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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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| Vydáno v: | Environ Sci Technol |
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| Hlavní autoři: | , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
American
Chemical Society
2019
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| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6978810/ https://ncbi.nlm.nih.gov/pubmed/31846315 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1021/acs.est.9b04235 |
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