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  1. NTU Theses and Dissertations Repository
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  3. 應用力學研究所
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/15996
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dc.contributor.advisor葉超雄(Chau-Shioung Yeh)
dc.contributor.authorYu-Liang Chenen
dc.contributor.author陳昱良zh_TW
dc.date.accessioned2021-06-07T17:57:33Z-
dc.date.copyright2012-08-16
dc.date.issued2012
dc.date.submitted2012-08-13
dc.identifier.citation參考文獻
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[2] Biot, M.A. (1955),“Theory of elasticity and consolidation for a porous anisotropic solid”, Journal of Applied Physics, Vol. 26, pp.182-185.
[3] Biot, M.A. (1956), “Theory of deformation of a porous viscoelastic anisotropic solid”, Journal of Applied Physics, Vol. 27, pp.459-467.
[4] Biot, M.A. (1956), “Theory of propagation of elastic waves in fluid saturated porous solid”, Journal of the Acoustical Society of America Vol. 28, pp.168-178.
[5] Biot, M.A. (1962), “Mechanics of deformation and acoustic propagation in porous media”, Journal of Applied Physics, Vol. 33, pp.1482-1498.
[6] Biot, M.A. (1940), “The influence of initial stress on elastic wave”, Journal of Applied Physics, Vol. 11, pp.522-530.
[7] Biot, M.A. (1963), ”Theory of stability and consolidation of a porous medium under initial stress”, Journal of Mathematics And Mechanics,Vol. 12,pp.521-542.
[8] Biot, M.A. (1965), “Mechanics of Incremental Deformation”, John Wiley and Sons Inc., New York.
[9] Deresiewicz, H. (1960), “The effect of boundaries on wave propagation in a liquid filled porous solid-I”, Bulletin of the Seismological Society of America Vol.50,pp.599-607.
[10] Deresiewicz, H. (1961), “The effect of boundaries on wave propagation in a liquid filled porous solid-II, Love waves in a porous layer”, Bulletin of the Seismological Society of America Vol. 51, pp.51-59.

[11] Deresiewicz, H. (1962), “The effect of boundaries on wave propagation in a liquid filled porous solid-IV”, Bulletin of the Seismological Society of America, Vol. 52, pp.627-638.
[12] Deresiewicz, H. (1964), “The effect of boundaries on wave propagation in a liquid filled porous solid-VI”, Bulletin of the Seismological Society of America, Vol.54, pp.417-423
[13] Deresiewicz, H. (1965), “The effect of boundaries on wave propagation in a liquid filled porous solid-IX”, Bulletin of the Seismological Society of America, Vol.55, pp. 919-923.
[14] Bose, S.K. (1962), “Wave propagation in marine sediments and water saturated soils”, Pure and Applied Geophysics, Vol. 52, pp. 27-40.
[15] Deresiewicz, H. and Rice, J.T. (1962), “The effect of boundaries on wave propagation in a liquid porous solid-III”, Bulletin of the Seismological Society of America, Vol.52, pp.595-625.
[16] Rao, R.V.M. and Sarma, R.K. (1978), “Love wave propagation in poro-elasticity”, Defence Science Journal, Vol. 28, pp.157-160.
[17] Burridge, R. and Vargas, C.A. (1979), “The fundamental solution in dynamic poro-elasticity”, Geophysical Journal of the Royal Astronomical Society, Vol.58, pp.61-90.
[18] Guz, A.N. (1986), “Elastic Waves in a Body with Initial Stresses. I. General Theory”, Naukova Dumka, Kiev (in Russian).
[19] Guz, A.N. (1986), “Elastic Waves in a Body with Initial Stresses. II. Propagation Laws”, Naukova Dumka, Kiev (in Russian).
[20] Guz, A.N. (2002), “Elastic waves in bodies with initial (residual) stresses”, Int. Appl. Mech., Vol.38,pp.23–59.
[21] Guz, A.N. (2004), “Elastic Waves in Bodies with Initial (Residual) Stresses”, A.S.K., Kiev (in Russian).
[22] Akopyan, Zh.S., Guz, A.N. and Navoyan, A.V. (1974), “Problems of stability of vertical mimings, Prikl. Mekhan.”, Vol. 10, No. 5, pp.54-62.
[23] Asamidinov, F.M., Guz, A.N. and Kuliev, G.G. (1977), “Stability of horizontal mine workings of noncircular form”, Prikl. Mekhan., Vol. 13, No. 6, pp.112-115.
[24] Rayleigh L., “On Waves Propagated along Plane Surface of an Elastic Solid,” Proceedings of the London Mathe-matical Society.
[25] Meissner, E. (1921), ‘‘Elastic oberflachenwellen mit Dispersion in einem inhomogenen Mmedium’’, Viertelgahrsschr Naturforsch. Ges. in Zuerich, Vol.66, pp.181–195..
[26] Vardoulakis, I. (1984), ‘‘Torsional surface waves in inhomogeneous elastic media’’, Int. J. Numer. Anal. Methods Geomech., Vol.8, pp.287–296.
[27] Dey, S., Gupta, A.K. and Gupta, S. (1996), “Torsional surface waves in nonhomogeneous and anisotropic medium”, J. Acoust. Soc. Am., Vol.99, pp.2737–2741
[28] Selim M.M. (2007), “Propagation of torsional surface waves in heterogeneous half-space with irregular free surface”, Appl. Math. Sci., Vol.1, No.29, pp.1429–1437.
[29] Gupta S. , Chattopadhyay A. and Majhi D.K. (2010), “Effect of Irregularity on the Propagation of Torsional Surface Waves in an Initially Stressed Anisotropic Poro-Elastic Layer”, Appl. Math. Mech., Vol. 31, pp.481–492.
[30] ]Dey, S., Gupta, A.K., Gupta, S. and Prasad, A.M. (2000), “Torsional surface waves in nonhomogeneous anisotropic media under initial stress”, J. Eng. Mech.,Vol.126, No.11, pp.1120–1123.
[31] Dey S. and Sarkar, M.G. (2002), “Torsional surface wave in initially stressed anisotropic porous medium”, J. Eng. Mech., Vol.128, No.2, pp.184–189.
[32] Achenbach, J.D. (1973), “Wave Propagation in Elastic Solids,” North Holland Publishing Comp., New York.
[33] Dey, S. (1971), “Torsional waves under initial stress”, Pure and Applied Geophysics, pp.53-59.
[34] Chattaraj, R., Samal, S.K. and Mahanti, N.C. (2011), “Propagation of torsional surface wave in anisotropic poroelastic medium under initial stress”, Wave Motion , Vol.48, pp.184–195.
[35] Dey, S., Gupta, S. and Gupta, A. K. (1993), “Torsional Surface Wave in an Elastic Half Space with Void Pores”, Int. J. Numer. Anal. Methods Geomech., Vol. 17, pp. 197-204.
[36] http://www.forshang.org
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/15996-
dc.description.abstract由文獻中可以知道扭轉表面波無法在均質的彈性半空間中傳播,本文主要是要探討有初始應力作用下扭轉表面波在非均質異向性彈性介質與液體飽和孔隙彈性介質的可能性與其波傳特性。
本文的分析方法,主要是利用Biot增量變形彈性理論及孔隙彈性理論來分析扭轉表面波的波傳問題,首先我們由Biot彈性理論中得到問題的控制方程式,解出其位移場後,將邊界條件代入位移場中,可以得到扭轉表面波的相速度方程式並加以分析。
本文的問題主要分成兩個部分,第一部分是扭轉表面波在有初始應力作用下的非均質異向性彈性半空間中的波傳特性分析;第二部分是扭轉表面波在有初始應力作用下的液體飽和孔隙彈性半空間的波傳特性分析。
研究的結果顯示出扭轉表面波可以在非均質與液體飽和孔隙彈性半空間中傳播,而初始應力的存在會降低扭轉表面波的波速,其他因素,例如:非均質性、異向性因子、孔隙率等也會影響扭轉表面波的傳遞波速。
zh_TW
dc.description.abstractIt is well known that torsional surface wave cannot propagate in the homogeneous elastic half space. The present article studies the propagation of torsional surface wave in nonhomogeneous anisotropic medium and fluid saturated poroelastic medium under initial stress.
In this article, we try to use Biot’s incremental deformation theory of elasticity and poroelastic theory analyzing the wave propagation problem. Firstly, we obtaine the governing equations from Biot’s theory. By solving the governing equations, we can obtain the displacement field. Taking the displacement field into the boundary condition ,we can get the velocity equation of torsional surface wave.
The problem of this paper is divided into two parts. The first part is that propagation of torsional surface wave in nonhomogeneous anisotropic medium under initial stress; the second part is that propagation of torsional surface wave in fluid saturated poroelastic medium under initial stress.
The results of the study show that torsional surface wave can propagate in nonhomogeneous anisotropic medium and fluid saturated poroelastic medium under initial stress. The presence of initial stress diminishes the velocity of torsional surface wave. The other factors also influence the velocity of torsional surface wave as non-homogeneity, anisotropy factor etc.
en
dc.description.provenanceMade available in DSpace on 2021-06-07T17:57:33Z (GMT). No. of bitstreams: 1
ntu-101-R99543093-1.pdf: 2863288 bytes, checksum: facec014cdab673507495a8bf12d282e (MD5)
Previous issue date: 2012
en
dc.description.tableofcontents第一章 緒論 1
1.1研究動機與背景 1
1.2文獻回顧 2
1.3研究內容概述 14
1.4論文架構 15
第二章 Biot增量變形彈性理論 17
2.1二維的增量應力(incremental stresses) 17
2.2三維的增量應力 17
2.3三維的增量應力平衡方程式 25
2.4液體飽和孔隙材料之應力與應變 32
2.5液體飽和孔隙材料中增量應力與應變關係 36
2.6導入慣性力 39
第三章 問題分析 44
3.1扭轉表面波於有初始應力作用之異向性非均質彈性半空間傳播 44
3.1.1問題敘述 44
3.1.2受初始應力作用之非均質異向性彈性介質的控制方程式與位移場 45
3.1.3邊界條件 53
3.1.4數值結果分析 56
3.2扭轉表面波於有初始應力作用之異向性非均質與飽和液體孔隙彈性半空間之傳播 67
3.2.1問題敘述 67
3.2.2受初始應力作用之液體飽和孔隙彈性半空間的控制方程式與位移場 68
3.2.3邊界條件 74
3.2.4數值結果分析 77
第四章 結論與未來展望 80
4.1 結論 80
4.1.1扭轉表面波於有初始應力作用之異向性非均質彈性半空間傳播 80
4.1.2扭轉表面波於有初始應力作用之異向性非均質與飽和液體孔隙彈性半空間之傳播 81
4.2 未來展望 81
參考文獻 83
dc.language.isozh-TW
dc.subject初始應力zh_TW
dc.subject扭轉表面波zh_TW
dc.subject異向性zh_TW
dc.subject非均質zh_TW
dc.subject孔隙材料zh_TW
dc.subjectBiot彈性理論zh_TW
dc.subjectporous mediumen
dc.subjecttorsional surface waveen
dc.subjectinitial stressen
dc.subjectanisotropicen
dc.subjectBiot’s theoryen
dc.subjectinhomogeneousen
dc.title扭轉表面波在初始應力作用下於非均質與異向性及飽和液體孔隙彈性半空間之傳播zh_TW
dc.titleTorsional Surface Wave in Nonhomogeneous Anisotropic Medium and Fluid Saturated Poroelastic Medium under Initial Stressen
dc.typeThesis
dc.date.schoolyear100-2
dc.description.degree碩士
dc.contributor.oralexamcommittee陳東陽(Tung-Yang Chen),鄧崇任(Tsung-Jen Teng),施博仁(Po-Jen Shih)
dc.subject.keyword扭轉表面波,初始應力,異向性,非均質,孔隙材料,Biot彈性理論,zh_TW
dc.subject.keywordtorsional surface wave,initial stress,anisotropic,inhomogeneous,porous medium,Biot’s theory,en
dc.relation.page86
dc.rights.note未授權
dc.date.accepted2012-08-14
dc.contributor.author-college工學院zh_TW
dc.contributor.author-dept應用力學研究所zh_TW
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