Kinematics of Particles at Entrainment and Disentrainment
We address the issue of characterizing experimentally entrainment and disentrainment of sediment particles of cohesionless granular beds in turbulent open channel flows. Employing Particle Image Velocimetry, we identify episodes of entrainment and of disentrainment of bed particles by analysing the...
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doaj-dbdae95c2d7c49f1ba483bdb86a8f56c2020-11-25T03:51:39ZengMDPI AGWater2073-44412020-07-01122110211010.3390/w12082110Kinematics of Particles at Entrainment and DisentrainmentRui Aleixo0Federica Antico1Ana M. Ricardo2Rui M.L. Ferreira3CERIS—Civil Engineering Research and Innovation for Sustainability, Av. Rovisco Pais, 1049-003 Lisboa, PortugalCERIS—Civil Engineering Research and Innovation for Sustainability, Av. Rovisco Pais, 1049-003 Lisboa, PortugalCERIS—Civil Engineering Research and Innovation for Sustainability, Av. Rovisco Pais, 1049-003 Lisboa, PortugalCERIS—Instituto Superior Técnico, Universidade de Lisboa, Av. Rovisco Pais, 1048-001 Lisboa, PortugalWe address the issue of characterizing experimentally entrainment and disentrainment of sediment particles of cohesionless granular beds in turbulent open channel flows. Employing Particle Image Velocimetry, we identify episodes of entrainment and of disentrainment of bed particles by analysing the raw PIV images. We define a reference velocity for entrainment or disentrainment by space-averaging the flow field in the vicinity of the (entrained or disentrainned) particle and by time-averaging that space-average over a short duration encompassing the observed episode. All observations and measurements took place under generalized movement conditions and in non-controlled geometrical set-ups, resulting in unique databases of conditionally sampled turbulent flow kinematics associated with episodes of particle entrainment and of particle disentrainment. Exploring this database, the objective of this paper is to prove further insights on the dynamics of fluid-particle and particle-particle interactions at entrainment and disentrainment and to polemicize the use of a reference velocity to serve as a proxy for hydrodynamics actions responsible for entrainment or disentrainment. In particular, we quantify the reference velocity associated with entrainment and disentrainment episodes and discuss its potential to describe the observed motion <i>vis-a-vis</i> local bed micro-topography and the type of entrainment or disentrainment event. Entrainment may occur at a wide range of reference velocities, including smaller than mean (double-averaged) velocities. Anecdotal evidence was collected for some typologies of entrainment: (i) momentum transfer from flow to a single particle, (ii) momentum transfer from a perturbed local flow to a single particle, (iii) collective entrainment associated to momentum transfer between a moving and a resting particle and (iv) collective entrainment considered to be a dislodgment of several particles involving momentum transfer from other particles. In some of these cases, e.g., (ii) and (iii), the use of a reference velocity seems inadequate to characterize the entrainment episode. A word of caution about the use of entrainment models based on reference velocities is henceforth issued and contextualized. In the case of disentrainment, a reference velocity seems to constitute a better descriptor of the observed behaviour. The scatter in the observed values seems to express the contribution of bed micro-topography. All particles were found to experience frictional contacts with the resting bed surface particles, but some particles were stopped more abruptly due to the presence of an obstacle along their path. Most disentrainment of particles took place when the near-bed flow was featuring ejection events.https://www.mdpi.com/2073-4441/12/8/2110sediment kinematicsentrainmentdisentrainmentturbulence |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Rui Aleixo Federica Antico Ana M. Ricardo Rui M.L. Ferreira |
spellingShingle |
Rui Aleixo Federica Antico Ana M. Ricardo Rui M.L. Ferreira Kinematics of Particles at Entrainment and Disentrainment Water sediment kinematics entrainment disentrainment turbulence |
author_facet |
Rui Aleixo Federica Antico Ana M. Ricardo Rui M.L. Ferreira |
author_sort |
Rui Aleixo |
title |
Kinematics of Particles at Entrainment and Disentrainment |
title_short |
Kinematics of Particles at Entrainment and Disentrainment |
title_full |
Kinematics of Particles at Entrainment and Disentrainment |
title_fullStr |
Kinematics of Particles at Entrainment and Disentrainment |
title_full_unstemmed |
Kinematics of Particles at Entrainment and Disentrainment |
title_sort |
kinematics of particles at entrainment and disentrainment |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2020-07-01 |
description |
We address the issue of characterizing experimentally entrainment and disentrainment of sediment particles of cohesionless granular beds in turbulent open channel flows. Employing Particle Image Velocimetry, we identify episodes of entrainment and of disentrainment of bed particles by analysing the raw PIV images. We define a reference velocity for entrainment or disentrainment by space-averaging the flow field in the vicinity of the (entrained or disentrainned) particle and by time-averaging that space-average over a short duration encompassing the observed episode. All observations and measurements took place under generalized movement conditions and in non-controlled geometrical set-ups, resulting in unique databases of conditionally sampled turbulent flow kinematics associated with episodes of particle entrainment and of particle disentrainment. Exploring this database, the objective of this paper is to prove further insights on the dynamics of fluid-particle and particle-particle interactions at entrainment and disentrainment and to polemicize the use of a reference velocity to serve as a proxy for hydrodynamics actions responsible for entrainment or disentrainment. In particular, we quantify the reference velocity associated with entrainment and disentrainment episodes and discuss its potential to describe the observed motion <i>vis-a-vis</i> local bed micro-topography and the type of entrainment or disentrainment event. Entrainment may occur at a wide range of reference velocities, including smaller than mean (double-averaged) velocities. Anecdotal evidence was collected for some typologies of entrainment: (i) momentum transfer from flow to a single particle, (ii) momentum transfer from a perturbed local flow to a single particle, (iii) collective entrainment associated to momentum transfer between a moving and a resting particle and (iv) collective entrainment considered to be a dislodgment of several particles involving momentum transfer from other particles. In some of these cases, e.g., (ii) and (iii), the use of a reference velocity seems inadequate to characterize the entrainment episode. A word of caution about the use of entrainment models based on reference velocities is henceforth issued and contextualized. In the case of disentrainment, a reference velocity seems to constitute a better descriptor of the observed behaviour. The scatter in the observed values seems to express the contribution of bed micro-topography. All particles were found to experience frictional contacts with the resting bed surface particles, but some particles were stopped more abruptly due to the presence of an obstacle along their path. Most disentrainment of particles took place when the near-bed flow was featuring ejection events. |
topic |
sediment kinematics entrainment disentrainment turbulence |
url |
https://www.mdpi.com/2073-4441/12/8/2110 |
work_keys_str_mv |
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