4.8 Article

Photochemical and Photophysical Dynamics of the Aqueous Ferrate(VI) Ion

期刊

JOURNAL OF THE AMERICAN CHEMICAL SOCIETY
卷 144, 期 49, 页码 22514-22527

出版社

AMER CHEMICAL SOC
DOI: 10.1021/jacs.2c08048

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资金

  1. U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences [DE-SC0019429]
  2. U.S. National Science Foundation, Division of Chemical Bioengineering, Environmental, and Transport Systems (CBET) under CAREER Award [2046383]
  3. US Department of Energy, Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences and Biosciences Division [DE-AC02-06CH11357]
  4. DOE Office of Science [DE-AC02-06CH11357]
  5. Directorate For Engineering
  6. Div Of Chem, Bioeng, Env, & Transp Sys [2046383] Funding Source: National Science Foundation
  7. U.S. Department of Energy (DOE) [DE-SC0019429] Funding Source: U.S. Department of Energy (DOE)

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This study investigates the formation and fate of Fe(V) and Fe(IV) species in aqueous potassium ferrate(VI) through a combination of optical and X-ray transient absorption spectroscopies. The results improve the mechanistic understanding and accelerate the development of novel advanced oxidation processes for water treatment applications.
Ferrate(VI) has the potential to play a key role in future water supplies. Its salts have been suggested as green alternatives to current advanced oxidation and disinfection methods in water treatment, especially when combined with ultraviolet light to stimulate generation of highly oxidizing Fe(V) and Fe(IV) species. However, the nature of these intermediates, the mechanisms by which they form, and their roles in downstream oxidation reactions remain unclear. Here, we use a combination of optical and X-ray transient absorption spectroscopies to study the formation, interconversion, and relaxation of several excited-state and metastable high-valent iron species following excitation of aqueous potassium ferrate(VI) by ultraviolet and visible light. Branching from the initially populated ligand-to-metal charge transfer state into independent photophysical and photochemical pathways occurs within tens of picoseconds, with the quantum yield for the generation of reactive Fe(V) species determined by relative rates of the competing intersystem crossing and reverse electron transfer processes. Relaxation of the metal-centered states then occurs within 4 ns, while the formation of metastable Fe(V) species occurs in several steps with time constants of 250 ps and 300 ns. Results here improve the mechanistic understanding of the formation and fate of Fe(V) and Fe(IV), which will accelerate the development of novel advanced oxidation processes for water treatment applications.

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