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Collapsible soils are problematic by nature. They undergo collapse or sudden settlement or subsidence under a given stress when their water content is increased. Collapse is characterised by collapse potential expressed as ΔH/H x 100, where ΔH is collapse compression. The amount of stress applied and the water content at the time of collapse govern the amount of collapse. In other words, collapse potential depends upon the amount of stress and the water content. Loess and other wind-blown silts are examples of collapsible soils. This paper presents a parametric study on the collapse behaviour of a lateritic soil. Remoulded specimens of a lateritic soil passing through a 425 µm sieve were compacted in 1-D consolidometer or oedometer at a density of 13 kN/m3 for studying collapse under varied initial moisture contents and initial surcharge pressures. Collapse compression of the samples was induced by saturating the specimens with water contents corresponding to 100% degree of saturation. After collapse occurred, the 1-D consolidation tests were continued up to an applied stress of 160 kPa. Collapse behaviour was studied for the applied initial pressures (σi) of 10, 20 and 40 kPa and for the initial water contents (wi) of 5%, 10%, 15% and 20%. Collapse compression and collapse potential decreased with increasing wi for all σi. 相似文献
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CFS桩处理软弱地基的试验研究 总被引:2,自引:0,他引:2
介绍了一种新兴的地基处理技术--水泥粉煤灰钢渣桩(CFS)。采用现场大面积堆放钢坯的方式,模拟研究了CFS桩复合地基工作期间的承载特性,得出了堆载条件下基底的最终沉降量、桩间土体深层水平位移及竖向附加应力分布、临近的人工挖孔桩水平位移及其桩体前(后)附加应力变化等规律,探讨了堆载作用下CFS桩复合地基-临近桩体的共同作用机理。此外,研究了CFS桩施工所引起的环境效应,得出了CFS桩成桩过程中地基土侧向附加应力在水平、垂直方向上的变化规律及A,B试验区受桩体施工影响的地面隆起量。 相似文献
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通过对桩端置于含泥圆砾卵石层超短静压预制桩桩底注浆及注浆前后静载试验,分析了桩竖向极限承载力的提高机理。试验表明,桩底注浆可较大幅度地提高以砂卵石为持力层的静压预制桩的竖向承载力。 相似文献
157.
The literature contains limited information on variations in the factors of safety (FOS) of riverbank stability associated with river water level (RWL) fluctuations. This paper analyses a case study on the portion of the Red River flowing through Hanoi using the finite element method and extending the mechanics of saturated and unsaturated soils to understand how the riverbank’s FOS varies with RWL fluctuations. The results show that hydrostatic force is one of the key parameters influencing the FOS when the soil’s hydraulic conductivity is less than 10−6 m/s. However, the pore-water pressure and rate of RWL change are the key parameters influencing the FOS when the hydraulic conductivity is greater than 10−6 m/s. The study also indicates that a surcharge of 50 kPa or higher significantly weakens the riverbank stability and influences the FOS when the RWL rises. The construction of residential or other structures without taking special protection measures within 50 m of the lateral riverbank should be avoided for safety reasons. 相似文献
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