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Este documento aborda a teoria e os resultados fundamentais sobre as equações de navier-stokes incompressíveis em r3, incluindo as contribuições de jean leray, o problema da existência de soluções fracas, dificuldades em matemática, teoremas clássicos e critérios de regularidade. Além disso, é apresentado um estudo sobre soluções axialmente simétricas e equações modelo.
Tipologia: Notas de estudo
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School of Mathematical SciencesFudan University
(^3) Incompressible Navier-Stokes Equations in R– p. 1/
√^ Fundamental Work by Jean Leray √^ Key Question and Its Main Difficulties √^ Existence Theory under Small Data (Large Viscosity) √^ Criterions, Caffarell-Kohn-Nirenberg √^ No Self-similar Blowup √^ Axially Symmetric Navier-Stokes^ ⋆^ Without Swirl, Partial Results with Swirl^ ⋆^ Gap between Known and Needed √^ Role of Convection: A 3D Model^ ⋆^ Theoretical Similarities Between Model and NS^ ⋆^ Singularities of Model Equations
Incompressible Navier-Stokes Equations in
(^3) R– p. 2/
Navier The Navier-Stokesequations were first derived byClaude-Louis Navier on 1822,based on a molecular theory ofattraction and repulsion betweenneighbouring molecules.
(^3) Incompressible Navier-Stokes Equations in R– p. 4/
Stokes George Gabriel Stokesre-derived the Navier-Stokesequations on 1845
(^3) Incompressible Navier-Stokes Equations in R– p. 5/
Leray Leray’s Contributions:^ √^ For smooth, divergence-freeinitial data^ u(0, x
(^23) ) ∈ L(R), there is a unique local solution √^ There is at least a global weaksolution, which coincideswith the local smooth onebefore singularity time. Theweak solutions satisfy thenatural energy inequality^ ∫^2 ‖u(t,^ ·)‖+2ν^2 L
t^2 ‖∇u(s,^ ·)‖ds^ ≤ ‖^2 L 0
(^2) u(0, ·)‖.^2 L^3 Incompressible Navier-Stokes Equations in^ R
T<^ ∞, then⋆^ ‖u(t,^ ·)‖p^3 ≥^ L(R)^
(^13) − (1−^ ) 2 p^ ǫ(T− t)p⋆ as^ t^ →^ T.⋆ √ For a given weak solution, there exists a closedset^ S ⊂^ (0,^ ∞)^ of measure zero such that thesolution is smooth on
c.^3 Incompressible Navier-Stokes Equations in^ R– p. 8/
)^ solves the Navier-Stokes equations, then so does the solution pair
λλ (u, p)^ for any^ λ >^0 which is defined byλ^ u(t, x) =^ λu(λ
2 λt, λx),^ p(t, x) =
(^22) λp(λt, λx). λ Remark: ‖u(t, x 2 −^1 )‖=^ λ‖u(t, x^2 L
(^2) )‖.^2 L^ Incompressible Navier-Stokes Equations in (^3) R– p. 10/
a priori estimate become worse.Unfortunately, the 3D Navier-Stokes equations fallinto this kind of supercritical case. Heuristically,nonlinearities would dominate the dynamics whichmay develop turbulent behavior.This is the essence of difficulty of solvingNavier-Stokes equations for mathematicians.
(^3) Incompressible Navier-Stokes Equations in R– p. 11/
u= 0. For two Leray-Hopf^0 weak solutions^ u,
(q v, if u ∈ L[0, T )^ p (^3) ], L(R)for some^ p, q^ satisfying
23 +^ = 1,^ p >^3 q^ p^ , then^ u^ =^ v^ and u, v^ are smooth on
Local version: Serrin (1962, ARMA), Struwe (1988CPAM)The case^ p^ = 3: Escauriaza, Seregin and Sverak(2003).^
(^3) Incompressible Navier-Stokes Equations in R– p. 13/
∞^3 (s, ·)‖ds <^ L(R)
Then^ u^ is smooth up to
t^ =^ T^. Beale-Kato-Majda’s Criterion has been slightlyimproved by Kozono who proved that on the left-handside in the above inequality, the
∞ L-norm can be replaced by the BMO norm.
(^3) Incompressible Navier-Stokes Equations in R– p. 14/
∫^2 |u| t<t<t^ B(x) 00 r^0 dy < ǫ∗ implies the regularity of
z.^0 Incompressible Navier-Stokes Equations in
(^3) R– p. 16/
x^3 √),^ U^ ∈^ L( T^ −^ t
(^1) and U ∈ H, thenloc u^ = 0. A local version by Tsai (1998, ARMA)
(^3) Incompressible Navier-Stokes Equations in R– p. 17/
θ^2 (u)z r (^) ∂u+ p− = (∆zr r^ 1 r − )u,^2 r θ^ rθ^ z∂u+^ u∂u+^ u∂tr
r^ θuu^1 θ (^) u+ = (∆^ −^ z r^ r θ)u, 2 z^ rz^ z^ ∂u+^ u∂u+^ u∂tr z^ zu+^ p= ∆u.zz^
(^3) R– p. 19/
θ^ ψbe the angular stream function so thatr^ u=^ −
(^1) θz (^) ∂ψ, u= ∂zr^ r θ(rψ). Then^ θ^ rθ^ ∂u+^ u∂u+^ tr
r^ θuuz θ (^) u∂u+ = (∆^ z^ r^ 1 θ− )u,^2 r θ^ rθ^ z^ ∂ω+^ u∂ω+^ u∂tr
θ^2 r θ∂(u)uωz (^) θ (^) ω− = (^) z r r 1 θ+ (∆ − )ω.^2 r^3 Incompressible Navier-Stokes Equations in^ R– p. 20/