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首页> 外文期刊>Bulletin of engineering geology and the environment >Investigation on the macro‑ and microdeformation characteristics of silty clay under different shield construction stress paths
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Investigation on the macro‑ and microdeformation characteristics of silty clay under different shield construction stress paths

机译:不同盾构施工应力路径下粉质粘土宏观和微道和微道和微码特性的研究

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Geotechnical investigation and design show that when evaluating the settlement of ground with soft soil ground, the use of a single stress path results in a larger error than in the case of a multistress path. To understand the influence of a multistress path on the deformation properties and microstructure characteristics of soil, a two-stage stress path (corresponding to three stress states: the in situ state, unloading-loading state, and grouting pressure state) of soil was examined by analytical solution. Then, a series of triaxial tests was conducted to analyze macroscopic deformation properties considering four influencing factors, i.e., the relative distance between the soil and tunnel, stress paths, type of silty clay, and drainage conditions. The results show that axial strain of silty clay caused by the two-stage stress path increases by 31.6% with the relative distance decreasing from 1.67R (R means tunnel radius) to 1.25R on tunnel side, while the volume strain increases by 80% with the relative distance decreasing from 1.21R to 1.06R on tunnel bottom. In addition, the deformation caused by the two-stage stress path (or reconstituted soil or undrained condition) is larger than that caused by the one-stage stress path (or undisturbed soil or drained condition). Finally, through scanning electron microscopy and mercury intrusion porosimetry, the pore size, distribution, shape, and arrangement of silty clay on the bottom and sides of the tunnel were investigated. The research shows that under the two-stage stress path, the number of large pores decrease and that of small pores increase. The probability entropy of pore orientation ranges from 0.834 to 0.971 when silty clay is subjected to a two-stage stress path. This illustrates that the pore order of the soil on tunnel side is better than that on the tunnel bottom.
机译:岩土性调查设计表明,当用软土地划分地面沉降时,使用单个应力路径的使用比多级路径的情况更大。为了了解多级路径对土壤变形性能和微观结构特征的影响,检查了土壤的两级应力路径(对应于三次应力状态:原位状态,卸载加载状态和灌浆压力状态)通过分析解决方案。然后,考虑到四种影响因素,即土壤和隧道,应力路径,粉质类型之间的相对距离和排水条件,分析一系列三轴试验以分析宏观变形特性。结果表明,由两级应力路径引起的粉质粘土的轴向应变增加31.6%,相对距离从1.67r(r表示隧道半径)降低到隧道侧1.25r,而体积应变增加80%在隧道底部的1.21R至1.06R中相对距离降低。此外,由两级应力路径(或重构的土壤或不统治条件)引起的变形大于由单阶段应力路径(或未受干扰的土壤或排水条件)引起的变形。最后,通过扫描电子显微镜和汞入侵孔隙孔测定法,研究了孔径,分布,形状和围绕隧道底部和侧面的粉质粘土的布置。研究表明,在两级应力路径下,大孔隙的数量减少,小孔隙增加。当粉质粘土进行两级应力路径时,孔取向的概率熵范围为0.834至0.971。这说明隧道侧的土壤的孔径优于隧道底部。

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