高铁地基冻结弱膨胀土孔隙特征演化及未冻水含量模型研究

    Evolution of pore characteristics and modeling of unfrozen water content in frozen weakly expansive soils for high-speed rail foundations

    • 摘要: 冻结过程中弱膨胀土地基未冻水含量是新型高铁路堑桩-板结构设计需要考虑的重要因素之一。本文以兰新高铁地基弱膨胀土为研究对象,采用低场核磁共振系统(NMR)对弱膨胀土冻结过程中(+15℃~-30℃)的未冻水含量进行测试,分析温度、膨胀值、初始含水率对弱膨胀土孔隙特征和未冻水含量的影响规律,揭示弱膨胀土冻结机理,建立弱膨胀土未冻水含量预测模型。结果表明:冻结过程中弱膨胀土大孔孔隙水先冻结、小孔孔隙水后冻结,孔隙率呈阶梯式降低,-2℃~-4℃时内部发生急剧水冰相变。冻结阶段,膨胀值越大,冰点越低,小、中孔未冻水含量越高、大孔越少;初始含水率越高,冰点与未冻水含量均越高,-6℃时大孔未冻水完全冻结。膨胀值、初始含水率、温度与未冻水含量均呈正相关。建立了弱膨胀土未冻水含量模型,结合室内试验与外部数据,通过开展模型误差分析、计算拟合系数,验证了模型的合理性。

       

      Abstract: Unfrozen water content of weakly expansive soil foundations during freezing is a key factor to be considered in the design of new type high-speed railway cutting pile-slab structures. Taking the weakly expansive soil from the foundation of the Lanzhou-Xinjiang High-Speed Railway as the research object, this study used a low-field NMR system to test its unfrozen water content during freezing (+15℃~-30℃), analyzed effects of temperature, swelling value and initial water content on its pore characteristics and unfrozen water content, revealed its freezing mechanism, and established a prediction model for weakly expansive soil’s unfrozen water content. Results show: during freezing, water in macropores of weakly expansive soil freezes first, then that in micropores; porosity decreases stepwise, with drastic water-ice phase transition inside at -2℃~-4℃. In the freezing stage, larger swelling value brings lower freezing point, higher unfrozen water content in micropores/mesopores and fewer macropores; higher initial water content leads to higher freezing point and unfrozen water content, with macropore unfrozen water fully frozen at -6℃. Swelling value, initial water content and temperature all positively correlate with unfrozen water content. The unfrozen water content model was verified rationality via error analysis and fitting coefficient calculation based on laboratory tests and external data.

       

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