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Julian Brehm Julian Brehm Christian Laforsch, Bashir Olasunkanmi Ayinde, Bashir Olasunkanmi Ayinde, Julian Brehm Julian Brehm Christian Laforsch, Julian Brehm Julian Brehm Julian Brehm Bashir Olasunkanmi Ayinde, Julian Brehm Wolfgang Babel, Julian Brehm Julian Brehm Julian Brehm Wolfgang Babel, Wolfgang Babel, Wolfgang Babel, Daniel Wagner, Wolfgang Babel, Wolfgang Babel, Julian Brehm Christoph Thomas, Julian Brehm Julian Brehm Johannes Olesch, Christian Laforsch, Johannes Olesch, Christian Laforsch, Johannes Olesch, Johannes Olesch, Christian Laforsch, Wolfgang Babel, Christian Laforsch, Christian Laforsch, Christian Laforsch, Wolfgang Babel, Wolfgang Babel, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Johannes Olesch, Christoph Thomas, Christoph Thomas, Julian Brehm Julian Brehm Wolfgang Babel, Daniel Wagner, Christoph Thomas, Julian Brehm Wolfgang Babel, Julian Brehm Wolfgang Babel, Daniel Wagner, Daniel Wagner, Daniel Wagner, Wolfgang Babel, Christian Laforsch, Christoph Thomas, Christian Laforsch, Wolfgang Babel, Christoph Thomas, Seema Agarwal, Christoph Thomas, Seema Agarwal, Julian Brehm Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Seema Agarwal, Christoph Thomas, Christoph Thomas, Christoph Thomas, Christian Laforsch, Christian Laforsch, Julian Brehm Julian Brehm Julian Brehm Christoph Thomas, Julian Brehm Christian Laforsch, Anke Christine Nölscher, Anke Christine Nölscher, Anke Christine Nölscher, Anke Christine Nölscher, Christian Laforsch, Anke Christine Nölscher, Christian Laforsch, Christian Laforsch, Anke Christine Nölscher, Christoph Thomas, Christoph Thomas, Christoph Thomas, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christoph Thomas, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Christian Laforsch, Julian Brehm Julian Brehm

Summary

Researchers used a wind tunnel and machine-learning image analysis to measure precisely how much wind force is needed to dislodge tire wear particles — a major source of airborne microplastic pollution — from a surface, finding that larger and more irregularly shaped particles require significantly more wind energy to become airborne than smaller, rounder ones. Standard models developed for sand and dust underestimated the stickiness of tire particles, likely because their irregular, jagged shapes create more contact points with surfaces. These measurements are needed to build better models of how tire microplastics spread through the air from roads.

Polymers

<strong class="journal-contentHeaderColor">Abstract.</strong> The transport dynamics of tire wear particles (TWPs) remain poorly understood despite their growing contribution to airborne microplastic (MP) pollution. This study addresses this gap by experimentally quantifying the TWP detachment rate and threshold friction velocities (<em>u<sub>*</sub></em><sup>th</sup> ) from an idealised reference surface. Detachment experiments were conducted in a boundary layer wind tunnel over glass substrates seeded with a near-monolayer of particles. Time resolved imaging at 0.1 Hz was combined with automatic particle detachment and segmentation using an open source You Only Look Once version 8 nano (YoloV8n) model, which allowed individual detachment events and particle size and shape to be tracked with a mean average precision at an intersection-over-union threshold of 0.5 (mAP@50) above 85 % for both the bounding box and mask outputs. For the detachment experiments, pristine tire wear particles generated on a laboratory test stand with passenger car (PC) test tire were supplied by Continental GmbH, providing a well characterised and idealised TWP source. Among the three deposition method tested, the low-cost pressurised seeding approach produced the most uniform and reproducible particle distribution for detachment analysis. Across the analysed size range (80 to 300 &mu;m), larger and more irregularly shaped particles exhibited significantly higher detachment (<em>u<sub>*</sub></em><sup>th</sup>) than smaller and more rounded fragments. Ensemble fits yield a bulk <em>u<sub>*</sub></em><sup>th</sup> of approximately 0.36 m s<sup>&minus;1</sup>, with size and shape resolved <em>u<sub>*</sub></em><sup>th</sup> values varying by roughly a factor of 1.5 between the most easily detached and most resistant classes. The application of the Shao and Lu semi-empirical fluid threshold model reproduced the size-dependent <em>u<sub>*</sub></em><sup>th</sup> of smooth PE microsphere, but underestimates the TWP <em>u<sub>*</sub></em><sup>th</sup> unless the effective cohesion and/or aerodynamic scaling parameter are increased beyond values typically used for dust and sand. This behaviour is consistent with TWPs experiencing stronger effective adhesion than smooth, spherical grains of similar size, due to their irregular morphology and multiple contact points with the substrate. The density differences between TWPs (&sim;1300 kg m<sup>&minus;3</sup>) and microspheres (&sim;1025 kg m<sup>&minus;3</sup>) showed negligible influence within the studied size range (106 to 125 &mu;m). We conclude that particle morphology, incorporating both size and shape, plays a dominant role in controlling the aerodynamic detachment of TWPs on the idealised glass substrate, while density effects are secondary under the tested conditions. Because controlled laboratory studies using well defined particles and simplified surfaces are a neccessary step towards isolating these fundamental mechanisms, our findings provide insights for improving MP and TWP resuspension models and highlight the need for future studies on more realistic environmental surfaces and broader particle sizes and density ranges.

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