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dc.contributor.authorBERNARDI, A. C. de C.
dc.contributor.authorSEGNINI, A.
dc.contributor.authorPRIMAVESI, O. M. A. S. P. R.
dc.contributor.authorOLIVEIRA, P. P. A.
dc.contributor.authorPEZZOPANE, J. R. M.
dc.contributor.authorBERNDT, A.
dc.contributor.authorBAYER, C.
dc.contributor.authorMILORI, D. M. B. P.
dc.contributor.authorSILVA, W. T. L. da
dc.contributor.authorSIMOES, M. L.
dc.contributor.authorMARTIN NETO, L.
dc.date.accessioned2021-11-18T12:01:20Z-
dc.date.available2021-11-18T12:01:20Z-
dc.date.created2021-11-18
dc.date.issued2021
dc.identifier.citationIn: FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS. Recarbonizing global soils: a technical manual of recommended management practices. Rome: FAO, 2021. (Cropland, grassland, integrated systems and farming approaches: case studeis, v.4). Cap. 32.
dc.identifier.isbn978-92-5-134897-0
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1136264-
dc.descriptionThis study case aimed to evaluate the impact of liming and mineral fertilization of a Signalgrass pasture on C accumulation in surface and deeper layers of a Brazilian Oxisol. A 27-yr old Signalgrass pasture ((Urochloa decumbens cv. Basilisk Stapf (Syn: Brachiaria)) was used in the trial. This pasture has been grazed in a stocking rate of one animal per ha and did not receive any liming and fertilizer until the beginning of the experiment. Treatments used in a 6-year trial are described in Table 129, and both limestone and fertilizers were applied to the soil surface with no soil plowing or disc-harrowing. Soil C stocks were calculated in equivalent soil mass, taking the native Cerrado (Savanna forest) soil mass as reference. Limed soil (0-100 cm) under non-fertilized pasture showed an annual increase of 1.71 tC/ha after 6 years over the soil under native vegetation. In contrast, fertilization of low productive and degraded pasture resulted in C accumulation rates varying from 5.4 to 7.2 t/ha/yr. The results illustrate that despite the C saturation in the surface soil layer, as evidenced by a sigmoid relationship between C contents in the whole soil and the clay fraction through the soil profile, the large proportion of C accumulation (from 55 to 68 percent) in deeper soil layers makes tropical pasture soils suitable long-term C sinks.
dc.language.isoeng
dc.rightsopenAccesseng
dc.subjectMineral fertilization
dc.subjectSoil organic carbon stocks
dc.subjectAdaptation to climate change
dc.subjectMitigation to climate change
dc.subjectPotential drawbacks
dc.subjectILPFeng
dc.titleIncreasing yield and carbon sequestration in a signalgrass pasture by liming and fertilization in São Carlos, São Paulo, Brazil.
dc.typeParte de livro
dc.subject.nalthesaurusSoil management
dc.subject.nalthesaurusLiming
dc.subject.nalthesaurusNo-tillage
dc.subject.nalthesaurusGrasslands
dc.subject.nalthesaurusGreenhouse gas emissions
dc.format.extent2p.352-363.
riaa.ainfo.id1136264
riaa.ainfo.lastupdate2021-11-18
dc.contributor.institutionALBERTO CARLOS DE CAMPOS BERNARDI, CPPSE; ALINE SEGNINI, USP; ODO MARIA ARTUR S P R PRIMAVESI, CPPSE; PATRICIA PERONDI ANCHAO OLIVEIRA, CPPSE; JOSE RICARDO MACEDO PEZZOPANE, CPPSE; ALEXANDRE BERNDT, CPPSE; CIMÉLIO BAYER, UFRGS; DEBORA MARCONDES BASTOS PEREIRA, CNPDIA; WILSON TADEU LOPES DA SILVA, CNPDIA; MARCELO LUIZ SIMOES, CNPDIA; LADISLAU MARTIN NETO, CNPDIA.
Aparece nas coleções:Capítulo em livro científico (CPPSE)

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