Long-Time Behavior of a Point Mass in a One-Dimensional Viscous Compressible Fluid and Pointwise Estimates of Solutions

Abstract

A. We consider the motion of a point mass in a one-dimensional viscous compressible barotropic fluid. The fluid-point mass system is governed by the barotropic compressible Navier-Stokes equations and Newton's equation of motion. Our main result concerns the long-time behavior of the fluid and the point mass, and it gives pointwise convergence estimates of the volume ratio and the velocity of the fluid to their equilibrium values. As a corollary, it is shown that the velocity V(t) of the point mass satisfies a decay estimate |V(t)| = O(t −3/2 ) -a faster decay compared to t −1/2 known for the motion of a point mass in the viscous Burgers fluid [J. L. Vázquez and E. Zuazua, Comm. Partial Differential Equations 28 (2003), 1705-1738]. The rate −3/2 is essentially related to the compressibility and the nonlinearity. As a consequence, it follows that the point mass is convected only a finite distance as opposed to the viscous Burgers case. The main tool used in the proof is the pointwise estimates of Green's function. It turns out that the understanding of the time-decay properties of the transmitted and reflected waves at the point mass is essential for the proof.2For initial data with certain symmetry, it could happen that h ′ (t) = 0 for all t ≥ 0; see the footnote in Remark 1.3.