[1]YANG Xiaolin,HE Bin.Infrared Thermography Imaging of Geodynamic Observatory Tunnel at Qianling Station, Shaanxi Province[J].Journal of Seismological Research,2019,42(03):411-418.
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Journal of Seismological Research[ISSN 1000-0666/CN 53-1062/P] Volume:
42
Number of periods:
2019 03
Page number:
411-418
Column:
Public date:
2019-07-24
- Title:
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Infrared Thermography Imaging of Geodynamic Observatory Tunnel at Qianling Station, Shaanxi Province
- Author(s):
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YANG Xiaolin1; 2; 3; HE Bin4
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(1. Institute of Geodesy and Geophysics,Chinese Academy of Sciences,Wuhan 430077,Hubei,China)(2. University of Chinese Academy of Sciences,Beijing 100049,China)(3. Shaanxi Earthquake Agency,Xi'an 710068,Shaanxi,China)(4. Jiangsu Earthquake Agency,Nanjing 210014,Jiangsu,China)
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- Keywords:
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Shaanxi Qianling observatory; thermoelastic deformation; air temperature inside tunnel; temperature of surrounding rock; infrared thermography
- CLC:
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P315.725; TN219
- DOI:
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- Abstract:
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Taking the Shaanxi Qianling Observatory as an example,we systematically detect and image the temperature in lining for the front,NS,and EW parts of the tunnel using the powerful infrared thermal camera. The results show that lining temperature in the front is much higher,varying from 20.7 ℃ to 14.8 ℃,and exhibits a linearly decrease with an increase in distance from the entrance. The lining temperature in the NS part is slightly higher than the EW part,the mean temperatures are approximately 13.5 ℃ and 13.1 ℃ respectively,but each of which is basically uniform and stable. Generally,slight temperature fluctuations widely exist in three main parts of tunnel,the dispersions are larger at a few individual points among them. Furthermore,temperatures in lining and air are significantly discrepant at the same point,this means the difference is drastic. Additionally,infrared thermograms of the eastern end of tunnel show that the temperature in ceiling is clearly larger than that in the sidewalls.