Please use this identifier to cite or link to this item: http://repositorio.ufla.br/jspui/handle/1/32758
Full metadata record
DC FieldValueLanguage
dc.creatorBispo, Diêgo Faustolo Alves-
dc.creatorSilva, Alexandre Christofaro-
dc.creatorChristofaro, Cristiano-
dc.creatorSilva, Marx Leandro Naves-
dc.creatorBarbosa, Maurício Soares-
dc.creatorSilva, Bárbara Pereira Christofaro-
dc.creatorBarral, Uidemar Morais-
dc.creatorFabris, José Domingos-
dc.date.accessioned2019-02-08T18:57:42Z-
dc.date.available2019-02-08T18:57:42Z-
dc.date.issued2016-08-
dc.identifier.citationBISPO, D. F. A. et al. Hydrology and carbon dynamics of tropical peatlands from Southeast Brazil. Catena, Amsterdam, v. 143, p. 18-25, Aug. 2016.pt_BR
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S0341816216301278#!pt_BR
dc.identifier.urihttp://repositorio.ufla.br/jspui/handle/1/32758-
dc.description.abstractPeatlands are important natural carbon reservoirs and regulators of water flow and of its dynamic in many natural areas. The structural integrity of these systems has been recognizably threatened by anthropic interventions but has also been significantly influenced by the global climate changes. This study aimed to characterize the water and carbon dynamics in watersheds of two peats independently supplying the Araçuaí River basin in the northeastern Minas Gerais state, Brazil. The peats, which were found to be in different states of natural conservation, were investigated for their physical and chemical characteristics, both of the peats and of their stored water. The 14C isotopic analyses of the peat and measurements of the water and organic carbon storage capacity of these peats were performed. The geneses of the corresponding profiles were found to have initiated between the early Holocene (7664 years BP) and the late Pleistocene (11,129 years BP) periods with a vertical growing rate between 0.10 and 0.61 mm y− 1. The difference in the degree of natural conservation on the dynamic of water and carbon between these peats was checked by the water and soil attributes. Large quantities of water (mean value for these two peats, approximately 10,108 m3 ha− 1) and organic carbon (200 ton C ha− 1) were presumably stored during its pedogenetic history. The more anthropically altered peat presented a negative carbon balance and lower water flow in the dry season. The influence of human activities on their carbon and water dynamics reinforces the importance of protecting and conserving these native areas.pt_BR
dc.languageen_USpt_BR
dc.publisherElsevierpt_BR
dc.rightsrestrictAccesspt_BR
dc.sourceCatenapt_BR
dc.subjectWater qualitypt_BR
dc.subjectCarbon flowpt_BR
dc.subjectCarbon stockpt_BR
dc.subjectWater stockpt_BR
dc.subjectHydrologypt_BR
dc.subjectQualidade da águapt_BR
dc.subjectFluxo de carbonopt_BR
dc.subjectEstoque de carbonopt_BR
dc.subjectEstoque de águapt_BR
dc.subjectHidrologiapt_BR
dc.titleHydrology and carbon dynamics of tropical peatlands from Southeast Brazilpt_BR
dc.typeArtigopt_BR
Appears in Collections:DCS - Artigos publicados em periódicos

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.