黄土
石灰
微观结构
收缩率
粉煤灰
水泥
霜冻(温度)
冻胀
材料科学
体积热力学
岩土工程
多孔性
复合材料
地质学
冶金
地貌学
物理
量子力学
作者
Shenglin Wang,Qingfeng Lv,Hassan Baaj,Xiaoyuan Li,Zhao Yan-xu
标识
DOI:10.1139/cjce-2016-0052
摘要
Freeze–thaw action is considered to be one of the most destructive actions that can induce significant damage in stabilized subgrades in seasonally frozen loess areas. Laboratory tests including frost heave – thaw shrinkage and microstructure change during freeze–thaw cycles were conducted to evaluate the volume change rate of loess stabilized with cement, lime, and fly ash under the impact of cyclic freeze–thaw conditions. The loess specimens collapsed after eight freeze–thaw cycles (192 h), but most stabilized loess specimens had no visible damage after all freeze–thaw cycles were completed. All of the stabilized loess samples underwent a much smaller volume change than the loess alone after the freeze–thaw cycles. Although surface porosity and equivalent diameter of stabilized loess samples increased, the stabilized loess can retain its microstructure during freeze–thaw cycles when the cement content was less than 6%. To ensure freeze–thaw resistance of stabilized loess subgrades, the mix proportions of the three additives was recommended to be 4 to 5% cement, 6% lime, and 10% fly ash.
科研通智能强力驱动
Strongly Powered by AbleSci AI