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Simple shear tests on unsaturated soils

机译:在不饱和土壤上简单的剪切测试

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摘要

Rainfall induces landslides in several geo-environmental contexts through a variety of triggering mechanisms. In shallow covers of unsaturated silts or loose sands, static liquefaction may occur upon shearing or wetting. The paper proposes simple shear and wetting tests performed on remoulded specimens of air-fall volcanic pyroclastic silty sands from Sarno site (Italy), where huge flowslides occurred. Simple shear wetting tests reproduce the initial stress conditions in the field as well as the stress path of the most common triggering mechanisms which take place during critical rainfalls. The tests are carried out through the Unsaturated Simple Shear apparatus designed at the University of Salerno. First, simple shear tests are performed in dry and saturated conditions and the results compared in terms of shear strength and volumetric response. Then, wetting tests-under constant vertical stress or constant shear stress-are performed. The experimental results are presented and the future research is outlined.
机译:通过各种触发机制,降雨在几个地理环境背景下引起滑坡。在不饱和淤泥或松散砂的浅盖中,剪切或润湿时可能发生静电液化。本文提出了对来自Sarno位点(意大利)的空落火山粘性粉状沙滩的重新熔化和润湿试验,发生了巨大的絮凝物。简单的剪切润湿试验再现领域的初始应力条件以及在临界降雨期间发生的最常见触发机制的应力路径。测试是通过在萨勒诺大学设计的不饱和简单的剪切装置进行。首先,在剪切强度和体积反应方面,在干燥和饱和条件下进行简单的剪切试验和结果。然后,进行润湿试验 - 在恒定的垂直应力或恒定剪切应力下进行。提出了实验结果,并概述了未来的研究。

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