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Modelling the sedimentation of macro-, micro- and nanoplastics in the ocean from surface to sediment
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Researchers modeled the sedimentation of macro-, micro-, and nanoplastics from the ocean surface to the seafloor, finding that biofouling and particle aggregation dramatically accelerate sinking rates and that most plastics eventually reach benthic environments.
The ocean is considered a sink for plastic waste, with buoyant plastics remaining at the surface for up to 50 years. Removal of plastic waste from the ocean by manpower is not feasible, but natural-based removal strategies are promising. Among these, the biological pump stands out as a crucial process responsible for transferring materials and nutrients from the surface to the deep ocean. In this context, plastic particles can be incorporated into and transported with marine snow aggregates, providing a potential mechanism for removing plastic waste from the upper ocean (human food chain) to the deep ocean. However, the longevity of plastic debris at the ocean surface remains poorly understood. To address this gap, we developed a degradation-aggregation model to predict the longevity of different types, sizes and shapes of buoyant plastics at the ocean surface. Our results show that the longevity of plastic debris is primarily determined by the time it takes for plastic debris to degrade sufficiently and become small enough (< 100 µm) to be incorporated into marine snow aggregates. Larger plastics take decades to degrade into small microplastics that can be trapped in marine snow, prolonging their presence in surface waters. Conversely, once microplastics are small enough to be incorporated into marine snow, they can reach the seafloor sediment within two years. Interestingly, our model highlights that vertical settling of microplastics occurs through multiple incorporation and settling via vector transport of marine snow, which differs from previous studies reporting oscillations of microplastics in the ocean subsurface. This study explains the mechanisms of plastic debris removal by the biological pump and the longevity of plastic debris at the ocean surface. In addition, this theoretical model can be extended to different aquatic ecosystems to predict the fate and longevity of plastic debris in different environments.
More Papers Like This
Modelling the sedimentation of macro-, micro- and nanoplastics in the ocean from surface to sediment
AI summary Read the abstract
This study modeled the sedimentation of macro-, micro-, and nanoplastics in the ocean, focusing on the role of the biological pump and marine snow aggregation in removing plastics from the surface and transporting them to depth. Models showed that natural settling processes driven by biologically produced particles are a significant mechanism for transferring plastic pollution to the seafloor.
Modelling the sedimentation of macro-, micro- and nanoplastics in the ocean from surface to sediment
AI summary Read the abstract
This study modeled the sedimentation of macro-, micro-, and nanoplastics in the ocean, focusing on how the biological pump and marine snow aggregation transfer plastic from surface waters to the deep sea. The model showed that biological processes dramatically accelerate the removal of plastic particles from the ocean surface, with implications for estimates of marine plastic residence times.
Global Modeled Sinking Characteristics of Biofouled Microplastic
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Researchers developed a global model of microplastic biofouling and sinking using satellite oceanographic data to estimate where and when buoyant plastic particles sink out of the surface ocean, finding that sinking timescales ranged from days in tropical waters to months in high-latitude regions depending on temperature and productivity.
Global modeled sinking characteristics of biofouled microplastic
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Researchers used a global ocean circulation model coupled with a biofouling submodel to estimate sinking timescales for microplastics globally, finding that most buoyant particles sink to depth within weeks to months due to algal colonization. The modeling results explain why ocean surface plastic concentrations are much lower than expected based on input estimates.
Rapid aggregation of biofilm-covered microplastics with marine biogenic particles
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Researchers demonstrated that biofilm-covered microplastics rapidly aggregate with marine biogenic particles such as algal cells and fecal pellets, which accelerates their sinking from surface waters. The study helps explain why microplastic concentrations at the ocean surface are lower than expected — biofouling causes the particles to be transported to deeper waters and sediments faster than previously assumed.
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When a large batch of papers lands in the Atlas, we read through it and send a short write-up of what stood out.