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 of transparent soil on the effect of particle shape on erosion within interrupted graded soils

    • 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。自主设计了基于透明土技术的渗流内侵蚀试验装置,利用球谐算法和3D打印技术,制备了具有指定形状特征的3D打印透明颗粒试样,开展了不同颗粒形状下间断级配土的渗流内侵蚀试验,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小的长条形颗粒组成的试样相比球形颗粒组成的试样具有更高的细粒侵蚀率和更快的侵蚀速度,在内侵蚀过程中渗透系数的增长率也更大;球谐因子d2-8 (颗粒形状参数)更大的棱角型颗粒形成的骨架具有更好的稳定性,其细粒侵蚀率、侵蚀速度以及渗流过程中的渗透系数的增长率都更小。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. A transparent soil seepage test device was designed independently. Based on the spherical harmonic algorithm and 3D printing technology, samples with 3D printed transparent particle with specified shape characteristics were prepared. Seepage internal erosion tests of discontinuous graded soils with different particle shapes were carried out to explore the influence of particle shape on the development of internal erosion in discontinuous graded soils. The mesoscopic mechanism of the erosion development process in soils with different particle shapes was further revealed by combining transparent soil technology. The test results show that particle shape is an important factor in determining the characteristics of internal erosion. The sample composed of elongated particles with a small aspect ratio AR have a higher fine particle erosion ratio and a faster erosion speed than the sample composed of spherical particles, and the growth rate of permeability coefficient during internal erosion is also greater; the skeleton formed by angular particles with a larger spherical harmonic factor d2-8 (particle shape parameter) has better stability, and its fine particle erosion ratio, erosion speed, and growth rate of permeability coefficient during seepage are smaller. In addition, the internal mesoscopic map of transparent soil reveals that the differences in pore throat structure between the coarse particle skeletons is the fundamental reason for the different development of internal erosion under different particle shapes.

       

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