Soil compaction at the depth of mobilization by tillage implements may occur under some soil conditions. The objective of this study was to ver'/> Minimum tillage: effects of compaction and deformation under chisel plow
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Minimum tillage: effects of compaction and deformation under chisel plow

机译:最小耕作:凿犁下的压实和变形影响

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> face="Verdana, Arial, Helvetica, sans-serif" size="2">Soil compaction at the depth of mobilization by tillage implements may occur under some soil conditions. The objective of this study was to verify the existence of compaction under the working depth and evaluate the effect of chisel plow in soil under determined levels of compaction. The treatments in study were 13 years of no-tillage and no-tillage with additional compaction. Horizontal force (FH), Draught (FT), vertical forces (FV), and moment (Mo) associated the chisel tool, operation specific resistance, mobilized area, elevation area, swelling, soil penetration resistance, and physical properties of soil were determined. The additional compaction showed an increment of 18.9% in the horizontal force and draught. The greatest contribution of additional compaction was in vertical force, which provided an increment of 78.2%, showing that the load action is mainly in the vertical direction. No-tillage demonstrated smaller draught demand per mobilized soil area compared to additional compaction treatment. Instead of occurring compaction under the chisel action depth, there was soil mobilization, resulting in smaller soil mechanical penetration resistance in this layer.
机译:> face =“ Verdana,Arial,Helvetica,sans-serif” size =“ 2”>在某些土壤条件下,耕作机具动员深度的土壤压实。这项研究的目的是验证在工作深度下是否存在压实,并在确定的压实水平下评估凿犁在土壤中的作用。研究中的处理方式为免耕13年,再压实免耕。水平力(F H ),吃水(F T ),垂直力(F V )和力矩(M o <确定与凿子工具相关的操作比电阻,动员面积,高程区域,膨胀,土壤渗透阻力和土壤物理性质。额外的压实表明水平力增加了18.9%,并且吃水了。附加压实的最大作用是在垂直力上,增加了78.2%,这表明载荷作用主要在垂直方向上。与其他压实处理相比,免耕表明动员土壤面积的吃水需求少。土壤动员不是在凿子作用深度下进行压实,而是使土壤动机械阻力减小。

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