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Entropy Weak Solutions Analysis

Updated 31 January 2026
  • Entropy weak solutions are defined as distributional solutions to PDEs that additionally satisfy convex entropy inequalities, ensuring physical admissibility.
  • They are often constructed via vanishing-viscosity limits and analyzed using techniques like Glimm’s scheme to yield unique and stable solutions.
  • The entropy framework extends to nonlocal, stochastic, and multiphysics models, underpinning rigorous numerical methods and error analysis.

An entropy weak solution is a function (or vector of functions) that solves a system of partial differential equations in an integral or distributional sense and additionally satisfies a set of entropy inequalities associated with convex entropy–entropy flux pairs. This concept arises in the analysis of nonlinear conservation laws, where classical solutions may not exist due to the formation of discontinuities such as shocks, or in the presence of degeneracy, stochasticity, nonlocal interactions, or multiscale phenomena. The entropy solution framework enforces admissibility criteria—quantitative, variational, or statistical—on otherwise weak (distributional) solutions, thereby ensuring physical consistency, stability, and uniqueness under broad regularity regimes. It permeates hyperbolic systems, degenerate parabolic equations, nonlocal fractional models, stochastic conservation laws, and multi-component coupled PDEs.

1. Foundational Definition and Role in Conservation Laws

Let u:R×[0,)Rnu:\mathbb{R}\times [0,\infty)\to\mathbb{R}^n be a solution to a system of conservation laws, e.g.,

ut(x,t)+f(u(x,t))x=0,xR,t>0,u(x,0)=u0(x)u_t(x,t) + f(u(x,t))_x = 0, \quad x\in\mathbb{R},\, t>0,\qquad u(x,0) = u_0(x)

with f:RnRnf:\mathbb{R}^n\to\mathbb{R}^n smooth and strictly hyperbolic. A function uu is a weak solution if, for every test function ϕCc([0,)×R)\phi\in C_c^\infty([0,\infty)\times \mathbb{R}),

0R[uϕt+f(u)ϕx]dxdt+Ru0(x)ϕ(0,x)dx=0.\int_0^\infty\int_{\mathbb{R}} [u\,\phi_t + f(u)\,\phi_x]\,dx\,dt + \int_{\mathbb{R}} u_0(x)\,\phi(0,x)\,dx = 0.

However, weak solutions may fail to be unique; entropy conditions are required to select the physically correct solution. Given a (convex) entropy functional η:RnR\eta:\mathbb{R}^n\to\mathbb{R} with associated entropy flux q:RnRq:\mathbb{R}^n\to\mathbb{R} defined via q(u)=η(u)f(u)q'(u) = \eta'(u) f'(u), an entropy weak solution uu satisfies

0R[η(u)ϕt+q(u)ϕx]dxdt+Rη(u0(x))ϕ(0,x)dx0,ϕ0\int_0^\infty\int_{\mathbb{R}} [\eta(u)\,\phi_t + q(u)\,\phi_x]\,dx\,dt + \int_{\mathbb{R}} \eta(u_0(x))\,\phi(0,x)\,dx \ge 0, \quad \forall \phi\ge0

or, distributionally, tη(u)+xq(u)0\partial_t\eta(u)+\partial_x q(u)\leq 0 (Zhou, 2022). Entropy inequalities are imposed for all convex entropy pairs.

2. Existence, Uniqueness, and Persistence of Regularity

Entropy weak solutions are often constructed as vanishing-viscosity limits: utε+f(uε)x=εuxxε,uε(0)=u0,u_t^\varepsilon + f(u^\varepsilon)_x = \varepsilon u^\varepsilon_{xx}, \quad u^\varepsilon(0)=u_0, with a uniform bound in LL^\infty and total variation. Kružkov's theorem yields existence and L1L^1-contraction, ensuring uniqueness in L([0,)×R)L^\infty([0,\infty)\times\mathbb{R}) (Zhou, 2022). For strictly hyperbolic systems, Glimm’s scheme or front tracking methods extend existence and uniqueness, typically for initial data in BV.

The regularity of entropy weak solutions typically deteriorates as solutions develop shocks; for instance, solutions cannot remain in H1H^1 due to the Sobolev embedding theorem. However, by changing variables along generalized characteristics—e.g., using a strictly increasing homeomorphism a(t,x)a(t,x) solving ta+λ(u)xa=0\partial_t a+\lambda(u)\partial_x a=0, a(0,x)=xa(0,x)=x—one can represent u(t,x)=U(t,a(t,x))u(t,x) = U(t,a(t,x)). The pullback aU(t,a)a\mapsto U(t,a) retains the Sobolev regularity inherited from the initial condition, a phenomenon termed "generalized persistence" (Zhou, 2022).

3. Entropy Weak Solutions in Nonstandard PDEs: Nonlocal, Stochastic, and Complex Systems

Entropy weak solution methodology extends to broader classes of PDEs, including:

  • Nonlocal fractional conservation laws:

ut+f(u)=(Δ)λ/2A(u)u_t + \nabla\cdot f(u) = -(-\Delta)^{\lambda/2}A(u)

Entropy solutions involve intricate integral inequalities encoding both the nonlocal diffusion and Kružkov entropies. Well-posedness (existence, L1L^1-contraction, uniqueness) is proven under minimal regularity (Cifani et al., 2010).

  • Stochastic conservation laws:

For equations driven by stochastic forcing du+xF(u)dt=σ(x,u)dW(t)du + \nabla_x\cdot F(u)\,dt = \sigma(x,u)\,dW(t), entropy solutions enforce inequalities "weak in time and space," and may require strong entropy conditions to control noise–noise interactions, ensuring uniqueness via L1L^1-contractions and existence via vanishing-viscosity and stochastic compensated compactness (Biswas et al., 2013).

  • Multi-component systems/coupled models:

Entropy-based solution concepts are adapted for e.g., compressible chemically-reactive flows, capillarity models, or thermally-driven phase transitions, relying on entropy production inequalities tailored to the structural mechanics or thermodynamics of the system (Piasecki et al., 2016, Hömberg et al., 2020).

4. Variational Entropy Solutions and Extensions

For systems where classical weak solutions may not exist (e.g., density close to vacuum, low regularity in temperature or free energy), the notion of variational entropy solution is introduced. Here, the total energy balance is replaced by a global entropy inequality: Ω1ϑS(ϑ,u):u+k(ϑ)ϑ2ϑ2+0,\int_\Omega \frac{1}{\vartheta}\, \mathbb{S}(\vartheta,\nabla\mathbf{u}):\nabla\mathbf{u} + \frac{k(\vartheta)}{\vartheta^2}|\nabla\vartheta|^2 + \cdots \leq 0, admitting existence of solutions for broader parameter regimes (γ>1\gamma>1) through enhanced compactness from entropy dissipation (Piasecki et al., 2016). This variational framework allows phase transition laws, sharp free energies, and physically realistic dissipation to be included without requiring strong regularity.

5. Theoretical and Computational Implications: Uniqueness, Nonuniqueness, and Numerical Approximation

Entropy weak solutions generally guarantee L1L^1-contraction and uniqueness for scalar laws and certain well-posed systems, but may fail to be unique for multi-dimensional systems due to convex integration constructions (Baba et al., 2018). Nonuniqueness of admissible entropy solutions is demonstrated for 2D Euler systems with Riemann initial data via fan subsolution and oscillatory constructions.

On the numerical side, entropy-preserving schemes (e.g., monotone conservative finite-difference methods for nonlocal laws (Cifani et al., 2010), entropy-stable finite-volume schemes for compressible Navier–Stokes (Svärd, 2022), and neural architectures such as wPINNs (Ryck et al., 2022)) are analyzed for convergence in the entropy sense, with rigorous error bounds and empirical validation that approximate entropy weak solutions faithfully, even at discontinuities.

6. Key Classes and Representative Models

PDE Class Entropy Solution Features Reference
Scalar conservation laws Kružkov entropies, L1L^1-contraction, persistence of BV/Sobolev regularity in Lagrangian variables (Zhou, 2022)
Nonlocal fractional equations Integral entropy inequalities, L1L^1-contraction, monotone schemes (Cifani et al., 2010)
Generalized Camassa–Holm equations Nonlocal operators, BV/H1 regularity, viscous approximations (Guan et al., 2017)
Stochastic conservation laws Weak-in-time/space entropy, strong entropy conditions, stochastic compactness (Biswas et al., 2013)
Multiphysics: induction hardening Coupled PDE-ODE-Maxwell, entropy production, weak–strong uniqueness (Hömberg et al., 2020)
Compressible Navier–Stokes systems Entropy dissipation, variational formulation, finite-volume convergence (Svärd, 2022, Piasecki et al., 2016)

7. Contemporary Directions and Open Problems

Entropy weak solutions remain central in the rigorous study of multi-scale and multi-physics PDEs. The analysis of regularity persistence under nonlinear degeneracy, development of sharp variational principles for nonclassical dissipation, full characterization of nonuniqueness regimes (convex integration), and interplay with machine learning–based approximation techniques are active research questions. The entropy solution concept links physical admissibility, mathematical stability, and computational tractability, but new evidence indicates that uniqueness may fail for systems with intricate coupling, demanding refined admissibility criteria and analysis (Baba et al., 2018).

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