4.7 Article

Abiotic plastic leaching contributes to ocean acidification

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 854, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2022.158683

Keywords

Plastic leaching; Ocean acidification; DOC leaching; Microplastics

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Ocean acidification and plastic pollution are escalating threats to global societies and ecosystems. Laboratory experiments show that abiotic plastic degradation results in a decrease in seawater pH, particularly in aged plastics. Solar radiation enhances the pH decrease, likely due to the release of organic acids and the production of CO2. Plastic leaching could lead to a seawater pH decrease up to 0.5 units in coastal areas, comparable to the projected decrease by the end of the twenty-first century.
Ocean acidification and plastic pollution are considered as potential planetary boundary threats for which crossing certain thresholds could be very harmful for the world's societies and ecosystems well-being. Surface oceans have acidified around 0.1 units since the Industrial Revolution, and the amount of plastic reaching the ocean in 2018 was quantified to 13 million metric tonnes. Currently, both ocean threats are worsening with time. Plastic leaching is known to alter the biogeochemistry of the ocean through the release of dissolved organic matter. However, its impact in the inorganic chemistry of the seawater is less studied. Here we show, from laboratory experiments, that abiotic plastic degradation induces a decrease in seawater pH, particularly if the plastic is already aged, as that found in the ocean. The pH decrease is enhanced by solar radiation, and it is probably induced from a combination of the release of organic acids and the production of CO2.It is also related to the amount of leached dissolved organic carbon, with higher acidification as leaching increases. In coastal areas, where plastic debris accumulates in large quantities, plastic leaching could lead to a seawater pH decrease up to 0.5 units. This is comparable to the projected decrease induced in surface oceans by the end of the twenty-first century for the most pessimistic anthropogenic emissions scenarios.

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