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SMALL STRAIN STIFFNESS AND NON-LINEAR STRESS-STRAIN BEHAVIOUR OF CEMENT-MIXED GRAVELLY SOIL

机译:水泥混合砂土的小应变刚度和非线性应力应变行为

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摘要

The stiffness at small strains and non-linear stress-strain relation of compacted cement-mixed well-graded gravelly soil as well as the ageing effects were evaluated by drained triaxial compression tests on compacted moist specimens cured for different periods at isotropic and different anisotropic stress states. In all the tests, the initial stress-strain relation at small strains less than about 0.001% was essentially elastic and the initial Young's modulus, E_0, was essentially the same as the E_(eq) value evaluated by applying unload/reload cycles under otherwise the same conditions. The E_(eq) values were rather independent of strain rate. The E_(eq) value from the first unload/reload cycle applied during otherwise continuous ML became noticeably lower than the elastic modulus evaluated at the same stress state, more as approaching the peak stress state. After a number of small unload/reload cycles and long sustained loading, the E_(eq) value became closer to the elastic modulus due to a decrease in the viscous effects. The ratio of E_0 to the compressive strength (q_(max)) was similar to that of concrete but noticeably larger than those of uncompacted cement-mixed soil, sedimentary softrock and unbound gravelly soil. Both E_0 and q_(max) increased with time by ageing, while the E_0/q_(max) ratio decreased with time. When ML was restarted at a constant strain rate after ageing with a shear stress, the tangent stiffness became very high for a large stress range with a substantial change in the non-linearity of stress-strain relation.
机译:通过排水三轴压缩试验,对在各向同性和不同各向异性应力下不同时间固化的压实潮湿试样进行排水三轴压缩试验,评估了压实水泥拌匀的砾石土的小应变刚度和非线性应力-应变关系以及老化效果。状态。在所有测试中,小于0.001%的小应变时的初始应力-应变关系基本上是弹性的,初始杨氏模量E_0与通过在其他情况下应用卸载/重新加载循环评估的E_(eq)值基本相同相同的条件。 E_(eq)值与应变率无关。在其他情况下连续ML期间施加的第一个卸载/重新加载循环的E_(eq)值明显低于在相同应力状态下评估的弹性模量,甚至接近峰值应力状态。经过多次较小的卸载/重新加载循环和长期持续加载后,由于粘性效应的降低,E_(eq)值变得更接近于弹性模量。 E_0与抗压强度之比(q_(max))与混凝土相似,但明显大于未压实的水泥混合土,沉积软岩和未结合的砾石土。随着年龄的增长,E_0和q_(max)均随时间增加,而E_0 / q_(max)之比随时间而减小。在通过剪切应力老化后以恒定的应变速率重新开始ML时,在较大的应力范围内,切线刚度变得非常高,应力-应变关系的非线性发生了显着变化。

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