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Ferryl Ion in the Photo-Fenton Process at Acidic pH: Occurrence, Fate, and Implications
Guowei Deng1,2, Zhen Wang1,2, Jinxing Ma1,2
1Key Laboratory for City Cluster Environmental Safety and Green Development of the Ministry of Education, School of Ecology, Environment and Resources, Guangdong University of Technology, Guangzhou 510006, China.
This study demonstrates ferryl ion (FeIV O2+) generation in UV/Fe(III) systems, clarifying its formation pathways and role in pollutant degradation. The findings enhance understanding of reactive species in photo-Fenton processes for environmental remediation.
Area of Science:
- Environmental Chemistry
- Photocatalysis
- Oxidation Processes
Background:
- Fenton processes are crucial for oxidizing organic compounds using reactive species.
- Hydroxyl radical (HO•) generation in Fenton reactions is well-established under acidic conditions.
- The formation and role of ferryl ion (FeIV O2+) in these systems require further elucidation.
Purpose of the Study:
- To demonstrate the generation of ferryl ion (FeIV O2+) in UV/Fe(III) and UV/Fe(III)/H2O2 systems at pH 2.8.
- To elucidate the parallel formation mechanisms of FeIV O2+ via Fe(III) oxidation by HO• and O-O homolysis of [FeIII-OOH]2+.
- To develop an optimized kinetic model incorporating FeIV O2+ reactions for predicting contaminant decay.
Main Methods:
- Utilized methyl phenyl sulfoxide (PMSO) as a probe compound to detect reactive species.
- Employed laser flash photolysis to measure the rate constant for HO• and Fe3+ reaction.
- Determined rate constants and quantum yield for [FeIII-OOH]2+ O-O homolysis by fitting PMSO2 formation.
- Developed and optimized a kinetic model by integrating FeIV O2+ reactions into the photo-Fenton model.
Main Results:
- Demonstrated FeIV O2+ generation in UV/Fe(III) and UV/Fe(III)/H2O2 systems at pH 2.8.
- Quantified the rate constant for HO• + Fe3+ reaction (4.41 × 10^7 M^-1 s^-1) and O-O homolysis of [FeIII-OOH]2+ (1.4 × 10^-2 s^-1, quantum yield 0.3).
- Showed that FeIV O2+ formation predominantly involves HO• + Fe3+ in the absence of H2O2, while its contribution from [FeIII-OOH]2+ O-O homolysis depends on reactant ratios, scavenging, and irradiance.
- The optimized kinetic model accurately predicted Fe(II) formation and contaminant decay.
Conclusions:
- Elucidated the formation mechanisms of reactive oxidative species, particularly FeIV O2+, in photo-Fenton processes.
- Highlighted the significant role of FeIV O2+ in modulating the iron cycle and pollutant abatement.
- The developed kinetic model provides a robust tool for understanding and optimizing UV/Fe-based oxidation systems.
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