Use este identificador para citar ou linkar para este item: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1127465
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dc.contributor.authorJAROSCH, K.
dc.contributor.authorHURTARTE, L. C. C.
dc.contributor.authorGAVAZOV, K.
dc.contributor.authorMUNIZ, A. W.
dc.contributor.authorMÜLLER, C.
dc.contributor.authorSCHWEIZER, S.
dc.date.accessioned2020-12-03T09:04:01Z-
dc.date.available2020-12-03T09:04:01Z-
dc.date.created2020-12-02
dc.date.issued2020
dc.identifier.citationIn: EGU GENERAL ASSEMBLY, 2020, Vienna, Austria. Abstracts... Vienna, EGU, 2020.
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1127465-
dc.descriptionThe conversion of tropical forest for cassava cultivation is widely known to decrease the soil organic matter (OM) and nutrient contents of highly weathered soils in the tropics. Amazonian Dark Earth (ADE) might be affected less due to their historical anthropogenic amelioration with e.g. charcoal, ceramics and bones, leading to higher soil OM and nutrient concentrations. In this study, we analysed the effect of land use change on the OM dynamics and its composition under tropical conditions, using ADE and an adjacent Acrisol (ACR) as model systems.eng
dc.language.isoeng
dc.rightsopenAccesseng
dc.subjectTerra Preta de Índio
dc.titleLand use change in Amazonian Dark Earth and Acrisol: responses of organic carbon, organic matter composition and microbial carbon utilisation.
dc.typeResumo em anais e proceedings
riaa.ainfo.id1127465
riaa.ainfo.lastupdate2021-01-11 -02:00:00
dc.identifier.doihttps://doi.org/10.5194/egusphere-egu2020-19752
dc.contributor.institutionKlaus Jarosch, University of Bern; Luis Carlos Colocho Hurtarte, Technical University of Munich; Konstantin Gavazov, Swiss Federal Institute for Forest; ALEKSANDER WESTPHAL MUNIZ, CPAA; Christoph Müller, Justus-Liebig University Giessen; Steffen Schweizer, Technical University of Munich.
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