土结构参数化设计与场性能

R. Paranthaman, S. Azam
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引用次数: 0

摘要

土结构的稳定性受材料特性、环境载荷和边坡几何形状引起的场不确定性的影响。本研究设计了一种系统的方法来捕捉野外不确定性对天然和人工边坡稳定性的影响。通过逐步改变边坡几何形状,随机生成抗剪强度参数,形成新的设计图形。采用子集模拟方法确定了不同坡度下土壤性质的安全范围。这些图表应用于三个已发表的案例研究,这些案例研究具有复杂油田环境导致的不同触发机制。在没有地下水位的情况下,所有被调查的边坡在报告的几何形状和抗剪强度参数下都是稳定的(安全系数(FOS) bbb1.0)。通过历史拟合,捕捉了土壤性质变化和环境条件对地下水位波动的影响。结果表明了三种不同的破坏机制:在施工过程中,由于孔隙水压力的增加,冰碛垄(弗农,不列颠哥伦比亚省)地基沉降(无护堤的FOS = 1.45,有护堤的FOS = 2.24);由层状冰湖黏土(Labret, Saskatchewan)组成的自然切口(FOS = 0.98)由于长时间降雨导致整个斜坡饱和而不稳定;冰川冰碛垄(艾伯塔省Hamelin Creek)上的压实填充物(FOS = 0.98)因斜坡上冻结层融化引起的土壤饱和而坍塌。这一验证表明,新方法完全捕捉了环境荷载(导致斜坡的地下水位变化),并通过土壤特性部分捕捉了施工实践和现场地质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Parametric Design and Field Behavior of Earthen Structures
The stability of earthen structures is governed by field uncertainties arising from material properties, environment loading, and slope geometry. This research devised a systematic approach to capture the effects of field uncertainties on the stability of natural and manmade slopes. New design charts were developed by incrementally changing slope geometry and randomly generating shear strength parameters. Subset simulation was used to determine the safe range of soil properties for various slopes. The charts were applied to three published case studies with distinct triggering mechanisms resulting from complex field settings. All of the investigated slopes were found to be stable (factor of safety (FOS) > 1.0) under the reported geometry and shear strength parameters while assuming no water table. The effects of soil properties’ variation and environmental conditions on fluctuating water table were captured through history matching. Results indicated three distinct failure mechanisms: foundation settlement of a glacial moraine till (Vernon, British Columbia) due to an increased pore water pressure during construction of the compacted fill (FOS = 1.45 without berms and 2.24 with berms); instability in the natural cut (FOS = 0.98) comprising layered glacio-lacustrine clays (Labret, Saskatchewan) due to saturation of the entire slope resulting from a long duration rainfall; and collapse of a compacted fill (FOS = 0.98) on a glacial moraine till (Hamelin Creek, Alberta) due to soil saturation arising from thawing of a frozen layer in the slope. This validation illustrates that the new approach fully captures environmental loading (resulting in water table variation in the slope) and partly captures construction practice and site geology via soil properties.
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