Conservation Laws with Dissipation,

Abstract

The conservation laws of isothermal, isentropic or adiabatic thermoelasticity, in all their standard variants (Lagrangean or Euclidean formulation, solids or fluids, one or several space dimensions, etc.), lead to systems of quasilinear hyperbolic equations. A feature of such systems in that the Cauchy problem does not have global smooth solutions, even when the initial data are very smooth, due to the formation of shock waves. However, global solutions exist in the class of functions of bounded variations. A dissipative mechanism may affect, in general, the asymptotic behavior as well as the smoothness of solutions. Ranked according to effectiveness, dissipative mechanisms may be classified into those which are so powerful as to smoothen out even rough initial data, always yielding smooth solutions; those that preserve the smoothness of smooth initial data but are incapable of smoothening rough initial data; those that preserve the smoothness of smooth and 'small' initial data but cannot prevent the breaking of smooth waves of large amplitude; and those that are not capable to prevent even the breaking of smooth waves of small amplitude.

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1980
Accession Number
ADA088762

Entities

People

  • C. M. Dafermos

Organizations

  • Brown University

Tags

Communities of Interest

  • C4I

DTIC Thesaurus Topics

  • Adiabatic Processes
  • Applied Mathematics
  • Cauchy Problem
  • Discontinuities
  • Dissipation
  • Elastic Materials
  • Equations
  • Equations Of Motion
  • Formulas (Mathematics)
  • Materials
  • Mathematics
  • Military Research
  • Rhode Island
  • Shock
  • United States
  • Volterra Equations
  • Waves

Fields of Study

  • Mathematics

Readers

  • Coastal Oceanography
  • Finite Element Method (FEM) for solving Partial Differential Equations (PDEs)

Technology Areas

  • Space