PhD (DPhil) candidate, University of Oxford (he/him)
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Patrick FarrellWe propose a general strategy for enforcing multiple conservation laws and dissipation inequalities in the numerical solution of initial value problems. […] We demonstrate these ideas by their application to the Navier-Stokes equations. We generalize […] the energy-dissipating and helicity-tracking scheme of Rebholz for the incompressible […] equations, and devise the first time discretization of the compressible equations that conserves mass, momentum, and energy, and provably dissipates entropy.
In my earlier work with Patrick Farrell, we proposed a framework for the construction of finite-element integrators that preserve multiple conservation laws and dissipation inequalities, alongside various applications to different PDE systems. This preprint serves as part 1 of a partition of this work.
We re-establish the framework, including alongside the discussions of its applications to the Navier–Stokes equations, deriving (to arbitrary order) integrators that:
For further details, check out my earlier manuscript here.
As stated above, this work represents part 1 of a resubmission of an earlier manuscript with Patrick Farrell, partitioned into multiple parts.
For a neat and related application of these ideas to a problem in magnetic relaxation that really highlights their importance, check out my subsequent work with Mingdong He, Patrick Farrell & Kaibo Hu, on structure-preserving integrators for the magneto-frictional equations.
Problem | Reward |
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Application of the auxiliary variable framework to a viscoelastic fluid system | ★★☆☆☆ |
Structure-preserving integrators for compressible MHD | ★☆☆☆☆ |
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University of Oxford
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High-order conservative and accurately dissipative numerical integrators via auxiliary variables / Topology-preserving discretization for the magneto-frictional equations arising in the Parker conjecture / Enforcing conservation laws and dissipation inequalities numerically via auxiliary variables / An augmented Lagrangian preconditioner for natural convection at high Reynolds number*