Iron mobilization in mineral dust: Can anthropogenic SO2emissions affect ocean productivity?


Journal Article

For Fe contained in long-range transported acolian dust to act as a micronutrient for oceanic phytoplankton it must be first dissolved or mobilized. We propose that Femobilization can occur in mineral dust from East Asia by the incorporation of SO2into the advecting dust plumes and subsequent acidification of the dust through heterogeneous SO2oxidation. To test this hypothesis, we consider a dust plume that originated from the gobi-deserts and advected over the Pacific Ocean. Data collected over the Yellow Sea confirm that this plume contained high concentrations of dust and SO2. Significant gaseous HNO3concentrations indicate that the dust particles were acidified (i.e., pH < 2). At these pH's, 1-2% of the Fe contained in a deliquescent mineral dust particle would be mobilized within 3-5 days. These results suggest a possible link between the rate of C-fixation in so-called High-Nitrate-Low-Chlorophyll regions of the Pacific Ocean and SO2emissions from East Asia. Copyright 2003 by the American Geophysical Union.

Duke Authors

Cited Authors

  • Meskhidze, N; Chameides, WL; Nenes, A; Chen, G

Published Date

  • November 1, 2003

Published In

Volume / Issue

  • 30 / 21

International Standard Serial Number (ISSN)

  • 0094-8276

Citation Source

  • Scopus