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首页> 外文期刊>Proceedings of the institution of civil engineers >Unconf ined shear strength of compacted unsaturated plastic soils
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Unconf ined shear strength of compacted unsaturated plastic soils

机译:压实的非饱和塑性土的无侧限抗剪强度

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摘要

A central goal in unsaturated soil mechanics research is to create a smooth transition between traditional soil mechanics approaches and an approach that is applicable to unsaturated soils. Undrained shear strength and the liquidity index of reconstituted or remoulded saturated soils are consistently correlated, which has been demonstrated by many studies. In the liquidity index range from 1 (at W_1) to 0 (at w_p), the shear strength ranges from approximately 2 kPa to 200 kPa. Similarly, for compacted soil, the shear strength at the plastic limit ranges from 150 kPa to 250 kPa. When compacted at their optimum water content, most soils have a suction that ranges from 20 kPa to 500 kPa; however, in the field, compacted materials are subjected to drying and wetting, which affect their initial suction and as a consequence their shear strength. Unconfined shear tests were performed on five compacted tropical soils and kaolin. Specimens were tested in the as-compacted condition, and also after undergoing drying or wetting. The test results and data from prior literature were examined, taking into account the roles of void ratio, suction, and relative water content. An interpretation of the phenomena that are involved in the development of the undrained shear strength of unsaturated soils in the contexts of soil water retention and Atterberg limits is presented, providing a practical view of the behaviour of compacted soil based on the concept of unsaturated soil. Finally, an empirical correlation is presented that relates the unsaturated state of compacted soils to the unconfined shear strength.
机译:非饱和土壤力学研究的中心目标是在传统的土壤力学方法和适用于非饱和土壤的方法之间实现平稳过渡。未排水的抗剪强度与重新配制或重塑的饱和土的流动性指数始终相关,这已被许多研究证明。在从1(在W_1)到0(在w_p)的流动性指数范围内,剪切强度在大约2kPa至200kPa的范围内。同样,对于压实的土壤,塑性极限处的剪切强度范围为150 kPa至250 kPa。当以最佳含水量压实时,大多数土壤的吸力范围为20 kPa至500 kPa。然而,在现场,压实的材料要经受干燥和润湿,这会影响其最初的吸力并因此影响其剪切强度。在五种压实的热带土壤和高岭土上进行了无边限剪切测试。在压缩的条件下以及在干燥或湿润后对样品进行测试。考虑到空隙率,吸力和相对含水量的作用,检查了测试结果和来自先前文献的数据。对土壤保水和阿特伯格极限条件下非饱和土壤不排水抗剪强度发展过程中涉及的现象进行了解释,为基于非饱和土壤概念的压实土壤特性提供了实用的观点。最后,提出了一种经验相关性,将压实土壤的不饱和状态与无侧限剪切强度相关联。

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