Large-Scale Numerical Analysis of Three-Dimensional Seismic Waves.

Abstract

This report concludes our study of large-scale vectorized numerical analysis applied to time domain seismic wave phenomena in filled basins. Applications include calculations of waves from simple surface or buried sources in a variety of idealized 2-D Basin and Range models (36,000 to 120,000 nodes) described in an interim report, and one large 3-D model (400,000 nodes) from Yucca Flat, Nevada Test Site, described here. Analysis is based on an explicit, finite element, elastic wave solver designed for vectorized execution on the CRAY-1. The primary result of the present 3-D study is that, given the database available from investigations in Yucca Flat, Nevada Test Site, the size of feasible 3-D computational models on the CRAY-1S is adequate to simulate elastic wave fields and interpret arrivals for comparison with existing 3-D ground motion data. Synthetic seismograms from a 400,000 element 3-D simulation of the COALORA event a Yucca Flat indicate that a significant source of transverse motion on radial lines through the source is diffraction from a discontinuity in the Rainier Mesa tuff layer across the Yucca fault. Successful time-domain simulations in 3-D are feasible with pipelined supercomputers but optimal processing requires careful tailoring of the algorithm to vectorize inner code loops and eliminate nonessential arithmetic.

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Document Details

Document Type
Technical Report
Publication Date
May 31, 1984
Accession Number
ADA144610

Entities

People

  • D. K. Vaughan
  • G. L. Wojcik

Tags

Communities of Interest

  • Energy and Power Technologies
  • Weapons Technologies

DTIC Thesaurus Topics

  • Air Force
  • Computers
  • Databases
  • Diffraction
  • Eigenvalues
  • Eigenvectors
  • Elastic Waves
  • Equations
  • Finite Element Analysis
  • Geometry
  • Numerical Analysis
  • Seismic Waves
  • Three Dimensional
  • Time Domain
  • Two Dimensional
  • Wave Phenomena
  • Waves

Readers

  • Parallel and Distributed Computing.
  • Seismology
  • Structural Dynamics.