Bioavailable iron production in airborne mineral dust: Controls by chemical composition and solar flux

Eshani Hettiarachchi, Richard L. Reynolds, Harland L. Goldstein, Bruce Moskowitz, Gayan Rubasinghege

Research output: Contribution to journalArticle

2 Citations (Scopus)

Abstract

A large part of oceanic biological production is limited by the scarcity of dissolved iron. Mineral dust aerosol, processed under acidic atmospheric conditions, is the primary natural source of bioavailable iron to oceanic life. However, synergistic and antagonistic effects of non-Fe-containing minerals on atmospheric processing of Fe-containing minerals and Fe solubilization are poorly understood. The current study focuses on mineralogical influences of non-Fe-bearing semiconductor minerals, such as titanium dioxide (TiO2), on the dissolution of iron in selected natural mineral dust aerosols under atmospherically relevant conditions. Further, the role of elevated Ti concentrations in dust is evaluated using magnetite, a proxy for Fe(II) containing minerals, under both dark and light conditions. Our results highlight that relatively higher Ti:Fe ratios, regardless of their total Fe content, enhances the total iron dissolution in mineral dust aerosols as well as in magnetite. Moreover, elevated Ti percentages also yield high Fe(II) fractions in mineral dust systems under dark conditions. Upon irradiation however, dissolved Fe(II) is suppressed by high Ti levels due to the involvement of photochemical redox cycling reactions with hydroxyl radicals (OH). These synergistic and antagonistic effects of Ti are further evaluated by altering the chemical composition of natural dusts with artificially added anatase (TiO2) and synthetic amorphous titania. The current study reveals important mineralogical controls by non-Fe-bearing minerals on dust iron dissolution to better understand global iron mobilization.

Original languageEnglish (US)
Pages (from-to)90-102
Number of pages13
JournalAtmospheric Environment
Volume205
DOIs
StatePublished - May 15 2019

Fingerprint

chemical composition
dust
iron
mineral
dissolution
aerosol
magnetite
biological production
anatase
solubilization
hydroxyl radical
titanium
mobilization
irradiation

Keywords

  • Bioavailable iron
  • Iron dissolution
  • Mineralogy effects
  • Photochemistry
  • Redox cycling
  • Titanium dioxide

Cite this

Bioavailable iron production in airborne mineral dust : Controls by chemical composition and solar flux. / Hettiarachchi, Eshani; Reynolds, Richard L.; Goldstein, Harland L.; Moskowitz, Bruce; Rubasinghege, Gayan.

In: Atmospheric Environment, Vol. 205, 15.05.2019, p. 90-102.

Research output: Contribution to journalArticle

Hettiarachchi, Eshani ; Reynolds, Richard L. ; Goldstein, Harland L. ; Moskowitz, Bruce ; Rubasinghege, Gayan. / Bioavailable iron production in airborne mineral dust : Controls by chemical composition and solar flux. In: Atmospheric Environment. 2019 ; Vol. 205. pp. 90-102.
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