Articles | Volume 25, issue 18
https://doi.org/10.5194/acp-25-11087-2025
https://doi.org/10.5194/acp-25-11087-2025
Research article
 | 
24 Sep 2025
Research article |  | 24 Sep 2025

Atmospheric chemistry in East Asia determines the iron solubility of aerosol particles supplied to the North Pacific Ocean

Kohei Sakata, Shotaro Takano, Atsushi Matsuki, Yasuo Takeichi, Hiroshi Tanimoto, Aya Sakaguchi, Minako Kurisu, and Yoshio Takahashi

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Cited articles

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Bonneville, S., van Cappellen, P., and Behrends, T.: Microbial reduction of iron(III) oxyhydroxides: effects of mineral solubility and availability, Chem. Geol., 212, 255–268, https://doi.org/10.1016/j.chemgeo.2004.08.015, 2004. 
Bray, A. W., Oelkers, E. H., Bonneville, S., Wolff-Boenisch, D., Potts, N. J., Fones, G., and Benning, L. G.: The effect of pH, grain size, and organic ligands on biotite weathering rates, Geochim. Cosmochim. Ac., 164, 127–145, https://doi.org/10.1016/j.gca.2015.04.048, 2015. 
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Deposition of aerosol iron (Fe) into the ocean stimulates primary production and influences the global carbon cycle, although the factors governing the aerosol Fe solubility remain uncertain. Our observations in Japan revealed that both mineral dust and anthropogenic aerosols are significant sources of dissolved Fe, and that atmospheric chemical weathering enhances their solubility. This finding is expected to play a crucial role in estimating the supply of dissolved iron to the ocean.
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