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Scholte wave dispersion and particle motion mode in ocean and ocean crust

海洋和洋壳中Scholte波的频散及质点运动方式

作     者:Xu Xin Wan Yong-Ge Li Zhen-Yue Sheng Shu-Zhong 许鑫;万永革;李振月;盛书中

作者机构:Institute of Disater Prevention of Science and TechnologySanhe 065201China University of Science and Technology of ChinaHefei 230026China Institute of GeophysicsChina Earthquake AdministrationBeijing 100081China School of Geophysics and Measurement-control TechnologyEast China University of TechnologyNanchang 330013China 

出 版 物:《Applied Geophysics》 (应用地球物理(英文版))

年 卷 期:2022年第19卷第1期

页      面:132-142,146页

核心收录:

学科分类:081801[工学-矿产普查与勘探] 081802[工学-地球探测与信息技术] 08[工学] 0818[工学-地质资源与地质工程] 

基  金:supported by the National Natural Science Fondation of China(Nos.42174074,41674055,41704053) the Earthquake Science Spark Program of Hebei Province(No.DZ20200827053) Fundamental Research Funds for the Central Universities(No.ZY20215117) the Hebei Key Laboratory of Earthquake Dynamics(No.FZ212105) 

主  题:Scholte waves in the ocean and oceanic crust dispersion equation propagation velocity amplitude,mode of motion 

摘      要:The dispersion equation of the Scholte wave was reviewed using the homogeneous elastic half-space covered by a liquid layer,and the range of the Scholte wave propagation velocity was examined using the dispersion *** displacement expressions of the Scholte waves in liquid and solid were ***,the mode of motion of Scholte waves in liquid and solid and their variation with depth was *** following results were obtained:The dispersion equation shows that the propagation velocity of the fundamental Scholte wave was greater than the P-wave in liquid and less than that of the Scholte wave in homogeneous elastic *** contrast,the velocity of higher-order Scholte waves was greater than that of P waves in liquid and S-waves in *** the fundamental Scholte wave has no cutoff *** Scholte wave at the liquid surface moved only vertically,while the particles inside the liquid medium moved *** amplitude variation with depth in the solid medium caused the particle motion to change from a retrograde ellipse to a prograde *** above results imply the study of Scholte waves in the ocean and oceanic crust and help estimate ocean depths.

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