冻融循环及不同粗粒含量对粗粒土力学性质的影响研究

    STUDY ON THE INFLUENCE OF FREEZE-THAW CYCLES AND DIFFERENT COARSE PARTICLE CONTENTS ON THE MECHANICAL PROPERTIES OF COARSE-GRAINED SOIL

    • 摘要: 为研究新疆天山地区粗粒土在冻融循环及不同粗粒含量变化下的力学性能,进行了室内不固结不排水三轴试验,探讨了应力-应变曲线、弹性模量、压缩强度、抗剪强度的变化规律。试验表明:(1)同一围压不同冻融循环次数对试样应力-应变曲线形态影响不大都为弱应变硬化特征,但在不同冻融循环作用下偏应力都出现了不同程度的衰减,在7~10次冻融循环以后试样偏应力随冻融循环次数有所回升,且粗粒含量的增加使得试样的应力-应变曲线从弱应变硬化向强应变硬化转化;(2)弹性模量在冻融循环过程中表现为先减小后趋于稳定,且随着粗粒含量的增加先增大后减小;(3)压缩强度随着冻融循环先减小后趋于稳定,随粗粒含量呈先逐渐增大后趋于稳定的变化规律;(4)黏聚力随着冻融循环呈初期递减趋势后趋于稳定,且黏聚力与粗粒含量呈正相关;(5)内摩擦角随着冻融循环呈先减小后增大的变化趋势,而随着粗颗粒含量的增加呈现出先减小后增加再减小的变化趋势。冻融损伤具有累积性首次冻融影响最大后续循环影响较小,研究成果为新疆高寒地区粗粒土路基填方边坡稳定性分析提供参考数据。

       

      Abstract: To investigate the mechanical properties of coarse-grained soils in the Tianshan region of Xinjiang under freeze-thaw cycles and varying coarse-grain content, a series of unconsolidated undrained triaxial tests were conducted. The study focused on stress-strain curves, elastic modulus, compressive strength, and shear strength, examining their variations under different conditions. The experimental results indicate that: (1)Under the same confining pressure, the stress-strain curve morphology is not significantly affected by the number of freeze-thaw cycles, exhibiting weak strain-hardening behavior. However, deviatoric stress shows varying degrees of attenuation under different freeze-thaw cycles. After 7 to 10 cycles, deviatoric stress tends to recover with further cycles. Additionally, increasing coarse-grain content transforms the stress-strain curve from weak strain hardening to strong strain hardening. (2)The elastic modulus initially decreases during the freeze-thaw process and then stabilizes. With increasing coarse-grain content, the elastic modulus first increases and then decreases. (3)Compressive strength initially decreases and then stabilizes with freeze-thaw cycles, while it gradually increases and then stabilizes with increasing coarse-grain content. (4)Cohesion initially decreases with freeze-thaw cycles and then stabilizes, showing a positive correlation with coarse-grain content. (5)The internal friction angle first decreases and then increases with freeze-thaw cycles, while it exhibits a more complex trend with increasing coarse-grain content. Freeze-thaw damage is cumulative, with the first cycle having the greatest impact. These findings provide reference data for analyzing the stability of coarse-grained soil slopes in high-altitude cold regions of Xinjiang.

       

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