Partitioning of Dissolved Iron and Iron Isotopes into Soluble and Colloidal Phases along the GA03 GEOTRACES North Atlantic Transect
Document Type
Article
Publication Date
6-2015
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
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.
Was this content written or created while at USF?
No
Citation / Publisher Attribution
Deep Sea Research Part II: Topical Studies in Oceanography, v. 116, p. 130-151
Scholar Commons Citation
Fitzsimmons, Jessica N.; Carrasco, Gonzalo G.; Wu, Jingfeng; Roshan, Saeed; Hatta, Mariko; Measures, Christopher I.; Conway, Tim M.; John, Seth G.; and Boyle, Edward A., "Partitioning of Dissolved Iron and Iron Isotopes into Soluble and Colloidal Phases along the GA03 GEOTRACES North Atlantic Transect" (2015). School of Geosciences Faculty and Staff Publications. 1506.
https://digitalcommons.usf.edu/geo_facpub/1506
