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A model of stress distribution and cracking in cohesive soils produced by simple tillage implements.

机译:简单耕作工具产生的粘性土壤应力分布和开裂模型。

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摘要

The objective of this research was to further understand the behavior of the soil under the action of a tillage tool, with the purpose of finding a relation between the tool geometry and the resultant soil seed bed. Thus the problem consisted of understanding the mechanics of producing soil break up and to find a logical method of analyzing it.; The problem was solved using fundamental principles of soil mechanics and force equilibrium analyzis. As a result, a mathematical model was developed which describes three failure zones within the cut soil volume. The model can be programmed into a computer to generate maps of normal and shear stresses to visualize the three failure zones.; The failure zones are the shear failure zone, the tensile fracturing zone and the no failure zone. The tensile fracturing zone is delimited by the tensile stress reaching the tensile strength of the soil at the given soil moisture content and soil density. The tensile strength of the soil was measured using an apparatus and method designed in this research.; The mathematical model gives an explanation of the mechanics of crumbling and the shape of the failed volume, but it does not give information concerning soil aggregate quality and arrangement within the soil furrow. Then, a method of analyzing the formed aggregates was developed which considers some soil physical properties of aggregates.; The study concluded that the smaller tool width and the smaller tool rake angle, among the ones used in this research, produced the most efficient geometry in producing the largest amount of soil break up, the most uniform aggregate formation and the most stable aggregate arrangement. The same tool geometry requires less energy per unit volume of soil disturbed. The best performance is produced at the lowest soil water content among those tested.
机译:这项研究的目的是进一步了解耕作工具作用下土壤的行为,以期发现工具的几何形状与所得土壤种子床之间的关系。因此,问题在于理解产生土壤破裂的机理,并找到分析它的逻辑方法。使用土壤力学的基本原理和力平衡分析法解决了该问题。结果,开发了一个数学模型,该模型描述了切土体积内的三个破坏区域。可以将模型编程到计算机中,以生成正应力和切应力图,以可视化三个破坏区域。破坏区域是剪切破坏区域,拉伸断裂区域和无破坏区域。在给定的土壤水分含量和土壤密度下,达到土壤的拉伸强度的拉伸应力限定了拉伸断裂区域。用本研究设计的设备和方法测量土壤的抗张强度。数学模型解释了破碎的机理和破坏体积的形状,但没有提供有关土壤骨料质量和土壤沟内排列的信息。然后,开发了一种分析形成的骨料的方法,该方法考虑了骨料的一些土壤物理性质。该研究得出的结论是,在本研究中使用的工具中,较小的工具宽度和较小的工具前角可产生最有效的几何形状,从而产生最大的土壤破碎量,最均匀的骨料形成和最稳定的骨料排列。相同的工具几何形状每单位体积的土壤扰动需要较少的能量。在测试的土壤中,最低的土壤含水量可获得最佳性能。

著录项

  • 作者单位

    McGill University (Canada).;

  • 授予单位 McGill University (Canada).;
  • 学科 Engineering Agricultural.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 135 p.
  • 总页数 135
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 农业工程;
  • 关键词

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