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Abstract
Long-lived basaltic volcanic eruptions are a globally important source of environmentally reactive, volatile metal pollutant elements such as selenium, cadmium and lead. The 2018 eruption of Kilauea, Hawai'i produced exceptionally high discharge of metal pollutants, and was an unprecedented opportunity to track them from vent to deposition. Here we show, through geochemical sampling of the plume that volatile metal pollutants were depleted in the plume up to 100 times faster than refractory species, such as magnesium and iron. We propose that this rapid wet deposition of complexes containing reactive and potentially toxic volatile metal pollutants may disproportionately impact localised areas close to the vent. We infer that the relationship between volatility and solubility is an important control on the atmospheric behaviour of elements. We suggest that assessment of hazards from volcanic emissions should account for heterogeneous plume depletion of metal pollutants.
Publisher
Communications Earth & Environment
Published On
May 04, 2021
Authors
Evgenia Ilyinskaya, Emily Mason, Penny E. Wieser, Lacey Holland, Emma J. Liu, Tamsin A. Mather, Marie Edmonds, Rachel C. W. Whitty, Tamar Elias, Patricia A. Nadeau, David Schneider, James B. McQuaid, Sarah E. Allen, Jason Harvey, Clive Oppenheimer, Christoph Kern, David Damby
Tags
volcanic eruptions
metal pollutants
Kilauea
environmental impact
geochemical sampling
volatility
atmospheric behaviour
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