2017
DOI: 10.1016/j.envpol.2017.01.085
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Microplastics in sea coastal zone: Lessons learned from the Baltic amber

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Cited by 100 publications
(47 citation statements)
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“…This plays a role in the coastal zone, where waves steepen and ultimately break (see section 4.11), and during storms, when waves rapidly steepen and the Stokes drift rapidly increases. This change is crucial for plastic debris beaching: developing steep stormy waves may 'grab' plastics and sediments from the beach, and transport these offshore; whilst smoother waves, which remain after the wind ceases, slowly return plastics and sediments back to shore (Chubarenko and Stepanova 2017).…”
Section: Open Ocean Stokes Driftmentioning
confidence: 99%
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“…This plays a role in the coastal zone, where waves steepen and ultimately break (see section 4.11), and during storms, when waves rapidly steepen and the Stokes drift rapidly increases. This change is crucial for plastic debris beaching: developing steep stormy waves may 'grab' plastics and sediments from the beach, and transport these offshore; whilst smoother waves, which remain after the wind ceases, slowly return plastics and sediments back to shore (Chubarenko and Stepanova 2017).…”
Section: Open Ocean Stokes Driftmentioning
confidence: 99%
“…Song et al 2017) and fragmentation in the sea swash and wave breaking zone, especially during storm events(Chubarenko and Stepanova 2017, Chubarenko et al 2018, Efimova et al 2018. The fragmentation rate of beached plastic might be closely related to the residence time on beaches Hinata 2015, Fanini and Bozzeda 2018) and is dependent on polymer type(Song et al 2017) and temperature (Andrady 2011).…”
mentioning
confidence: 99%
“…As for today's knowledge, plastics are not biodegraded to considerable extent under environmental (especially marine) conditions (Andrady, 2011;Duis and Coors, 2016), and mineralisation of plastics appears to be extremely slow as well (Shah et al, 2008;Andrady, 2011). In the sea, however, new mechanisms appear (Shah et al, 2008;Chubarenko et al, 2016), most effective being mechanical abrasion by sediments and fragmentation in the sea swash and wave breaking zone, especially during stormy events (Chubarenko and Stepanova, 2017;Chubarenko et al, 2018;Efimova and Chubarenko, 2018). Here, properties and qualities of the generated MP particles are very difficult to predict, which does not make this question less important.…”
Section: Introductionmentioning
confidence: 99%
“…Fragments of harder plastics (FRAG) and industrial pellets (IND) making up the majority of the microplastic particles. These differences in migration, breakdown and deposition of different microplastic types may be explained by the re-suspension of sediments; the nature of fragments and rounded pellets behaving in a different way to films, flakes and fibres (Chubarenko and Stepanova, 2017). Indeed modelling of microplastics in the marine environment has revealed that foamed plastics travel fastest over surface water and films and fibres typically sink due to higher rates of bio-fouling than fragments or spheres which could explain their lack of abundance upon beaches (Chubarenko et al, 2016).…”
Section: Variance Among Plastic Categoriesmentioning
confidence: 99%