Fechar

@PhDThesis{Ribeiro:2022:EfUsCo,
               author = "Ribeiro, Kelly",
                title = "Efeito do uso e cobertura da terra na din{\^a}mica do carbono e 
                         nitrog{\^e}nio em turfeiras na v{\'a}rzea do rio 
                         Para{\'{\i}}ba do Sul",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2022",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2021-09-23",
             keywords = "turfeiras, gases de efeito estufa, estoque de carbono, peatlands, 
                         greenhouse gases, carbon stock.",
             abstract = "As turfeiras armazenam grande quantidade de carbono (C) e t{\^e}m 
                         atuado como sumidouros de CO2 atmosf{\'e}rico, mas tamb{\'e}m 
                         podem se comportar como importantes fontes de Gases de Efeito 
                         Estufa (GEE) para a atmosfera (CO2, CH4 e N2O) quando submetidas a 
                         drenagem e mudan{\c{c}}a no seu uso alterando a cobertura da 
                         terra. Quantificar os estoques de carbono em turfeiras, bem como 
                         os par{\^a}metros que regulam a din{\^a}mica de C e tamb{\'e}m 
                         do nitrog{\^e}nio (N) {\'e} essencial para subsidiar 
                         pol{\'{\i}}ticas p{\'u}blicas que visem a prote{\c{c}}{\~a}o 
                         desses ecossistemas. Este estudo teve como objetivo avaliar o 
                         efeito da mudan{\c{c}}a do uso e da cobertura da terra na 
                         din{\^a}mica do carbono e nitrog{\^e}nio em turfeiras na 
                         v{\'a}rzea do Rio Para{\'{\i}}ba do Sul, considerando as 
                         coberturas da terra, bem como a an{\'a}lise temporal feita em 
                         cronossequ{\^e}ncia. Coleta de amostras de solo e de ar foram 
                         realizadas em 24 locais entre 2019 e 2020 nas esta{\c{c}}{\~o}es 
                         secas e chuvosas bem como na transi{\c{c}}{\~a}o entre elas. Os 
                         fluxos foram medidos utilizando-se c{\^a}maras est{\'a}ticas de 
                         PVC com coletas de amostras em per{\'{\i}}odos de 30 minutos, em 
                         solos cobertos por florestas, pastagens e agricultura e em 
                         {\'a}reas >10 anos e <10 anos. Os resultados evidenciam solos 
                         org{\^a}nicos, altamente {\'a}cidos (pH <4,3) e de alta 
                         densidade 0,87 g/cm³), com teor de mat{\'e}ria org{\^a}nica por 
                         volta de 39%. Concentra{\c{c}}{\~o}es elevadas de macro e 
                         micronutrientes foram observadas na regi{\~a}o, especialmente 
                         nitrog{\^e}nio (m{\'e}dia 0,47%), Fe (m{\'e}dia 266,67 mg/kg) e 
                         Ca (m{\'e}dia de 640,47mg/kg), associadas principalmente {\`a} 
                         deposi{\c{c}}{\~a}o seca e ao manejo agr{\'{\i}}cola. Os 
                         resultados mostram fluxo m{\'e}dio de (1660,79 ± 1729,86) g m-2 
                         ano-1 de CO2 , (0,30 ± 1,41) g m-2 ano-1 de CH4 e (0,45 ± 0,9) g 
                         m-2 ano-1 de N2O, n{\~a}o apresentando diferen{\c{c}}as 
                         significativas entre as coberturas do solo nem mesmo nas 
                         cronossequ{\^e}ncias adotadas. Os resultados indicaram que, neste 
                         ecossistema, as emiss{\~o}es foram reguladas por 
                         caracter{\'{\i}}sticas qu{\'{\i}}micas e f{\'{\i}}sicas do 
                         solo, principalmente a profundidade do n{\'{\i}}vel 
                         fre{\'a}tico que regulou os n{\'{\i}}veis de 
                         satura{\c{c}}{\~a}o do solo. Os fluxos de CO2 foram maiores 
                         quando o n{\'{\i}}vel fre{\'a}tico atingiu 1,5 metros de 
                         profundidade e menores quando atingiu a superf{\'{\i}}cie do 
                         solo, favorecendo a emiss{\~a}o de CH4. O estoque de carbono 
                         acumulado nas camadas de 0-20cm variou entre 159,2 e 470,5 Mg C 
                         ha-1, totalizando 482 Tg de C e a decomposi{\c{c}}{\~a}o da 
                         mat{\'e}ria org{\^a}nica do solo promoveu a perda m{\'e}dia de 
                         carbono de 1164,63 GgCO2eq.ano-1 (varia{\c{c}}{\~a}o entre 
                         -52,20 e 7458,21 GgCO2eq.ano-1) representando valores at{\'e} 
                         5,4% das emiss{\~o}es totais no estado de S{\~a}o Paulo, 
                         evidenciando que as turfeiras s{\~a}o fontes significativas de 
                         GEE e devem ser consideradas nos invent{\'a}rios regionais. 
                         Assim, fica evidente que aprofundar o entendimento da 
                         din{\^a}mica do carbono e do nitrog{\^e}nio, bem como dos 
                         par{\^a}metros que regulam as emiss{\~o}es de GEE, nestes solos, 
                         s{\~a}o de extrema import{\^a}ncia na conserva{\c{c}}{\~a}o 
                         dos estoques de carbono na regi{\~a}o. ABSTRACT: Peatlands store 
                         large amounts of carbon (C) and have acted as sinks of atmospheric 
                         CO2, but they can also act as important sources of Greenhouse 
                         Gases (GHG) to the atmosphere (CO2, CH4 and N2O) when subjected to 
                         drainage and change in its use by altering the land cover. 
                         Quantifying carbon stocks in peatlands, as well as the parameters 
                         that regulate the dynamics of C (carbon) and also of N (nitrogen) 
                         is essential to support public policies aimed at protecting these 
                         ecosystems. This study aimed to evaluate the effect of changes of 
                         use and cover lands on the carbon and nitrogen dynamics in 
                         peatlands in the Para{\'{\i}}ba do Sul River 
                         floodplain,considering land cover, as well as a temporal analysis 
                         performed with chronosequence. . Soil and air sample collections 
                         were carried out at 24 sites in 2019 and 2020 during the dry and 
                         rainy seasons as well as in the transition between them. Fluxes 
                         were measured using static PVC chambers and samples were collected 
                         in periods of 30 minutes per chamber, in soils covered by forests, 
                         pastures and agriculture and in areas >10 years and <10 years. The 
                         results show organic, highly acidic (pH <4.3) and high density 
                         (0.87 g/cm³) soils with organic matter content around 39%. High 
                         concentrations of macro and micronutrients were observed in the 
                         region, especially nitrogen (average 0.47%), Fe (average 266,67 
                         mg/kg) and Ca (640,47mg/kg ), mainly caused by dry deposition and 
                         agricultural management. The results show mean fluxes of (1660.79 
                         ± 1729.86) g m-2 year-1 of CO2 , (0.30 ± 1.41) g m-2 year-1 of CH4 
                         and (0.40 ± 0 .8) g m-2 yr-1 of N2O, not showing significant 
                         differences between the soil covers, not even in the adopted 
                         chronosequences. The results indicated that, in this ecosystem, 
                         emissions were regulated by chemical and physical characteristics 
                         of the soil, mainly the depth of the water table that regulates 
                         the levels of soil saturation. The CO2 fluxes were higher when the 
                         water table reached 1.5 meters deep and the were lower when it 
                         reached the soil surface, favoring the emission of CH4. The carbon 
                         stock accumulated in the 0-20 cm varied between 159.20 and 470,50 
                         Mg C ha- 1, totaling 482 Tg C and the decomposition of soil 
                         organic matter promoted an average carbon loss of 1164.63 
                         GgCO2eq.year-1 (variation between -52.20 and 7458.2079 
                         GgCO2eq.y-1) representing values up to 5.4% of total emissions in 
                         the state of S{\~a}o Paulo, showing that peat is a significant 
                         source of GHG and should be considered in regional inventories. 
                         Thus, it is evident that deepening the understanding of the 
                         dynamics of carbon and nitrogen, as well as the parameters that 
                         regulate GHG emissions into the atmosphere in these soils, are 
                         extremely important in the conservation of carbon stocks in the 
                         region.",
            committee = "Ometto, Jean Pierre Henry Balbaud (presidente) and Alval{\'a}, 
                         Pl{\'{\i}}nio Carlos (orientador) and Pacheco, Felipe Siqueira 
                         (orientador) and Forti, Maria Cristina and Almeida, J{\'u}lio 
                         C{\'e}sar Raposo de and Nogueira, Sandra Furlan",
         englishtitle = "Effect of land use and coverage on the dynamics of carbon and 
                         nitrogen in peatlands in the Para{\'{\i}}ba do Sul river 
                         floodplain",
             language = "pt",
                pages = "121",
                  ibi = "8JMKD3MGP3W34T/45GRKCH",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34T/45GRKCH",
           targetfile = "publicacao.pdf",
        urlaccessdate = "02 maio 2024"
}


Fechar