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Study on the Shear Strength Parameters under Different Freezing and Thawing Cycles of Soil Slope in China

机译:土壤坡度不同冰冻循环下剪切强度参数研究

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In seasonal frozen regions, shallow landslide hazards in soil slopes usually happen. The type of failure surface is always on the freezing and thawing surface in the soil slope. So the direct influence factor of soil slope failure is the soil shear strength of the freezing and thawing (F-T) surface. The shear strength of the soil is determined by the two parameters of Cohesion "c" and Friction angle "Φ". In this study model experiment of F-T soil interface with different aggregate materials is designed by alternating the F-T cycle times, then the parameters c and the Φ were obtained. Finally the deterioration modal of the two shear strength parameters of soil interface was put forward. The results demonstrated when the slope stability in the seasonal frozen regions was analyzed using shear strength reduction method, the two deterioration modals can provide the data reference for the analysis.
机译:在季节性冷冻区域,通常发生土壤斜坡的浅滑坡危险。 故障表面的类型总是在土坡中的冻结和解冻表面上。 因此,土坡衰竭的直接影响因素是冷冻和解冻(F-T)表面的土壤剪切强度。 土壤的剪切强度由凝聚力“C”和摩擦角“φ”的两个参数决定。 在本研究模型中,通过交替F-T循环时间来设计具有不同聚集材料的F-T土壤界面,然后获得参数C和φ。 最后提出了土壤界面两种剪切强度参数的劣化模态。 结果表明,使用剪切强度还原法分析季节性冷冻区域的斜率稳定性,两个劣化模块可以为分析提供数据参考。

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