The effects of sediment properties on the aeolian abrasion and surface characteristics of microplastics
Microplastics (<5 mm diameter) are significant environmental contaminants whose small sizes and low densities facilitate transport by wind. Transport by wind erosion alongside soils or sediments results in mechanical abrasion of the plastic surfaces which can alter their physical and chemical properties. This paper uses laboratory simulations to determine the effects of up to 216 hours of aeolian abrasion on polyethylene microplastics by angular, subrounded and rounded mineral sediments. During the abrasion process the mineral particles break down producing small fragments which adhere to the microplastic surfaces altering their surface roughness and chemistry. With increasing duration of abrasion the microplastic surface becomes coated with mineral fragments changing the dominant surface element from carbon to oxygen and silicon reflecting the composition of the erodents. The coating develops more rapidly when microplastics are abraded with angular sediments as these produce a lot of small fragments within the first 1-2 hours. However, after >200 hours of abrasion all the erodents had similar effects. A conceptual model of microplastic surface change is presented in which the plastic cracks and fractures, then flattens alongside the increasing density of sediment fragment cover. Surface changes may affect the ability of the plastics to transport airborne contaminants.
Funding
Microplastic entrainment, transport and fragmentation in atmospheric boundary-layer flows
Natural Environment Research Council
Find out more...History
School
- Aeronautical, Automotive, Chemical and Materials Engineering
- Science
- Social Sciences and Humanities
Department
- Chemistry
- Geography and Environment
- Materials
Published in
Philsophical Transactions of the Royal Society APublisher
The Royal SocietyVersion
- AM (Accepted Manuscript)
Publisher statement
This paper was accepted for publication in the journal Philsophical Transactions of the Royal Society A and the definitive published version is available at [insert DOI link http://dx.doi.org/. This article has been published under a CC BY licence. For more information please see https://creativecommons.org/licenses/by/4.0/Acceptance date
2025-03-12ISSN
1364-503XeISSN
1471-2962Publisher version
Language
- en