A rapid detection method of towed array seismic surface wave for leakage passage of dyke-dam

被引:3
作者
Lu, Xinglin [1 ]
Wang, Wei [2 ]
Luo, Chaopeng [4 ]
Wu, Muyang [2 ]
Yang, Chao [3 ]
Liao, Xian [5 ]
Liu, Longhuan [5 ]
Fu, Zhihong [2 ]
机构
[1] Chongqing Jiaotong Univ, Sch Smart City, 66 Xuefudadao, Chongqing 400074, Peoples R China
[2] Chongqing Univ, Sch Elect Engn, 174 Shazhengjie, Chongqing 400044, Peoples R China
[3] Chongqing Univ, Sch Resources & Safety Engn, 174 Shazhengjie, Chongqing 400044, Peoples R China
[4] Sci & Technol Near Surface Detect Lab, Wuxi, Peoples R China
[5] Chongqing Triloop Prospecting Technol Co Ltd, Chongqing 402660, Peoples R China
关键词
Dyke; -dam; Fast imaging; Inversion; Surface wave; Towed array; LOCALIZATION; IMAGE;
D O I
10.1016/j.jappgeo.2023.105189
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Rapid detection of leakage passage in dykes has become a committed step in flood prevention work. The seismic surface wave method can be given the S-wave velocity information of the near-surface (<= 20 m), and qualitatively evaluate the transverse position, depth range, and direction of the leakage passage. The low acquisition efficiency of the cone geophone in the conventional point measurement mode does not meet the requirements of rapid detection. A single survey line has a small coverage area and lacks comparison with neighboring survey lines, so it is not possible to obtain the direction of extension of the leakage passage. In this paper, we propose a rapid detection method of the towed array seismic surface wave for leakage passage of a dyke-dam. Forty-eight gravity geophones are arranged in three columns, 16 in each column, to form the array geometry. Surface wave imaging methods are inversion and fast imaging. The main shortcomings of inversion calculation are (1) lacking shallow information, (2) low vertical resolution, and (3) multiple solutions. To overcome the above issues, the imaging calculation of the surface wave dispersion curve is implemented using fast imaging method. The proposed array geometry is used to collect seismic data. The simulated data and measured data show that fast imaging has the following advantages: (1) It can make full use of the dispersion curve of broadband seismic data, does not lose shallow information, and has high imaging accuracy. (2) It uses the dispersion curve directly for imaging, does not lose any details of velocity changes, and has a high vertical resolution. (3) The imaging results are unique. In contrast to the inversion results, the fast imaging results clearly distinguish the location of the leakage passage and highlight the lateral variability of the leakage passage. The results of the model data and measured data demonstrate the efficiency and high resolution of the towed array seismic geometry and the fast imaging method for leakage passage detection.
引用
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页数:12
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