The effect of the 2014-15 Bárðarbunga volcanic eruption on chemical denudation rates and the CO2 budget

dc.contributorHáskóli Íslandsen_US
dc.contributorUniversity of Icelanden_US
dc.contributor.authorGaleczka, Iwona
dc.contributor.authorOelkers, Eric H.
dc.contributor.authorGíslason, Sigurður Reynir
dc.contributor.departmentRaunvísindastofnun (HÍ)en_US
dc.contributor.departmentScience Institute (UI)en_US
dc.contributor.schoolVerkfræði- og náttúruvísindasvið (HÍ)en_US
dc.contributor.schoolSchool of Engineering and Natural Sciences (UI)en_US
dc.date.accessioned2020-08-24T11:28:59Z
dc.date.available2020-08-24T11:28:59Z
dc.date.issued2018-07
dc.descriptionPublisher's version (útgefin grein)en_US
dc.description.abstractChemical denudation rates during the 2014–15 Bárðarbunga eruption, calculated using river chemical fluxes, increased substantially confirming that volcanic activity and its products such as fresh lava, and acidic volatiles accelerates these rates. Although the long-term net effect of the combined input of volcanic gases and basalt from the eruption appears to be the overall net drawdown of CO2, it is found that the rapid release of acid gases to surface waters once the basaltic lava comes in contact with surface waters will lead to a short-term release of CO2 from these waters.en_US
dc.description.sponsorshipThis study was funded by Ríkislögreglustjórinn Almannavarnadeild – The National Commissioner of the Icelandic Police, Jarðvísindastofnun Háskólans – Institute of Earth Sciences University of Iceland, Veðurstofa Íslands – IMO, and Rannsóknamiðstöð Íslands – The Icelandic Centre for Research RANNÍS (Grant # 163531-051 and 163531-052). The authors would like to thank to all of those who helped to collect the water samples. We also thank all the colleagues and co-workers from Institute of Earth Sciences and IMO for fruitful discussions during the time of the Bárðarbunga unrest.en_US
dc.description.versionPeer revieweden_US
dc.format.extent53-58en_US
dc.identifier.citationGaleczka, I., Oelkers, E. H., & Gislason, S. R. (2018). The effect of the 2014-15 Bárðarbunga volcanic eruption on chemical denudation rates and the CO2 budget. Energy Procedia, 146, 53-58. doi:https://doi.org/10.1016/j.egypro.2018.07.008en_US
dc.identifier.doi10.1016/j.egypro.2018.07.008
dc.identifier.issn1876-6102
dc.identifier.journalEnergy Procediaen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11815/2005
dc.language.isoenen_US
dc.publisherElsevier BVen_US
dc.relation.ispartofseriesEnergy Procedia;146
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectGeneral Energyen_US
dc.subjectDenudation rateen_US
dc.subjectDissolved fluxen_US
dc.subjectVolcanic eruptionen_US
dc.subjectBárðabungaen_US
dc.subjectEldgosen_US
dc.subjectGosefnien_US
dc.subjectKoltvíoxíðen_US
dc.titleThe effect of the 2014-15 Bárðarbunga volcanic eruption on chemical denudation rates and the CO2 budgeten_US
dc.typeinfo:eu-repo/semantics/articleen_US
dcterms.licenseThis article is available under the Creative Commons CC-BY-NC-ND license and permits non-commercial use of the work as published, without adaptation or alteration provided the work is fully attributed.en_US

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