杨振北, 胡东旭, 汪时机. 膨胀土胀缩裂隙演化及其扰动规律分析[J]. 农业工程学报, 2019, 35(17): 169-177. DOI: 10.11975/j.issn.1002-6819.2019.17.021
    引用本文: 杨振北, 胡东旭, 汪时机. 膨胀土胀缩裂隙演化及其扰动规律分析[J]. 农业工程学报, 2019, 35(17): 169-177. DOI: 10.11975/j.issn.1002-6819.2019.17.021
    Yang Zhenbei, Hu Dongxu, Wang Shiji. Quantitative study of evolution law of expansion-shrinkage crack and its disturbance rule of expansive soil[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(17): 169-177. DOI: 10.11975/j.issn.1002-6819.2019.17.021
    Citation: Yang Zhenbei, Hu Dongxu, Wang Shiji. Quantitative study of evolution law of expansion-shrinkage crack and its disturbance rule of expansive soil[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2019, 35(17): 169-177. DOI: 10.11975/j.issn.1002-6819.2019.17.021

    膨胀土胀缩裂隙演化及其扰动规律分析

    Quantitative study of evolution law of expansion-shrinkage crack and its disturbance rule of expansive soil

    • 摘要: 为定量研究膨胀土胀缩裂隙的演化特征及其对土体的扰动规律,从而探究其引发工程和生态环境灾害的机理。论文对合肥膨胀土进行干湿循环-CT(computed tomography)扫描试验,从获取的CT图中提取灰度值以及灰度共生矩阵特征值:角二阶矩(angular second moment,ASM)和对比度(contrast,CON),研究在干湿循环作用下裂隙图像的灰度值及其纹理的变化规律;并通过三轴剪切试验研究了在干湿循环作用下膨胀土的强度特征。结果表明:1)图像灰度值随裂隙的发育状态而变化;初始阶段灰度值沿试样轴向分布比较离散,但在后期逐渐均匀,离散系数在3次干湿循环后达到最大值,比干湿循环前增加了106%,随后逐渐减小;2)ASM随干湿循环次数的增加而减小,并且在0°和90°方向上的值比在45°和135°方向上的值大9%;CON随干湿循环次数的增加而减小,并且在0和90°方向上的值比在45°和135°方向上的值小52%,其对纹理的方向差异性更加敏感;3)胀缩裂隙对原状膨胀土的结构性会造成破坏,强度劣化显著;在5次干湿循环后,2种土强度分别降低62%和46%,并且原状膨胀土与重塑膨胀土强度的差值也由347.3 kPa降至21.3 kPa ;4)由ASM和CON定义的扰动函数与由土体原生联结结构强度定义的扰动函数,扰动过程中函数变化曲线吻合度高,故基于灰度共生矩阵特征值的扰动函数能很好地描述胀缩裂隙扰动下的膨胀土强度特性。

       

      Abstract: Abstract: Expansive soil is a kind of multi-fissure clay rich in hydrophilic minerals. Its strong characteristics of water absorption expansion and water loss contraction make it very sensitive to the change of environmental humidity. In the process of rainfall and evaporation under natural conditions, the structure of expansive soil shows softening characteristics after the initiation and development of dilatant cracks. Its strength and deformation resistance gradually decline and easily lead to slope collapse, subgrade settlement and damage of water conservancy facilities. The degradation of soil strength has a negative impact on the agricultural ecological environment. In order to quantitatively study the evolution characteristics of swelling and shrinkage cracks of expansive soil and the law of disturbance to soil mass, so as to analyze the mechanism of the engineering and ecological environment disasters caused by soil strength degradation, drying and wetting cycle-CT tests on Hefei expansive soil are carried out to obtain the CT images of the internal structure of soil mass under different drying-wetting cycles. The gray value of CT image is extracted to study the change rule of gray value with the action of dry and wet circulation and the distribution characteristics along the axial direction of the sample. Based on the texture feature research method of grayscale symbiosis matrix, the feature values of grayscale symbiosis matrix (Angular Second Moment, ASM and Contrast, CON) are extracted from the CT images to analyze the texture change rules of the crack images in the dry-wet cycle disturbance of expansive soil. In addition, the structural strength of natural expansive soil under the action of drying-wetting cycle is studied by triaxial shear test. The results show that the image gray value reduces along the development of cracks gradually. In the early stage of the drying-wetting cycle, the average gray value is distributed in the axial direction of the sample, but it is gradually uniform in the later stage. The discrete coefficient reaches to its maximum value after three drying-wetting cycles, which increase to 106% compared with that before the dry and wet cycle. The angular second moment (ASM) decreases with the increase of the times of drying-wetting cycles. Moreover, its value in the directions of 0° and 90° is higher than that in the directions of 45° and 135° to 9%. Contrast (CON) decreases with the increase of the numbers of drying-wetting cycles. The value in the 0 °and 90° directions is smaller than that in the 45° and 135° directions to 52%. Thus, it is more sensitive to the direction of texture. The expansion and contraction cracks damage the structure of the undisturbed expansive soil. After five drying-wetting cycles, the strength of the two soils decrease by 62% and 46% respectively, and the difference between the strength of undisturbed expansive soil and remold expansive soil also decrease from 347.3 to 21.3 kPa. The curves of the disturbance functions defined by angular second moment, contrast and the strength of the original soil connection structure are highly coincident. The eigenvalue disturbance function can better describe the strength characteristics of expansive soil under the disturbance of the expansion and contraction cracks.

       

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