[1]BA Zhenning,ZHANG Enwei,LIANG Jianwen,et al.Scattering by a Transverse Isotropic Saturated Alluvial Valley for Incident Plane qP1 Wave[J].Journal of Seismological Research,2019,42(04):474-482.
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Journal of Seismological Research[ISSN 1000-0666/CN 53-1062/P] Volume:
42
Number of periods:
2019 04
Page number:
474-482
Column:
Public date:
2019-12-15
- Title:
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Scattering by a Transverse Isotropic Saturated Alluvial Valley for Incident Plane qP1 Wave
- Author(s):
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BA Zhenning1; 2; ZHANG Enwei1; 2; LIANG Jianwen1; 2; WU Mengtao1; 2
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(1.Department of Civil Engineering,Tianjin University,Tianjin 300350,China)(2.Key Laboratory of Coast Civil Structure Safety,Ministry of Education,Tianjin 300350,China)
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- Keywords:
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alluvial valley; transverse isotropic saturated; plane qP1 wave; seismic wave scattering; indirect boundary element method(IBEM)
- CLC:
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P315.9
- DOI:
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- Abstract:
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Based on Biot's theory of fluid saturated medium,the Indirect Boundary Element Method(IBEM)is used to solve the scattering problem of the plane qP1 wave from transversely isotropic(TI)saturated alluvial valley in frequency domain.The correctness of the method is verified by comparing with the results of isotropic saturated sites.Numerical calculation and analysis of different situations were carried out,with emphasis on the influence of TI properties of alluvial valley on the dynamic response of the surface.The results show that the TI properties have significant influence on the amplitude and spatial distribution of surface displacement,and the degree of influence depends on the incident angle,incident frequency and observation point location of the qP1 wave.Considering the TI properties,the scattering of the plane qP1 waves by alluvial valleys can be simulated more accurately.