EGU2020-9858
https://doi.org/10.5194/egusphere-egu2020-9858
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Solubility of metals in aerosol samples from Mount Etna during the EPL-REFLECT campaign

Chiara Giorio1, Sara D'Aronco1, Lidia Soldà1, Salvatore Giammanco2, Alessandro La Spina2, Giuseppe Salerno2, Alessia Donatucci2, Tommaso Caltabiano2, and Pasquale Sellitto3
Chiara Giorio et al.
  • 1Dipartimento di Scienze Chimiche, Università degli Studi di Padova, Padova, Italy (chiara.giorio@unipd.it)
  • 2Istituto Nazionale di Geofisica e Vulcanologia, sezione di Catania, Osservatorio Etneo, Italy
  • 3Laboratoire Interuniversitaire des Systèmes Atmosphériques - LISA, UMR CNRS 7583, Université Paris-Est Créteil, Université de Paris, Institut Pierre Simon Laplace, Créteil, France

Volcanoes emit a chemically complex cocktail of gases and aerosols into the atmosphere, which can affect Earth’s climate (1) and human health. The vast majority of volcanogenic fatalities involve the obvious thermal and physical injuries resulting from an eruption, but many of the emissions from volcanoes are toxic and include compounds such as sulfates and metals, which are known to disrupt biological systems (2). Yet, there is a lack of knowledge on the toxicity of compounds found in volcanic plumes and their fate in the atmosphere.

Research has focussed on the impacts of large-magnitude explosive eruptions. While emissions from many non-explosive eruptions are continuous and prolonged, their climatic and potential effects on human health have not been studied extensively. Once the plume disperses in the atmosphere, the aerosol particle components can mix and interact with oxidants and organic compounds present in the atmosphere. How these chemical components interact and how the interactions affect the Earth’s climate, particle toxicity and human health is largely unknown especially for trace metals.

In the framework of the EPL-REFLECT (Etna Plume Lab – near-source estimations of Radiative EFfects of voLcanic aErosols for Climate and air quality sTudies), a field campaign on Mount Etna was done in July 2019 in which samples of atmospheric aerosol were collected during non-explosive degassing activity. Samples were collected both at the crater and in a transect following the volcanic plume down slope to the closest inhabited areas. Samples were analysed for trace metals and organic compounds, including solubility tests (3) to assess how tropospheric processing of the aerosol affects metal bioavailability and potentially the toxicity of the aerosol.

 

(1) von Glasow, R. 2010. Atmospheric chemistry in volcanic plumes. Proceedings of the National Academy of Sciences, vol. 107, pp. 6594–6599., DOI: 10.1073/pnas.0913164107

(2) Weinstein, P., Horwell, C.J., Cook, A. 2013. Volcanic Emissions and Health. In: Essentials of Medical Geology, Springer Netherlands, Dordrecht, pp. 217–238., DOI: 10.1007/978-94-007-4375-5_10

(3) Tapparo, A., Di Marco, V., Badocco, D., D’Aronco, S., Soldà, L., Pastore, P., Mahon, B.M., Kalberer, M., Giorio, C. 2019. Formation of metal-organic ligand complexes affects solubility of metals in airborne particles at an urban site in the Po Valley. Chemosphere, in press., DOI: 10.1016/j.chemosphere.2019.125025

How to cite: Giorio, C., D'Aronco, S., Soldà, L., Giammanco, S., La Spina, A., Salerno, G., Donatucci, A., Caltabiano, T., and Sellitto, P.: Solubility of metals in aerosol samples from Mount Etna during the EPL-REFLECT campaign, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9858, https://doi.org/10.5194/egusphere-egu2020-9858, 2020

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