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Physics theoremStatement: AI-adaptedProof: AI-generatedPipeline-generatedprecheck pendingverified 2026-10-23 (gpt-6.1-sol)
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Mass density reconstruction and incompressibility

Physical scope

Conditional on the adopted smooth single-component mass balance, a C2 orientation-preserving material motion with positive Jacobian, and a C1 positive density. Vacuum, shocks, weak solutions, non-injective motions, and empirical validity are excluded.

Statement

Let I⊆R be an open time interval containing 0, let B⊆R3 be a bounded C1 reference domain, and let χ∈C2(I×U,R3) be an orientation-preserving family of diffeomorphisms on an open neighborhood U⊇B‾, with χ(0,a)=a and J(t,a)=det⁡Daχ(t,a)>0. Set u(t,χ(t,a))=∂tχ(t,a). Let the current density ρ∈C1 be positive on the swept material region, and define ρ0(a)=ρ(0,a). Assume the adopted single-component mass balance with no sources or diffusion relative to u, on every bounded C1 material subregion. Then this integral material-mass balance is equivalent, under these smoothness hypotheses, to ∂tρ+div⁡(ρu)=0. It also forces ρ(t,χ(t,a))J(t,a)=ρ0(a). Consequently, for positive density, Dtρ=0 throughout the material region if and only if div⁡u=0 there. This is a conditional deduction within the adopted smooth model; it asserts no result for vacuum, shocks, weak solutions, or empirical applicability.

Facts & Assumptions

Given: The stated C2 orientation-preserving motion, its positive Jacobian, a C1 positive current density, the reference normalization χ(0,a)=a, and the adopted no-mass-source material balance.

[A1]

Single-component nonpolar continuum and material balances: for each bounded C1 material subregion, its total mass is constant; the adopted branch has no mass sources or diffusion relative to u.

[F1]

Smooth transport, Jacobian and advected reference density: for a C2 orientation-preserving motion and a C1 scalar field ρ on the swept open set, every compact Jordan material set K has MK(t)=∫χt(K)ρ(t,x) dx with MK′(t)=∫χt(K)(∂tρ+div⁡(ρu)) dx. The same statement supplies the change-of-variables formula for χt(K), the identity ddt[ρ(t,χ(t,a))J(t,a)]=J(Dtρ+ρdiv⁡u)(t,χ(t,a)), and the equivalence between continuity, constancy of all compact-Jordan material integrals, and invariance of the density-Jacobian product. This remains a draft mathematical supplier, and the proof uses its stated interface as a mathematical premise.

[F2]

Classical frames, primitive quantities and SI units: u is the Eulerian velocity, Dt=∂t+u⋅∇ is the material derivative, θ=div⁡u, and div⁡(ρu) is the spatial divergence of the mass flux.

[F3]

C1 material regions have compatible Jordan volume integrals: for a bounded open region with the stated local C1 graph boundary, its compact closure and its image under a C1 diffeomorphism are Jordan measurable; the boundaries have content zero, and integration over the open current region equals integration over its compact closure.

[F4]

Continuous residuals localize on C1 domains: for a continuous scalar residual, zero integrals on every bounded C1 subdomain force pointwise zero, and nonnegative integrals on all such subdomains force pointwise nonnegativity.

Proof

Given: [A1], [F1], the stated smooth motion and density, and J>0.

1.1A1F3

For each bounded C1 subdomain V⋐B, put K=V‾. The adopted mass balance [A1] makes ∫χt(V)ρ constant in time. The Jordan-interface lemma [F3] identifies this with MK(t)=∫χt(K)ρ, so MK′(t)=0.

1.2F1F3given

Conversely, suppose R:=∂tρ+div⁡(ρu)=0. Then [F1] makes MK constant for every compact Jordan K. For K=V‾ and each bounded C1 subdomain V⋐B, [F3] identifies the open-region mass integral with MK; its value at t=0 is ∫Vρ0. Thus the adopted integral balance follows, proving the reverse implication.

2.1F1F3step 1.1

Apply [F1] to q=ρ and K from step 1.1. Since MK′=0, its material-transport formula and change of variables give ∫VR(t,χ(t,a))J(t,a) da=0,R:=∂tρ+div⁡(ρu). Here [F3] replaces the integral over the compact closure by the equal integral over the open region V. This holds for every bounded C1 subdomain V⋐B.

3.1F4step 2.1algebra

For fixed t, the function a↦R(t,χ(t,a))J(t,a) is continuous on B. Step 2.1 and [F4] therefore imply that it vanishes throughout B. Since J>0, the local continuity equation R=0 holds on the swept material region.

4.1F1F2step 3.1algebra∎

Along each material label, [F1] gives ddt(ρ(t,χ(t,a))J(t,a))=J(Dtρ+ρdiv⁡u). By [F2] and step 3.1 this derivative vanishes. The initial conditions χ(0,a)=a, J(0,a)=1, and ρ(0,a)=ρ0(a) give ρ(t,χ(t,a))J(t,a)=ρ0(a). Since ρ>0, Dtρ+ρdiv⁡u=0 is equivalent to Dtρ=0 exactly when div⁡u=0.

Authoring status

The mathematical motion and transport carriers are present and their complete statements/proofs were checked against this use. The transport lemma remains a draft mathematical supplier, and the proof's reliance on its stated interface is explicit. The open-to-compact Jordan conversion and continuous localization are supplied by C1 material regions have compatible Jordan volume integrals and Continuous residuals localize on C1 domains.

Depends on

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