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The decrease of the Fe 2p3/2 FWHM can be interpreted from the aspect of crystallographic structure of the iron silicide.
By scanning electron microscopy technique (SEM) was possible to observe the structure of the iron ore particles after treatment with microwave energy.
This could include softening the structure of the iron ligand (M234EH) and the QA binding pocket (M265IT) and/or increase of the multiplicity of the electron transfer of charge separation in the acceptor side upon mutation.
Synthetic C-terminal amidated cationic ferrocenoyl peptide bioconjugates Fc-Orn-Orn-Orn (1) and Fc-Tyr-Orn-Orn-Orn (2) were rationally designed as superoxide dismutase (SOD) mimics based on the structure of the iron SOD from Escherichia coli.
Regarding the interest of such preliminary data, new structural analysis (by FTIR or Raman spectroscopy for instance) should be done to precise the composition of the paint layers, the mineral structure of the iron oxides and green earth, such as the presence of organic materials.
Rietveld refinement established that the Fe3O4 samples were phase pure, while the extended X-ray absorption fine structure (EXAFS) and X-ray absorption near edge structure (XANES) provided insight into the local geometries and electronic structure of the iron centers, including oxidation state assignment.
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While all studies are consistent with a localized electronic structure of the irons in the reduced state, a Cys → Ser mutant of a thioredoxin-like ferredoxin showed a valence-delocalized S = 9/2 feature in EPR, which was further analyzed by variable temperature magnetic circular dichroism.
Similar to the SPE, the growth temperature of the RDE also has an important influence on the crystal structures of the iron silicides.
Information on high-resolution morphologies and structures of the iron oxide nanocages can be gleaned from Fig. 4, and the HRTEM images obtained near the center region of hollow nanocages.
The crystal structure of these iron oxide particles was analyzed by XRD and is shown in Figure 1d.
The results showed that the trinuclear iron cluster was successfully intercalated into the layers of montmorillonite and the structure of the active iron species was an amorphous FeO(OH -like structure after 500 °C pOH -liketment.
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