颗粒形状对间断级配土内侵蚀影响的透明土试验研究

    Experimental study on effect of particle shape on erosion intermittenting graded soils using transparent soil

    • 摘要: 内侵蚀是造成天然沉积物或土工建筑物发生渗透破坏的主要原因之一。在渗流过程中,颗粒形状是影响土体内侵蚀发展的重要因素。当前,对于土体渗流内侵蚀的试验研究受限于真实的土体和常规的渗透仪,对内侵蚀的作用机制和影响因素的研究尚存不足,而涉及颗粒形状对土体渗流内侵蚀影响的试验研究则更为有限。着眼于上述关键问题,基于复杂形状的颗粒生成算法、3D打印技术和透明土技术,利用研发的透明土渗流内侵蚀试验装置,开展了不同颗粒形状下间断级配土的渗流内侵蚀试验研究,探究了颗粒形状对间断级配土内侵蚀发展的影响规律,揭示了不同颗粒形状下土体内侵蚀发展过程的细观机理。试验结果表明,颗粒形状是决定内侵蚀特性的一个重要因素。平均纵横比(AR)低的细长颗粒组成的试样相较于球形颗粒试样,在渗流过程中有更高的细粒侵蚀率和更快的侵蚀速率;而形状参数d2-8值高的棱角状颗粒组成的试样,细粒侵蚀率和侵蚀速率都更小,较小的细粒侵蚀率也导致了渗透系数增长率的减少。此外,透明土内部细观图揭示了粗颗粒骨架间的孔隙喉道结构差异是导致不同颗粒形状下内侵蚀发展不同的根本原因。

       

      Abstract: Internal erosion is one of the main causes of seepage damage in natural sediments or geotechnical structures. In the seepage process, particle shape is an important factor affecting the development of erosion in soil. At present, the experimental research on the internal erosion of soil seepage is limited by real soil and conventional permeameters. The research on the mechanism and influencing factors of internal erosion is still insufficient, and the experimental research on the effect of particle shape on the internal erosion of soil seepage is even more limited. Focusing on the above key issues, this paper uses the transparent soil seepage internal erosion test device developed based on the complex shape particle generation algorithm, 3D printing technology and transparent soil technology to carry out the seepage internal erosion test of discontinuous graded soil with different particle shapes. The influence of particle shape on the development of internal erosion in discontinuous graded soil is explored, and the mesoscopic mechanism of the erosion development process in soil with different particle shapes is revealed. The experimental results show that particle shape is an important factor in determining the characteristics of internal erosion. The samples composed of elongated particles with low average aspect ratio (AR) have higher fine-grain erosion rate and faster erosion rate during seepage compared with spherical particles; while the samples composed of angular particles with high shape parameter d2-8 values have smaller fine-grain erosion rate and erosion rate. The smaller fine-grain erosion rate also leads to a decrease in the permeability coefficient growth rate. In addition, the internal mesoscopic map of transparent soil reveals that the difference in pore throat structure between coarse particle skeletons is the fundamental reason for the distince development of internal erosion under different particle shapes.

       

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