煤炭工程 ›› 2018, Vol. 50 ›› Issue (9): 107-111.doi: 10.11799/ce201809028

• 研究探讨 • 上一篇    下一篇

深厚冲积层人工冻土力学性能试验研究

宋朝阳   

  1. 煤炭科学研究总院
  • 收稿日期:2018-04-20 修回日期:2018-04-26 出版日期:2018-09-20 发布日期:2018-12-18
  • 通讯作者: 宋朝阳 E-mail:18600103089@126.com

Mechanical property test on artificially frozen soils in deep alluvium

  • Received:2018-04-20 Revised:2018-04-26 Online:2018-09-20 Published:2018-12-18

摘要: 为了获得深厚冲积层的冻土物理力学参数,从施工现场获得了十个层位(-193~-624m)的原状土样,在实验室中完成了十个层位重塑土冻结后的物理力学参数测试。试验结果表明:相同冻结温度条件下,第2层冻土冻胀力最大,第8层冻土冻胀力次之,而第9层冻胀力最低|第5土层冻结后单轴抗压强度最高,地层冻结稳定性较好,相比较第8层单轴抗压强度最低,地层冻结稳定性较差|第4~6层土层的粘聚力受冻结温度影响较为敏感|-15℃的冻结土层条件下,不同恒定应力剪切时第3、4、5层黏土的剪切蠕变变形量相对较大。地层土层结构特征、含水率、温度、应力与时间是影响冻土强度的关键因素。

关键词: 冲积层, 冻土力学, 力学特性, 温度, 蠕变

Abstract: The freezing technology for constructing deep shafts and long inclined shafts is always a key and difficult point in mine construction on complex geological conditions. The construction of shafts with complex engineering specifications in areas with deep, complex formation conditions needs to use freezing process in alluvium of thousands of meters thick. To obtain the physical and mechanical parameters of frozen soil in deep alluvium, undisturbed soil samples were collected at ten horizons (-193m~-624m) at the construction site. Then, the physical and mechanical parameters of the remolded frozen soils at the ten horizons were detected in the laboratory. The experiment showed that at the same freezing temperature, the frozen soil at the second horizon showed the largest frozen-heave force, followed by that of the eighth horizon, while the lowest frozen-heave force was observed at the ninth horizon. After being frozen, the soil at the fifth horizon presented the highest uniaxial compressive strength and desirable freezing stability of the formation. In comparison, the frozen soil at the eighth horizon exhibited the lowest uniaxial compressive strength and poor freezing stability of the formation. The cohesion of the soils at the fourth to sixth horizons was sensitive to the influences of freezing temperature. After being frozen at -15°C, the clay at the third to fifth horizons had relatively larger shear creep deformation while being sheared under different constant stresses. Meanwhile, structural characteristics and moisture content of the soil in the formation, temperature, stress and time are key factors influencing the strength of the frozen soil. The research results can be directly used to guide the design and construction of frozen walls of shafts to improve the design and construction quality.

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