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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,ropa ed hardy, 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,ed hardy danmark, Associate Professor ,christian louboutin shoes, 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.,Oakley juliet, + 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,Ed Hardy mexico, C1pC a C .197 buckle c. ÷ G + {G a c a a ÷ c G. Yue one.] G: + cj go to one = once = 2C,, C c 3 b 3, each down on a £ ±: ri (Ca + e.) 6Dl-C -L-K
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