Finite-Difference Simulations of Rayleigh-Wave Scattering by Shallow Heterogeneity.

Abstract

Rayleigh waves normally incident upon 2-D shallow heterogeneity are simulated by the linear finite-difference method to study attenuation, transmission, and reflection of Rayleigh waves and to measure the Rayleigh-to-P and -SV body wave conversion. Transmission, reflection, and scattering depend on the depth, average scale size of the heterogeneity and the amplitude of the spatial fluctuation of velocity. As expected, larger spatial variation in velocity attenuates Rayleigh waves more than smooth media and the attenuation is roughly proportional to the variance of the velocity fluctuation. The attenuation and scattering due to shallow heterogeneity is weaker than attenuation due to moderately rough topography. Keywords: Finite difference; Scattering; Rayleigh wave; Attenuation; Heterogeneity.

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Document Details

Document Type
Technical Report
Publication Date
Nov 01, 1987
Accession Number
ADA194961

Entities

People

  • Keith L. Mclaughlin
  • Rong-song Jih

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Doppler Effect
  • Earth Sciences
  • Elastic Waves
  • Energy
  • Explosions
  • Frequency Bands
  • Geography
  • Geology
  • Geophysics
  • Phase Velocity
  • Planetary Sciences
  • Rayleigh Waves
  • Scattering
  • Surface Waves
  • Topography
  • Two Dimensional
  • Wave Propagation

Fields of Study

  • Physics

Readers

  • Acoustical Oceanography.
  • Electromagnetic Wave Scattering and Antenna Radiation Engineering
  • Seismology