首页> 外文期刊>International Journal of Civil Engineering,Transaction A:Civil Engineering >Advanced Triaxial Tests on Partially Saturated Soils Under Unconfined Conditions
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Advanced Triaxial Tests on Partially Saturated Soils Under Unconfined Conditions

机译:在无核条件下部分饱和土的高级三轴试验

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A series of partially drained (pore air pressure drained and pore water pressure undrained), fully undrained (both pore air and water pressures undrained) and fully drained (both pore air water and pressures drained) triaxial tests were conducted in unconfined conditions to explore the mechanical behaviour of an unsaturated silty soil. The water contents of test specimens were kept at 10, 15, 20 and 25% with the respective degree of saturation of 24, 36, 49 and 59.5%. The void ratio was 1.10 with a dry density of 1.25 g/cm(3) while maintaining the relative compaction of all specimens at 80%. During the constant water content (CW) and fully undrained (FU) tests, the peak shear strength was within an axial strain range of 0-2.75% and the volumetric strain of all specimens did not vary within this range. Under shearing infiltration (SI) and constant loading infiltration (CLI) conditions, it was revealed that a significant magnitude of matric suction still exists in the specimens at the peak/post-peak deviatoric stress which depicts that a slope can fail during a rainfall under an unsaturated condition due to negative pore water pressure (matric suction) in the soil. The results of the triaxial tests suggest that the peak shear strength increases with matric suction linearly up to a matric suction of 15 kPa and the rate of increase gradually decreases with further increase in matric suction. Moreover, the failure envelopes have revealed an existence of a critical suction value of 15 kPa corresponding to 27% water content (i.e. on the dry side of optimum water content) and the increase in shear strength due to suction becomes insignificant afterwards. It is also observed that the peak shear strength increases nonlinearly with the increase in matric suction with a good agreement between the failure envelopes for CW, FU and SI tests.
机译:一系列部分排水(孔隙空气压力和孔隙水压),完全不受约束的(孔隙空气和水压不介绍)和完全排出的(孔隙空气和压力干燥)在不合适的条件下进行三轴试验,以探索不饱和粉状土壤的力学行为。试样的水含量保持在10,15,20和25%,其饱和度为24,36,49和59.5%。空隙率为1.10,干密度为1.25g / cm(3),同时保持所有样品的相对压实在80%。在恒定的含水量(CW)和完全不驱涉(FU)测试期间,峰值剪切强度在0-2.75%的轴向应变范围内,并且所有样品的体积菌株在该范围内没有变化。在剪切渗透(Si)和恒定的负载渗透(CLI)条件下,据揭示了在峰/后峰值偏离偏离应力的标本中仍然存在显着的测量幅度,这描绘了在降雨期间坡度可能发生故障土壤中负孔隙水压(磷脂吸力)引起的不饱和条件。三轴试验的结果表明,峰值剪切强度随着测距的抗剪切强度而增加,直到15kPa的原料吸力,并且增加速率逐渐降低,进一步升高了原味抽吸。此外,故障包络揭示了对应于27%的含水量(即最佳水含量的干燥侧的15kPa的关键吸力值,并且之后由于抽吸引起的剪切强度的增加变得微不足道。还观察到,峰值剪切强度随着Matric抽吸的增加而增加,CW,FU和Si测试的故障包膜之间具有良好的一致性。

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