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Shear behaviour of a geogrid-reinforced coarse-grained soil based on large-scale triaxial tests

机译:基于大型三轴试验的土工格栅加筋粗粒土的剪切特性

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In China, weathered mudstone geogrid-reinforced coarse-grained soil is used extensively for road embankments. However, the microstructure and disintegration process of weathered mudstone remain unclear. Furthermore, few studies have investigated the shear behaviour of this kind of geogrid-reinforced fill through large-scale triaxial tests against grain size effects. To bridge this gap, this study reports results from large scale consolidated undrained (CU) and consolidated drained (CD) triaxial tests as well as scanning electron microscopy (SEM), energy-dispersive X-ray (EDX), and disintegration tests on weathered mudstone geogrid-reinforced coarse-grained soil. EDX spectrograms and SEM images show that coarse grains disintegrate rapidly mainly owing to the high clay mineral content and loose microstructure. Therefore, a suitable disintegration time (~ 15 days) is recommended for embankment sits. The shear behaviour of this geogrid-reinforced fill is investigated in detail through large-scale triaxial tests. The shear deformation tends toward strain hardening behaviour with an increase in the number of geogrid layers and the confining pressure. Geogrids significantly improve the apparent cohesive strength of coarse-grained soil. The pore water pressure is found to develop rapidly in the 0% -4% axial strain phase but dissipate slowly in the 4%-12% axial strain phase. During shear, the pore pressure coefficient A values of 0.2-0.4 are indicative of the partial saturation of specimens. Consequently, pore water pressure development is mainly attributed to the movement and rearrangement of coarse particles in coarse-grained soil. Experimental data show that the geogrid-reinforcement coefficients increase with the number of geogrid layers, and a 20-cm separation between geogrid layers is recommended for embankment construction sites. The number of geogrid layers influences the geogrid -soil interface's mobilization and the slip surface type. Test results revealed three types of slip surfaces related to the failure shapes of specimens. Then, based on CU experimental data, the parameters of the Duncan-Chang constitutive model are discussed.
机译:在中国,风化的泥岩土工格栅加固的粗粒土被广泛用于路堤。然而,风化泥岩的微观结构和崩解过程仍不清楚。此外,很少有研究通过针对粒度影响的大型三轴试验研究这种土工格栅加筋的填料的剪切行为。为了弥合这一差距,本研究报告了大型固结不排水(CU)和固结排水(CD)三轴测试以及扫描电子显微镜(SEM),能量色散X射线(EDX)和风化分解测试的结果泥岩土工格栅加筋的粗粒土。 EDX谱图和SEM图像显示,粗粒快速崩解主要是由于粘土矿物含量高和微观结构疏松。因此,建议路堤采用合适的崩解时间(〜15天)。通过大型三轴试验详细研究了土工格栅加筋填充物的剪切特性。随着土工格栅层数和围压的增加,剪切变形趋向于应变硬化行为。土工格栅显着提高了粗粒土的表观粘结强度。发现孔隙水压力在0%-4%轴向应变阶段迅速发展,而在4%-12%轴向应变阶段缓慢消散。在剪切过程中,孔隙压力系数A值为0.2-0.4表示样品部分饱和。因此,孔隙水压力的升高主要归因于粗粒土壤中粗粒的运动和重排。实验数据表明,土工格栅的加固系数随土工格栅层数的增加而增加,建议在路堤施工现场土工格栅层之间的距离为20厘米。土工格栅层的数量会影响土工格栅-土壤界面的活动性和滑动面类型。测试结果表明,三种类型的滑移表面与试样的破坏形状有关。然后,基于CU实验数据,讨论了Duncan-Chang本构模型的参数。

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