季节性冻土区能量桩位移变化规律研究
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重庆大学土木工程学院

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TU443

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国家自然科学(No. 51908087);重庆市“博士后创新人才支持计划”项目(CQBX201903);中国博士后科学基金(2019M663439);重庆市博士后科学(cstc2019jcyj-bshX0051)


Study on displacement of energy piles in seasonally frozen regions
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Chongqing University

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    摘要:

    能量桩是一种既可以与土体进行能量交换,又可以承担上部荷载的新型桩基结构形式。而在季节性冻土地区中,上部土层冻结,下部土层未冻结。由温度变化引起的桩体自身变形以及土体的冻胀融沉引发的桩体位移是能量桩在季节性冻土地区推广过程中亟待解决的主要问题。针对季节性冻土地区土体温度分布特点,将土体分为冻结层和非冻结层分别开展模型试验进行研究,测得冻结层和非冻结层中能量桩多次温度循环后的桩-土温度分布,桩周土体孔隙水压力及桩体沉降变形的变化规律。研究结果表明:在非冻结土层中,多次循环制冷后会桩顶产生不可逆的沉降位移,5次制冷循环之后,桩顶沉降达到了0.95% D(D为桩体直径),且桩体沉降未达到稳定;在冻结层中,能量桩在制热过程中会发生桩体融沉现象,在恢复过程中会发生桩体冻胀现象,融沉导致的沉降位移随着循环次数的增加逐渐减小,在第3轮制热循环后消失。第1、2和3轮的融沉位移分别为5.9% D、0.93% D、0.11 D%。每轮循环过程中,冻胀引起的上升位移虽逐轮减小,但在5轮循环之后依旧存在,且冻胀引发的总位移呈阶梯状上升,桩体最终产生上升位移,并达到3.8 D%。

    Abstract:

    Energy pile is a new type of structure which can not only exchange energy with soil, but also bear the upper load. In the seasonal frozen soil area, the upper soil layer would be frozen, and thawing settlement, frost heaving and self-deformation of the pile caused by temperature variation are the main problems to be solved for the application of energy pile in this area. According to the distribution characteristics of ground temperature in seasonal frozen soil areas, the soil is divided into frozen layer and non-frozen layer, and the model tests are carried out respectively. The pile and soil temperature distribution, pore water pressure of the soil surrounding the pile and settlement deformation of the pile of the energy pile after multiple temperature cycles in frozen and non-frozen layers were measured. The results show that irreversible settlement displacement of the pile top will occur after multiple cycles of cooling. After 5 cycles of cooling, the settlement of the pile top reached 0.95%D (D is the diameter of the pile), while the settlement of the pile would not reach stable state. In the frozen layer, thawing settlement of the pile would occur in the heating process, and frost heaving of the pile would occur in the recovery process. The settlement displacement caused by thawing settlement gradually decreased with the increase of thermal cycles, and disappears after the third heating cycle. The first, second and third thaw settlement displacements reached 5.9% D, 0.93% D and 0.11% D, respectively. During each cycle, although the rising displacement caused by frost heaving decreases in each following cycle, it still existed after five cycles, and the displacement caused by frost heaving rose in a ladder shape. The pile heave was produced in the end and reached 3.8%D.

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  • 收稿日期:2022-01-12
  • 最后修改日期:2022-06-21
  • 录用日期:2022-06-22
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