ISSN 1000-3665 CN 11-2202/P
    李志杰, 宋晶, 赵洲, 杨守颖, 黄坚森. 吹淤取样扰动的数值分析——层理分析法[J]. 水文地质工程地质, 2020, 47(2): 120-125. DOI: 10.16030/j.cnki.issn.1000-3665.201909023
    引用本文: 李志杰, 宋晶, 赵洲, 杨守颖, 黄坚森. 吹淤取样扰动的数值分析——层理分析法[J]. 水文地质工程地质, 2020, 47(2): 120-125. DOI: 10.16030/j.cnki.issn.1000-3665.201909023
    LIZhijie, . Sample disturbance numerical analysis of hydraulically dredged mud sampling——bedding analysis method[J]. Hydrogeology & Engineering Geology, 2020, 47(2): 120-125. DOI: 10.16030/j.cnki.issn.1000-3665.201909023
    Citation: LIZhijie, . Sample disturbance numerical analysis of hydraulically dredged mud sampling——bedding analysis method[J]. Hydrogeology & Engineering Geology, 2020, 47(2): 120-125. DOI: 10.16030/j.cnki.issn.1000-3665.201909023

    吹淤取样扰动的数值分析——层理分析法

    Sample disturbance numerical analysis of hydraulically dredged mud sampling——bedding analysis method

    • 摘要: 航道疏浚淤泥通过吹填成为了目前扩充城市土地的主要手段之一,分析吹填淤泥样品的扰动情况是工程的关键环节。本文基于吹填淤泥颗粒流3D模型,研究了取土器贯入过程对样品结构的扰动特征,提出了通过拟合的旋转抛物面来评价样品结构扰动的微观信息。其中:层理拟合曲面表征样品的表观变形,结构性拟合曲面的系数量化界定样品的微扰动区与破坏区。该模拟试验能够为工程地质的评价提供参考依据,优化取土器的设计参数,减少实际工况中过于保守的设计和施工产生的费用。试验结果表明:土样颗粒整体表现为向上的微隆起且层理呈倒U型分布,不同层理的扰动程度不同,同一层理的不同部位扰动程度也不同;层理的表观变形可用旋转抛物面公式拟合,各层理的特征拐点分布规律亦可用旋转抛物面公式拟合;曲面外的区域为强扰动区,曲面内的区域为微扰动区,这两个区域的体积积分占比可作为样品原状性评价的参考依据。

       

      Abstract: Dredging of the channel has become one of the main means of expanding urban land through dredging. Analyzing the disturbance of dredging samples is a key part of the project. Based on the particle flow 3D model, we studied the disturbance characteristics of the sample structure during the penetration and proposed a fitting rotating paraboloid to evaluate the microscopic information of sample structure disturbance. Among them: the layered fitting surface characterizes the apparent deformation of the sample, and the coefficient of the structurally fitted surface quantizes the micro-disturbing zone and the destruction zone of the sample. The test can provide a reference for evaluation of engineering geology and optimization of sampler’s design, and reduce the costs on over-conservative design and construction in actual work. The results indicate that the soil particles show an upward micro-uplift and an inverted U-shaped bedding. The degree of disturbance of different bedding is different, and the degree of disturbance of different parts of the same bedding is different. The apparent deformation of the bedding can be fitted by a rotating paraboloid formula. The distribution law of the feature inflection points of each layer can also be fitted by the paraboloid of rotation paraboloid; the area outside the surface is a strong disturbance zone, and the area inside the surface is a micro-disturbance zone. The volume integral ratio of these two regions can be used as the evaluation of the originality of the sample.

       

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