Please use this identifier to cite or link to this item: https://repositorio.inpa.gov.br/handle/1/18977
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dc.contributor.authorTelles, Everaldo de Carvalho Conceia?o-
dc.contributor.authorCamargo, Plínio Barbosa de-
dc.contributor.authorMartinelli, Luiz Antônio-
dc.contributor.authorTrumbore, Susan Elizabeth-
dc.contributor.authorCosta, Enir Salazar da-
dc.contributor.authorSantos, Joaquim dos-
dc.contributor.authorHiguchi, Niro-
dc.contributor.authorOliveira, Raimundo Cosme-
dc.date.accessioned2020-06-15T22:04:19Z-
dc.date.available2020-06-15T22:04:19Z-
dc.date.issued2003-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/18977-
dc.description.abstractStable and radiocarbon isotopes were used to investigate the role of soil clay content in the storage and dynamics of soil carbon in tropical forest soils. Organic matter in clay-rich Oxisols and Ultisols contains at least two distinct components: (1) material with light δ13C signatures and turnover times of decades or less; and (2) clay-associated, 13C-enriched, carbon with turnover times of decades at the surface to millennia at depths &gt;20 cm. Soil texture, in this case clay content, exerts a major control on the amount of slowly cycling carbon and therefore influences the storage and dynamics of carbon in tropical forest soils. Soils in primary tropical forest have been proposed as a potentially large sink for arthropogenic carbon. Comparison of carbon stocks in Oxisols sampled near Manaus, Brazil, shows no measurable change in organic carbon stocks over the past 20 years. Simple models estimating the response of soil carbon pools to a sustained 0.5% yr<sup/> increase in productivity result in C storage rates of 0.09 to 0.13 MgC ha-1 yr-1 in soil organic matter, with additional potential storage of 0.18 to 0.27 MgC ha-1 yr-1 in surface litter and roots. Most storage occurs in organic matter pools with turnover times less than a decade. Export of carbon in dissolved form from upland terra firme Oxisols likely accounts for &lt;0.2 MgC ha-1 yr-1, but more work is required to assess the export potential for periodically inundated Spodosols.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 17, Número 2, Pags. 9-1pt_BR
dc.rightsRestrito*
dc.subjectCarbon Balanceen
dc.subjectCarbon Cycleen
dc.subjectForest Soilen
dc.subjectSoil Textureen
dc.subjectTropical Soilsen
dc.subjectSouth Americaen
dc.titleInfluence of soil texture on carbon dynamics ans storage potential in tropical forest soils of Amazoniaen
dc.typeArtigopt_BR
dc.publisher.journalGlobal Biogeochemical Cyclespt_BR
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