2016
DOI: 10.1590/1809-4392201500193
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Variação temporal do efluxo de CO2do solo em sistemas agroflorestais com palma de óleo na Amazônia Oriental

Abstract: A dinâmica do efluxo de dióxido de carbono (CO 2 ) do solo e seus fatores controladores em sistemas agroflorestais da Amazônia são pouco compreendidas. O objetivo deste estudo foi avaliar a variação temporal do efluxo de CO 2 do solo em sistemas agroflorestais onde a palma de óleo é a cultura principal e sua relação com fatores bióticos (carbono microbiano do solo, carbono total do solo, respiração microbiana do solo, raízes finas do solo, indivíduos componentes dos sistemas agroflorestais (SAFs) ) e abióticos… Show more

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Cited by 17 publications
(16 citation statements)
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References 27 publications
(27 reference statements)
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“…The rainiest season caused a rise in C SMB in all planting areas (Table 2). Aragão et al (2012) and Silva et al (2016) also found increases in C content in biomass during the rainiest season. This may be associated with an increase in nutrient availability with increasing precipitation as well as a decrease in aluminum saturation.…”
Section: Resultsmentioning
confidence: 78%
“…The rainiest season caused a rise in C SMB in all planting areas (Table 2). Aragão et al (2012) and Silva et al (2016) also found increases in C content in biomass during the rainiest season. This may be associated with an increase in nutrient availability with increasing precipitation as well as a decrease in aluminum saturation.…”
Section: Resultsmentioning
confidence: 78%
“…It is known that, due to its extraordinary carbon retention capacity and greater CO 2 flow in the soil in agroforestry systems, oil palm lays basis for the implementation of a clean development mechanism capable of improving environmental quality (Dias et al, 2010;Pezarico et al, 2013;Silva et al, 2016). However, prior to planting, it must be mainly assessed whether rainfall is enough to ensure the productivity of planted areas.…”
Section: Resultsmentioning
confidence: 99%
“…O FCO 2 é resultado da atividade microbiana e respiração das raízes, todavia, por adição dos fatores ambientais temperatura e umidade, pode haver aumento ou diminuição das emissões devido a variabilidade temporal, conforme destacam Silva et al (2016). Verifica-se também que a Tsolo apresentou valores médios idênticos estatisticamente nas duas áreas estudadas, variando 26,14 ºC para área de cacau, e 27,83ºC para área de café.…”
Section: Resultsunclassified