大温差下乌兹别克斯坦盐渍土力学特性及路基边坡稳定性研究

    Mechanical properties of saline soil and stability of subgrade slope in Uzbekistan under large temperature difference

    • 摘要: 随着国家“一带一路”战略的深入推进,中亚等丝路沿线国家盐渍土地区的交通基础设施建设急剧增加,受特殊气候条件的影响,盐渍土道路工程建设中易出现沉陷、边坡失稳等工程问题。以乌兹别克斯坦A380公路项目为依托,基于大温差冻融循环及不固结不排水三轴剪切试验,研究大温差下不同冻融循环次数及含盐量下盐渍土的破坏强度及抗剪强度参数的演化规律;对不同含盐量、不同冻融循环次数下的路基边坡稳定性进行数值模拟分析。结果表明:在不同冻融循环次数及含盐量下,随着含盐量增加,破坏强度不断减小呈线性衰减特征,黏聚力和内摩擦角呈二次函数衰减特征;随着冻融循环次数增加,破坏强度及黏聚力不断减小,呈对数函数衰减特征,而内摩擦角呈对数函数的增长特征;盐渍土路基边坡安全系数随着含盐量和冻融循环次数的增加均呈现不断减小的特征。

       

      Abstract: With the deepening of the "One Belt and One Road" strategy in China, the construction of transportation infrastructure in saline land areas along the Silk Road in Central Asia and other countries has increased sharply. Affected by special climatic conditions, the road construction in saline soil is prone to engineering problems such as subsidence and slope instability. Based on the Uzbekistan A380 highway project, the evolution laws of failure strength and shear strength parameters of saline soil under different freeze-thaw cycles and salt contents under large temperature difference are studied based on the freeze-thaw cycles with large temperature difference and unconsolidated undrainage triaxial shear tests. The stability of subgrade slope under different salt contents and different freeze-thaw cycles is analyzed through numerical simulation. The results show that under different freeze-thaw cycles and salt contents, with the increase of the salt content, the failure strength decreases continuously with linear attenuation characteristics, and the cohesion and internal friction angle show quadratic function attenuation characteristics. With the increase of the number of freeze-thaw cycles, the failure strength and cohesion continue to decrease, showing a logarithmic function attenuation characteristics, and the internal friction angle shows a logarithmic function growth characteristic. The safety factor of roadbed slope of saline soil decreases with the increase of the salt content and the number of freeze-thaw cycles.

       

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