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Field investigation of deformation characteristics and stress mobilisation of a soil slope

机译:土质边坡变形特征与应力动员的现场研究

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摘要

Stress mobilisation and deformation of a slope are important for engineers to carry out reliable design of retaining systems. However, most case histories reported mainly on the response of pore-water pressure (PWP), whereas knowledge about the stress-deformation characteristics of slope is limited. In this study, a saprolitic soil slope was instrumented to monitor not only the responses of PWP but also horizontal stress and horizontal displacement. To assist in the interpretation of field data, a series of laboratory tests was conducted to characterise the volume change behaviour of soil taken from the site, under the effects of both net stress and suction. During a rainstorm event when positive PWP built up, a remarkably large displacement of 20 mm was recorded between 5.5 and 6 m depths, and the top 5 m of the slope exhibited translational down-slope movement. This caused an increase in effective horizontal stress by 350%, which reached a peak value close to 40% of an effective passive stress. During the subsequent dry season when suction was recovered, an up-slope rebound of 10 mm was recorded. Comparison of field and laboratory data reveals that the rebound was attributed to suction-induced soil shrinkage. This rebound led to a decrease in the effective horizontal stress previously built up during the storm event.
机译:应力的移动和边坡变形对于工程师进行可靠的固定系统设计很重要。但是,大多数案例历史报告主要是关于孔隙水压力(PWP)的响应,而关于边坡应力变形特征的知识是有限的。在这项研究中,使用了一种不饱和土壤边坡,不仅可以监测PWP的响应,还可以监测水平应力和水平位移。为了帮助解释现场数据,在净应力和吸力的作用下,进行了一系列实验室测试以表征取自现场的土壤的体积变化行为。在暴雨事件中,当正PWP累积时,记录到5.5 mm至6 m深度之间20 mm的显着大位移,并且斜坡的顶部5 m出现平移下坡运动。这导致有效水平应力增加了350%,达到的峰值接近有效被动应力的40%。在随后的干旱季节,当吸力恢复时,记录到了10毫米的上坡反弹。田间和实验室数据的比较表明,回弹归因于吸力引起的土壤收缩。这种反弹导致先前在风暴事件期间建立的有效水平应力减小。

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