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Article
Partitioning of Dissolved Iron and Iron Isotopes into Soluble and Colloidal Phases along the GA03 GEOTRACES North Atlantic Transect
Deep Sea Research Part II: Topical Studies in Oceanography
  • Jessica N. Fitzsimmons, Massachusetts Institute of Technology
  • Gonzalo G. Carrasco, Massachusetts Institute of Technology
  • Jingfeng Wu, University of Miami
  • Saeed Roshan, University of Miami
  • Mariko Hatta, University of Hawaii, Manoa
  • Christopher I. Measures, University of Hawaii, Manoa
  • Tim M. Conway, University of South Carolina
  • Seth G. John, University of South Carolina
  • Edward A. Boyle, Massachusetts Institute of Technology
Document Type
Article
Publication Date
6-1-2015
Keywords
  • Iron,
  • Colloids,
  • Ultrafiltration,
  • Anopore,
  • Cross flow filtration,
  • Iron isotopes,
  • North Atlantic Ocean,
  • GEOTRACES,
  • Trace metals,
  • Chemical oceanography
Digital Object Identifier (DOI)
https://doi.org/10.1016/j.dsr2.2014.11.014
Disciplines
Abstract

The size partitioning of dissolved Fe (dFe<0.2 µm) into soluble (sFe<0.02 µm) and colloidal (0.02 µm56Fe of +1.3‰ to +1.5‰) relative to dFe (δ56Fe~+0.5‰) in the surface ocean where sFe and cFe cycle independently, and identical sFe and dFe isotope ratios below 250 m where sFe and cFe are constantly partitioned and exchanged.

Citation / Publisher Attribution

Deep Sea Research Part II: Topical Studies in Oceanography, v. 116, p. 130-151

Citation Information
Jessica N. Fitzsimmons, Gonzalo G. Carrasco, Jingfeng Wu, Saeed Roshan, et al.. "Partitioning of Dissolved Iron and Iron Isotopes into Soluble and Colloidal Phases along the GA03 GEOTRACES North Atlantic Transect" Deep Sea Research Part II: Topical Studies in Oceanography Vol. 116 (2015) p. 130 - 151
Available at: http://works.bepress.com/tim-conway/15/