4.7 Article

Frost heaving strain monitoring for lining structure in extreme cold and high-altitude area with FBG strain sensors

期刊

MEASUREMENT
卷 196, 期 -, 页码 -

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.measurement.2022.110918

关键词

Extreme cold and high-altitude tunnels; Frost heaving strain; Thermal strain; Applied stress-strain; Fiber Bragg Grating strain sensors

资金

  1. National Natural Science Founda-tion of China [62103174]
  2. Applied Basic Foundation of Yunnan Province [202001AU070046]

向作者/读者索取更多资源

This study proposes a method for monitoring and measuring the frost heaving strain, thermal strain, and applied stress strain in extreme cold and high-altitude tunnel structures. The results show that thermal strain is the main cause of frost damage to the lining structure.
Due to the extreme temperature with significant variation in the alpine region, the tunnels in this area are subjected to intense freeze-thaw cycles and frost heaves, which leads to the cracking of the second lining structure. We propose an approach to monitor the frost heaving strain of the second lining and simultaneously measure the thermal strain and applied stress strain of the structure. The Fiber Bragg Grating (FBG) strain sensors are installed on the structure surface to measure the strains caused by the thermal strain and loaded stress. Meanwhile, one FBG temperature sensor is installed on the structure surface to measure the local temperature. Then, the structure thermal strain and applied stress strain are simultaneously measured based on the sensitivity difference for temperature and strain response of the above two measurement methods. The proposed approach is implemented in an alpine region tunnel. The results show that the local temperature is inversely proportional to the total strain and the thermal apparent strain of the second lining. The applied stress-strain of the lining fluctuates in a small range, and the thermal strain from the daily temperature difference incremental demodulation is very close to the daily strain difference. Therefore, the main cause of lining frost damage is the thermal strain due to the local temperature variation, and there is no frost heave occurred in the surrounding rock. Thus, the method is offered to monitor the freeze-thaw cycles and freeze-swelling effects in the extreme cold and high-altitude tunnels.

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