Understanding the environmental impacts of large fissure eruptions: Aerosol and gas emissions from the 2014–2015 Holuhraun eruption (Iceland)

Ilyinskaya, Evgenia and Schmidt, Anja and Mather, Tamsin A. and Pope, Francis D. and Witham, Claire and Baxter, Peter and Jóhannsson, Thorsteinn and Pfeffer, Melissa and Barsotti, Sara and Singh, Ajit and Sanderson, Paul and Bergsson, Baldur and McCormick Kilbride, Brendan T. and Donovan, Amy and Peters, Nial and Oppenheimer, Clive and Edmonds, Marie (2017) Understanding the environmental impacts of large fissure eruptions: Aerosol and gas emissions from the 2014–2015 Holuhraun eruption (Iceland). Earth and Planetary Science Letters, 472. pp. 309-322. ISSN 0012-821X DOI https://doi.org/10.1016/j.epsl.2017.05.025

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Abstract

The 2014–2015 Holuhraun eruption in Iceland, emitted ∼11 Tg of SO2 into the troposphere over 6 months, and caused one of the most intense and widespread volcanogenic air pollution events in centuries. This study provides a number of source terms for characterisation of plumes in large fissure eruptions, in Iceland and elsewhere. We characterised the chemistry of aerosol particle matter (PM) and gas in the Holuhraun plume, and its evolution as the plume dispersed, both via measurements and modelling. The plume was sampled at the eruptive vent, and in two populated areas in Iceland. The plume caused repeated air pollution events, exceeding hourly air quality standards (350 μg/m3) for SO2 on 88 occasions in Reykjahlíð town (100 km distance), and 34 occasions in Reykjavík capital area (250 km distance). Average daily concentration of volcanogenic PM sulphate exceeded 5 μg/m3 on 30 days in Reykjavík capital area, which is the maximum concentration measured during non-eruptive background interval. There are currently no established air quality standards for sulphate. Combining the results from direct sampling and dispersion modelling, we identified two types of plume impacting the downwind populated areas. The first type was characterised by high concentrations of both SO2 and S-bearing PM, with a high Sgas/SPM mass ratio (SO2(g)/View the MathML source(PM) > 10). The second type had a low Sgas/SPM ratio (<10). We suggest that this second type was a mature plume where sulphur had undergone significant gas-to-aerosol conversion in the atmosphere. Both types of plume were rich in fine aerosol (predominantly PM1 and PM2.5), sulphate (on average ∼90% of the PM mass) and various trace species, including heavy metals. The fine size of the volcanic PM mass (75–80% in PM2.5), and the high environmental lability of its chemical components have potential adverse implications for environmental and health impacts. However, only the dispersion of volcanic SO2 was forecast in public warnings and operationally monitored during the eruption. We make a recommendation that sulphur gas-to-aerosol conversion processes, and a sufficiently large model domain to contain the transport of a tropospheric plume on the timescale of days be utilized for public health and environmental impact forecasting in future eruptions in Iceland and elsewhere in the world.

Item Type:	Article
Uncontrolled Keywords:	2017AREP; IA72;
Subjects:	05 - Petrology - Igneous, Metamorphic and Volcanic Studies
Divisions:	05 - Petrology - Igneous, Metamorphic and Volcanic Studies 07 - Gold Open Access
Journal or Publication Title:	Earth and Planetary Science Letters
Volume:	472
Page Range:	pp. 309-322
Identification Number:	https://doi.org/10.1016/j.epsl.2017.05.025
Depositing User:	Sarah Humbert
Date Deposited:	12 Jun 2017 10:51
Last Modified:	25 Sep 2017 11:42
URI:	http://eprints.esc.cam.ac.uk/id/eprint/3988

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