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ExampleConstruction: AI-generatedVerification: AI-generatedPipeline-generatedprecheck pendingverified 2026-10-23 (gpt-6.1-sol)
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Volume dilation and bulk production

Physical scope

Conditional worked calculation for a smooth positive-density material motion and a specified local-equilibrium compressible Newtonian/Fourier model branch. It derives a model entropy-production identity from adopted balances and constitutive assumptions; it is not a measurement or a claim of universal material response.

Example

Assume the Axiom of Countable Choice. Let I be an open time interval containing 0, with time measured in seconds; let B⊆R3 be a bounded C1 reference body, and let U⊆R3 be an open neighborhood of B‾. Let α∈C2(I,(0,∞)) be dimensionless with α(0)=1, so α′ is measured in s−1, and define χ:I×U→R3 by χ(t,a)=α(t)a. This is a C2 orientation-preserving motion with χ(0,a)=a and positive reference density ρ0∈C1(B‾) in kg m−3. Assume the adopted smooth material mass, linear-momentum, total-energy, and entropy balances on every bounded C1 material subregion. On the example's local-equilibrium branch, e=e(v,s)∈C2 on an open state domain, with specific volume v=1/ρ in m3 kg−1, T=es>0 in K, p=−ev in Pa, and de=T ds−p dv. Adopt the specified symmetric Newtonian stress and Fourier heat-flux closure

σ=−pI3+τ,τ=2μD0+ζθI3,q=−κT∇T,

with constant coefficients μ,ζ,κT≥0 in Pa s, Pa s, and W m−1 K−1, respectively. Assume ρ,u,e,T,s,q,σ∈C1 and b,r∈C0 on the relevant swept regions, with ρ,T positive. Then F=αI3, J=α3, u(t,x)=(α′(t)/α(t))x, and θ=3α′/α, so D0=0 while the mass theorem gives ρ(t,χ(t,a))=ρ0(a)/α(t)3. The local entropy-production residual g=ρDts+div⁡(q/T)−ρr/T is

g=ζθ2T+κT∣∇T∣2T2≥0.

In the spatially uniform-temperature case, the heat-conduction term vanishes and the bulk-viscous production is ζθ2/T. The residual has units W m−3 K−1. This is a conditional deduction for the stated closure and balances, not a claim that actual fluids universally obey them.

Facts & Assumptions

Given: Countable Choice, the stated C2 positive dilation, C1 positive density and temperature, material integral balances, local-equilibrium Gibbs identity, and the stated Newtonian/Fourier closure.

[F1]

Mass density reconstruction and incompressibility: under the adopted mass balance, ∂tρ+div⁡(ρu)=0, ρ(t,χ(t,a))J(t,a)=ρ0(a), and, for positive density, Dtρ=0 if and only if div⁡u=0. This physical theorem is conditional on the stated mass-balance and smoothness hypotheses.

[F2]

Single-component nonpolar continuum and material balances: adopt material mass, linear-momentum, total-energy, and local-temperature entropy balances on the stated bounded C1 material regions; this postulate is an assumption, not an experimental finding.

[F3]

Smooth transport, Jacobian and advected reference density: for a C2 orientation-preserving motion and a C1 scalar field on the swept set, the derivative of its compact-Jordan material integral is the integral of ∂tq+div⁡(qu); the statement also gives change of variables and density-Jacobian invariance. This remains a draft mathematical supplier used as a mathematical premise.

[F4]

Divergence on a bounded C1 Euclidean domain: if Ω⊆R3 is bounded C1 and F∈C1(Ω‾;R3), then ∫Ωdiv⁡F dx=∫∂ΩF⋅n dS, assuming ACω.

[F5]

The Axiom of Countable Choice (ACω): ACω says every countable family of nonempty sets has a choice function; this is the exact choice strength assumed by [F4], not full arbitrary-index choice as a premise of this calculation.

[F6]

Classical frames, primitive quantities and SI units: Dt=∂t+u⋅∇, Lij=∂jui, D=(L+LT)/2, θ=tr⁡D=div⁡u, D0=D−(θ/3)I3, and S:T=∑i,jSijTij; the adopted stress uses traction σn and tension-positive sign.

[F7]

C1 material regions have compatible Jordan volume integrals: bounded open regions with locally C1 graph boundaries and their diffeomorphic images are bounded C1 domains; their compact closures and images are Jordan measurable, and open-region and compact-closure integrals agree.

[F8]

Continuous residuals localize on C1 domains: a continuous residual with zero integral on every bounded C1 subdomain is pointwise zero; nonnegative integrals imply a pointwise nonnegative residual.

[F9]

Change of variables for an injective C1 map on a compact Jordan set: an injective C1 map with invertible derivative transforms integrals over compact Jordan sets by the absolute Jacobian determinant.

[F10]

A continuous real function on a compact Jordan measurable set is Riemann integrable over that set: every continuous real function on a compact Jordan set is Riemann integrable there.

[A1]

Local equilibrium is adopted only for this example: e(v,s)∈C2, T=es>0, p=−ev, and de=T ds−p dv.

[A2]

The symmetric constitutive branch is adopted only for this example: σ=−pI3+2μD0+ζθI3 and q=−κT∇T, with constant μ,ζ,κT≥0. This is a model input; no empirical universality or positivity theorem is asserted.

Verification

Given: Countable Choice, [F1]–[F10], [A1]–[A2], the smoothness hypotheses in the example, and the material motion χ(t,a)=α(t)a.

1.1F6givenalgebra

For each t, χt(a)=α(t)a maps U bijectively onto the open set α(t)U with inverse x↦x/α(t); jointly this inverse is C2 because α>0. Differentiating χ in a and t gives F=αI3, J=α3>0, and u(t,x)=(α′/α)x. Using the velocity-gradient and strain-rate definitions [F6], L=(α′/α)I3, D=(α′/α)I3, θ=3α′/α, and D0=0.

1.2F1F2F3F4F5F6F7F8F9F10algebra

Fix a bounded C1 material subregion V⋐B and put K=V‾, Ωt=χt(V). Apply [F3] componentwise to the linear-momentum integral in [F2]; [F7] identifies the open-region integrals with their compact-closure versions. The divergence theorem [F4], under the stated choice premise [F5], converts ∫∂Ωtσn to ∫Ωtdiv⁡σ. The continuous residual is integrable on the compact Jordan region by [F10]: Rm=∂t(ρu)+div⁡(ρu⊗u)−ρb−div⁡σ has integral zero on χt(K). Change variables by [F9], use [F7] to return to V, and apply [F8] to the continuous reference residual Rm(t,χ(t,a))J(t,a). Since J>0, Rm=0 pointwise. Expanding with the conventions [F6] and the continuity equation [F1] yields ρDtu=ρb+div⁡σ.

1.3F2F3F4F5F7F8F9F10algebra

Set E=e+∣u∣2/2. Apply [F3] to ρE in the total-energy balance [F2]. The surface-work integrand is (σn)⋅u=(σTu)⋅n; apply [F4] with [F5] to σTu and q. The continuous total-energy residual is integrable by [F10] and has zero integral on every Ωt=χt(V). By [F7], [F9], and the zero-integral conclusion of [F8], it vanishes pointwise: ∂t(ρE)+div⁡(ρEu)=ρb⋅u+div⁡(σTu)−div⁡q+ρr.

1.4F1F2F3F4F5F6F7F8F9F10given

Apply [F3] to ρs in the entropy inequality [F2]. By the continuity equation [F1], ∂t(ρs)+div⁡(ρsu)=ρDts+s(∂tρ+div⁡(ρu))=ρDts. The surface term has the local-temperature flux q/T; [F4] with [F5] converts it to the volume divergence. Convert each open-region integral to the compact-Jordan and then reference-domain form using [F7] and [F9]. The residual is continuous and integrable by [F10]; its nonnegative integral on every bounded C1 V⋐B and [F8] make it pointwise nonnegative. Since J>0, this gives g=ρDts+div⁡(q/T)−ρr/T≥0.

2.1givenF1step 1.1

Apply [F1] to this motion. Since J=α3, the density reconstruction is ρ(t,χ(t,a))=ρ0(a)/α3; the density remains positive because ρ0>0 and α>0.

2.2A2F1F6step 1.2step 1.3algebra

Dot the local momentum equation in step 1.2 with u. The identity u⋅div⁡σ=div⁡(σTu)−σ:∇u, the symmetry of the adopted stress [A2], and the continuity equation from [F1] give the kinetic-energy balance ∂t(ρ∣u∣2/2)+div⁡(ρ∣u∣2u/2−σTu)=ρb⋅u−σ:D, where D is the symmetric velocity gradient from [F6]. Subtract this balance from step 1.3; the ρb⋅u and div⁡(σTu) terms cancel, leaving ρDte=σ:D−div⁡q+ρr.

3.1A1A2F1F6step 2.2algebra

From [A1], Dte=TDts−pDt(1/ρ). The continuity equation in [F1] gives Dt(1/ρ)=θ/ρ, using θ=div⁡u from [F6], so ρTDts=ρDte+pθ. Substitute step 2.2 and σ=−pI3+τ from [A2]; since I3:D=θ, the pressure terms cancel and ρTDts=τ:D−div⁡q+ρr.

4.1A2F6step 1.1step 1.4step 3.1algebra∎

Substitute this identity into step 1.4 and use div⁡(q/T)=div⁡q/T−q⋅∇T/T2. The definitions [F6] give D0:I3=0, D0:D=∣D0∣2, and τ:D=2μ∣D0∣2+ζθ2; also q=−κT∇T. Therefore g=2μ∣D0∣2/T+ζθ2/T+κT∣∇T∣2/T2. Step 1.1 has D0=0, giving the stated bulk-production formula and its uniform-temperature special case.

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