Transport and retention of sinking microplastics in a well-mixed estuary
Estuaries have been shown to be potential hotspots of microplastic accumulation, but the hydrodynamic conditions and particle properties that control this process need further investigation. We have designed a series of numerical particle-tracking experiments to examine the sensitivity of retention...
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Veröffentlicht in: | Marine pollution bulletin 2024-06, Vol.203, p.116417-116417, Article 116417 |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Estuaries have been shown to be potential hotspots of microplastic accumulation, but the hydrodynamic conditions and particle properties that control this process need further investigation. We have designed a series of numerical particle-tracking experiments to examine the sensitivity of retention in estuaries to particle size, particle density and varying tides and freshwater flow. At the end of the simulation, over 90 % of sinking particles are retained in the estuary, and the retention rate is further increased by high river runoff. In contrast, increased river discharge increases the number of marginally-buoyant (i.e. density close to estuarine water) particles that escape the estuary. Larger particle size tends to limit the downstream transport of sinking particles but can facilitate the transport of marginally-buoyant particles. Tidal asymmetry, vertical turbulent mixing and the vertical structure of the subtidal circulation are proposed as the underlying mechanisms controlling the fate of particles.
•Over 90 % of sinking microplastics are likely to be retained in an estuary.•Freshwater input facilitates the sinking and retention of heavy microplastics.•Subtidal current due to the negative buoyancy of freshwater increases retention.•Particles with density close to estuarine water have the greatest chance of escape.•Competition between sinking and mixing a major control on the fate of microplastics |
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ISSN: | 0025-326X 1879-3363 |
DOI: | 10.1016/j.marpolbul.2024.116417 |