Iron oxides and aluminous clays selectively control soil carbon storage and stability in the humid tropics

Clay minerals and pedogenic metal (oxyhydr)oxides are the most reactive soil mineral constituents controlling the long-term persistence of organic carbon (OC) in terrestrial ecosystems. However, their co-occurrence in most soils complicates direct assessment of their individual contribution to OC pe...

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Detalles Bibliográficos
Autores principales: Kirsten, Maximilian, Mikutta, Robert, Vogel, Cordula, Thompson, Aaron, Mueller, Carsten W., Kimaro, Didas N., Bergsma, Huig L. T., Feger, Karl-Heinz, Kalbitz, Karsten
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7970839/
https://www.ncbi.nlm.nih.gov/pubmed/33658688
http://dx.doi.org/10.1038/s41598-021-84777-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7970839/
https://www.ncbi.nlm.nih.gov/pubmed/33658688
http://dx.doi.org/10.1038/s41598-021-84777-7

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