Sistemas de uso e manejo do solo: acúmulo de carbono e atributos físicos
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Data
2013-07-25
Autores
Seben Junior, Getulio de Freitas [UNESP]
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Editor
Universidade Estadual Paulista (Unesp)
Resumo
Os solos tropicais sob mata nativa (MN) apresentam uma redução acentuada no estoque de carbono orgânico (CO) e, consequentemente, na sua qualidade estrutural, após a conversão para sistemas de manejo, como o sistema de cultivo convencional do solo (SCC) e o sistema de semeadura direta (SSD). Entretanto, a redução na mobilização do solo associado ao cultivo intensivo e diversificado de plantas em sequências de culturas pode incrementar CO no solo e proporcionar melhorias à qualidade estrutural do solo. Assim, os objetivos deste estudo foram: i) avaliar a dinâmica do CO e os atributos físicos do solo sob SCC e SSD em comparação à MN; ii) avaliar o efeito de sequências de culturas em SSD, por oito anos, sobre a dinâmica do CO e os atributos físicos do solo, e iii) avaliar o efeito de sequências de culturas em SSD, por nove anos, sobre a dinâmica do CO e, os efeito deste, sobre a agregação do solo. Foi amostrado a camada de 0 – 10 cm de um Latossolo Vermelho argiloso. Os sistemas de uso e manejo avaliados foram: MN (fragmento de Mata Atlântica); SCC (mais de 50 anos); SSD (9 anos). As sequências de culturas em SSD foram: três culturas de verão: milho/milho (MM); soja/soja (SS); e soja/milho (SM); e, sete culturas de inverno: milho, girasol, nabo forrageiro, milheto, feijão guandu, sorgo e crotalária, conduzidas seguindo o delineamento experimental em faixas, com três repetições. O SSD e o SCC reduziram o conteúdo e o estoque de CO, o índice de estabilidade de agregados (IEA), o diâmetro médio geométrico (DMG), a porosidade total (PT), a macroporosidade (MA) e o intervalo hídrico ótimo (IHO) e incrementaram a densidade do solo (DS) e a resistência tênsil dos agregados (RT) do solo em comparação à MN. O SSD incrementou o IEA, o DMG, a DS, a RT e microporosidade (MI) e reduziu a PT e a MA do solo em comparação ao SCC. O solo sob MN não apresentou limites para o IHO
Soils of the tropics under native forest (NF) exhibit a marked reduction in soil organic carbon (SOC) and also the structural quality after conversion to management systems, such as conventional tillage system (CT) and the no-tillage system (NT). However, absence of soil mobilization associated with an intense/diverse cropping sequence can return SOC into the soil and enhance soil structural quality. Thus, the objectives of this study were: i) evaluate the SOC dynamic and soil physical attributes under CT and NT in comparison than soil under NF; ii) evaluate the effects of cropping sequences in NT, after eight years, on SOC dynamic and soil physical attributes; and iii) evaluate the effect of cropping sequences in NT, after nine years, on SOC dynamic and its influences on soil aggregation. The soil studied was a clayey Oxisol at 0 to 10 cm depth. The use and management systems were: NF (Mata Atlântica forest); CT (more than 35 years); and NT (9 years). The cropping sequences were compost by three summer crops: corn/corn (CC); soybean/soybean (SS); and soybean/corn, and by seven winter crops: corn, sunflower, oilseed radish, pearl millet, pigeon pea, grain sorghum and sunn hemp, carried out according to a split-block design, with three replications. The NT and CT decreased SOC content and stock, water stable aggregates (WSA) mean weight diameter of soil aggregates (MWD), total soil porosity (TP), macroporosity (MA), and the least limiting water range (LLWR), and increased soil bulk density (BD) and tensile strength (TS) than those under NF. Soil under NT had higher MWD, BD, TS and microporosity (MI) but, smaller TP and MA than those under CT. Soil under NF did not attain critical values for LLWR. Soil under CT presented critical BD of 1.46 Mg m-3 and under NT of 1.40 Mg m-3. After eight years, soil under SC and CC had higher MWD (3.63 and 3.55 mm, respectively). Soil under CC had the highest ...
Soils of the tropics under native forest (NF) exhibit a marked reduction in soil organic carbon (SOC) and also the structural quality after conversion to management systems, such as conventional tillage system (CT) and the no-tillage system (NT). However, absence of soil mobilization associated with an intense/diverse cropping sequence can return SOC into the soil and enhance soil structural quality. Thus, the objectives of this study were: i) evaluate the SOC dynamic and soil physical attributes under CT and NT in comparison than soil under NF; ii) evaluate the effects of cropping sequences in NT, after eight years, on SOC dynamic and soil physical attributes; and iii) evaluate the effect of cropping sequences in NT, after nine years, on SOC dynamic and its influences on soil aggregation. The soil studied was a clayey Oxisol at 0 to 10 cm depth. The use and management systems were: NF (Mata Atlântica forest); CT (more than 35 years); and NT (9 years). The cropping sequences were compost by three summer crops: corn/corn (CC); soybean/soybean (SS); and soybean/corn, and by seven winter crops: corn, sunflower, oilseed radish, pearl millet, pigeon pea, grain sorghum and sunn hemp, carried out according to a split-block design, with three replications. The NT and CT decreased SOC content and stock, water stable aggregates (WSA) mean weight diameter of soil aggregates (MWD), total soil porosity (TP), macroporosity (MA), and the least limiting water range (LLWR), and increased soil bulk density (BD) and tensile strength (TS) than those under NF. Soil under NT had higher MWD, BD, TS and microporosity (MI) but, smaller TP and MA than those under CT. Soil under NF did not attain critical values for LLWR. Soil under CT presented critical BD of 1.46 Mg m-3 and under NT of 1.40 Mg m-3. After eight years, soil under SC and CC had higher MWD (3.63 and 3.55 mm, respectively). Soil under CC had the highest ...
Descrição
Palavras-chave
Matéria orgânica, Rotação de cultivos, Solo - Uso, Solos - Manejo, Solos - Agregação, Fisica do solo, Soil-binding
Como citar
SEBEN JUNIOR, Getulio de Freitas. Sistemas de uso e manejo do solo: acúmulo de carbono e atributos físicos. 2013. x, 88 p. Tese (doutorado) - Universidade Estadual Paulista, Faculdade de Ciências Agrárias e Veterinárias de Jaboticabal, 2013.