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Accumulated deformation and microstructure of deep silty clay subjected to two freezing-thawing cycles under cyclic loading

机译:循环载荷下两次冷冻解冻循环的深粉状粘土的累积变形和微观结构

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The problem of the settlement and deformation of soft clay is becoming more and more prominent under the subway vibration loading. Due to the complexity of the construction environment in the soft soil areas, the artificial freezing method is often used to reinforce the soil, and sometimes it is also subjected to twice freezing. The Shanghai subway line crosses vertically and horizontally. The deepest excavation depth reaches 33.1 m, so the construction of the subway tunnel will develop to a deeper stratum. In this paper, the GDS dynamic triaxial tests were conducted to study the accumulated deformation of the gray silty clay of layer no.8 in Shanghai, 60 m in depth. Considering the influence of vibration time, frequencies, freezing temperatures, and freezing-thawing cycles, the axial strain of the deep silty clay before and after freezing-thawing was analyzed. The results show that the strain of the soil subjected to one freezing-thawing cycle and two freezing-thawing cycles increases by 39.6% and 72.8% comparing with the unfrozen soil, respectively. With the increase of vibration time, the rates of increasing of the axial strain gradually decrease. The higher the frequency and the lower the freezing temperature, the more deformation produces to the soil. The microstructures of the soil before and after freezing-thawing were obtained by mercury intrusion porosimetry (MIP) tests. There is a bottleneck with the pressure about 100 psi in the mercury intrusion process. Under the same cyclic loading, the lower the freezing temperatures and the more the freezing-thawing cycles, the more the mercury intrusion volume and the cumulative pore area. The most probable pore diameter of the unfrozen soil is about 524 nm smaller than that of the thawing soil, which is about 1050 nm. The pores 10-100 nm in diameter account for a large part. This research is of great guiding significance for the construction of deep subway tunnels.
机译:软粘土的沉降和变形的问题在地铁振动加载下变得越来越突出。由于柔软土壤区域的施工环境的复杂性,人为冷冻方法通常用于增强土壤,有时它也会冻结两次。上海地铁线垂直和水平交叉。最深的挖掘深度达到33.1米,因此地铁隧道的结构将发展到更深层次的层次。本文采用了GDS动态三轴试验,研究了上海灰色粉质粘土的累积变形,深入60米。考虑到振动时间,频率,冻结温度和冷冻循环的影响,分析了冷冻解冻前后深层粘土的轴向菌株。结果表明,与解冻的土壤相比,对一个冻融循环和两个冰冻解冻循环进行的土壤的菌株增加了39.6%和72.8%。随着振动时间的增加,增加轴向应变的速率逐渐减小。频率越高,冷冻温度越低,越差地产生土壤。通过汞侵入孔隙瘤(MIP)试验获得冻融前后土壤的微观结构。汞入侵过程中有大约100psi的瓶颈。在相同的循环载荷下,冻结温度越低,冷冻循环越多,汞侵入体积和累积孔隙区域越多。未分解的土壤的最可能孔径为约524nm,比解冻土壤的524nm,约为1050nm。孔径为10-100nm的直径占占大部分。该研究对深层地铁隧道建设具有巨大的指导意义。

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