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Next article >> << Previous article Environmental pressure from the 2014–15 eruption of Bárðarbunga volcano, Iceland

2015; Linguagem: Inglês

10.7185/geochemlet.1509

2410-3403

S.R. Gíslason, Gerður Stefánsdóttir, Melissa Pfeffer, Sara Barsotti, Th. Jóhannsson, Iwona Gałeczka, Enikö Bali, Olgeir Sigmarsson, Andri Stefánsson, N.S. Keller, Árni Sigurðsson, Baldur Bergsson, B. Galle, V.C. Jacobo, Santiago Arellano, Alessandro Aiuppa, Elín Björk Jónasdóttir, Eydís Salome Eiríksdóttir, Sigurður Jakobsson, Guðmundur H. Guðfinnsson, Sæmundur A. Halldórsson, Haraldur Gunnarsson, Baptiste Haddadi, Ingibjörg S. Jónsdóttir, T. Thórdarson, Morten S. Riishuus, Þórdís Högnadóttir, Tobias Dürig, Gro B. M. Pedersen, Ármann Hóskuldsson, M. T. Guđmundsson,

Atmospheric chemistry and aerosols

The effusive six months long 2014-2015 Bárðarbunga eruption (31 August-27 February) was the largest in Iceland for more than 200 years, producing 1.6 ± 0.3 km 3 of lava.The total SO 2 emission was 11 ± 5 Mt, more than the amount emitted from Europe in 2011.The ground level concentration of SO 2 exceeded the 350 µg m -3 hourly average health limit over much of Iceland for days to weeks.Anomalously high SO 2 concentrations were also measured at several locations in Europe in September.The lowest pH of fresh snowmelt at the eruption site was 3.3, and 3.2 in precipitation 105 km away from the source.Elevated dissolved H 2 SO 4 , HCl, HF, and metal concentrations were measured in snow and precipitation.Environmental pressures from the eruption and impacts on populated areas were reduced by its remoteness, timing, and the weather.The anticipated primary environmental pressure is on the surface waters, soils, and vegetation of Iceland.