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Experimental Investigation of Three-dimensional Densely Packed Sand Cutting Processes

机译:三维密集堆砂切割工艺的实验研究

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2D and 3D models of the process of cutting saturated soil with an infinitely wide blade that is at an inclined angle to the cutting direction have been developed and used in the dredging industry. However, in practice, the width of the cutting blade used is limited. In order to obtain more insight into the three-dimensional process of cutting saturated soil, laboratory experiments on soil cutting were made. This paper relates to the preparation of the densely packed and 'reproducible' sand in the laboratory and the determination of the relationship between the porosity obtained from density tests and the in situ penetration force. This force can be obtained by using cone penetration tests to determine the porosity of the soil in situ. The paper gives results of measurements of the pore water pressures on the surface of the cutting blade and their distribution in the longitudinal and transverse directions and also includes graphs showing the pore water pressure during the cutting process. For a blade of limited width, the experimental results showed that in the longitudinal direction the excess pore water pressure on the surface increases nearly linearly from the top of the blade, reaching its maximum value at the about 4/5 of the length of the blade and then decreases. In the transverse direction the excess pore water pressure on the surface of the blade is systemically distributed; the maximum value is at the centre of the blade and this value decreases from the centre to the side of the blade.
机译:已经开发了2D和3D模型,该模型使用与切割方向成倾斜角度的无限宽的铲刀切割饱和土壤。但是,实际上,所使用的切割刀片的宽度是有限的。为了更深入地了解切割饱和土壤的三维过程,我们进行了土壤切割的实验室实验。本文涉及在实验室中制备密实且“可复制”的砂子,以及确定从密度试验获得的孔隙率与原位穿透力之间关系的方法。可以通过使用圆锥体渗透测试确定原位土壤的孔隙度来获得该​​力。本文给出了切割刀片表面孔隙水压力的测量结果及其在纵向和横向上的分布,还提供了显示切割过程中孔隙水压力的图表。对于宽度有限的叶片,实验结果表明,沿纵向方向,表面上的多余孔隙水压力从叶片顶部开始几乎呈线性增加,在叶片长度的约4/5处达到最大值。然后减少。在横向方向上,叶片表面的多余孔隙水压力系统地分布。最大值位于刀片的中心,并且该值从刀片的中心到侧面减小。

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