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Formation of hydrogen peroxide and depletion of oxalic acid in atmospheric water by photolysis of iron(III)-oxalato complexes

Zuo, Yuegang, Hoigne, Juerg·1992·Environmental Science & Technology

Abstract

The generation of hydrogen peroxide (H2O2) and the depletion of oxalic acid by photochemical/chemical cycling of Fe(III)/Fe(II)-oxalato complexes in sunlight has been studied under the conditions typical for acidified atmospheric water. H2O2 is produced through the reduction of oxygen by intermediates formed from photoreactions of Fe(III)-oxalato complexes. The rate of H2O2 formation increases with sunlight intensity, and with oxalate and Fe(III) concentration within the concentration range used. This rate is 3.7 nM s-1 when 1 μM Fe(III) and 5 μM oxalate at pH 4 is exposed to September noon sunlight. Speciation calculations based on the concentration range of Fe(III) and oxalic acid in atmospheric water indicate that Fe(III)-oxalato complexes are often the predominant species of dissolved Fe(III). The concentrations of Fe(III)-oxalato complexes are sufficiently large to make their photolysis a dominant source of in-cloud H2O2, O2·-, HO2, and OH radicals and a major sink for atmospheric oxalic acid.

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Metadata

Authors
Zuo, Y., & Hoigne, J.
Venue
Environmental Science & Technology
Published
1992-05
Volume
26
Issue
5
Pages
1014-1022
ISSN
  • 0013-936X (ISSN-L)
  • 1520-5851
OpenAlex
W1975707464
Cited by
778
References
0
FWCI
12.99
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Formation of hydrogen peroxide and depletion of oxalic acid in atmospheric water by photolysis of iron(III)-oxalato complexes. https://app.cochat.ai/papers/10.1021/es00029a022
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Zuo, Y., & Hoigne, J. (1992). Formation of hydrogen peroxide and depletion of oxalic acid in atmospheric water by photolysis of iron(III)-oxalato complexes. Environmental Science & Technology. https://doi.org/10.1021/es00029a022

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