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Bounded-domain Stokes residual estimate

Statement

Assume ACω. Let n≥2 and let Ω⊂Rn be a bounded C1 domain, meaning a bounded connected open set whose boundary is locally a C1 graph and which lies on one side of that graph after a rigid change of coordinates. Let μ>0, w∈C2(Ω‾;Rn), q∈C1(Ω‾), and f∈C(Ω‾;Rn); Ck(Ω‾) means that derivatives through order k extend continuously to the closure. For ordinary Euclidean coordinates x1,…,xn, set ∂j=∂/∂xj, define ∇r=(∂1r,…,∂nr) for scalar r, define ∇⋅v=∑i=1n∂ivi and (∇v)ij=∂jvi for vector v, define (v⋅∇)v=∑j=1nvj∂jv, and define the vector Laplacian by (Δv)i=∑j=1n∂j2vi. For a=(ai)i=1n∈Rn set ∣a∣=(∑i=1nai2)1/2, so ∣∇v∣2=∑i,j=1n∣∂jvi∣2. For vector fields g,v, write ∥g∥2=(∫Ω∣g∣2 dx)1/2 and ∥∇v∥2=(∫Ω∑i,j=1n∣∂jvi∣2 dx)1/2. Suppose pointwise that ∇⋅w=0, w∣∂Ω=0, and −μΔw+∇q=f. Also assume that a stated constant CΩ>0 satisfies the zero-trace Poincare inequality ∥v∥2≤CΩ∥∇v∥2 for every v∈C1(Ω‾;Rn) with v∣∂Ω=0. Then

∥∇w∥2≤CΩμ∥f∥2,∥w∥2≤CΩ2μ∥f∥2.

For Lx,Lz,h>0, set TL=R/(LZ) for L>0 and Q=TLx×(0,h)×TLz, the periodic channel cell. A field on Q‾ is identified with its lift to R×[0,h]×R periodic with periods Lx,Lz in the first and third coordinates. Integrals on Q use Lebesgue measure on one fundamental cell in each periodic coordinate; ∥v∥L2(Q)2=∫Q∣v∣2 and ∥∇v∥L2(Q)2=∫Q∑i,j=13∣∂jvi∣2. Every v∈C1(Q‾;R3) periodic in the two torus variables and zero on y=0,h satisfies ∥v∥L2(Q)≤h∥∇v∥L2(Q). This channel inequality is a separate direct estimate on the periodic cell; it does not treat that cell as a bounded C1 Euclidean domain.

In dimension three, let ρ0>0, ν=μ/ρ0, and suppose already-existing time-independent fields uNS,uS∈C2(Ω‾;R3) and pNS,pS∈C1(Ω‾) are divergence-free, have the same boundary velocity, and satisfy the constant-density incompressible Navier-Stokes and Stokes equations ρ0(uNS⋅∇)uNS+∇pNS−μΔuNS=0 and ∇pS−μΔuS=0. If f=−ρ0(uNS⋅∇)uNS, then the preceding estimate applies to w=uNS−uS and q=pNS−pS whenever the stated Poincare bound holds. This is an a-posteriori residual estimate for already-given fields; it asserts no solution existence, no exterior-domain bound, and no error bound from Reynolds number alone. The constant CΩ=h established for the periodic channel is not transferred to an exterior domain.

Facts & Assumptions

Given: The fields, domain, residual equation, zero trace, and Poincare bound in [A1]. For the comparison clause, use the exact formal Navier-Stokes/Stokes conventions in [F1].

[A1]

Assume ACω. Let n≥2, let Ω⊂Rn be a bounded connected C1 domain, μ>0, w∈C2(Ω‾;Rn), q∈C1(Ω‾), f∈C(Ω‾;Rn), ∇⋅w=0, w∣∂Ω=0, −μΔw+∇q=f, and ∥v∥2≤CΩ∥∇v∥2 for every C1 zero-trace vector field.

[F1]

Formal parameterized fluid systems and observables on fd−x01 defines, for constants ρ0>0 and μ>0 with ν=μ/ρ0, the pointwise constant-density incompressible equation ut+(u⋅∇)u+ρ0−1∇p−νΔu=0, ∇⋅u=0. Its steady Stokes system is ρ0−1∇p−νΔu=0, ∇⋅u=0, and omits both the time derivative and convection.

[F3]

Divergence on a bounded C1 Euclidean domain: assuming ACω, for n≥2, bounded C1 Euclidean Ω, and G∈C1(Ω‾;Rn), ∫Ω∇⋅G dx=∫∂ΩG⋅ν dS, with outward normal on every boundary component.

[F4]

The Axiom of Countable Choice (ACω): ACω states that every sequence (Xj)j∈N of nonempty sets has a function c with c(j)∈Xj for every j. This exact countable-choice assumption is used only to invoke [F3]; the proof assumes no full Axiom of Choice.

Proof

1.1givenA1F3F4constructalgebra

For each component i, set Gi=wi∇wi∈C1(Ω‾;Rn). The product rule gives ∇⋅Gi=∣∇wi∣2+wiΔwi. Since wi=0 on the boundary, Gi⋅ν=wi∂νwi=0 there. Apply [F3] to each Gi and sum over i to obtain −∫Ωw⋅Δw dx=∫Ω∣∇w∣2 dx.

1.2givenA1F3F4constructalgebra

The field G=qw is C1 on Ω‾. Its divergence is ∇q⋅w+q∇⋅w, and its boundary flux is qw⋅ν=0. Applying [F3] and using ∇⋅w=0 yields ∫Ω∇q⋅w dx=0.

1.3givenA1F2algebra

Put A=∫Ω∣f∣2 dx, B=∫Ω∣w∣2 dx, and C=∫Ω∣f∣ ∣w∣ dx. By [F2], ∣∫Ωf⋅w dx∣≤C. For every t∈R, 0≤∫Ω(∣f∣−t∣w∣)2 dx=A−2tC+t2B; if B>0, choosing t=C/B gives C2≤AB, while if B=0, continuity forces w=0 throughout Ω and hence C=0. Thus ∣∫Ωf⋅w dx∣≤∥f∥2∥w∥2.

1.4givenF2algebra

On the periodic channel, fix (x,z,y) and set g(s)=∂yv(x,s,z), so v(x,y,z)=∫0yg(s) ds because v vanishes at y=0. By bilinearity and repeated integration, ∣v(x,y,z)∣2=∫0y∫0yg(s)⋅g(t) ds dt. By [F2] and 2ab≤a2+b2, this is at most y∫0y∣g(s)∣2 ds≤h∫0h∣g(s)∣2 ds. Integrating over 0<y<h and the two periodic coordinates gives ∥v∥L2(Q)2≤h2∥∂yv∥L2(Q)2≤h2∥∇v∥L2(Q)2; periodic faces are identified and no C1 Euclidean-domain theorem is invoked on this cell.

1.5givenA1F1algebra

For already-existing stationary fields in the comparison clause, [F1] gives −μΔuNS+∇pNS=−ρ0(uNS⋅∇)uNS and −μΔuS+∇pS=0. Subtraction shows w=uNS−uS has zero trace and satisfies the residual equation with q=pNS−pS and the stated f; it does not assert either field exists.

2.1givenA1step 1.1step 1.2algebra

Take the Euclidean inner product of −μΔw+∇q=f with w, integrate over Ω, and substitute steps 1.1 and 1.2. The result is μ∥∇w∥22=∫Ωf⋅w dx.

3.1givenA1step 2.1step 1.3algebra

Let r=∥∇w∥2. Steps 2.1 and 1.3 and the assumed Poincare inequality give μr2≤CΩ∥f∥2r. If r=0 the gradient bound is immediate; if r>0, division by μr gives r≤CΩ∥f∥2/μ.

4.1givenA1step 3.1algebra

Apply the Poincare inequality once more to w and then use step 3.1 to obtain ∥w∥2≤CΩr≤CΩ2∥f∥2/μ. This proves both residual estimates.

5.1givenA1step 1.5step 3.1step 4.1∎

The residual fields in step 1.5 satisfy the hypotheses of the first estimate, so steps 3.1 and 4.1 give the stated a-posteriori bounds whenever the explicit Poincare inequality holds.

Depends on

Dependency tree · 2 levels

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