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Sedimentary Characteristics of Microplastics Transported by Turbidity Currents in a Straight Canyon Topography

Journal of marine environmental engineering 2026 Score: 40 ? 0–100 AI score estimating relevance to the microplastics field. Papers below 30 are filtered from public browse.
Qingsheng Meng, Xiaotian Xie, Yang Lu, Heyu Yu, Guangwei Cheng, Xiaolei Liu

Summary

Physical model experiments revealed that ocean turbidity currents — sediment-laden underwater flows — transport and deposit microplastics in predictable patterns within submarine canyons, with higher-concentration flows retaining more particles and depositing them preferentially in wave-shaped seafloor areas. This understanding helps predict where microplastics accumulate in the deep sea, which matters for assessing long-term ecological impacts in some of the ocean's most remote and poorly studied habitats.

Study Type Environmental

The advancement of ocean observation technology has confirmed that submarine canyons are important sedimentary sites for microplastics. Turbidity currents serve as a medium for transporting microplastics through submarine canyons to the deep sea. However, the transport and deposition of microplastics in these canyons by turbidity currents remain unclear. This study, through physical model experiments, explores how the initial conditions of turbidity currents affect the distribution of microplastics in a canyon topography. Results reveal that different concentrations of turbidity currents create varying depositional patterns along the middle to the upper reaches of the canyon. At low concentrations, uniformly distributed crescent-shaped structures are formed, whereas at high concentrations, the deposits are irregularly shaped and tend to migrate toward the head of the canyon. Microplastics are predominantly deposited in areas with wavy sedimentary topography, and in situations with low turbidity current concentrations, abundant microplastics are exposed and accumulated. Additionally, the retention rate of microplastics in 6% volume concentration of turbidity currents is considerably higher than that in 1% volume concentration, and high flow rates promote the migration of microplastic enrichment areas along the canyon. The maximum enrichment zones of microplastics are always located in areas with wave-shaped topography where the sediment particles are large, making them the main deposition zones for microplastics. This research provides valuable insights for predicting the accumulation sites of microplastics in submarine canyons and their effects on the ecological environment.

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