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Wave-induced transport of non-buoyant microplastic particles: Phase-resolved experiments and excess-Shields scaling

Coastal Engineering 2026 Score: 40 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Giovanni Passalacqua, Giovanni Passalacqua, Claudio Iuppa, Giulia Bonanno, Giulia Bonanno, Claudio Iuppa, Carla Faraci Carla Faraci Claudio Iuppa, Carla Faraci Claudio Iuppa, Carla Faraci Carla Faraci

Summary

Laboratory wave flume experiments showed that non-buoyant microplastic particles (such as PLA) move with incoming wave action and accumulate onshore, with the drift increasing with wave steepness. These findings help explain the observed buildup of denser microplastics in coastal sediments and improve models predicting where microplastics ultimately settle.

Polymers
Study Type Environmental

The present study investigates the bed-load dynamics of non-buoyant microplastic particles subjected to wave forcing, with emphasis on the phase-resolved relationship between particle motion and near-bed hydrodynamics. Specifically, five groups of PLA particles, differing in shape and density, were tested in a wave flume under five regular wave conditions representative of intermediate-depth coastal environments. Based on high quality video analysis, particle mobilisation occurred when the modified Shields parameter for plastics exceeded the incipient-motion threshold derived from previous work. The experiments highlighted a residual onshore drift that depends on the particle characteristics and increases with wave steepness, resulting from asymmetries in the near-bed velocity field. For the first time, a link has been established between the phase-resolved particle velocity, normalised by the near-bed flow velocity, and the ratio of the modified Shields number for plastics to the incipient motion threshold, revealing a clear non-linear dependence between particle mobility and the applied force. • Phase-resolved experiments investigate non-buoyant microplastics under waves. • Blob-analysis tracking quantifies oscillatory motion and onshore drift. • Particle velocity follows a power-law relation with excess shear stress. • Results reveal a unified scale for sediment and plastic transport.

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