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浅部地下洞穴散射波对波场扰动分析

柴华友, 柯文汇, 陈健, 黄祥国, 李忠超

柴华友, 柯文汇, 陈健, 黄祥国, 李忠超. 浅部地下洞穴散射波对波场扰动分析[J]. 岩土工程学报, 2018, 40(8): 1473-1480. DOI: 10.11779/CJGE201808013
引用本文: 柴华友, 柯文汇, 陈健, 黄祥国, 李忠超. 浅部地下洞穴散射波对波场扰动分析[J]. 岩土工程学报, 2018, 40(8): 1473-1480. DOI: 10.11779/CJGE201808013
CHAI Hua-you, KE Wen-hui, CHEN Elton J, HUANG Xiang-guo, LI Zhong-chao. Disturbances of surface wave field due to wave scattering at shallow cavities[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(8): 1473-1480. DOI: 10.11779/CJGE201808013
Citation: CHAI Hua-you, KE Wen-hui, CHEN Elton J, HUANG Xiang-guo, LI Zhong-chao. Disturbances of surface wave field due to wave scattering at shallow cavities[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(8): 1473-1480. DOI: 10.11779/CJGE201808013

浅部地下洞穴散射波对波场扰动分析  English Version

基金项目: 国家自然科学基金面上项目(41474113); 武汉工程大学人才专项经费资助项目; 湖北省建设科技计划项目(2016)
详细信息
    作者简介:

    柴华友(1965-),男,博士,副研究员,主要从事多相介质动力响应及波动特性研究。E-mail: chy_rsm@hotmail.com。

Disturbances of surface wave field due to wave scattering at shallow cavities

  • 摘要: 均匀介质体表面源激发的瑞利波能量在介质浅部占主导地位,当前行瑞利波遇体浅部洞穴时,质点位移形状及轨迹会发生改变,瑞利波在洞穴发生散射。散射波导致波场能量出现扰动,波场不同区域扰动特征不同。在洞穴前方,反射瑞利波与入射瑞利波相干,能量谱出现干涉条纹;在洞穴上方,透射波发生频散,相速度不同于瑞利波,在某些条件下,透射波传播特性类似于自由板中兰姆波,透射波在洞穴后边界面绕射会导致表面波场能量减小;在后方区域,受几何衰减影响,表面波场逐渐由透射瑞利波主导,其低频成份相对高频成份能量减少较多。本文基于散射波理论, 分析洞穴埋深/波长比对波场扰动影响,由数值模拟计算验证理论分析,结果表明由测点距—波长域能量谱扰动对应的临界波长可预测洞穴埋深。
    Abstract: In homogenous half spaces, the wave fields at shallow depth are dominated by Rayleigh waves activated by the surface sources. When the forward Rayleigh waves encounter a shallow cavity, the displacement shapes and the particle orbit are changed. Rayleigh waves are scattered at the cavity. The wave field is disturbed by the scattering waves. The different features of the disturbances can be found in different regions of the surface wave field. In the region in front of the cavity, the reflected and the incident Rayleigh waves interfere constructively or destructively with each other. The interference fringes are formed. In the region over the cavity, the transmitted waves are dispersive. The phase velocities are different from those of Rayleigh waves. Under certain conditions, the behaviour of the transmitted waves is similar to that of Lamb waves in the free plates. The diffraction of the transmitted waves along the back boundary results in the energy reduction in the surface wave field over the boundary. Influenced by the geometrical attenuation, the transmitted Rayleigh waves gradually dominate the surface wave field in the back region. The components at low frequencies have greater energy reduction as compared to those at high frequencies. Based on the wave scattering theory, the effects of the ratio of the buried depth to the wavelength of Rayleigh waves on the disturbances of the surface wave field are analyzed. The numerical simulations are used to verify the analyses. It is shown from the results that the buried depth can be estimated from the critical wavelength corresponding to the energy reduction in the offset-wavelength domain.
  • [1] CJJ/T 7—2017城市工程地球物理探测标准[S]. 2018.
    (CJJ/T 7—2017 Standard for urban engineering geophysical exploration[S]. 2018. (in Chinese))
    [2] GUCUNSKI N, GANJI V, MAHER M H.Effects of obstacles on Rayleigh wave dispersion obtained from the SASW test[J]. Soil Dynamics and Earthquake Engineering, 1996, 15: 223-231.
    [3] GANJI V, GUCUNSKI N, MAHER M H.Detection of underground obstacles by SASW method: numerical aspects[J]. Journal of Geotechnical and Geoenviromental Engineering, 1997, 123(3): 212-219.
    [4] GRANDJEAN G, LEPAROUX D.The potential of seismic methods for detecting cavities and buried objects: experimentation at a test site[J]. Journal of Applied Geophysics, 2004, 56(2): 93-106.
    [5] GELIS C, LEPAROUX D, VIRIEUX J, BITRI A, OPERTO S, GRANDJEAN G.Numerical modeling of surface waves over shallow cavities[J]. Journal of Environmental and Engineering Geophysics, 2005, 10(2): 111-121.
    [6] NASSERI-MOGHADDAM A, CASCANTE G, PHILLIPS C, et al.Effects of underground cavities on Rayleigh waves: field and numerical experiments[J]. Soil Dynamics and Earthquake Engineering, 2007, 27(4): 300-313.
    [7] XIA J H, NYQUIST J E, XU Y X, et al.Feasibility of detecting near-surface feature with Rayleigh-wave diffraction[J]. Journal of Applied Geophysics, 2007: 62(3): 244-253.
    [8] TALLAVÓ F, CASCANTE G, PANDEY M.Experimental and numerical analysis of MASW tests for detection of buried timber trestles[J]. Soil Dynamics and Earthquake Engineering, 2009, 29(1): 91-102.
    [9] 夏宇靖. 稳态表面波实测地下异质体D-VR曲线的类型[J]. 煤田地质与勘探, 1996, 24(1): 50-55.
    (XIA Yu-jing.Types of D-VR curves obtained by steady Rayleigh wave testing[J]. Coal Geology and Prospecting, 1996, 24(1): 50-55. (in Chinese))
    [10] 柴华友, 卢应发, 刘明贵, 等. 表面波谱分析影响因素研究[J]. 岩土力学, 2004, 25(3): 347-353.
    (CHAI Hua-you, LU Ying-fa, LIU Ming-gui, et al.Influences of measuring factors on spectral analysis in surface wave testing[J]. Rock and Soil Mechanics, 2004, 25(3): 347-353. (in Chinese))
    [11] 柴华友, 卢应发, 李祺, 等. 半无限体介质内异质体方位探测数值研究[J]. 岩土力学, 2007, 28(1): 188-192.
    (CHAI Hua-you, LU Ying-fa, LI Qi, et al.Numerical study on detection of heterogeneities in an half space[J]. Rock and Soil Mechanics, 2007, 28(1): 188-192. (in Chinese))
    [12] 柴华友, 崔玉军, 卢应发, 等. 地下洞穴对表面波表观相速度影响的数值分析[J]. 岩石力学与工程学报, 2006, 25(5): 956-962.
    (CHAI Hua-you, CUI Yu-jun, LU Ying-fa, et al.Numerical analysis of influences of underground cavity on apparent phase velocities of surface waves[J]. Chinese Journal of Rock Mechanics and Engineering, 2006, 25(5): 956-962. (in Chinese))
    [13] VAN WIJK K.Multiple scattering of surface waves[D]. Colorado: Center for Wave Phenomena, Colorado School of Mines, 2003.
    [14] CAMPMAN X H, VAN WIJK K, SCALES J A, et al.Imaging and suppressing near-receiver scattered surface waves[J]. Geophysics, 2005, 70(2): 21-29.
    [15] CAMPMAN X H.Imaging and suppressing near-receiver scattered seismic waves[D]. Delft: Delft Institute of Applied Mathematics, Delft University of Technology, 2005.
    [16] RIYANTI C D.Modeling and inversion of scattered surface waves[D]. Delft: Delft Institute of Applied Mathematics, Delft University of Technology, 2005.
    [17] 伊文, 贾戴茨基, 普瑞斯. 层状介质中的弹性波[M]. 刘光鼎, 译. 北京: 科学出版社, 1966.
    (EWING W M, JARDETZKY W S, PRESS F.Elastic waves in layered media[M]. LIU Guang-ding, tran. Beijing: Science Press, 1966. (in Chinese))
    [18] FOINQUINOS R, ROËSSET J M. Elastic layered half-spaces subjected to dynamic surface loads[M]. KAUSEL E, MANOLIS G, eds. Southampton: WIT Press, 2001.
    [19] KAUSEL E, PEEK R.Dynamic loads in the interior of a layered stratum: an explicit solution[J]. Bulletin of the Seismological Society of America, 1982, 72(5): 1459-1481.
    [20] KAUSEL E.Dynamic point sources in laminated media via the thin-layer method[J]. International Journal of Solids and Structures, 1999, 36(31): 3614-3631.
    [21] CHAI H Y, PHOON K K, GOH S H, et al.Some theoretical and numerical observations on scattering of Rayleigh waves in media containing shallow rectangular cavities[J]. Journal of Applied Geophysics, 2012, 83: 107-119.
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出版历程
  • 收稿日期:  2017-04-24
  • 发布日期:  2018-08-24

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