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An experimental study on the mechanical properties of silty soils under repeated freeze-thaw cycles

机译:反复冻融循环下粉质土力学特性的试验研究

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摘要

In this study, the subgrade fill material from the Nagqu Logistics Center Yard (NLCY) along the Qjnghai-Tibet Railway was investigated. And the thaw subsidence properties and dynamic properties were thoroughly analysed in laboratory tests. 1) From the determined thaw subsidence properties, the following results were obtained: samples with a higher degree of compactness exhibited heave deformation, whereas those with a lower degree of compactness exhibited compressive deformation after repeated freeze-thaw cycles. However, there is a critical compactness level at which the height of the samples does not change after repeated freeze-thaw cycles. The consolidation effect of the load restrains frost heave deformation; however, the amount of thaw subsidence deformation increases. The thaw subsidence ratio first increases, then decreases and becomes steady after the fifth freeze-thaw cycle as the number of freeze-thaw cycles increases. It is recommended that the thaw subsidence properties of silty soils be assessed after 5-6 freeze-thaw cycles. 2) From the determined dynamic properties, the following results were obtained: the dynamic stress vs. strain curves clearly show a nonlinear trend. The dynamic modulus greatly decreases, whereas the damping ratio increases with additional freeze-thaw cycles; and changes level off after the sixth freeze-thaw cycle; the dynamic properties after 6-7 freeze-thaw cycles are suggested for use in designing and calculating indexes. Moreover, the dynamic modulus increases and the damping ratio decreases as the confining pressure and compactness increase.
机译:在这项研究中,调查了沿青藏铁路那曲物流中心场(NLCY)的路基填料。并在实验室测试中彻底分析了融化后的沉降特性和动态特性。 1)从确定的融化沉降性质获得以下结果:紧密度高的样品表现出胀形变形,而紧密度低的样品经过反复的冻融循环后表现出压缩变形。但是,存在一个严格的压实度水平,在该水平下,样品的高度在重复的冻融循环后不会改变。荷载的固结作用抑制了冻胀变形;但是,融化沉降变形量增加。随着第五次冻融循环次数的增加,融化沉降率首先增加,然后下降,并在第五次冻融循环后变得稳定。建议在5-6次冻融循环后评估粉质土壤的融化沉降特性。 2)从确定的动态特性中获得以下结果:动态应力与应变曲线清楚地显示出非线性趋势。动态模量大大降低,而阻尼比随着额外的冻融循环而增加;在第六次冻融循环后变平;建议将6-7次冻融循环后的动态特性用于设计和计算指标。此外,随着围压和密实度的增加,动模量增加,阻尼比减小。

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  • 来源
    《Cold regions science and technology》 |2015年第4期|51-65|共15页
  • 作者单位

    School of Civil Engineering, Shijiazhuang Tiedao University, Shijiazhuang 050043, China,Key Laboratory of Roads and Railway Engineering Safety Control of Ministry of Education, Shijiazhuang Tiedao University 050043, China;

    School of Civil Engineering, Shijiazhuang Tiedao University, Shijiazhuang 050043, China,Key Laboratory of Roads and Railway Engineering Safety Control of Ministry of Education, Shijiazhuang Tiedao University 050043, China;

    Northwest Corp., China Railway Construction Engineering Group, Xi'an 710119, China;

    School of Civil Engineering, Shijiazhuang Tiedao University, Shijiazhuang 050043, China,Key Laboratory of Roads and Railway Engineering Safety Control of Ministry of Education, Shijiazhuang Tiedao University 050043, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Silty soil; Freeze-thaw cycle; Unidirectional freezing; Dynamic modulus; Thaw subsidence ratio;

    机译:粉质土壤;冻融循环;单向冻结;动态模量解冻沉降率;

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