Search arXiv⌕ Search

arXiv · 2610.07236

Well-posed by Design: Learning Constitutive Laws from Velocity Data using Convex Neural Network Potentials

Abstract

Learning constitutive laws of complex fluids from velocity data (i.e. indirect observations) is a PDE-constrained inverse problem in which expressive neural parameterizations risk breaking the well-posedness of the forward physics model. We address this tension by learning, rather than the constitutive law itself, the dissipation potential: a scalar function whose convexity, frame-indifference, and dissipativity propagate into the underlying continuum mechanics and guarantee the structural properties needed for a well-posed and generalizable forward PDE. We introduce ICNNE, an input-convex neural architecture that exactly enforces convexity, frame-indifference, and evenness in the second strain-rate invariant via symmetrization, alleviating the numerical instabilities that occur at small strain rates in standard formulations. By weakly enforcing zero gradients in the origin of the potential via penalization, ICNNE also satisfies the dissipativity property. The loss objective and its gradient are computed using a combination of finite element and neural network methods, coupling the Firedrake and PyTorch libraries. We evaluate on four problems spanning compressible and incompressible regimes: compressible Navier-Stokes, Herschel-Bulkley yield-stress flow, Hibler's viscous-plastic sea-ice model, and discrete-element-method data with no known constitutive law. We show that the learned potentials (i) recover ground-truth physics where it is known, (ii) transfer accurately to geometries unseen during training, and (iii) succeed in regimes where unstructured methods diverge. These results suggest that embedding mathematical structure into the parameterization, rather than into the loss, is a robust path to learning physics from indirect data.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

Gonzalo G. de Diego, Georg Stadler. 2026-10-05. Well-posed by Design: Learning Constitutive Laws from Velocity Data using Convex Neural Network Potentials. https://arxiv.org/abs/2610.07236

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related papers

Tandem jets in crossflow: a one-parameter dilution law for the trajectory and the velocity decay

The front jet of a tandem pair in crossflow is not passive. This paper treats the mean-flow phenomenology and its scaling; the mechanism is left to the companion paper. In 40\ kHz time-resolved PIV measurements covering nine spacing--velocity-ratio conditions ($L=2d$, $3d$, $4d$; $r\approx3$, $5$, $7$) and a single-jet baseline, the front-jet $rd$-normalized trajectory lies below the single-jet reference in every condition (near-field segment up to 40\% shorter), while the shielded rear jet rises above the reference in eight of the nine and penetrates $1.4$--$2.0$ times deeper than the front jet. The mean pressure and reverse-flow statistics are inconsistent with the two classical explanations: the inter-jet region is pressurized rather than sub-atmospheric, the lateral pressure difference across the front jet is weakened rather than enhanced (within reconstruction uncertainty), and the reverse-flow region does not follow the ordering of the modification. In natural coordinates the centerline decay re-scales onto the single-jet law at the effective velocity ratio (seven of nine within 18\%), so bending and decay are two readouts of one dilution, which whole-trajectory matching condenses into the one-parameter law $r_{\mathrm{eff}}/r=r/(r+c)$, $c=3.31$, with the velocity ratio as the primary control and the spacing entering through the near-field capacity ($c_h=2.50$--$3.30$). The law has one fitted constant and needs only the single-jet reference family; leave-one-condition-out predictions reproduce each held-out condition within 15\%, so the procedure is portable to any tandem array in which the gap recirculation closes.

physics.flu-dyn↗

On buoyancy in disperse two-phase flow and its impact on the well-posedness of two-fluid models

The Maxey--Riley--Gatignol equation for the flow around a sphere at low particle Reynolds number tells us that the fluid-particle interaction force decomposes into a contribution from the local flow disturbance caused by the particle's boundary---consisting of the drag, virtual-mass, and history forces, and their Faxén corrections---and another contribution from the stress of the background flow, termed generalized-buoyancy force. There is also a consensus that, for general disperse two-phase flow, the interfacial force density, coupling the average fluid phase and dispersed-phase momentum balances, decomposes in a like manner. However, there has been a long-standing controversy about the physical closure separating the generalized-buoyancy from the interfacial force density, especially whether or not pseudo-stresses, such as the Reynolds stress, should be attributed to the background flow. Furthermore, most existing propositions for this closure involve small-particle approximations. Here, we show that all existing buoyancy closures are inconsistent with particle-resolving numerical simulations and/or at least one of two simple thought experiments designed to determine the roles of pseudo-stresses and small-particle approximations. We then derive the unique consistent closure. It requires no approximation and implies that all stresses and pseudo-stresses in the average fluid phase momentum balance, except the Reynolds stress, fully contribute to the background flow responsible for buoyancy. Remarkably, it exhibits a low-pass filter property, attenuating buoyancy at short wavelengths, that prevents it from causing Hadamard instabilities, constituting a first-principles-based solution to the long-standing ill-posedness problem of two-fluid models. When employing the derived closure, even simplistic two-fluid models are linearly well-posed.

physics.flu-dyn↗

Global non-equilibrium thermodynamics of stationary states applied to the Rayleigh-Bénard convection

Classical thermodynamics describes physical systems in thermodynamic equilibrium, characterized in particular by the absence of macroscopic motion. Global non-equilibrium thermodynamics extends this framework to include physical systems in stationary states (Hołyst et al., EPL 149, 30001 (2025)). Here, we demonstrate that this extended theory captures macroscopic motion in stationary states, thereby providing a unified framework for global thermodynamics and fluid mechanics. We apply the theory to stationary Rayleigh-Bénard convection and show how the second law of global non-equilibrium thermodynamics determines the direction of changes in fluid motion.

physics.flu-dyn↗