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The viscous entropy dissipation identity

Statement

Let n≥1, ε>0, f∈C1(R;Rn) and let uε∈C1,2(ΠT) be a classical solution of the viscous conservation law utε+div⁡xf(uε)=εΔuεin ΠT (Scalar conservation laws, fluxes and Cauchy data, The Laplacian of a C2 function and of a C2 vector field). For every convex η∈C2(R) and entropy flux q with q′(s)=η′(s)f′(s), the pointwise viscous entropy balance is η(uε)t+div⁡xq(uε)=εΔxη(uε)−εη′′(uε)∣∇xuε∣2≤εΔxη(uε). The nonpositive term is the entropy dissipation; for fixed ε>0 this is a balance with diffusion, not the first-order entropy inequality (Convex entropy--entropy flux pairs, Divergence and curl of a C1 vector field).

Facts & Assumptions

Given: n≥1, ε>0, f∈C1(R;Rn), a classical solution uε∈C1,2(ΠT) of the viscous conservation law, and a convex η∈C2(R) with entropy flux q, q′=η′f′.

Proof

technique · direct
1.1F1F2

By [F1] the two left-hand terms are η(uε)t=η′(uε)utε and div⁡xq(uε)=η′(uε)f′(uε)⋅∇xuε, and by [F2] the diffusion term is Δxη(uε)=η′(uε)Δuε+η′′(uε)∣∇xuε∣2.

2.1step 1.1F1algebra

Multiplying the viscous equation pointwise by η′(uε) and adding the second identity of step 1.1 gives η(uε)t+div⁡xq(uε)=η′(uε)(utε+div⁡xf(uε)−εΔuε)+εΔxη(uε)−εη′′(uε)∣∇xuε∣2=εΔxη(uε)−εη′′(uε)∣∇xuε∣2, which is the asserted balance.

3.1step 2.1F2∎

The convexity assumption gives η′′≥0, so the dissipation term −εη′′(uε)∣∇xuε∣2 is nonpositive pointwise and the balance implies the stated inequality; the term εΔxη(uε) may change sign and cannot be dropped pointwise for fixed ε>0.

Depends on

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