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Hydroxyl Radical Photoproduction in the Sea and Its Potential Impact on Marine Processes

Mopper, Kenneth, Zhou, Xianliang·1990·Science

Abstract

Photochemical production rates and steady-state concentrations of hydroxyl radicals (⋅OH) were measured in sunlight-irradiated seawater. Values ranged from 110 nanomolar per hour and 12 × 10 -18 molar in coastal surface water to 10 nanomolar per hour and 1.1 × 10 -18 molar in open ocean surface water. The wavelengths responsible for this production are in the ultraviolet B region (280 to 320 nanometers) of the solar spectrum. Dissolved organic matter (DOM) appears to be the main source for ⋅OH over most of the oceans, but in upwelling areas nitrite and nitrate photolysis may also be important. DOM in the deep sea is degraded more readily by ⋅OH (and its daughter radicals), by a factor of 6 to 15, than is DOM in open-ocean surface water. This finding may in part bear on major discrepancies among current methods for measuring dissolved organic carbon in seawater.

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Metadata

Authors
Mopper, K., & Zhou, X.
Venue
Science
Published
1990-11-02
Volume
250
Issue
4981
Pages
661-664
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1983822766
Cited by
544
References
0
FWCI
7.98
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Hydroxyl Radical Photoproduction in the Sea and Its Potential Impact on Marine Processes. https://app.cochat.ai/papers/10.1126/science.250.4981.661
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Mopper, K., & Zhou, X. (1990). Hydroxyl Radical Photoproduction in the Sea and Its Potential Impact on Marine Processes. Science. https://doi.org/10.1126/science.250.4981.661

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