地下圆形衬砌隧洞对弹性波的散射
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摘要
大型地下隧道结构对地震波的散射会影响隧道附近场地的地震动,进而会影响附近地面上的建筑物。因此,对此类问题的求解,不仅在理论上,而且在工程应用上都有着重要的意义。
     本文采用一种特殊的边界积分方程法,研究了半空间内地下衬砌隧洞对弹性波P、SV、Rayleigh波的散射情况,介质内总波场由自由场和散射场叠加而得,根据单层位势理论,由虚拟源面上的分布线源构造散射波场,通过边界条件建立方程,求解得到虚拟波源密度,进而求得总的波场。
     本文从边界条件的满足情况以及与现有解析解的对比两个方面来检验结果的正确性。研究了弹性入射P、SV波以及Rayleigh面波的不同入射波频率、入射角、衬砌材料的性质等因素对地下圆形衬砌隧洞附近场地的地表位移和衬砌隧洞洞周环向动应力集中因子的影响。数值结果表明,地下隧洞的存在对附近场地的地表位移以及洞室的动应力集中因子有很大的放大作用,柔性衬砌对中低频波的放大作用大一些,刚性衬砌对高频波的放大作用明显一些,刚性衬砌能够有效降低半空间介质中的应力。本文的研究对该领域的理论研究及工程应用都有重要的意义,为地下洞室群的抗震设计提供了科学依据。
Scattering and diffraction of earthquake waves by the large, underground tunnelstructures can affect the ground motion near the tunnels, still, it can also affect thebuildingsonthegroundnearby.Therefore,tosolvethiskindofproblemhasimportantmeaningonboththeoryandengineeringapplication.
     In this paper, a special boundary integral equation method will be used to studythe scattering of elastic P、SV and Rayleigh waves by underground, circular linedtunnel. The total wave field is superposed by free field and scattered field. Based onthe theory of simple layer potential, scattered wave field is constructed by distributedlinesources onthe virtual source plane. The densityofthe virtual wavesource can begained by solving the equations which are derived by boundary conditions. Finally,thewholewavefieldcanbeachieved.
     The accuracy of the numerical result is checked up by the analytic solution andresidual errors of boundary conditions. At the same time, the effects of some factorssuch as the frequencyof the incident waves, the incident angle, the lining’s propertieson the surface ground motion of the lined tunnels and the lining’s properties on thehoop stress amplitude on the wall of the lined tunnel are illustrated. The numericalresults show that, the underground tunnel will amplify the amplitude of the surfaceground motion and the dynamic stress concentration factor, the tunnel with soft linerhas great effect on the low frequency incident waves, while the tunnel with stiff linerhas great effect on the high frequency incident waves, and the tunnel with stiff linercan also decrease the stress in the half-space. And some useful conclusions arederived in this thesis, which have great significance both in theoryand in engineeringapplication and provide foundations for the anti-seismic design of undergroundcavities.
引文
[1] Trifunac, M. D., Surface motion of a semi-cylindrical alluvial valley for incidentplane SH wave, Bulletin of Seismological and Society of America, 1971, 61(6):1755-1770
    [2] Pao.Y.H, MOW.C.C., Diffraction of Elastic Waves and Dynamic StressConcentrations[M].NewYork::CraneRussakandCompany,1973.
    [3] Vincent W.Lee, On deformations near a circular underground cavity subjected toincident plane SH waves, Proceedings of the Application of Computer Methodsin Engineering Conference, Vol.Ⅱ, University of Southern California. LosAngeles,Calif.,1977,105:951~962
    [4] Vincent W.Lee, Mihailo D.Trifunac, Response of tunnels to incident SH-waves,Journal of Engineering Mechanics, American Society of Civil Engineers, 1979,105:643~659
    [5] Vincent W.Lee, James Karl, Diffraction of SV waves by underground circularcylindrical cavities, Soil Dynamics and Earthquake Engineering, 1992, 11:445~456
    [6] Vincent W.Lee, James Karl, On deformations near a circular underground cavitysubjected to incident plane P waves, European Earthquake Engineering, 1993,7(1):29~36
    [7] Trifunac, M. D., Scattering of plane SH wave by a semi-cylindrical canyon,EarthquakeEngineeringandStructuralDynamics,1973,1:267-281
    [8] H.L.Wong, M.D.Trifunac, Scattering of plane SH waves by a semi-ellipticalcanyon,EarthquakeEngineeringandStructuralDynamics,1974,3:157~169
    [9] H.L.Wong, M.D.Trifunac, Surface motion of a semi-elliptical alluvial valley forincident plane SH waves, Bulletin of Seismological and Society of America,1974,64:1389~1408
    [10] Sanchez-Sesma, F.J. and J.A.Esquivel, Ground motion of alluvial valleys underincident plane SH waves, Bulletin of Seismological and Society of America,1979,69(4):1107-1120
    [11]H.L.Wong,Effect of surfacetopographyonthediffractionofP,SV,andRayleighwaves, Bulletin of Seismological and Society of America, 1982, 72(4):1167-1183
    [12] Cao, H., Vincent W.Lee, Scattering of plane SH waves by circular cylindricalCanyons with various depth-to-width ratios, European Journal of EarthquakeEngineering,1989,3(2):29~37
    [13] M.I.Todorovska, Vincent W.Lee, Surface motion of shallow circular alluvialvalleys for incident plane SH waves-analytical solution, Soil Dynamics andEarthquakeEngineering,1991,10(4):192~200
    [14] Vincent W.Lee, Xiaoyun Wu, Application of the weighted residual method todiffraction by 2-D canyon of arbitrary shape:Ⅰ. Incident SH waves, SoilDynamicsandEarthquakeEngineering,1994,13(5):355~364
    [15] Vincent W.Lee, Michael E.Manoogian, Surface motion above an arbitraryshapeUnderground cavity for incident SH waves, European Earthquake Engineering,1995,Patroneditore:3~11
    [16] Michael E.Manoogian, Vincent W.Lee, Diffraction of SH waves by subsurfaceinclusions of arbitrary shape, ASCE Journal of Engineering Mechanics, 1996,122(2):123~129
    [17] Ohsaki, Y. On movements of a rigid body in semi-infinite elastic medium [J].Proc.oftheJapaneseEarthquakeEngng.Symp.Tokyo,Japan.
    [18] Wong H L. Effect of surface topography on the diffraction of P, SV, andRayleigh waves, Bulletin of Seismological Society of America, 72: 1167-1183,1982
    [19]纪晓东,地下圆形衬砌隧道对入射平面P波的散射:[硕士学位论文],天津:天津大学,2002
    [20]罗昊,圆弧形凸起地形中圆形隧洞对平面SH波的散射解析解:[硕士学位论文],天津:天津大学,2003
    [21]张浩,SH波对半空间洞室群的散射的分析及应用:[硕士学位论文],天津:天津大学,2003
    [22]梁建文,张浩,V.W.Lee,地下洞室群对地面运动影响问题的级数解答—P波入射,地震学报,2004,26(3):269~280
    [23]丁美,地下圆形衬砌隧洞对柱面SH波的散射解析解:[硕士学位论文],天津:天津大学,2004
    [24]李宁,地下双线衬砌洞室对SV波散射的解析解:[硕士学位论文],天津:天津大学,2005
    [25]李艳,地下圆形洞室对柱面SH波的散射:[硕士学位论文],天津:天津大学,2006
    [26]张敏,地下圆形夹塞区及衬砌隧洞对柱面SH波的散射:[硕士学位论文],天津:天津大学,2006
    [27]林宏,刘殿魁,半无限空间中圆形孔洞周围SH波的散射,地震工程与工程振动,2002,22(2):9~16
    [28]姜艳,黄富荣,刘殿魁等,SH波在浅埋多个圆孔处的散射与地震动,地震工程与工程振动,2004,24(1):7~14
    [29]熊洪允,曾绍标,毛云英,应用数学基础(上下册),天津:天津大学出版社,1994
    [30]胡聿贤,地震工程学,北京:地震出版社,1988
    [31]廖振鹏,工程波动理论导引,北京:科学出版社,1996
    [32]徐芝纶,弹性力学简明教程(第三版),北京:高等教育出版社,2002
    [33]郭自强,固体中的波,北京:地震出版社,1982
    [34]阿肯巴赫(美),弹性固体中波的传播(徐植信,洪锦如),上海:同济大学出版社,1985
    [35]鲍亦兴,毛昭宙,弹性波的衍射与动应力集中(刘殿魁,苏先樾),北京:科学出版社,1993
    [36]钟伟芳,聂国华,弹性波的散射理论,武汉:华中理工大学出版社,1997
    [37]李军伟,平面P波入射下浅圆谷场地地震反应的解析解及其工程应用:[硕士学位论文],天津:天津大学,1997
    [38]张郁山,圆弧形层状沉积河谷与凹陷地形在平面SH波入射下的场地反应:[硕士学位论文],天津:天津大学,1999
    [39]秦东,平面SV波入射下浅圆谷场地地震反应的解析解及其工程应用:[硕士学位论文],天津:天津大学,1999
    [40]严林隽,浅圆层状沉积河谷与凹陷地形在平面P波与SV波入射下的场地反应:[硕士学位论文],天津:天津大学,2001
    [41]梁建文,张郁山,顾晓鲁,圆弧形层状沉积河谷场地在平面SH波入射下动力响应分析,岩土工程学报,2000,22(4):396~401
    [42]梁建文,严林隽,李军伟,V.W.Lee,圆弧形沉积河谷场地在平面P波入射下的响应,岩土力学,2001,22(3):138~143
    [43]梁建文,严林隽,V.W.Lee,圆弧形层状沉积谷地对入射平面P波的散射解析解,地震学报,2001,23(2):167~184
    [44]梁建文,严林隽,V. W. Lee,圆弧形凹陷地形表面覆盖层对入射平面SV波的影响,地震学报,2001,23(6):622~636
    [45]刘晶波,廖振鹏,地震波散射问题的数值解,地震工程与工程振动,1987,7(2):1~13
    [46]袁晓铭,廖振鹏,圆弧形凹陷地形对平面SH波散射问题的级数解答,地震工程与工程振动,1993,13(2):1~11
    [47]袁晓铭,廖振鹏,圆弧形沉积盆地对平面SH波的散射,华南地震,1995,15(2):1~8
    [48]杜修力,熊建国,波动问题的级数解边界元法,地震工程与工程振动,1988,8(1):39~49
    [49]杜修力,熊建国,关慧敏,平面SH波散射问题的边界积分方程分析法,地震学报,1993,15(3):331~338