Expressing turbulent kinetic energy as coarse-grained enstrophy or strain deformations
Damiano Capocci

TL;DR
This paper derives an exact identity linking velocity gradient norms to kinetic energy in turbulence, enabling decomposition into strain and enstrophy contributions, and provides a real-space based energy spectrum consistent with Kolmogorov scaling.
Contribution
It introduces a novel exact identity connecting velocity gradients with kinetic energy, allowing for a new decomposition into strain and enstrophy contributions in turbulence.
Findings
Decomposition shows 55% energy from strain deformations, 40% from enstrophy, and 5% from indefinite stresses.
The real-space energy spectrum reproduces Kolmogorov's power-law scaling.
The identities enable a new characterization of the Kolmogorov constant.
Abstract
In turbulent flows, the fluid element gets deformed by chaotic motion due to the formation of sharp velocity gradients. A direct connection between the element of fluid stresses and the energy balance still remains elusive. Here, an exact identity of incompressible turbulence is derived linking the velocity gradient norm across the scales with the total kinetic energy. In the context of three-dimensional (3D) homogeneous turbulence, this relation can be specialised obtaining the expression of total kinetic energy decomposed either in terms of deformations due to strain motion or via the resolved-scale enstrophy of the fluid element. Applied to data from direct numerical simulations (DNS) describing homogeneous and isotropic turbulence, the decomposition reveals that, beyond the scales dominated by the external forcing, contractile and extensional deformations account approximately for…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsFluid Dynamics and Turbulent Flows · Aeolian processes and effects
