王晓燕, 姚志华, 党发宁, 董忠级. 裂隙膨胀土细观结构演化试验[J]. 农业工程学报, 2016, 32(3): 92-100. DOI: 10.11975/j.issn.1002-6819.2016.03.014
    引用本文: 王晓燕, 姚志华, 党发宁, 董忠级. 裂隙膨胀土细观结构演化试验[J]. 农业工程学报, 2016, 32(3): 92-100. DOI: 10.11975/j.issn.1002-6819.2016.03.014
    Wang Xiaoyan, Yao Zhihua, Dang Faning, Dong Zhongji. Meso-structure evolution of cracked expansive soils[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2016, 32(3): 92-100. DOI: 10.11975/j.issn.1002-6819.2016.03.014
    Citation: Wang Xiaoyan, Yao Zhihua, Dang Faning, Dong Zhongji. Meso-structure evolution of cracked expansive soils[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2016, 32(3): 92-100. DOI: 10.11975/j.issn.1002-6819.2016.03.014

    裂隙膨胀土细观结构演化试验

    Meso-structure evolution of cracked expansive soils

    • 摘要: 为研究裂隙膨胀土的细观结构特征,对重塑膨胀土进行了干湿循环、三轴浸水和各向等压加载试验。利用CT(computerized tomography)机对试验过程中进行无损实时动态扫描,从细观上分析膨胀土裂隙的产生以及裂隙在水和外力作用下的闭合全过程。将细观扫描数据与宏观物理参数相联系,研究裂隙对膨胀土变形特征的影响。结果表明:无约束情况下对膨胀土进行干湿循环,试样边缘以及孔洞聚集区易形成裂隙;干湿循环造成膨胀土体积收缩存在一个稳定渐近线,体缩会趋于1个稳定值。裂隙膨胀土在浸水初期产生膨胀力并出现湿胀变形;随着浸水量的增加,软化效应产生且膨胀力逐渐减小,在围压和偏应力压缩作用下继而出现体缩现象;浸水后期,在偏应力作用下试样产生剪胀破坏,再次出现轻微剪胀变形。在水和荷载作用下,不规则裂隙和孔洞逐渐演化为较规则的圆形孔洞,且圆形孔洞趋于闭合;仅在外力作用时,裂隙较难完全闭合;水和外力的共同作用使得膨胀土裂隙的闭合效果要优于单纯施加荷载时的闭合效果。裂隙膨胀土在各向等压加载过程中存在明显屈服现象,以屈服点为分界,扫描数据和孔隙比随荷载的增大分为快速体缩段和缓慢体缩段,前者与裂隙在荷载作用下闭合并演化成孔洞有关;后者与加载后期孔洞较难闭合且形成的新结构具备抵御外部荷载的能力有关。研究成果可为进一步认识裂隙对膨胀土力学特性的影响提供参考。

       

      Abstract: Abstract: The crack property of expansive soil is one of the important characteristics, which is different from other types of soils. The development of cracks greatly affects the engineering properties of expansive soils. In order to study the meso-structural characteristic of cracked expansive soil, the dry-wet cycle test, triaxial soaking test and isotropic loading test were carried out on the remolded expansive soil in scientific research station of Logistics Engineering University in Hanzhong city, Shanxi province, China. The data including volumetric strain and deviatoric strain were obtained by these tests. Using CT (computerized tomography), test samples were scanned nondestructively in real-time to obtain CT images. The whole evolving process of cracks in expansive soils was investigated under the action of water and external force from the microscopic view. The effect of the crack on the macro-meso deformation behavior of expansive soil was studied by the relationship between the micro data and macro physical parameters. Test results showed that, under unconstrained conditions of dry-wet cycles, the edges and the gathering holes area of expansive soil sample were easy to form crack. Volume shrinkage caused by dry-wet cycle of expansive soil had a stable asymptote line and would tend to a stable value. The volume change of the expansive soil had experienced 3 stages in triaxial soaking test with the water and external force. Firstly, in the initial stage of triaxial soaking test, expansive force caused by soaking water led to wetting expansive deformation of cracked expansive soil. Secondly, the softening effect appeared and the expansion force gradually decreased with the increase of water content, under the influence of confining pressure and deviatoric stress, the shearing shrinkage was followed. Thirdly, in the late period of soaking test, the shear failure of the specimen under the effect of deviatoric stress caused the phenomenon of slight dilation. Cracked expansive soil during isotropic loading process had obvious yield phenomenon, taking yield point as the cut-off point, the curve of scanning data and pore ratio with the load increases was divided into rapid and slow volume shrink period. The rapid volume shrinkable period was related to cracks and holes closure, and the slow volume shrinkable period was related to the formation of the new structure which had ability to resist the external load. From the CT-scanning images of triaxial soaking test and isotropic loading test, under the action of water and external load, the irregular cracks and holes were gradually evolved into a regular circular hole, and the circular hole tended to close. With only the action of the external force, the crack was more difficult to complete closure. The interaction of water and external force made the expansive soil crack closure effect better than that of only external loading. Therefore, water plays a key role in the effect of the crack 'development of expansive soil. The results would provide valuble information for the further understanding of the influence of cracks on the mechanical properties of expansive soil.

       

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