隆起或凹陷的非均匀介质起伏地形中的表面波
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摘要
利用曲线坐标描绘局部隆起或凹陷的典型起伏地形,讨论了在介质性质随深度变化的非均匀起伏半空间中的Love波和Rayleigh波的传播规律。给出了决定频散关系的超越方程,并用数值方法计算出了频散曲线。
The problems of dispersion of Love and Rayleigh surface waves in ridge or canyon half space of inhomogeneous medium with varying elastic constants along with depth are studied by means of curvilinear coordinate method. The topography is described in curvilinear coordinate system, and the solutions of wave motion in the half space which satisfy the boundary conditions on the surface are given. The dispersions of Love waves and Rayleigh waves are found to vary with the local topography as well as the frequency. Finally, the dispersive curves of Love waves and Rayleigh waves in ridge or canyon half space are calculated.
引文
1EwingM,JardetzkyWandPressF.Elasticwavesinlayeredmedia.NewYork:McGraw-Hil,19572AkiKandRichardsPG.Quantitativeseismology.SanFrancisco:W.H.FrcemanCompany,19803Keilis-BorokVI.Seismicsurfacewavesinalateralyinhomogeneousearth.Derdrecht:KlumerAcademicPublishers,19894刘殿魁,刘国利.局部隆起或凹陷地形中的Love波.地震工程与工程振动,1992,12(4):16-245BostackMG.Surfacewavescateringfrom3-Dobstacles.Geophys.J.Int.,1991,104:350-3706冯锐,周海南,姚振生,孙克忠.面波的频散、反演和层析成像.中国地震,1987,3(1):15-287NewberHZ.应力集中.北京:科学出版社,19588WilsonJT.Surfacewavesinaheterogeneousmedium.Bul.Seism.Soc.Amer.,1942,32:297-3049DeNeyerJ.TheefectofvariationsinlayerthicknesonLovewaves.Bul.Seism.Soc.Amer.,1961,51:227-231

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