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Anisotropy of Rayleigh waves in layered soil dispersion characteristics

tropicseabedtooceanwaves. J. ofGeotechoica [Engineering-AS-CE. 1992; 118 (9)} 1295m13141O XIA Tang generation, Wu Shiming. Isotropic Rayleigh surface of the soil. Proceedings Fourth National Symposium on Soil Dynamics. Hangzhou 199411 XIA Tang on behalf of the other. Isotropic transition in layered soil dispersion characteristics of Love. Journal of Zhejiang University. 1995; 29 (4): 493500DispersionCharaq ~ teristicsofRayleighWaveinAnisotropicLayeredSoilsXTangdaiCaiYuanqiangWuShimingGongQuanmet (Dept.ofCivilEngr.ofZhejiangUniversityHangzhout310027) AbstractThedispersionsecularequationofRayleighwaveandtheformulationofdeterminingdisplace-meatdistribution (oreachmodev ~ aveinanisotropiclayeredsoilsaredevelopedbyusingfiniteelementmethodandanalyticalmethodinthispaper.ThemethodpresentedcanbeusedtocalculatethedispersioncurvesanddisplacmentvectorsofRayleighwaveinsoilswhoseshearwavevelocityincreaseswithdepthtpavementstructuresandintercalarysoils.ThedispersioncharacteristicsanddisplacementofRayleighwaveintransverseisotropiclayeredsoilswhoseshearwavevelocityincreaseswithdepthareemphaticallydiscussedinthispaper.Keywordssoildynamics; anisotropiclayeredsoil; Rayleighsurfacewave; disperionsecularequation; dispersioncu ~ ve XIA Tang on behalf of the first author. M, Associate Professor ,[link widoczny dla zalogowanych], Feb. 1965 students.} l789 2 XIA Tang on behalf of the other: anisotropy transition in layered soil dispersion characteristics Rayieigh which K1l-K rKlKl2K1】 KL ·] [K] a lKK - a {G. A c.,[link widoczny dla zalogowanych], + Sik e. Kl 'one of which Chu c a c ÷ G a ÷ c. Ⅱ 2 a ÷ cG. Report cK1 a word c + chu c. ÷ c ÷ cta + ÷ G.c BU report c chu cK23 a deduction of a fl {c ÷ c ÷ c. -] J a K as a K: D + = 2C,[link widoczny dla zalogowanych], C1pC a C .197 buckle c. ÷ G + {G a c a a ÷ c G. Yue one.] G: + cj go to one = once = 2C,[link widoczny dla zalogowanych],, C c 3 b 3, each down on a £ ±: ri (Ca + e.) 6Dl-C -L-K

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