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The method of $a$-contraction with shifts used for long-time behavior toward viscous shock

Sungho Han, Moon-Jin Kang, Hobin Lee

Abstract

We revisit the method of $a$-contraction with shifts used for long-time behavior of barotropic Navier-Stokes flows perturbed from a Riemann shock. For the usage of the method of $a$-contraction with shifts, we do not employ the effective velocity $h$ variable even for higher order estimates. This approach would be important when handling the barotropic Navier-Stokes system with other effects, for example, such as capillary effect and boundary effect.

The method of $a$-contraction with shifts used for long-time behavior toward viscous shock

Abstract

We revisit the method of -contraction with shifts used for long-time behavior of barotropic Navier-Stokes flows perturbed from a Riemann shock. For the usage of the method of -contraction with shifts, we do not employ the effective velocity variable even for higher order estimates. This approach would be important when handling the barotropic Navier-Stokes system with other effects, for example, such as capillary effect and boundary effect.

Paper Structure

This paper contains 21 sections, 14 theorems, 142 equations.

Key Result

Theorem 1.1

For a given state $(v_+,u_+)\in\mathbb R^+\times\mathbb R$, there exist positive constants $\delta_0$, and $\varepsilon_0$ such that the following holds: For any $(v_-,u_-)$ on the 2-shock curve $S_2(v_+,u_+)$, satisfying the Rankine-Hugoniot condition RH with $|v_+-v_-|<\delta_0$, consider the 2-vi where $\mathbb{R}_-:=-\mathbb{R}_+=(-\infty,0)$. Then, the Navier-Stokes system eq:NS admits a uniq

Theorems & Definitions (23)

  • Theorem 1.1
  • Remark 1.1
  • Remark 1.2
  • Lemma 2.1
  • proof
  • Lemma 2.2
  • Proposition 3.1
  • proof
  • Proposition 3.2
  • Proposition 3.3
  • ...and 13 more