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    含水率变化对四川山矾根土摩阻特性和边坡稳定性影响

    Effects of soil moisture content changes on friction characteristics and slope stability of Symplocos setchuensis

    • 摘要: 含水率是土壤物理性质中变化最频繁的指标,不但影响土体的表观强度,还影响根土力学作用。目前浅层边坡稳定性评估研究中,关于土壤含水率对根系固土能力影响的考虑较少。为明确根土界面特性—土壤含水率的关系,并探讨在边坡稳定分析中考虑该关系的必要性,本研究开展以土壤含水率为变量的根土直剪摩擦试验,并将3种不同模型下根土界面摩阻特性(“本文动态模型”、Wu模型和FBM模型)分别纳入对根系附加强度的估算中,最后采用GEO-Studio软件对边坡稳定性进行模拟。结果表明:1)随着土壤含水率的增加,四川山矾根系抗拉和拔强度均与根径呈负幂函数关系,2条曲线通常具有交点,其对应的根径随着含水率升高先增后减,范围为0.12~2.75 mm;2)随着土壤含水率的增加,实测的根土界面摩擦系数先增后减;3)3种模型估算的根增附加黏聚力crcr(f) < cr(FBM) < cr(Wu),且含水率越高,cr(f)与cr(FBM)和cr(Wu)的偏差越大;4)将3种模型下根增附加黏聚力cr纳入边坡稳定性评估中,边坡稳定系数均随含水率升高而降低,“本文动态模型”稳定系数的估算值更保守,Wu和FBM模型约为“本文动态模型”的1.53和1.02倍,说明分析植被边坡稳定性时应考虑根土界面摩擦特性随土壤含水率的动态变化。

       

      Abstract:
      Background Moisture content is the most frequently changing indicator of soil physical properties, which not only affects the apparent strength of the soil, but also affects the root-soil mechanical action. In the current shallow slope stability assessment researches, the impact of soil moisture content on the root reinforcement is rarely considered.
      Methods In order to clarify the relationship between the root-soil interfacial characteristics and the soil moisture content, and to study the influence of soil moisture on the friction coefficient of root-soil complex, root shear strength and root failure mode, we carried out Symplocos setchuensis root tensile test, root-soil friction experiment based on nine soil moisture content gradients. Then we estimated the additional cohesion of root (cr) under three models through BSTEM (bank stability and toe erosion model) to contrastively analyze root reinforcement. At last, we used GEO-Studio to evaluate slope stability and to analyze the change of slope stability under different soil moisture contents.
      Results 1) The tensile strength and pull-out strength of S. setchuensis roots decreased with the increase of root diameter, and the two curves usually had an intersection point and its corresponding root diameter first increased and then decreased (0.12 - 2.75 mm). 2) The friction coefficient of root-soil interface decreased with the increase of soil moisture content. 3) The additional cohesion of roots (cr) both increased with the increase of soil moisture content when considering the frictional characteristics of root-soil interface under different soil moisture content: cr(f) < cr(FBM) < cr(Wu), the deviation of cr(f) to cr(FBM) and cr(f) to cr(Wu). 4) The slope factor of safety (Fs) decreased with the increase of soil moisture content, and it was more conservative when considering the characteristics of root-soil interface. Fs(Wu) and Fs(FBM) were about 1.53 and 1.02 times of Fs(f).
      Conclusions Soil moisture content influenced the failure mode and pull-out strength of roots by affecting the frictional characteristics of root-soil interface, and thus influenced the soil reinforcement. This indicated that dynamic changes of frictional characteristics of root-soil interface should be considered in analyzing the stability of planted slope under dynamic soil moisture content. This research also provided a more conservative dynamic root reinforcement model compare with Wu and FBM model, which took the weakening mechanism of soil moisture content into account.

       

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