dc.contributorSantino, Marcela Bianchessi da Cunha
dc.contributorhttp://lattes.cnpq.br/2356641063223397
dc.contributorBianchini Junior, Irineu
dc.contributorhttp://lattes.cnpq.br/0659731944736389
dc.contributorhttp://lattes.cnpq.br/0572834860009727
dc.creatorGrando, Mariana Soares
dc.date.accessioned2018-07-03T14:02:12Z
dc.date.available2018-07-03T14:02:12Z
dc.date.created2018-07-03T14:02:12Z
dc.date.issued2018-02-26
dc.identifierGRANDO, Mariana Soares. Mudanças climáticas e ciclagem de carbono na decomposição aeróbia e anaeróbia de Myriophyllum aquaticum (Vellozo) Verdecourt. 2018. Dissertação (Mestrado em Ecologia e Recursos Naturais) – Universidade Federal de São Carlos, São Carlos, 2018. Disponível em: https://repositorio.ufscar.br/handle/ufscar/10247.
dc.identifierhttps://repositorio.ufscar.br/handle/ufscar/10247
dc.description.abstractAquatic macrophytes are key organisms in freshwater environments, as they are intrinsically linked to primary productivity, nutrient and carbon cycling and detritus formation in these environments. The temperature is one of the major factors that act directly in the detritus decomposition, performing functions in the enzymatic metabolism of the decomposing microorganisms. The hypothesis tested in the present study was that the labile and refractory macrophyte fractions are positively influenced by the increase in temperature at 2ºC during the detritus decomposition of Myriophyllum aquaticum. Thus, this study compared the aerobic and anaerobic decomposition of M. aquaticum at two temperatures (21 and 23ºC). In the laboratory, were set up decomposition chambers (n = 252), containing entire, particulate and dissolved detritus of the macrophyte, and water from the Monjolinho Reservoir. On each sampling day, the contents of the chambers were fractionated into particulate organic matter (MOP) and dissolved organic matter (MOD), which was subsequently converted into carbon basis. Carbon basis mass loss, temporal variations of pH, electrical conductivity and aromatization degree of the dissolved fraction in the decomposition chambers were evaluated according to detritus type, temperature and dissolved oxygen availability. With the obtained results, a mathematical model of first order was applied and it was possible to verified that: (i) from the kinetic model used, the particulate organic carbon (COP) presented two distinct fractions, a labile/soluble (COPLS) and a refractory (COPR); (ii) the labile content decayed faster than the refractory; (iii) there was formation of dissolved refractory substances (e.g. humic compounds) for all treatments; (iv) the increase in temperature at 2ºC positively influenced the mass loss of the labile/soluble and refractory fraction of the entire, particulate and dissolved detritus; (v) the global Q10 was higher in anaerobic condition; (vi) about pH, there were significant differences (p <0.05) between entire aerobic treatment at 21ºC and 23ºC and (vii) for electrical conductivity, there were significant differences for most of all treatments.
dc.languagepor
dc.publisherUniversidade Federal de São Carlos
dc.publisherUFSCar
dc.publisherPrograma de Pós-Graduação em Ecologia e Recursos Naturais - PPGERN
dc.publisherCâmpus São Carlos
dc.rightsAcesso aberto
dc.subjectCoeficiente de decaimento
dc.subjectEfeito estufa
dc.subjectMineralização
dc.subjectModelagem matemática
dc.subjectCoefficient decay
dc.subjectGreenhouse effect
dc.subjectMineralization
dc.subjectMathematical modeling
dc.titleMudanças climáticas e ciclagem de carbono na decomposição aeróbia e anaeróbia de Myriophyllum aquaticum (Vellozo) Verdecourt
dc.typeTesis


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