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A critical evaluation of predictive models for rooted soil strength with application to predicting the seismic deformation of rooted slopes

机译:植根土壤强度预测模型的关键评价,应用于预测生根斜坡的地震变形

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This paper presents a comparative study of three different classes of model for estimating the reinforcing effect of plant roots in soil, namely (i) fibre pull-out model, (ii) fibre break models (including Wu and Waldron's Model (WWM) and the Fibre Bundle Model (FBM)) and (iii) beam bending or p-y models (specifically Beam on a Non-linear Winkler-Foundation (BNWF) models). Firstly, the prediction model of root reinforcement based on pull-out being the dominant mechanism for different potential slip plane depths was proposed. The resulting root reinforcement calculated were then compared with those derived from the other two types of models. The estimated rooted soil strength distributions were then incorporated within a fully dynamic, plane-strain continuum finite element model to assess the consequences of the selection of rooted soil strength model on the global seismic stability of a vegetated slope (assessed via accumulated slip during earthquake shaking). For the particular case considered in this paper (no roots were observed to have broken after shearing), root cohesion predicted by the pull-out model is much closer to that the BNWF model, but is largely over-predicted by the family of fibre break models. In terms of the effects on the stability of vegetated slopes, there exists a threshold value beyond which the position of the critical slip plane would bypass the rooted zones, rather than passing through them. Further increase of root cohesion beyond this value has minimal effect on the global slope behaviour. This implies that significantly over-predicted root cohesion from fibre break models when used to model roots with non-negligible bending stiffness may still provide a reasonable prediction of overall behaviour, so long as the critical failure mechanism is already bypassing the root-reinforced zones.
机译:本文介绍了三种不同类别模型,用于估算土壤中植物根部的增强效果,即(i)纤维拉出模型,(ii)纤维突破模型(包括吴和沃尔沃隆(WWM)和纤维束模型(FBM))和(III)光束弯曲或PY模型(特别是在非线性Winkler-Foundation(BNWF)模型上的光束)。首先,提出了基于拉出的根加强件的预测模型是不同潜在滑动平面深度的主导机构。然后将得到的根加强件与来自其他两种模型的衍生的那些进行比较。然后将估计的生根土壤强度分布纳入完全动态的平面 - 应变连续体有限元模型,以评估根本土壤强度模型对植物坡度的全球地震稳定性的影响(通过地震摇动期间通过累积滑移评估)。对于本文考虑的特定情况(未观察到剪切后未破坏根),通过拉出模型预测的根凝聚力更接近BNWF模型,但大大预测了纤维突破的家族楷模。就植被斜坡稳定性的影响而言,存在阈值超出该阈值,于临界滑动平面的位置将绕过根区域,而不是通过它们。超出该值的根凝聚的进一步增加对全局坡度行为产生最小的影响。这意味着当用于模拟具有不可忽略的弯曲刚度的根部的纤维破裂模型显着过度预测的根凝聚力可能仍然可以提供合理的整体行为预测,只要临界失效机制已经绕过根加强的区域即可。

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