Linking Isotope Exchange with Fe(II)-Catalyzed Dissolution of Iron(hydr)oxides in the Presence of the Bacterial Siderophore Desferrioxamine-B

[Image: see text] Dissolution of Fe(III) phases is a key process in making iron available to biota and in the mobilization of associated trace elements. Recently, we have demonstrated that submicromolar concentrations of Fe(II) significantly accelerate rates of ligand-controlled dissolution of Fe(II...

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Detalles Bibliográficos
Autores principales: Biswakarma, Jagannath, Kang, Kyounglim, Schenkeveld, Walter D. C., Kraemer, Stephan M., Hering, Janet G., Hug, Stephan J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2019
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6978810/
https://www.ncbi.nlm.nih.gov/pubmed/31846315
http://dx.doi.org/10.1021/acs.est.9b04235

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6978810/
https://www.ncbi.nlm.nih.gov/pubmed/31846315
http://dx.doi.org/10.1021/acs.est.9b04235

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