中主应力影响下的上海深部砂土强度和变形特性

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  • 上海交通大学 土木工程系;上海市公共建筑和基础设施数字化运维重点实验室,上海 200240
邬  颢(1994—),博士生,从事土力学与土工试验方面的研究
陈锦剑,教授,博士生导师,电话(Tel.):021-34207003;E-mail:chenjj29@sjtu.edu.cn。

网络出版日期: 2025-05-28

基金资助

国家自然科学基金资助项目(42377136)

Effect of Intermediate Principal Stress on the Strength and Deformation Behaviors of Shanghai Deep Sands

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  • Department of Civil Engineering; Shanghai Key Laboratory for Digital Maintenance of Buildings and Infrastructure, Shanghai Jiao Tong University, Shanghai 200240, China

Online published: 2025-05-28

摘要

为探明上海深部砂土在中主应力σ2影响下的强度和变形特性,对上海第7、9和11层深部砂土开展了多组真三轴试验,分析了不同中主应力系数b下的应力-应变和体积应变行为,阐明了摩擦角和破坏包络线随b的变化规律并对比了3层砂土之间的参数差异。结果表明,σ2对上海深部砂土的强度和变形特性影响显著。砂土强度随b的增大而减小,而其剪胀性的变化规律则相反。第9层土展现出最明显的软化特性和剪胀性且强度最高;而第11层土则几乎展现出硬化和剪缩且强度最低。第7层土的特性处于第9和11层之间且更接近于第9层。SMP准则相较于L-D和M-C准则更适用于预测σ2影响下的上海深部砂土强度指标。

本文引用格式

邬 颢, 李明广, 陈锦剑 . 中主应力影响下的上海深部砂土强度和变形特性[J]. 上海交通大学学报, 0 : 1 . DOI: 10.16183/j.cnki.jsjtu.2024.527

Abstract

To investigate the strength and deformation behaviors of Shanghai deep sands under the effect of intermediate principal stress (σ2), multiple sets of true triaxial tests are conducted on Shanghai deep sand layers 7, 9, and 11. The stress-strain and volumetric strain behaviors under different coefficients of intermediate principal stress (b) are analyzed, and the variation laws of friction angles and failure envelopes with b are clarified. Additionally, the parameter differences between these 3 sand layers are compared. The results indicate that σ2 has a significant impact on the strength and deformation behaviors of Shanghai deep sands. The strength decreases with the increase of b, while dilatancy changes in the opposite direction. Layer 9 exhibits the most significant softening characteristics and dilatancy with the highest strength, while layer 11 almost exhibits hardening and contraction with the lowest strength. The behaviors of layer 7 are between the two and closer to those of layer 9. Compared to the L-D and M-C criteria, the SMP criterion is more suitable for predicting the strength index of Shanghai deep sands under the effect of σ2.
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