for molecular hydrogen evolution with no
structural decomposition or activity decrease for at least 6 days
at a mild overpotential in neutral water at room temperature
Comparison of Porous Iron Trimesates Basolite F300 and MIL-100(Fe) As Heterogeneous Catalysts for Lewis Acid and Oxidation Reactions: Roles of Structural Defects and Stability
Two porous iron trimesates, namely, commercial Basolite
F300 (FeĀ(BTC);
BTC = 1,3,5-benzenetricarboxylate) with unknown structure and synthetic
MIL-100Ā(Fe) (MIL stands for Material of Institut Lavoisier) of well-defined
crystalline structure, have been compared as heterogeneous catalysts
for four different reactions. It was found that while for catalytic
processes requiring strong Lewis acid sites, FeĀ(BTC) performs better,
MIL-100Ā(Fe) is the preferred catalyst for oxidation reactions. These
catalytic results have been rationalized by a combined in situ infrared
and <sup>57</sup>Fe MoĢssbauer spectroscopic characterization.
It is proposed that the presence of extra BrĆønsted acid sites
on the FeĀ(BTC) and the easier redox behavior of the MIL-100Ā(Fe) could
explain these comparative catalytic performances. The results illustrate
the importance of structural defects (presence of weak BrĆønsted
acid sites) and structural stability (MIL-100Ā(Fe) is stable upon annealing
at 280 Ā°C despite Fe<sup>3+</sup>-to-Fe<sup>2+</sup> reduction)
on the catalytic activity of these two solids, depending on the reaction
type
Isomorphous Substitution in a Flexible MetalāOrganic Framework: Mixed-Metal, Mixed-Valent MIL-53 Type Materials
Mixed-metal ironāvanadium
analogues of the 1,4-benzenedicarboxylate (BDC) metalāorganic
framework MIL-53 have been synthesized solvothermally in <i>N</i>,<i>N</i>ā²-dimethylformamide (DMF) from metal chlorides
using initial Fe:V ratios of 2:1 and 1:1. At 200 Ā°C and short
reaction time (1 h), materials (Fe,V)<sup>II/III</sup>BDCĀ(DMF<sub>1ā<i>x</i></sub>F<sub><i>x</i></sub>)
crystallize directly, whereas the use of longer reaction times (3
days) at 170 Ā°C yields phases of composition [(Fe,V)<sup>III</sup><sub>0.5</sub>(Fe,V)<sub>0.5</sub><sup>II</sup>(BDC)Ā(OH,F)]<sup>0.5ā</sup>Ā·0.5DMA<sup>+</sup> (DMA = dimethylammonium). The identity of
the materials is confirmed using high-resolution powder X-ray diffraction,
with refined unit cell parameters compared to known pure iron analogues
of the same phases. The oxidation states of iron and vanadium in all
samples are verified using X-ray absorption near edge structure (XANES)
spectroscopy at the metal K-edges. This shows that in the two sets
of materials each of the vanadium and the iron centers are present
in both +2 and +3 oxidation states. The local environment and oxidation
state of iron is confirmed by <sup>57</sup>Fe MoĢssbauer spectrometry.
Infrared and Raman spectroscopies as a function of temperature allowed
the conditions for removal of extra-framework species to be identified,
and the evolution of Ī¼<sub>2</sub>-hydroxyls to be monitored.
Thus calcination of the mixed-valent, mixed-metal phases [(Fe,V)<sup>III</sup><sub>0.5</sub>(Fe,V)<sub>0.5</sub><sup>II</sup>(BDC)Ā(OH,F)]<sup>0.5ā</sup>Ā·0.5DMA<sup>+</sup> yields single-phase MIL-53-type
materials, (Fe,V)<sup>III</sup>(BDC)Ā(OH,F). The iron-rich, mixed-metal
MIL-53 shows structural flexibility that is distinct from either the
pure Fe material or the pure V material, with a thermally induced
pore opening upon heating that is reversible upon cooling. In contrast,
the material with a Fe:V content of 1:1 shows an irreversible expansion
upon heating, akin to the pure vanadium analogue, suggesting the presence
of some domains of vanadium-rich regions that can be permanently oxidized
to VĀ(IV)
Superparamagnetic MFe<sub>2</sub>O<sub>4</sub> (M = Fe, Co, Mn) Nanoparticles: Tuning the Particle Size and Magnetic Properties through a Novel One-Step Coprecipitation Route
Superparamagnetic ferrite nanoparticles (MFe<sub>2</sub>O<sub>4</sub>, where M = Fe, Co, Mn) were synthesized through a novel
one-step
aqueous coprecipitation method based on the use of a new type of alkaline
agent: the alkanolamines isopropanolamine and diisopropanolamine.
The role played by the bases on the particlesā size, chemical
composition, and magnetic properties was investigated and compared
directly with the effect of the traditional inorganic base NaOH. The
novel MFe<sub>2</sub>O<sub>4</sub> nanomaterials exhibited high colloidal
stability, particle sizes in the range of 4ā12 nm, and superparamagnetic
properties. More remarkably, they presented smaller particle sizes
(up to 6 times) and enhanced saturation magnetization (up to 1.3 times)
relative to those prepared with NaOH. Furthermore, the nanomaterials
exhibited improved magnetic properties when compared with nanoferrites
of similar size synthesized by coprecipitation with other bases or
by other methods reported in the literature. The alkanolamines were
responsible for these achievements by acting both as alkaline agents
and as complexing agents that controlled the particle size during
the synthesis process and improved the spin rearrangement at the surface
(thinner magnetic ādeadā layers). These results open
new horizons for the design of water-dispersible MFe<sub>2</sub>O<sub>4</sub> nanoparticles with tuned properties through a versatile and
easily scalable coprecipitation route
Series of Porous 3-D Coordination Polymers Based on Iron(III) and Porphyrin Derivatives
A new series of 3-D coordination polymers based on iron(III) and nickel(II) tetracarboxylate porphyrin (Ni-TCPP) have been produced using solvothermal conditions. MIL-141(A) solids (MIL stands for Material from Institut Lavoisier), formulated Fe(Ni-TCPP)Aā¢(DMF)<sub><i>xĀ </i></sub>(A = Li, Na, K, Rb, Cs, DMF = N,N-dimethylformamide, <i>x</i> ā¼ 3), are built up from three anionic interpenetrated PtS-type networks charge-balanced by alkali cations (A) entrapped inside the pores. MIL-141(A) thus includes three types of cations, two of which may act as coordinatively unsaturated metal sites (Ni<sup>2+</sup> and A<sup>+</sup>). These solids all present a permanent porosity with a reasonably high surface area (S<sub>BET</sub> = 510ā860 m<sup>2</sup> g<sup>ā1</sup>) as well as some structural flexibility toward adsorption/desorption processes, modulated in both cases by the nature of A. Thermally Stimulated Current (TSC) measurements indicated that alkali cations are rather homogeneously distributed within the pores, while their interaction with the framework is stronger in MIL-141(A) than in the analogous cation-containing Faujasites X and Y zeolites. Finally, high pressure adsorption isotherms of N<sub>2</sub> and O<sub>2</sub> were measured. Whereas alkali ion-containing zeolites adsorb selectively N<sub>2</sub> toward O<sub>2</sub>, the opposite is observed for MIL-141(A). This result is interpreted in light of the TSC data and the possible preferential interaction of the porphyrinic linker with O<sub>2</sub>
Series of Porous 3-D Coordination Polymers Based on Iron(III) and Porphyrin Derivatives
A new series of 3-D coordination polymers based on iron(III) and nickel(II) tetracarboxylate porphyrin (Ni-TCPP) have been produced using solvothermal conditions. MIL-141(A) solids (MIL stands for Material from Institut Lavoisier), formulated Fe(Ni-TCPP)Aā¢(DMF)<sub><i>xĀ </i></sub>(A = Li, Na, K, Rb, Cs, DMF = N,N-dimethylformamide, <i>x</i> ā¼ 3), are built up from three anionic interpenetrated PtS-type networks charge-balanced by alkali cations (A) entrapped inside the pores. MIL-141(A) thus includes three types of cations, two of which may act as coordinatively unsaturated metal sites (Ni<sup>2+</sup> and A<sup>+</sup>). These solids all present a permanent porosity with a reasonably high surface area (S<sub>BET</sub> = 510ā860 m<sup>2</sup> g<sup>ā1</sup>) as well as some structural flexibility toward adsorption/desorption processes, modulated in both cases by the nature of A. Thermally Stimulated Current (TSC) measurements indicated that alkali cations are rather homogeneously distributed within the pores, while their interaction with the framework is stronger in MIL-141(A) than in the analogous cation-containing Faujasites X and Y zeolites. Finally, high pressure adsorption isotherms of N<sub>2</sub> and O<sub>2</sub> were measured. Whereas alkali ion-containing zeolites adsorb selectively N<sub>2</sub> toward O<sub>2</sub>, the opposite is observed for MIL-141(A). This result is interpreted in light of the TSC data and the possible preferential interaction of the porphyrinic linker with O<sub>2</sub>