4.7 Article

Global Modeled Sinking Characteristics of Biofouled Microplastic

期刊

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020JC017098

关键词

Biofouling; Lagrangian; microplastic; modeling

资金

  1. European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program [715386]
  2. SURF Cooperative [16371, 2019.034]
  3. Skempton Scholarship
  4. Swiss National Science Foundation [174124]

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The study estimates the sinking times of microplastic particles and finds differences in the movement and sinking rates of particles of different sizes globally. In oligotrophic regions, particles within a certain size range show no signs of sinking within 90 days. The research suggests that biological processes might play a role in the accumulation of microplastic debris in certain areas.
Microplastic debris ending up at the sea surface has become a known major environmental issue. However, how microplastic particles move and when they sink in the ocean remains largely unknown. Here, we model microplastic subject to biofouling (algal growth on a substrate) to estimate sinking timescales and the time to reach the depth where particles stop sinking. We combine NEMO-MEDUSA 2.0 output, that represents hydrodynamic and biological properties of seawater, with a particle-tracking framework. Different sizes and densities of particles (for different types of plastic) are simulated, showing that the global distribution of sinking timescales is largely size-dependent as opposed to density-dependent. The smallest particles we simulate (0.1 mu m) start sinking almost immediately around the globe and their trajectories take the longest time to reach their first sinking depth (relative to larger particles). In oligotrophic subtropical gyres with low algal concentrations, particles between 1 and 0.01 mm do not sink within the simulation time of 90 days. This suggests that in addition to the comparatively well-known physical processes, biological processes might also contribute to the accumulation of floating plastic (of 1-0.01 mm) in subtropical gyres. Particles of 1 mu m in the gyres start sinking largely due to vertical advection, whereas in the equatorial Pacific they are more dependent on biofouling. The qualitative impacts of seasonality on sinking timescales are small, however, localized sooner sinking due to spring algal blooms is seen. This study maps processes that affect the sinking of virtual microplastic globally, which could ultimately impact the ocean plastic budget.

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