Phosphorus (P) availability and P transformation rates in Amazonian Dark Earth determined by 33P isotopic dilution.

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dc.contributorKlaus Jarosch, University of Bern; Hao Chen, China Agricultural University; Amanda Barbosa Lima, Justus-Liebig University Giessen; ALEKSANDER WESTPHAL MUNIZ, CPAA; Timothy McLaren, Institute of Agricultural Sciences, ETH Zurich; Christoph Müller, Justus-Liebig University Giessen; Emmanuel Frossard, Institute of Agricultural Sciences, ETH Zurich; Astrid Oberson, Institute of Agricultural Sciences, ETH Zurich.
dc.creatorJAROSCH, K.
dc.creatorCHEN, H.
dc.creatorLIMA, A. B.
dc.creatorMUNIZ, A. W.
dc.creatorMcLAREN, T.
dc.creatorMÜLLER, C.
dc.creatorFROSSARD, E.
dc.creatorOBERSON, A.
dc.date2018-04-18T01:43:03Z
dc.date2018-04-18T01:43:03Z
dc.date2018-04-17
dc.date2018
dc.date2018-04-18T01:43:03Z
dc.date.accessioned2026-06-30T23:23:08Z
dc.descriptionAmazonian Dark Earth (ADE) often shows increased soil fertility compared to surrounding soils, likely linked to its increased concentration of soil organic matter and macronutrients such as phosphorus (P). For P, there is little knowledge whether the higher P availability is a result of increased biological processes (such as organic P mineralization) or physico-chemical processes (such as sorption/desorption), or both.
dc.identifierIn: EGU GENERAL ASSEMBLY 2018, Vienna, 2018. Geophysical Research Abstracts, v. 20, EGU2018-18352, 2018.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1090642
dc.identifier.urihttp://hdl.handle.net/123456789/380634
dc.languageeng
dc.rightsopenAccess
dc.subjectAmazonian Dark Earth
dc.subjectFósforo
dc.subjectterra preta
dc.titlePhosphorus (P) availability and P transformation rates in Amazonian Dark Earth determined by 33P isotopic dilution.
dc.typeResumo em anais e proceedings

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