The entrainment and energetics of turbulent plumes in a confined space

TL;DR

This study combines theory and direct numerical simulation to analyze the entrainment, energetics, and flow structures of turbulent air plumes in a confined space, revealing how aspect ratio influences flow bifurcation and energy distribution.

Contribution

It introduces a theoretical framework and simulation analysis of plume energetics and flow bifurcation in confined spaces, extending classical plume models to complex geometries.

Findings

Flow bifurcation occurs at larger aspect ratios.

Kinetic energy dissipation is equally split between jets and plumes.

Almost half of the available potential energy input is dissipated in the jets and plumes.

Abstract

We analyse the entrainment and energetics of equal and opposite axisymmetric turbulent air plumes in a vertically confined space at a Rayleigh number of $1.24\times 10^{7}$ using theory and direct numerical simulation. On domains of sufficiently large aspect ratio, the steady state consists of turbulent plumes penetrating an interface between two layers of approximately uniform buoyancy. As described by Baines and Turner (J. Fluid Mech. vol. 37, 1969, pp. 51-80), upon penetrating the interface the flow in each plume becomes forced and behaves like a constant-momentum jet, due to a reduction in its mean buoyancy relative to the local environment. To observe the behaviour of the plumes we partition the domain into sub-domains corresponding to each plume. Domains of relatively small aspect ratio produce a single primary mean-flow circulation between the sub-domains that is maintained by entrainment into the plumes. At larger aspect ratios the mean flow between the sub-domains bifurcates, indicating the existence of a secondary circulation within each layer associated with entrainment into the jets. To study the flow's energetics we use a local definition of available potential energy (APE). For plumes with Gaussian velocity and buoyancy profiles, the theory we develop suggests that the kinetic energy dissipation is split equally between the jets and the plumes and, collectively, accounts for almost half of the input of APE at the boundaries. In contrast, $1/4$ of the APE dissipation and background potential energy (BPE) production occurs in the jets, with the remaining $3/4$ occurring in the plumes. These bulk theoretical predictions agree with observations of BPE production from simulations to within $1\%$ and form the basis of a similarity solution that models the vertical dependence of APE dissipation and BPE production.