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Bearing capacity of strip footings on unsaturated soils by the slip line theory

机译:滑移线理论在非饱和土上条形基础的承载力

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The bearing capacity of strip footings on unsaturated soils is studied using slip line theory. The suction profiles considered are non-uniform with depth and correspond to vertical flow of water by infiltration or evaporation. The slip line theory assumes a plastic equilibrium state of a Mohr-Coulomb soil in which suction influences are included using the effective stress concept. This paper shows the similar and independent effects of cohesion and the contribution of suction to the effective stress in the governing equations. It shows that the influence of a non-uniform suction profile on bearing capacity is significant, and the depth to the ground water table and the footing width have significant roles in how much suction influences the bearing capacity. By approximating the contribution of suction to the effective stress as a function that varies linearly with depth, the effect of suction on bearing capacity is represented in dimensionless form in separate charts for smooth and rough footings. Using the charts the bearing capacity can be determined for any combination of friction angle, footing width, surcharge, soil unit weight and linear profiles of cohesion and the contribution of suction to the effective stress. An example is given which highlights the significant influence suction can have. These charts also permit assessment of bearing capacity changes that may occur when changes to suction are expected, due to seasonal fluctuations of soil moisture, drought or flooding. (C) 2016 Elsevier Ltd. All rights reserved.
机译:利用滑移线理论研究了带状地基在非饱和土上的承载力。所考虑的吸力曲线在深度上是不均匀的,并且对应于渗透或蒸发引起的垂直水流。滑移线理论假定Mohr-Coulomb土的塑性平衡状态,其中使用有效应力概念包括了吸力影响。本文显示了控制方程中内聚力和吸力对有效应力的相似和独立的影响。结果表明,不均匀的吸力曲线对承载力的影响是显着的,而地下水位的深度和基础宽度对吸力影响承载力的影响很大。通过将吸力对有效应力的贡献近似为随深度线性变化的函数,吸力对承载力的影响以无量纲形式在单独的图表中表示出来,以表示平滑和粗糙的基础。使用图表可以确定摩擦角,基脚宽度,附加力,土壤单位重量和内聚力的线性分布以及吸力对有效应力的贡献的任意组合。给出了一个示例,突出显示了吸力可能产生的重大影响。这些图表还允许评估由于土壤水分,干旱或洪水的季节性波动而在预期吸力发生变化时可能发生的承载力变化。 (C)2016 Elsevier Ltd.保留所有权利。

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