2014
DOI: 10.1016/j.agee.2013.12.003
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Soil carbon and nitrogen stocks and fractions in a long-term integrated crop–livestock system under no-tillage in southern Brazil

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Cited by 111 publications
(79 citation statements)
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“…No differences were found among grazing treatments regarding C released from soybean residue (Figures 1 D, E, F), which leads to lower stable organic matter formation, especially under high-intensity grazing systems (G10), as observed after 10 years of trial establishment (Assmann et al, 2014a). Carbon release was greater in soybean leaves, being approximately double the value of stem C release, reaching a total amount of 300 kg ha -1 .…”
Section: Resultsmentioning
confidence: 89%
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“…No differences were found among grazing treatments regarding C released from soybean residue (Figures 1 D, E, F), which leads to lower stable organic matter formation, especially under high-intensity grazing systems (G10), as observed after 10 years of trial establishment (Assmann et al, 2014a). Carbon release was greater in soybean leaves, being approximately double the value of stem C release, reaching a total amount of 300 kg ha -1 .…”
Section: Resultsmentioning
confidence: 89%
“…However, dung amounts increased with grazing intensity, but with low magnitude, from 0.46 Mg ha -1 for G40 to 1.22 Mg ha -1 for G10. Soil residue covering (litter and dung) is considered essential for maintaining C and N surpluses (Assmann et al, 2014a). It is important to consider that, for grazed areas, part of the consumed forage nutrients (grazed) returns to the system via dung and urine, being available for subsequent cropping (Haynes & Williams, 1993).…”
Section: Resultsmentioning
confidence: 99%
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“…Com o aumento das áreas de ILPF e SAFs, visa-se atingir um potencial de mitigação de 18 a 22 milhões Mg CO 2 -eq (Plano..., 2012). No entanto, o sistema de ILPF é complexo e pode ser usado em diversos tipos de arranjos, planejados de acordo com características intrínsecas de cada local (Assmann et al, 2014). Além disso, é importante ressaltar que o Brasil tem uma grande extensão territorial, o que implica ampla diversidade de ambientes físicos, que podem influenciar significativamente as emissões de gases de efeito estufa, uma vez que elas estão diretamente ligadas às condições edafoclimáticas, à tecnologia de produção agrícola e ao manejo da cultura utilizada.…”
Section: Introductionunclassified
“…This higher carbon concentration was due to plant residue accumulation during crop growth (Freixo et al, 2002;Lovato et al, 2004;Sisti et al, 2004;Hickmann and Costa, 2012;Asmann et al, 2014). Furthermore, it could be due to a decrease in mineralization rate (DICK, 1983).…”
Section: Resultsmentioning
confidence: 99%