Micronutrient availability in amazonian dark earths and adjacent soils

dc.contributor.authorSátiro, José Nivaldo De Oliveira
dc.contributor.authorMotta, Antônio Carlos Vargas
dc.contributor.authorDemetrio, Wilian Carlo
dc.contributor.authorSegalla, Rodrigo F.
dc.contributor.authorCremonesi, Marcus Vinicius
dc.contributor.authorAraújo, Eloá Moura
dc.contributor.authorFalcão, Newton Paulo de Souza
dc.contributor.authorMartins, Gilvan Coimbra
dc.contributor.authorMuniz, Aleksander Westphal
dc.contributor.authorTaube, Paulo Sérgio
dc.contributor.authorRebellato, Lilian
dc.contributor.authorOliveira Júnior, Raimundo Cosme de
dc.contributor.authorTeixeira, Wenceslau Geraldes
dc.contributor.authorNeves, Eduardo Goés
dc.contributor.authorLima, Helena Pinto
dc.contributor.authorShock, Myrtle Pearl
dc.contributor.authorKille, Peter
dc.contributor.authorCunha, Luis
dc.contributor.authorBrown, George G.
dc.contributor.authorNetwork, Tpi
dc.date.accessioned2021-05-14T21:12:34Z
dc.date.available2021-05-14T21:12:34Z
dc.date.issued2021
dc.description.abstractAmazonian Dark Earths (ADEs) are highly fertile soils in areas with predominance of unfertile soils. However, the variation in nutrient availability between regions and the resilience of ADEs to modern agricultural use is still little known, particularly regarding micronutrient contents. Hence, the present study synthesized current information of ADE impacts on extractable micronutrient (Cu, Ni, Fe, Mn, Zn, B) contents at different soil depths and assessed in detail the role of both soil depth and land-use type on extractable Cu, Ni, Fe, Mn and Zn in nine ADEs and adjacent (ADJ) soils from different Amazonian regions. The land-use systems chosen were secondary old (OF) or young (YF) forests, and agricultural systems (AS) in Iranduba, Belterra and Porto Velho. Only eight studies compared extractable (Mehlich-1) micronutrient contents at 21 sites with ADEs and ADJ soils, but only four studies included depths greater than 30 cm, and B and Ni were evaluated in only one study. Higher Mn and Zn, but lower Fe contents were found in ADEs both from literature data and in the present study, especially in the first 30 cm depth. Increases in extractable Ni and Cu in ADEs varied according to the site and the land use considered. Micronutrient contents tended to decrease with depth, but varied depending on the element, site, soil type and land use. Sites with modern agriculture showed few differences in extractable micronutrient contents, except for a decrease in Fe in Belterra and Mn in Porto Velho. Considering the high amounts of some micro- and macronutrients in ADEs further work is warranted concerning soil management and nutrient balance in plants grown on these soils. © 2021 The Authorspt_BR
dc.identifier.doi10.1016/j.geoderma.2021.115072
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/37685
dc.language.isoenpt_BR
dc.publisher.journalGeodermapt_BR
dc.relation.ispartofVolume 395; number 115072pt_BR
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Brazil*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/br/*
dc.subjectADEpt_BR
dc.subjectAnthropic activitypt_BR
dc.subjectFertilitypt_BR
dc.subjectTerra Pretapt_BR
dc.subjectTrace elementspt_BR
dc.titleMicronutrient availability in amazonian dark earths and adjacent soilspt_BR
dc.typeArtigopt_BR

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