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Surface motion of alluvial valley in layered half-space for incident plane P-waves

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Surface motion of alluvial valley in layered half-space for incident plane P-waves

Content Provider	Springer Nature Link
Author	Ba, Zhenning Liang, Jianwen
Copyright Year	2011
Abstract	The indirect boundary element method (IBEM) is used to study the surface motion of an alluvial valley in layered half-space for incident plane P-waves based on Wolf’s theory. Firstly, the free field response can be solved by the direct stiffness method, and the scattering wave response is calculated by Green’s functions of distributed loads acting on inclined lines in a layered half-space. The method is verified by comparing its results with literature and numerical analyses are performed by taking the amplification of incident plane P-waves by an alluvial valley in one soil layer resting on bedrock as an example. The results show that there exist distinct differences between the wave amplification by an alluvial valley embedded in layered half-space and that in homogeneous half-space and there is interaction between the valley and the soil layer. The amplitudes are relatively large when incident frequencies are close to the soil layer’s resonant frequencies.
Starting Page	157
Ending Page	165
Page Count	9
File Format	PDF
ISSN	10064982
Journal	Transactions of Tianjin University
Volume Number	17
Issue Number	3
e-ISSN	19958196
Language	English
Publisher	Tianjin University
Publisher Date	2011-06-22
Publisher Place	Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	layered half-space alluvial valley plane P-waves scattering one layer over bedrock indirect boundary element method Science Mechanical Engineering
Content Type	Text
Resource Type	Article
Subject	Multidisciplinary

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