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Hydro-mechanical reinforcements of live poles to slope stability

机译:带电杆的液压机械加固以提高边坡稳定性

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Soil bioengineering using live poles is an environmentally friendly technique for shallow slope stabilisation. However, it remains unclear in this technique whether the hydrological effects of pole transpiration are significant to slope stabilisation, compared to mechanical reinforcement by structural poles and their fibrous roots. The aims of this study were to investigate the hydro-mechanical reinforcement effects of live poles and to evaluate their effectiveness for shallow slope stabilisation, giving due consideration to the different pole growth stages. Finite-element seepage-stability models were developed and validated against centrifuge model tests that investigated the rainfall-induced instability of a 45-degree clayey sand slope subjected to intense rainfall. The short-term stability right after the installation of the poles is critical because only structural poles, i.e., without fibrous root reinforcement or water uptake, are insufficient for reinforcement, even those as long as 2 m. Due to the absence of pole transpiration, positive pore water pressure of up to 10 kPa was built up near the slope toe, causing the significant mobilisation of shear strain and consequentially slope failure. In longer term, during which fibrous roots developed and provided additional mechanical reinforcement (via root cohesion) and transpiration-induced suction, no slope failure occurred due to the considerable amount of suction that was retained within the pole zone. It was mainly the pole transpiration before the rainfall, i.e., antecedent drying, that retained the suction, rather than the transpiration that took place during the rainfall. (C) 2018 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society.
机译:使用带电杆进行土壤生物工程学是一种用于稳定浅层边坡的环保技术。但是,与通过结构杆及其纤维根进行机械加固相比,杆蒸发的水文影响是否对边坡稳定是否显着尚不清楚。这项研究的目的是研究活动杆的水力机械加固效果,并评估其对浅层边坡稳定的有效性,并适当考虑了不同的杆生长阶段。建立了有限元渗流稳定性模型,并通过离心模型试验进行了验证,该模型试验研究了降雨引起的强降雨下45度黏土砂质边坡的不稳定性。立杆安装后的短期稳定性至关重要,因为只有结构杆(即没有纤维状根部加固或不吸水)不足以进行加固,即使是长达2 m的结构。由于没有极地蒸腾作用,在斜坡脚趾附近建立了高达10 kPa的正孔隙水压力,从而引起了剪切应变的显着动员并因此导致了斜坡破坏。从长远来看,在此期间,纤维状根部发育并提供了额外的机械加固作用(通过根部内聚力)和蒸腾作用引起的吸力,但由于极区内保留了大量的吸力,因此没有发生边坡破坏。保持吸力的主要因素是降雨之前的极地蒸腾作用,即前期干燥,而不是降雨期间发生的蒸腾作用。 (C)2018年由Elsevier B.V.代表日本岩土工程学会制作和托管。

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