Slow Kinetics of Iron Binding to Marine Ligands in Seawater Measured by Isotope Exchange Liquid Chromatography-Inductively Coupled Plasma Mass Spectrometry.


Journal

Environmental science & technology
ISSN: 1520-5851
Titre abrégé: Environ Sci Technol
Pays: United States
ID NLM: 0213155

Informations de publication

Date de publication:
15 03 2022
Historique:
pubmed: 26 2 2022
medline: 14 4 2022
entrez: 25 2 2022
Statut: ppublish

Résumé

Current understanding of dissolved iron (Fe) speciation in the ocean is based on two fundamentally different approaches: electrochemical methods that measure bulk properties of a heterogeneous ligand pool and liquid chromatography mass spectrometry methods that characterize ligands at a molecular level. Here, we describe a method for simultaneously determining Fe-ligand dissociation rate constants (

Identifiants

pubmed: 35213147
doi: 10.1021/acs.est.1c06922
doi:

Substances chimiques

Isotopes 0
Ligands 0
Siderophores 0
Ferrichrome 15630-64-5
Iron E1UOL152H7

Types de publication

Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S.

Langues

eng

Sous-ensembles de citation

IM

Pagination

3770-3779

Auteurs

Rene M Boiteau (RM)

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97330, United States.
Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, Washington 99354, United States.

Daniel J Repeta (DJ)

Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, United States.

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Classifications MeSH