86 research outputs found

    High regularity of solutions of compressible Navier-Stokes equations

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    We study the Navier-Stokes equations for compressible {\it barotropic} fluids in a bounded or unbounded domain Ω\Omega of R3 \mathbf{R}^3. The initial density may vanish in an open subset of Ω\Omega or to be positive but vanish at space infinity. We first prove the local existence of solutions (ρ(j),u(j))(\rho^{(j)}, u^{(j)}) in C([0,T];H2(kj)+3×D01D2(kj)+3(Ω))C([0,T_* ]; H^{2(k-j)+3} \times D_0^1 \cap D^{2(k-j)+3} (\Omega ) ), 0jk,k10 \le j \le k, k \ge 1 under the assumptions that the data satisfy compatibility conditions and that the initial density is sufficiently small. To control the nonnegativity or decay at infinity of density, we need to establish a boundary value problem of (k+1)(k+1)-coupled elliptic system which may not be in general solvable. The smallness condition of initial density is necessary for the solvability, which is not necessary in case that the initial density has positive lower bound. Secondly, we prove the global existence of smooth radial solutions of {\it isentropic} compressible Navier-Stokes equations on a bounded annulus or a domain which is the exterior of a ball under a smallness condition of initial density

    On the semirelativistic equations

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    A Sobolev estimate for the adjoint restriction operator

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    In this note we consider the adjoint restriction estimate for hypersurface under additional regularity assumption. We obtain the optimal HsH^s-LqL^q estimate and its mixed norm generalization. As applications we prove some weighted Strichartz estimates for the propagator eit(Δ)α/2φe^{it(-\Delta)^{\alpha/2}}\varphi, α>0\alpha>0.Comment: 14 pages, 0 figure; correct some typos; to appear Math. An

    On small amplitude solutions to the generalized Boussinesq equations

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    We study the existence and scattering of global small amplitude solutions to generalized Boussinesq (Bq) and improved modified Boussinesq (imBq) equations with nonlinear term f(u)f(u) behaving as a power upu^p as u0u \to 0 in Rn,n1\mathbb{R}^n, n \ge 1
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