کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6426857 1634452 2015 15 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
An experimental study on the mechanical properties of silty soils under repeated freeze-thaw cycles
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علوم زمین و سیاره ای (عمومی)
پیش نمایش صفحه اول مقاله
An experimental study on the mechanical properties of silty soils under repeated freeze-thaw cycles
چکیده انگلیسی


- Systematically studied the deformation and strength properties of silty soils under repeated freeze-thaw cycles
- The thaw subsidence ratio determined after 5-6 freeze-thaw cycles is suggested for assessing thaw subsidence properties.
- With the critical compactness level, the height of samples doesn't change after repeated freeze-thaw cycles.
- The dynamic parameters determined after 6-7 freeze-thaw cycles are suggested for assessing strength properties.

In this study, the subgrade fill material from the Nagqu Logistics Center Yard (NLCY) along the Qinghai-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.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Cold Regions Science and Technology - Volume 112, April 2015, Pages 51-65
نویسندگان
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