Sulphur release from flood lava eruptions in the Veidivötn, Grímsvötn and Katla volcanic systems, Iceland
Published:January 01, 2003
T. Thordarson, S. Self, D. J. Miller, G. Larsen, E. G. Vilmundardóttir, 2003. "Sulphur release from flood lava eruptions in the Veidivötn, Grímsvötn and Katla volcanic systems, Iceland", Volcanic Degassing, C. Oppenheimer, D. M. Pyle, J. Barclay
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Emissions of SO2 by volcanic eruptions have been shown to be important for short-term environmental and climate changes. Stratospheric sulphur mass-loading by explosive silicic eruption is commonly considered to be the principal forcing factor for these changes. The SO2 emissions from basaltic flood lava eruptions have not featured strongly in the discussions on volcano-climate interactions, notwithstanding the fact that basaltic magma is typically richer in sulphur (by a factor of two to four), than silicic magmas, as well as the evidence of widespread atmospheric impact associated with historical flood lava eruption.
Fourteen Holocene flood lava eruptions are known from the Veidivötn, Grimsvötn, and Katla volcanic systems of the Eastern Volcanic Zone in South Iceland, which include the three largest of its kind in Iceland; the 1783-1784 Laki, 934-40 Eldgjá, and c.8600 years bp Thjórsá events. We present new data on the sulphur content in melt inclusions from the Veidivotn system and use this information, along with existing inclusion data from the Grímsvötn and Katla volcanic systems, to establish an empirical method for estimating the sulphur mass release from these basaltic flood lava eruptions. The results show that these eruptions released a total of c.700 Mt SO2 into the atmosphere in four 600- to 850-year-long eruption periods. During each period, between 98 and 328 Mt SO2 were emitted into the atmosphere, and the mass loadings from individual eruptions ranged from 5 to 210 Mt SO2. These flood lava eruptions are likely to have resulted in widespread atmospheric perturbations and, by analogy with the 1783-1784 Laki eruption, the effects of the largest eruptions may have been felt on a hemispheric scale.
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Humans have long marvelled at (and feared) the odorous and colourful manifestations of volcanic emissions, and, in some cases, have harnessed them for their economic value. The degassing process responsible for these phenomena is now understood to be one of the key factors influencing the timing and nature of volcanic eruptions. Moreover the surface emissions of these volatiles can have profound effects on the atmospheric and terrestrial environment, and climate. Even more fundamental are the relationships between the history of planetary outgassing, differentiation of the Earth’s interior, chemistry of the atmosphere and hydrosphere, and the origin and evolution of life. This book provides a compilation of 23 papers that investigate the behaviour of volatiles in magma, the feedbacks between degassing and magma dynamics, and the composition, flux, and environmental, atmospheric and climatic impacts of volcanic gas emissions.