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

Abstract 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...

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Autores principales: Maximilian Kirsten, Robert Mikutta, Cordula Vogel, Aaron Thompson, Carsten W. Mueller, Didas N. Kimaro, Huig L. T. Bergsma, Karl-Heinz Feger, Karsten Kalbitz
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/31989b93a3c64607ad5ba5b1b7b25a88
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