Abstract

We consider a scalar balance law with a strict convex flux. In this paper, we study inviscid limit to shocks for scalar balance laws up to a shift function, which is based on the relative entropy.

Highlights

  • We consider the following balance law in one-dimensional space R:∂tU + ∂xA (U) = g (U) + ε∂x2xU,U (0, x) = U0 (x), (1)t > 0, x ∈ R, where the flux A󸀠󸀠(V) := a󸀠(V) ≥ c for some constant c > 0 and U0 ∈ L∞(R)

  • The relative entropy method introduced by Dafermos [3, 4] and Diperna [5] provides an efficient tool to study the stability and asymptotic limits among thermomechanical theories, which is related to the second law of thermodynamics

  • For the relaxation there is an application for compressible models by Lattanzio and Tzavaras [16, 17] and we can see Berthelin et al [18, 19] as some applications of hydrodynamical limit problems

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Summary

Introduction

We consider the following balance law in one-dimensional space R:. t > 0, x ∈ R, where the flux A󸀠󸀠(V) := a󸀠(V) ≥ c for some constant c > 0 and U0 ∈ L∞(R). We consider the following balance law in one-dimensional space R:. We are interested in getting the optimal rate of convergence linked to a layer. Let us consider the shock solutions of the scalar conservation laws with the given source term (1) with the initial data. With two constants CL > CR, where the source term g is defined as follows:. For any convex functions η, and G󸀠 = η󸀠A󸀠. An easy dimensional analysis shows that, because of those layers, we may have in general. For some ε > 0 which means that the L2 stability for two solutions U, S does not hold. We are interested in deriving the extremal L2 stability up to a shift function.

Let CL such that
Relative Entropy and Some Properties
Estimates on the Hyperbolic and Parabolic Terms
Proof of Theorem 1
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