Reduced Fe Ions Research Articles

Retraction for Yadav et al., "The bidirectional extracellular electron transfer process aids iron cycling by Geoalkalibacter halelectricus in a highly saline-alkaline condition".

In our paper, we reported the bidirectional extracellular electron transfer capability of Geoalkalibacter halelectricus based on biochemical (i.e., with insoluble Fe-oxide and Fe(0)) and bioelectrochemical (i.e., with electrodes) experimental approaches. We noticed some issues and limitations of the methods and techniques that were used to analyze Fe species, particularly the reduced Fe ions in insoluble and precipitated Fe(II) minerals that led to incorrect interpretation of the results, specifically the reduction of Fe(III) to Fe(0) in this study. We were made aware of thermodynamic constraints that would make the biological reduction of Fe(III) to Fe(0) implausible. Hence, the conclusion about microbial Fe(III)-oxide reduction to Fe(0) is invalid. We also noticed errors in estimating the protein-based iron reduction/oxidation rates and faradic efficiencies, besides the limitations of the methods used for Fe analysis. For these reasons, we retract this article and sincerely apologize for the inconvenience it may have caused to the readers.

Biochar from Oil Palm Frond to Reduce Fe Ions in Artificial Solution and Peat Water

Raw oil palm fronds (OPF-R) converted into biochar (OPF-B) by torrefaction processes at temperatures range of 200 °C to 300 °C. This study aims to evaluate OPF-B performance to reduce iron ions in artificial solutions and peat water. Batch adsorption carried out at room temperature by stirring (175 rpm) using an orbital shaker. Some parameters observed included optimum torrefaction temperature, optimum conditions of Fe ions adsorption (optimum pH and contact time) and sorption isotherm. Metal content measured using atomic absorption spectroscopy (AAS). Functional groups on material surface characterized using Fourier Transform Infrared (FT-IR). Torrefaction at 260 °C produces biochar with the highest efficiency in removing iron ions. Both functional groups C=O and C-O attributed to lignocellulose on OPF-B were diminished and absorption band of aromatic (C=C) increased which caused by torrefaction. The optimum conditions for removal of Fe ions at pH 5 and 30 minutes contact time. Adsorption process follows the Langmuir Isotherm which indicates the formation of a monolayer with qmax 111.11 mg/g. Amount of 0.025 g OPF-B able to reduce iron concentration from 13.960 mg/L to 0.746 mg/L in 100 mL peat water (has complied with Indonesian clean water standard for iron concentration).

Laboratory Operando XAS Study of Sodium Iron Titanite Cathode in the Li-Ion Half-Cell.

Electrochemical characterization of the novel sodium iron titanate Na0.9Fe0.45Ti1.55O4 was performed upon cycling in the Li-ion half-cell. The material exhibited stable cycling in the voltage range 2–4.5 V, and the number of alkali ions extracted per formula unit was approximately half of the Na stoichiometry value. Using laboratory X-ray absorption spectrometry, we measured operando Fe K-edge X-ray absorption spectra in the first 10 charge–discharge cycles and quantified the portion of charge associated with the transition metal redox reaction. Although 3d metals are commonly accepted redox-active centers in the intercalation process, we found that in all cycles the amount of oxidized and reduced Fe ions was almost 20% less than the total number of transferred electrons. Using density functional theory (DFT) simulations, we show that part of the reversible capacity is related to the redox reaction on oxygen ions.

Catalytic ozonation of 4-chloronitrobenzene by goethite and Fe2+-modified goethite with low defects: A comparative study.

In this study, Fe2+-modified goethite with low defects (α-Fe(Fe2+)OOH) was synthesized and characterized. Results revealed that α-Fe(Fe2+)OOH is a nano magnetic material with goethite (α-FeOOH) -type structures and has fewer Lewis acid of Fe3+ on its surface. Moreover, α-Fe(Fe2+)OOH was effective in catalytic ozonation of 4-chloronitrobenzene (4-CNB), which is a probe contaminant that cannot be efficiently removed through sole ozonation. The removal of 4-CNB increased with ozone concentration and α-Fe(Fe2+)OOH dosage, but decreased with the presence of carbonate, sulfate and phosphate. The catalytic activity of α-Fe(Fe2+)OOH also showed a dependence on solution pH. The presence of humic acid accelerated 4-CNB removal at low concentration but inhibited the removal at high concentration. In comparison with α-FeOOH, α-Fe(Fe2+)OOH significantly enhanced hydroxyl radicals generation and reduced Fe ions release in this process. The hydroxyl groups of Fe3+ on α-FeOOH and α-Fe(Fe2+)OOH surface was active site for ozone decomposition into hydroxyl radicals. Introducing Fe2+ significantly increased the density of surface hydroxyl groups relative to α-FeOOH. This enhancement significantly promoted hydroxyl radicals generation and 4-CNB degradation in the solution.

Essential oil composition and antioxidant activity of four Asteraceae species from Bosnia

Hydrodistilled volatile oils from Achillea millefolium L., Arnica montana L., Artemisia absinthium L., and Artemisia annua L. were analyzed by GC/MS. One hundred sixty-seven compounds were identified in all samples, ranging from 74.3% to 96.4% of the total oil. A high percentage of oxygenated monoterpenes is the main characteristic of A. millefolium and A. absinthium oils with camphor (19.2%) and isoascaridol (21.9%) as the major constituents, respectively. In contrast, the main component of A. annua oil was oxygenated sesquiterpene selina-3,11-dien-6-α-ol (9.6%), while the chemical composition of A. montana oil was characterized by a high content of fatty acids with n-hexadecanoic acid (16.1%) as the main constituent. Antioxidant activity was tested using four different methods, DPPH, ABTS, Reducing power, and Phosphomolybdenum assay. The highest antioxidant activity had essential oil of A. montana using DPPH and Phosphomolibdenum assay, A. millefolium in ABTS method, while A. absinthium oil showed the best ability to reduce Fe ions.

Facile synthesis of carbon supported Pt-nanoparticles with Fe-rich surface: A highly active catalyst for preferential CO oxidation

Rational design and controlled preparation of highly effective catalysts towards the preferential oxidation of CO have significant importance for the utilization of hydrogen energy. In this work, PtFe/C bimetallic catalysts have been successfully prepared by a one-pot surfactant-free polyol process, where Pt metal nanoparticles serve as catalysts to reduce Fe ions to metallic form on the surface. The resulting PtFe/C catalysts are investigated for a PROX CO reaction and characterized by ICP-AES, XPS, XRD, TEM, HS-LEIS. It is found that PtFe/C with an optimal Fe loading shows extremely high activity and stability. These characterization results reveal that PtFe/C adopts a structure of Fe rich surface and Pt dominated cores. The excellent catalytic performances over PtFe/C catalysts are attributed to the efficient activation of O2 by Fe species located on the catalyst surface, indicated by the results of CO and O2 pulse experiments. Additionally, other PtM/C (M = Cu, Ni) catalysts possessing the similar structure with that of PtFe/C can also be synthesized using the established one-pot surfactant-free polyol process.

Oxidation-reduction mechanism of iron in dioctahedral smectites: II. Crystal chemistry of reduced Garfield nontronite

The crystallochemical structure of reduced Garfield nontronite was studied by X-ray absorption pre-edge and infrared (IR) spectroscopy, powder X-ray diffraction, polarized extended X-ray absorption fine structure (P-EXAFS) spectroscopy, and texture goniometry. Untreated and highly reduced (>99% of total Fe as Fe 2+ ) nontronite samples were analyzed to determine the coordination number and the crystallographic site occupation of Fe 2+ , changes in in-plane and out-of-plane layer structure and mid-range order between Fe centers, and to monitor the changes in structural and adsorbed OH/H 2 O groups in the structure of reduced nontronite. Contrary to earlier models predicting the formation of fivefold coordinated Fe in the structure of nontronites upon reduction, these new results revealed that Fe maintains sixfold coordination after complete reduction. In-plane P-EXAFS evidence indicates that some of the Fe atoms occupy trans-sites in the reduced state, forming small trioctahedral domains within the structure of reduced nontronite. Migration of Fe from cis- to trans sites during the reduction process was corroborated by simulations of X-ray diffraction patterns which revealed that about 28% of Fe 2+ cations exist in trans sites of the reduced nontronite, rather than fully cis occupied, as in oxidized nontronite. Out-of-plane P-EXAFS results indicated that the reduction of Fe suppressed basal oxygen corrugation typical of dioctahedral smectites, and resulted in a flat basal surface which is characteristic of trioctahedral layer silicates. IR spectra of reduced nontronite revealed that the dioctahedral nature of the nontronite was lost and a band near 3623 cm −1 formed, which is thought to be associated with trioctahedral [Fe 2+ ] 3 OH stretching vibrations. On the basis of these results, a structural model for the reduction mechanism of Fe 3+ to Fe 2+ in Garfield nontronite is proposed that satisfies all structural data currently available. The migration of reduced Fe ions from cis-octahedra to adjacent trans-octahedra is accompanied by a dehydroxylation reaction due to the protonation of OH groups initially coordinated to Fe. This structural modification results in the formation of trioctahedral Fe 2+ clusters separated by clusters of vacancies in which the oxygen ligands residing at the boundary between trioctahedral and vacancy domains are greatly coordination undersaturated. The charge of these O atoms is compensated by the incorporation of protons, and by the displacement of Fe 2+ atoms from their ideal octahedral position toward the edges of trioctahedral clusters, thus accounting for the incoherency of the Fe-Fe1 and Fe-Fe2 distances. From these results, the ideal structural formula of reduced Garfield nontronite is Na 1.30 [Si 7.22 Al 0.78 ] [Fe 2+ 3.65 Al 0.32 Mg 0.04 ]O 17.93 (OH) 5 in which the increased layer charge due to reduction of Fe 3+ to Fe 2+ is satisfied by the incorporation of protons and interlayer Na.