Regeneration of Fe(II) during EIFeX and SOFeX

  • P. L. Croot
  • , K. Bluhm
  • , C. Schlosser
  • , P. Streu
  • , E. Breitbarth
  • , R. Frew
  • , M. van Ardelan

Research output: Contribution to a Journal (Peer & Non Peer)Articlepeer-review

43 Citations (Scopus)

Abstract

Investigations into Fe(II) cycling during two Southern Ocean mesoscale iron enrichment experiments, SOFeX and EIFeX, clearly show the importance of Fe(II) to iron speciation during these experiments. In both cases the added Fe(II) persisted significantly longer than its expected oxidation time indicating a significant Fe reduction process at work. During EIFeX diel studies showed a strong photochemically induced cycle in Fe(II) production in sunlit surface waters. Our results suggest that the photochemical cycling of iron may also be important in unfertilized waters of the Southern Ocean.

Original languageEnglish
Article numberL19606
JournalGeophysical Research Letters
Volume35
Issue number19
DOIs
Publication statusPublished - 16 Oct 2008
Externally publishedYes

Fingerprint

Dive into the research topics of 'Regeneration of Fe(II) during EIFeX and SOFeX'. Together they form a unique fingerprint.

Cite this