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Evidence of beryllium isotope signatures in stratospheric air reveals long distance transport of micro/nano-plastics in the Southern Tibetan Plateau
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Scientists found tiny plastic particles high in the atmosphere above the Tibetan Plateau, one of the most remote places on Earth, and used a clever radioactive tracer trick to prove these plastics traveled down from the stratosphere (many miles up in the sky) rather than blowing in from nearby sources. This matters because it shows plastic pollution can circulate through the upper atmosphere and settle in far-flung, seemingly pristine locations, meaning there's essentially nowhere on the planet, including the air we breathe in remote high-altitude regions, that's fully protected from microplastic contamination.
The new threat from atmospheric Micro/nano-plastics (MNPs) emissions now reaches far beyond the conventional scope of plastic-related issues. While MNP horizontal transport within the planetary boundary layer is well understood, limited knowledge of their vertical transport in the free troposphere and stratosphere hinder comprehensive modeling of their global atmospheric circulation. Considering that the production rates of radioactive beryllium isotopes (7Be and 10Be) above the tropopause is over 100 times higher than that in the near surface atmosphere, if relatively high concentrations and ratios of 10Be and 7Be can be observed near the surface, this phenomenon can serve as a unique isotope "fingerprint" for the invasion of deep stratospheric air invasion. Here, we present evidence of MNPs at mass concentrations of 0.0059-0.11 μg/m³ detected in Lhasa, southern Tibetan Plateau. And through synchronous high-precision observations of 7Be and 10Be, we have discovered strong stratospheric air signals during periods of high MNP concentration. Through the atmospheric transport models to delineate the occurrence, magnitude, retention period, flux, and characteristics of MNP pollution driven by upper-atmospheric vertical circulation in this high-elevation region. We found that under special topographic and aerodynamic conditions, atmospheric vertical circulation will promote the accumulation of MNPs for the enrichment and redistribution of MNPs. This work reveals the importance of vertical circulation in the upper atmosphere in the dynamics of MNP circulation based on evidence from beryllium isotopes.
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