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    冻融循环对硫酸盐渍土-混凝土界面剪切特性的影响

    Effect of Freeze-Thaw Cycles on Shear Characteristics of the Interface Between Sulphate Saline Soil and Concrete

    • 摘要: 我国西北部季节性盐渍化冻土地区的铁路线路分布范围越来越广,因硫酸盐渍土冻融循环引发的铁路工程病害问题也越来越多.为了研究盐渍土与混凝土界面在冻融循环条件下的强度及变形特性,对不同含盐量(0、1%、2%、3%、4%)的自制硫酸钠盐渍粉质黏土与混凝土界面在±20℃下进行了不同次数(1次、3次、6次、10次)的冻融循环试验,以冻结融化各12h为1个循环周期,并在循环结束后开展了20℃恒温条件下的单调直剪试验和扫描电镜试验,从界面的抗剪强度、损伤占比、体变特征和微观结构等方面分析了冻融循环次数和含盐量等因素对盐渍土-混凝土界面剪切特性的影响.研究结果表明:盐渍土-混凝土界面的抗剪强度随冻融循环次数增大而逐渐降低,而其下降程度则随循环次数增大而减小.任意损伤过程中,盐渍土-混凝土界面盐蚀劣化作用效果比冻融劣化作用更明显.界面在含盐量为4%时出现剪胀现象,其余情况均表现为剪缩,并且冻融循环次数越大,剪缩现象越明显.基于扫描电镜试验发现,冻融循环作用会造成界面土颗粒整体性降低,界面土体的孔隙率在冻融循环作用下逐渐增大,冻融循环6次后,孔隙面积变化幅度减小,粒间小孔隙增多,土颗粒分布更均匀.

       

      Abstract: With the increasing distribution of railway lines in the seasonally salinized frozen soil area in Northwest China,more and more railway engineering diseases caused by the freezing and thawing cycle of sulfate saline soil have been caused.To explore the strength and deformation difference of the interface between saline soil and concrete under freeze-thaw cycles,this paper considered the interface of sulfate rich silty clay and concrete as the research object.The concrete and the sodium sulfate saline soil with the salt content of 0,1%,2%,3%,and 4% were tested for 1,3,6,and 10 freeze-thaw cycles at ±20℃,with 12 hours of freezing and thawing as a cycle.After the cycle,the monotonic direct shear and scanning electron microscope tests were carried out on the interface under constant temperature of 20℃.The influence of freeze-thaw cycles and salt content on the characteristics of the interface was analyzed from the aspects of shear strength,deterioration proportion,volume deformation characteristics and microstructure.The results show that the shear strength of the interface between saline soil and concrete decreases with the increase of freeze-thaw cycles.The degree of decline gradually decreases with the increase of cycles.In any damage process,the deterioration effect of salt erosion on the interface between saline soil and concrete is more obvious than that of freeze-thaw.Under the condition of 4% salt content,dilatancy is appeared in the interface,and shear shrinkage is shown in other cases.The larger the number of freeze-thaw cycles,the more obvious the phenomenon of shear shrinkage.The scanning electron microscope test shows that the freeze-thaw cycles reduce the integrity of the soil particles at the interface.The interfacial soil porosity increases under the action of freeze-thaw cycles.After the freeze-thaw cycles for 6 times,the change range of the pore area decreases,the small pores between the particles increase,and the soil particle distribution is more uniform.

       

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