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1)  normal frozen-heave force
法向冻胀力
1.
Analysis on effect of pre-increasing load on the clay normal frozen-heave force
预施荷载对黏土法向冻胀力的影响分析
2.
The relationships between the normal frozen-heave force produced in the frozen-heave process of low liquid-limit clay and the factors,such as clay temperature,water content,dry density and frozen-heave ratio,were analyzed based on the normal frozen-heave force experiment of zero displacement balance method and numerical statistics method.
首先,通过零位移平衡法的法向冻胀力试验,应用数理统计方法,分析了低液限黏土在冻结过程中产生的法向冻胀力与土体的温度、含水量、干密度、冻胀率等因素的关系,建立了法向冻胀力与冻胀率的线性回归方程,提出可以使用冻胀率对低液限黏土的法向冻胀力进行分级,并给出了适合路基填料的低液限黏土法向冻胀力分级标准;然后,通过加荷固结稳定后的冻胀试验,分析了上覆荷载对冻胀的影响;最后,将低液限黏土的法向冻胀力的分级标准与现有规范对比,得出各冻胀性类别的法向冻胀力界限值基本相同。
2)  tangential frozen heaving force
切向冻胀力
1.
Combining with a manual berth project in frozen area park,frictional resistance and uplift displacement of piles induced by tangential frozen heaving force are decided by in-site test.
结合寒冷地区某公园人工湖船台工程,通过现场试验,确定船台桩基切向冻胀力作用下的摩阻力值和上拔位移。
3)  frost heaving pressure
切向冻胀应力
1.
This paper analyzes the function process of frost heaving pressure which causes the quality problem of "upward freezing pulling" about shipway pile foundation,and research to conduct experiment survey on application effect of the developed engineering prevention measures.
论述了切向冻胀应力引起船台桩基础"冻拔"质量问题的作用机理;研究制定的"冻拔"质量问题的工程防治措施应用效果的实验监测。
4)  lateral frost heave
侧向冻胀
5)  frost-heaving ratio and frost-heaving stress
冻胀率和冻胀力
6)  frozen-heave force
冻胀力
1.
The design of frozen wall in deep alluvium is a difficult problem of freezing shaft sinking, at present, few research have reported in detail on the characteristic of frozen wall with loopy freezing pipe, not to mention the characteristic of its temperature field, moisture field and frozen-heave force of it.
深厚冲积层冻结壁的设计是冻结法凿井中的难题,目前对三圈管冻结壁的形成特性研究较少,而对三圈管冻结壁形成过程中的温度场、水分场和冻胀力应力研究至今还未见有详细的报道。
2.
The conclusion is that the frozen-heave force is most lager between center tubes , then outer tubus and inner tubus.
对三圈管冻结壁形成过程中冻胀力进行了室内相似模型试验,得出中圈管的管间冻胀力最大,而外圈管和内圈管的管间冻胀力相对较小。
补充资料:冻胀丘

冻胀丘是由于地下水受冻结地面和下部多年冻土层的遏阻,在薄弱地带冻结膨胀,使地表变形隆起,称冻胀丘。冰锥是在寒冷季节流出封冻地表和冰面的地下水或河水冻结后形成丘状隆起的冰体。

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