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The application of geophysical prospecting technology to tunnel advance prediction in Thousand-island Lake water distribution project |
Jun-Jie LI, Qing-Qiang XU, Jian-Qiang LI, Jian-She HE, Jia-Hao GUO |
Zhejiang Design Institute of Water Conservancy and Hydroelectric Power, Hangzhou 310002, China |
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Abstract The authors adopted TSP, ground penetrating radar and infrared acquisition technology to tunnel advance prediction of Thousand-island Lake water distribution project. Several conclusions have been drawn as follows: Firstly, TSP has a low resolution for detecting karst caves but has a good effect for detecting fractured rock mass, its anomaly features show that the Young’s modulus, density and P-wave velocity are low. Secondly, ground penetrating radar is very suitable for tunnel prediction in limestone area, radar reflection profile exhibiting strong amplitude and hyperbolic event usually indicates the development of karst caves. Thirdly, infrared acquisition is greatly influenced by hydration heat of shotcrete in tunnel so that it cannot be used alone in tunnel geological prediction; the defect is especially obvious when the quality of surrounding rock is poor.
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Received: 14 September 2018
Published: 10 April 2019
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The observation system of TSP
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岩性 | 围岩 类别 | 纵波波速 /(m·s-1) | 横波波速 /(m·s-1) | 密度 /(g·cm-3) | 杨氏模量 /GPa | 泥质粉砂岩 | Ⅳ~Ⅲ2 | 3699~4912 | 2081~2755 | 2.32~2.63 | 12~34 | 灰岩 | Ⅲ1~Ⅱ | 5200~6200 | 3100~3600 | 2.76~3.00 | 56~90 |
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Statistical results of TSP for common lithologic of Thousand Island Lake water transfer project
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Schematic diagram of infrared measuring points arrangement
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Prediction results of TSP of stake number K84+492~K84+342 in Wangjia tunnel
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GPR profiles of stake number K84+429~K84+399 as well as frequency spectrums of typical single-trace in Wangjia tunnel a—GPR profile;b—time-frequency spectrum of the 32nd trace
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Prediction results of TSP of stake number K7+985~K7+785 in Hong Qiu-tang tunnel
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The karst cave extends toward the left side of tunnel
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Thin layer mudstone in tunnel face
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GPR profiles of stake number K11+558~K11+528 as well as frequency spectrums of typical single-trace in Lianhua tunnel a—GPR profile;b—time-frequency spectrum of the 62nd trace
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Mud filled karst cave on the left and right sides of the tunnel near stake number K11+556 in Lianhua tunnel
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测点号 | 1 | 2 | 3 | 4 | 5 | 6 | 横向极差 | 1 | 254 | 252 | 253 | 253 | 253 | 253 | 2 | 2 | 253 | 252 | 253 | 254 | 253 | 253 | 2 | 3 | 252 | 253 | 254 | 253 | 253 | 252 | 2 | 4 | 251 | 251 | 252 | 251 | 250 | 251 | 2 | 纵向极差 | 3 | 2 | 2 | 3 | 3 | 2 | |
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Infrared detection results in Tunnel face in Xueao tunnelμW/cm2
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Infrared detection results along axial direction of tunnel in Xueao tunnel
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测点号 | 1 | 2 | 3 | 4 | 5 | 6 | 横向极差 | 第一行 | 262 | 263 | 257 | 258 | 260 | 261 | 6 | 第二行 | 261 | 260 | 257 | 254 | 255 | 260 | 7 | 第三行 | 257 | 252 | 251 | 246 | 251 | 252 | 11 | 第四行 | 250 | 252 | 248 | 245 | 247 | 248 | 7 | 纵向极差 | 12 | 11 | 9 | 13 | 13 | 13 | |
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Infrared detection results in Tunnel face in Fenshuijiang tunnelμW/cm2
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Infrared detection results along axial direction of tunnel in Fenshuijiang tunnel
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