Iron mineral dissolution releases iron and associated organic carbon during permafrost thaw

It has been shown that reactive soil minerals, specifically iron(III) (oxyhydr)oxides, can trap organic carbon in soils overlying intact permafrost, and may limit carbon mobilization and degradation as it is observed in other environments. However, the use of iron(III)-bearing minerals as terminal e...

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Detalles Bibliográficos
Autores principales: Patzner, Monique S., Mueller, Carsten W., Malusova, Miroslava, Baur, Moritz, Nikeleit, Verena, Scholten, Thomas, Hoeschen, Carmen, Byrne, James M., Borch, Thomas, Kappler, Andreas, Bryce, Casey
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7729879/
https://www.ncbi.nlm.nih.gov/pubmed/33303752
http://dx.doi.org/10.1038/s41467-020-20102-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7729879/
https://www.ncbi.nlm.nih.gov/pubmed/33303752
http://dx.doi.org/10.1038/s41467-020-20102-6

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