The Contribution of Two-Dimensional Source Effects to the Far-Field Seismic Signatures of Underground Nuclear Explosions

Abstract

Two-dimensional calculations of underground explosions are able to include free surface interaction effects and the depth dependence of overburden pressure and material properties, as well as the complex constitutive models for geologic materials developed in one-dimensional (spherically symmetric) studies. Eleven axisymmetric calculations of explosions in granite are analyzed in this study to determine the two-dimensional effects on the far-field body and surface waves and the magnitude mb and Ms. Seven of these are hypothetical 150 KT explosions at depths from 159 to 1000 meters calculated by Applied Theory, Inc. (ATI). These show depth effects that are different, though not strikingly so, from those calculated with one-dimensional source models. The other four calculations were done by Systems, Science and Software (S-Cubed). The first was for a specific event (PILEDRIVER), and the depth and yield were varied for the other three. the near- and far-field data for PILEDRIVER were matched rather well, except that the spallation was too large in the calculation.

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1980
Accession Number
ADA123664

Entities

People

  • J. T. Cherry
  • N. Rimer
  • T. Barker
  • Thomas C. Bache

Organizations

  • Utility Systems Science and Software (United States)

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Computational Science
  • Coordinate Systems
  • Doppler Effect
  • Earth Models
  • Far Field
  • Frequency Shift
  • Linear Momentum
  • Near Field
  • Nuclear Explosions
  • Rayleigh Waves
  • Seismic Signatures
  • Seismic Waves
  • Surface Waves
  • Systems Science
  • Three Dimensional
  • Two Dimensional
  • Wave Propagation

Fields of Study

  • Physics

Readers

  • Computational Fluid Dynamics (CFD)
  • Explosive Engineering.
  • Theoretical Analysis.