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dc.contributor.authorTONUCCI, R. G.pt_BR
dc.contributor.authorGARCIA, R.pt_BR
dc.contributor.authorNAIR, V.pt_BR
dc.date.accessioned2015-09-04T11:11:11Zpt_BR
dc.date.available2015-09-04T11:11:11Zpt_BR
dc.date.created2015-09-04pt_BR
dc.date.issued2015pt_BR
dc.identifier.citationIn: WORLD CONGRESS ON INTEGRATED CROP-LIVESTOCK-FOREST SYSTEMS; INTERNATIONAL SYMPOSIUM ON INTEGRATED CROP-LIVESTOCK SYSTEMS, 3., 2015, Brasília, DF. Towards sustainable intensification: proceedings. Brasília, DF: Embrapa, 2015.pt_BR
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1023312pt_BR
dc.descriptionAgroforestry systems have the potential to enhance carbon (C) sequestration in soil compared with treeless (agricultural) systems (Montagnini & Nair, 2004). When one type of vegetation is replaced with another, stable isotope contents (?13 C) values can be used to identify soil organic carbon (SOC) derived from residues in the native vegetation and the new vegetation based on discrimination between C3 and C4 plants. The present study aimed to assessing the impact of difference land-use systems on C3 and C4 contribution to SOC. The experimental area is located inside the Cerrado biome. Soil samples were taken from six different land-use sites: (i) native local forest; (ii) Eucalyptus forest (EF) established in 1985 (OEC); (iii) EF established in 2004 (NEC); (iv) pasture of B. decumbens; (v) Agroforestry System (AF) established on 1994 (OAF); and (vi) AF established on 2004 (NAF). The establishment on AF was placed first with the eucalyptus planted and rice (Oryza sativa), soybean (Glycine max) and braquiaria grass (B. Brizantha cv. Marandu) in between trees rows. Soil was collected from four depths (0-10; 10-20; 20-50 and 50-100 cm). For stable C isotope analysis, whole soil was analyzed mass spectrometer. The percentage of SOC derived from the Brachiaria ssp., a C4 plant, or from the eucalyptus or native forest, a C3 plant, was estimated based on the equations: % C4-derived SOC = (?- ?T)/(?G- ?T) x 100 (1); % C3-derived SOC = 100 - % C4-derived SOC (2) Based on the equations 1 and 2 were calculated the contributions of each C3 and C4 species in SOC C-derived, as follows: C3-devived SOC (Mg ha-1) = (% C3-derived SOC) x (SOC content, Mg ha-1) (3); C4-derived SOC (Mg ha-1) = (% C4-derived SOC) x (SOC content, Mg ha-1) (4). A complete randomized design was used with Tukey?s studentized. Statistical differences were considered significant at p <0.05.pt_BR
dc.language.isoengeng
dc.rightsopenAccesseng
dc.subjectSistema agroflorestalpt_BR
dc.subjectOrganic carbonpt_BR
dc.subjectBrasilpt_BR
dc.subjectMinas Geraispt_BR
dc.subjectAgroforestry systemspt_BR
dc.titleTrees and grass contribution to soil organic carbon in agroforestry systems.pt_BR
dc.typeResumo em anais e proceedingspt_BR
dc.date.updated2016-03-04T11:11:11Zpt_BR
dc.subject.thesagroSolopt_BR
dc.subject.thesagroCarbonopt_BR
dc.subject.thesagroComposto orgânicopt_BR
dc.subject.thesagroUso da terrapt_BR
dc.subject.thesagroCerradopt_BR
dc.subject.nalthesaurusSoilpt_BR
dc.subject.nalthesaurusOrganic compoundspt_BR
dc.subject.nalthesaurusLand usept_BR
dc.subject.nalthesaurusBrazileng
riaa.ainfo.id1023312pt_BR
riaa.ainfo.lastupdate2016-03-04pt_BR
dc.contributor.institutionRAFAEL GONCALVES TONUCCI, CNPC; Rasmo Garcia, Federal Univ. of Viçosa (UFV) - Viçosa, MG, Brazil; Vimala Nair, Soil and Water Science Dep. Univ. of Florida, Gainesville.pt_BR
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