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Updated: Jul 28, 2025
![Protein Film Infrared Electrochemistry Demonstrated for Study of H2 Oxidation by a [NiFe] Hydrogenase](/_next/image?url=https%3A%2F%2Fcloudfront.jove.com%2FCDNSource%2Fteasers%2F55858.jpg&w=3840&q=50)
Protein Film Infrared Electrochemistry Demonstrated for Study of H2 Oxidation by a [NiFe] Hydrogenase
Published on: December 4, 2017
Diverse performances for Pb(II) adsorption by in situ formed Fe(III) oxyhydroxide derived from ferrate(VI) reduction
Bingyan Lan1,2, Chenhui Hao1,2, Mengze Zhang1,2
1School of Environment, South China Normal University, Higher Education Mega Center, Guangzhou, 510006, People's Republic of China.
Abstract:
Two in situ formed Fe(III) oxyhydroxides (FeOx) originated from ferrate reduction (designated FeOx-FeVI) and ferrous oxidation by H2O2 (designated FeOx-FeII) were compared in the aspects of morphology, hydrolyzed species, surface binding mechanism of lead. The theoretical maximum adsorption capacity calculated from the Langmuir model toward Pb(II) was 929.54 and 810.37 mg/g Fe by FeOx-FeVI and FeOx-FeII, respectively. At pH 6 and the same Fe/Pb ratio, the kinetic rate of Pb removal by the FeOx-FeVI process was 8 times faster. FTIR, SEM, and Ferron assay suggest FeOx-FeVI was associated with a lesser polymerization degree and contained more reactive hydroxyl-Fe polymers than those in the FeOx-FeII sample. SAXS verified that the particles possessed a smaller, more homogeneous, and open structure when Fe was hydrolyzed by ferrate reduction than ferrous oxidation. XPS coupled with fractal analysis suggests the different sorption capacities of Pb(II) can be ascribed to their distinct growth patterns. Fast cluster agglomeration during FeOx-FeII fabrication decreased the exposure of effective adsorption sites. In comparison, the incompact assemblies of FeOx-FeVI clusters facilitated Pb(II) ions to access the interstices of octahedral FeO6 units and formed an edge-sharing complex. This work provides new insight into mechanisms of particle fabrication and heavy metal removal of Fe(III) formed in situ.
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