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应用地球物理  2024, Vol. 21 Issue (1): 13-30    DOI: 10.1007/s11770-024-1073-z
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基于Scholte波频散特性的深海海底横波速度反演
于鹏飞*, 江佳萌, 耿建华, 张宝金
1. 河海大学海洋学院,南京210024; 2. 海洋地质国家重点实验室,同济大学,上海200092; 3. 广州海洋地质调查局,广州525027
Shear wave velocity inversion of marine sediments using deep-water OBS Scholte-wave data
Yu Peng-Fei*, Jiang Jia-Meng, Geng Jian-Hua, and Zhang Bao-Jin
1. College of Oceanography, Hohai University, Nanjing 210024, China. 2. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China. 3. Guangzhou Marine Geological Survey, Guangzhou 525027, China.
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摘要 深海环境下海水的声波速度是非匀速的,变速的海水会影响海底Scholte波的频散特性,为了提高利用Scholte波频散特性反演海底横波速度的精度,需建立速度连续变化的水平分层海水-分层海底(HLSLS)模型。本文基于波动理论推导HLSLS模型Scholte波频散方程和振幅深度方程。然后,基于南海海水声速剖面和实际海底弹性介质参数,分析深海环境海水速度变化对Scholte波频散特性的影响。最后,将方法用于南海深水OBS地震数据反演得到一条二维海底横波速度剖面,反演结果很好的指示了海底天然气水合物储层的分布。结果表明:深海环境下,利用海底OBS数据中的Scholte波反演海底浅层横波速度结构是可行 的,南海实际深水OBS数据应用进一步验证了方法的准确性和实用性。
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关键词Scholte波   频散特性   变速海水   OBS   横波速度反演     
Abstract: Acoustic velocity varies in deep-water environments, and the variable-velocity seawater can affect the dispersion characteristics of Scholte wave. To improve the accuracy of inversion, a horizontal layered-seawater and layered-seabed (HLSLS) model is established with continuously varying velocities for seabed S-wave velocity inversion using Scholte wave. First, we deduced the Scholte wave dispersion equation and the amplitude-depth equation of the HLSLS model based on wave theory. Then, with the real acoustic velocity of the seawater and submarine sediments parameters of the Shenhu area in the South China Sea, we analyzed the influence of variable-velocity seawater on the dispersion characteristics of Scholte wave. Finally, we performed two-dimensional (2D) S-wave velocity inversion on the field OBS multi-component data in the South China Sea. The results showed that the variation of seawater acoustic velocity had a certain influence on the dispersion characteristics of Scholte wave in deep water. The accuracy and practicality of our method were verified through numerical and filed data experiments.
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收稿日期: 2023-10-24;
基金资助:This research is funded by the National Natural Science Foundation of China (grant no. 42074149), and the Natural Science Foundation of Jiangsu Province (grant no. BK20201318).
通讯作者: Yu Peng-Fei (E-mail: hhu_ypf@hhu.edu.cn)     E-mail: hhu_ypf@hhu.edu.cn
引用本文:   
. 基于Scholte波频散特性的深海海底横波速度反演[J]. 应用地球物理, 2024, 21(1): 13-30.
. Shear wave velocity inversion of marine sediments using deep-water OBS Scholte-wave data[J]. APPLIED GEOPHYSICS, 2024, 21(1): 13-30.
 
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