Javascript must be enabled to continue!
Numerical investigation of momentum exchange between particles and coherent structures in low Re turbulent channel flow
View through CrossRef
The interaction between particles and coherent structures is studied by using discrete particle simulation combined with direct numerical simulation of gaseous flow in a vertical channel. A conditional sampling scheme is used to examine the modifications of the near-wall quasistreamwise vortices by the momentum exchange between the phases. The particle effect on the fluid flow is modeled by a point-force approximation. The particle diameters are smaller than both the smallest flow length scales and the computational grid spacing. Results are obtained for particle ensembles with four response times ranging from 10 to 200 wall units in numerical simulations with and without gravitational settling in the streamwise direction and interparticle collisions. It is found that the size of the quasistreamwise vortices is increased up to 25% in the presence of particles. The increase is larger for the smallest inertia particles studied, which is partly due to their locally nonuniform spatial distribution. The underlying organized fluid motions induced by the structures are substantially attenuated due to the momentum coupling of the phases. A reduction of 5%–55% is observed in the coherent fluid velocities and vorticities. The size of the coherent structures is additionally augmented by streamwise gravitational settling and interparticle collisions, accompanied by more obvious modifications in the surrounding fluid flow. The latter findings are explained by the stronger direct particle effect in these cases, which is also reflected on the energy redistribution between the fluid velocity components, affecting further the fluid turbulence.
Title: Numerical investigation of momentum exchange between particles and coherent structures in low Re turbulent channel flow
Description:
The interaction between particles and coherent structures is studied by using discrete particle simulation combined with direct numerical simulation of gaseous flow in a vertical channel.
A conditional sampling scheme is used to examine the modifications of the near-wall quasistreamwise vortices by the momentum exchange between the phases.
The particle effect on the fluid flow is modeled by a point-force approximation.
The particle diameters are smaller than both the smallest flow length scales and the computational grid spacing.
Results are obtained for particle ensembles with four response times ranging from 10 to 200 wall units in numerical simulations with and without gravitational settling in the streamwise direction and interparticle collisions.
It is found that the size of the quasistreamwise vortices is increased up to 25% in the presence of particles.
The increase is larger for the smallest inertia particles studied, which is partly due to their locally nonuniform spatial distribution.
The underlying organized fluid motions induced by the structures are substantially attenuated due to the momentum coupling of the phases.
A reduction of 5%–55% is observed in the coherent fluid velocities and vorticities.
The size of the coherent structures is additionally augmented by streamwise gravitational settling and interparticle collisions, accompanied by more obvious modifications in the surrounding fluid flow.
The latter findings are explained by the stronger direct particle effect in these cases, which is also reflected on the energy redistribution between the fluid velocity components, affecting further the fluid turbulence.
Related Results
En skvatmølle i Ljørring
En skvatmølle i Ljørring
A Horizontal Mill at Ljørring, Jutland.Horizontal water-mills have been in use in Jutland since the beginning of the Christian era 2). But the one here described shows so close a c...
Numerical study of educed coherent structures in the near-wall region of a particle-laden channel flow
Numerical study of educed coherent structures in the near-wall region of a particle-laden channel flow
The interaction of small heavy solid particles with turbulence near the wall of a vertical downward channel flow is investigated by using direct numerical simulation (DNS) and Lagr...
Dynamics of fluid mixing in separated flows
Dynamics of fluid mixing in separated flows
Separated flows at high Re (>103) are highly turbulent. In some situations the turbulence generation and mixing processes associated with flow separation are desirable, e.g....
On the numerical simulation of compressible flows
On the numerical simulation of compressible flows
In this thesis, numerical tools to simulate compressible flows in a wide range of situations are presented. It is intended to represent a step forward in the scientific research of...
Clogging model of hyporheic exchange based on coupled lattice Boltzmann discrete element simulations
Clogging model of hyporheic exchange based on coupled lattice Boltzmann discrete element simulations
The hyporheic exchange between the surface water and the underground water is considered a significant process in the natural water cycle system. Some sediment particles in the riv...
Polymer-laden homogeneous shear-driven turbulent flow: a model for polymer drag reduction
Polymer-laden homogeneous shear-driven turbulent flow: a model for polymer drag reduction
Drag reduction (DR) under a turbulent boundary layer implies the suppression of turbulent momentum flux to the wall, a large-eddy phenomenon. Our hypothesis is that the essential m...
Large-eddy simulations of the mountain boundary layer : daytime exchange processes and nocturnal fog formation
Large-eddy simulations of the mountain boundary layer : daytime exchange processes and nocturnal fog formation
In this dissertation, different aspects of turbulent transport and thermally driven flows over complex terrain are investigated. Two publications concentrate on the vertical heat a...
Constraining the origins of terrestrial stratospheric solid aerosols over the 1981-2020 period
Constraining the origins of terrestrial stratospheric solid aerosols over the 1981-2020 period
MotivationThe injection of materials into the Earth's atmosphere has both a natural and an anthropogenic component. Natural solid aerosols that reach the stratosphere can come from...

