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Study of primary creep behavior of clayey soils in landslide area : suction effect

机译:滑坡区黏土主要蠕变特性研究:吸力效应

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Creep behavior of clayey soils plays an extremely important role in the landslide process. The soils that make up these sliding zones are often in unsaturated state. This point indicates the need to take into account the suction effect as hydric parameter on the long-term deformation of clayey soils. In this paper, a primary creep model named Modified Time Hardening (MTH) for unsaturated soils with different matric suction has been built. Based on the literature tests results[1][2], parameters C1 and C2 of the model have relations with suction and deviator stress level respectively. The primary creep strainwill be able to demonstrate unsaturated effect of the soils. comparison between the calculated results and the literature tests results shows a good coherence. The work underway at the university of Orleans will show later the relevance of model used in the present work.
机译:黏土的蠕变行为在滑坡过程中起着极其重要的作用。构成这些滑动带的土壤通常处于不饱和状态。这一点表明有必要将吸力效应作为水力参数考虑到黏土的长期变形上。在本文中,建立了具有不同基质吸力的非饱和土的基本蠕变模型,称为修正时间硬化(MTH)。根据文献测试结果[1] [2],模型的参数C1和C2分别与吸力和偏应力水平有关。初级蠕变应变将能够证明土壤的非饱和作用。计算结果与文献测试结果之间的比较显示出良好的一致性。奥尔良大学正在进行的工作将在以后显示当前工作中使用的模型的相关性。

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