The role of energetic flow structures on the aeolian transport of sediment and plastic debris

TL;DR

This study extends energy-based criteria to low-mobility aeolian sediment transport, linking flow structures to particle entrainment and distinguishing energy thresholds for rocking and rolling motions, validated through high-resolution wind tunnel experiments.

Contribution

It introduces a novel event-based framework connecting energetic flow structures to particle entrainment in aeolian transport, including plastics and natural sediments.

Findings

Flow events can be linked to particle rocking and rolling.

Distinct energy thresholds exist for different particle motions.

Energy transfer efficiency varies over an order of magnitude.

Abstract

Recently, significant progress has been made in conceptually describing the dynamic aspects of coarse particle entrainment, which has been explored experimentally for open channel flows. The aim of this study is to extend the application of energy criterion to the low mobility aeolian transport of solids (including both natural sediment and anthropogenic debris such as plastics), ranging from incomplete (rocking) to full (rolling) entrainments. This is achieved by linking particle movements to energetic flow events, which are defined as flow structures with the ability to work on particles, setting them into motion. It is hypothesized that such events should impart sufficient energy to the particles, above a certain threshold value. The concept's validity is demonstrated experimentally, using a wind tunnel and laser distance sensor (LDS) to capture the dynamics of an individual target particle, exposed on a rough bed surface. Measurements are acquired at a high spatiotemporal resolution, and synchronously with the instantaneous air velocity at an appropriate distance upwind of the target particle, using a hot film anemometer. This enables the association of flow events with rocking and rolling entrainments. Furthermore, it is shown that rocking and rolling may have distinct energy thresholds. Estimates of the energy transfer efficiency, normalized by the drag coefficient, range over an order of magnitude (from about 0.001 to 0.0048 for rocking, up to about 0.01, for incipient rolling). The proposed event-based theoretical framework is a novel approach to characterizing the energy imparted from the wind to the soil surface and could have potential implications for modelling intermittent creep transport of coarse particles and related aeolian bedforms.