7 research outputs found

    Chlorine Insertion Promoting Iron Reduction in Baā€“Fe Hexagonal Perovskites: Effect on the Structural and Magnetic Properties

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    BaFeCl<sub>0.13(2)</sub>O<sub>2.48(2)</sub> has been synthesized and studied. A proper tuning of the synthetic route has been designed to stabilize this compound as a single phase. The thermal stability and evolution, along with the magnetic and structural properties are reported here. The crystal structure has been refined from neutron powder diffraction data, and it is of the type (hhchc)<sub>2</sub>-10H. It is stable up to a temperature of 900 Ā°C, where the composition reads BaFeCl<sub>0.13(2)</sub>O<sub>2.34(2)</sub>. The study by electron microscopy shows that the crystal structure suffers no changes in the whole BaFeCl<sub>0.13(1)</sub>O<sub>3ā€“<i>y</i></sub> (2.34 ā‰¤ 3 ā€“ <i>y</i> ā‰¤ 2.48) compositional range. Refinement of the magnetic structure shows that the Fe is antiferromagneticaly ordered, with the magnetic moment parallel to the <i>ab</i> plane of the hexagonal structure. At higher temperature, a nonreversible phase transition into a (hchc)-4H structure type takes place with overall composition BaFeCl<sub>0.13(1)</sub>O<sub>2.26(1)</sub>. Microstructural characterization shows that, in some crystals, this phase intergrows with a seemingly cubic related phase. Differences between these two crystalline phases reside in the chlorine content, which keeps constant through the phase transition for the former and disappears for the latter

    Direct Atomic Observation in Powdered 4H-Ba<sub>0.8</sub>Sr<sub>0.2</sub>Mn<sub>0.4</sub>Fe<sub>0.6</sub>O<sub>2.7</sub>

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    A new hexagonal polytype in the BaMn<sub>1ā€‘<i>x</i></sub>Fe<sub><i>x</i></sub>O<sub>3ā€‘Ī“</sub> system has been stabilized. Powdered Ba<sub>0.8</sub>Sr<sub>0.2</sub>Mn<sup>IV</sup><sub>0.4</sub>Fe<sup>III</sup><sub>0.6</sub>O<sub>2.70</sub> crystallizes in the 4H hexagonal polytype (space group <i>P</i>6<sub>3</sub>/<i>mmc</i>) according to X-ray diffraction. HAADF images and chemical maps with atomic resolution have been obtained by combining Cs-corrected electron microscopy and EELS spectroscopy. The structure is formed by dimers of face-sharing octahedra linked by corners. EELS data show a random distribution of the transition metals ions identified by Fe and Mn-L2,3 chemical maps. A systematic difference in contrast observed in the Oā€“K signal mapping suggests that anion deficiency is randomly located along the hexagonal layers in agreement with ND data. The magnetic structure consists of ferromagnetic sheets with the magnetic moments aligned along the <i>x</i>-axis and coupled antiferromagnetically along the <i>c</i>-axis

    Nickel-Doped Sodium Cobaltite 2D Nanomaterials: Synthesis and Electrocatalytic Properties

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    In this work we report a synthetic pathway to two-dimensional nanostructures of high oxidation state lamellar cobalt oxides with thicknesses of only few atom layers, through the combined use of precipitation in basic water at room temperature and gentle solid state topotactic transformation at 120 Ā°C. The 2D nanomaterials are characterized by X-ray diffraction, nitrogen porosimetry, scanning electron microscopy, transmission electron microscopy and especially scanning transmission electron microscopy coupled to energy dispersive X-ray analysis and electron energy loss spectroscopy to assess the composition of the nanosheets and the oxidation state of the transition metal species. We show that the nanosheets preserve high oxidation states Co<sup>3+</sup> and Co<sup>4+</sup> of high interest for electrocatalysis of the oxygen evolution reaction (OER). By combining high Co oxidation state, surface-to-volume ratio and optimized nickel substitution, the 2D nanomaterials produced in a simple way exhibit high OER electrocatalytic activity and stability in alkaline aqueous electrolyte comparable to standard materials obtained in harsh thermal conditions

    Synthesis of 4H-SrMnO<sub>3.0</sub> Nanoparticles from a Molecular Precursor and Their Topotactic Reduction Pathway Identified at Atomic Scale

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    Stoichiometric 4H-SrMnO<sub>3.0</sub> nanoparticles have been synthesized from thermal decomposition of a new molecular heterometallic precursor [SrMnĀ­(edta)Ā­(H<sub>2</sub>O)<sub>5</sub>]Ā·<sup>3</sup>/<sub>2</sub>H<sub>2</sub>O whose crystal structure has been solved by single crystal X-ray diffraction. From this precursor, highly homogeneous 4H-SrMnO<sub>3.0</sub> nanoparticles, with average particle size of 70 nm, are obtained. The agglomeration of these nanoparticles maintains the sheet-assembling morphology of the metalā€“organic compound. Local structural information, provided by atomically resolved microscopy techniques, shows that 4H-SrMnO<sub>3.0</sub> nanoparticles exhibit the same general structural features as the bulk material, although structural disorder, due to edge dislocations, is observed. The nanometric particle size enables a topotactic reduction process at low temperature stabilizing a metastable 4H-SrMnO<sub>2.82</sub> phase. The oxygen deficiency is accommodated through extra cubic layers breaking the ...chch... 4H-sequence. These defect areas are Mn<sup>3+</sup> rich, as evidenced by high energy resolution EELS data. Magnetic characterization of nano-SrMnO<sub>3.0</sub> shows significant variations with respect to the bulk material. Besides the dominant antiferromagnetic interactions, a weak ferromagnetic contribution as well as exchange bias and a glassy-like component are present. After the reduction process, the stabilization of Mn<sup>3+</sup> in the 4H-structure gives rise to magnetic anomalies in the 40ā€“60 K temperature range. The origin of such magnetic features is discussed

    Unknown Aspects of Self-Assembly of PbS Microscale Superstructures

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    A lot of interesting and sophisticated examples of nanoparticle (NP) self-assembly (SA) are known. From both fundamental and technological standpoints, this field requires advancements in three principle directions: (a) understanding the mechanism and driving forces of three-dimensional (3D) SA with both nano- and microlevels of organization; (b) understanding disassembly/deconstruction processes; and (c) finding synthetic methods of assembly into continuous superstructures without insulating barriers. From this perspective, we investigated the formation of well-known star-like PbS superstructures and found a number of previously unknown or overlooked aspects that can advance the knowledge of NP self-assembly in these three directions. The primary one is that the formation of large seemingly monocrystalline PbS superstructures with multiple levels of octahedral symmetry can be explained only by SA of small octahedral NPs. We found five distinct periods in the formation PbS hyperbranched stars: (1) nucleation of early PbS NPs with an average diameter of 31 nm; (2) assembly into 100ā€“500 nm octahedral mesocrystals; (3) assembly into 1000ā€“2500 nm hyperbranched stars; (4) assembly and ionic recrystallization into six-arm rods accompanied by disappearance of fine nanoscale structure; (5) deconstruction into rods and cuboctahedral NPs. The switches in assembly patterns between the periods occur due to variable dominance of pattern-determining forces that include van der Waals and electrostatic (chargeā€“charge, dipoleā€“dipole, and polarization) interactions. The superstructure deconstruction is triggered by chemical changes in the deep eutectic solvent (DES) used as the media. PbS superstructures can be excellent models for fundamental studies of nanoscale organization and SA manufacturing of (opto)electronics and energy-harvesting devices which require organization of PbS components at multiple scales

    SrMnO<sub>3</sub> Thermochromic Behavior Governed by Size-Dependent Structural Distortions

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    The influence of particle size in both the structure and thermochromic behavior of 4H-SrMnO<sub>3</sub> related perovskite is described. Microsized SrMnO<sub>3</sub> suffers a structural transition from hexagonal (<i>P</i>6<sub>3</sub>/<i>mmc</i>) to orthorhombic (<i>C</i>222<sub>1</sub>) symmetry at temperature close to 340 K. The orthorhombic distortion is due to the tilting of the corner-sharing Mn<sub>2</sub>O<sub>9</sub> units building the 4H structural type. When temperature decreases, the distortion becomes sharper reaching its maximal degree at āˆ¼125 K. These structural changes promote the modification of the electronic structure of orthorhombic SrMnO<sub>3</sub> phase originating the observed color change. nano-SrMnO<sub>3</sub> adopts the ideal 4H hexagonal structure at room temperature, the orthorhombic distortion being only detected at temperature below 170 K. A decrease in the orthorhombic distortion degree, compared to that observed in the microsample, may be the reason why a color change is not observed at low temperature (77 K)

    Critical Influence of Redox Pretreatments on the CO Oxidation Activity of BaFeO<sub>3āˆ’Ī“</sub> Perovskites: An in-Depth Atomic-Scale Analysis by Aberration-Corrected and in Situ Diffraction Techniques

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    A BaFeO<sub>3āˆ’Ī“</sub> (Ī“ ā‰ˆ 0.22) perovskite was prepared by a solā€“gel method and essayed as a catalyst in the CO oxidation reaction. BaFeO<sub>3āˆ’Ī“</sub> (0.22 ā‰¤ Ī“ ā‰¤ 0.42) depicts a 6H perovskite hexagonal structural type with Fe in both III and IV oxidation states and oxygen stoichiometry accommodated by a random distribution of anionic vacancies. The perovskite with the highest oxygen content, BaFeO<sub>2.78</sub>, proved to be more active than its lanthanide-based counterparts, LnFeO<sub>3</sub> (Ln = La, Sm, Nd). Removal of the lattice oxygen detected in both temperature-programmed oxidation (TPO) and reduction (TPR) experiments at around 500 K and which leads to the complete reduction of Fe<sup>4+</sup> to Fe<sup>3+</sup>, i.e. to BeFeO<sub>2.5</sub>, significantly decreases the catalytic activity, especially in the low-temperature range. The analysis of thermogravimetric experiments performed under oxygen and of TPR studies run under CO clearly support the involvement of lattice oxygen in the CO oxidation on these Ba-Fe perovskites, even at the lowest temperatures. Atomically resolved images and chemical maps obtained using different aberration-corrected scanning transmission electron microscopy techniques, as well as some in situ type experiments, have provided a clear picture of the accommodation of oxygen nonstoichiometry in these materials. This atomic-scale view has revealed details of both the cation and anion sublattices of the different perovskites that have allowed us to identify the structural origin of the oxygen species most likely responsible for the low-temperature CO oxidation activity
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