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Mineralogical and Chemical Records of Icelandic Dust Sources Upon Ny-Ålesund (Svalbard Islands)

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dc.contributor Landbúnaðarháskóli Íslands
dc.contributor Agricultural University of Iceland
dc.contributor.author Moroni, Beatrice
dc.contributor.author Arnalds, Olafur
dc.contributor.author Dagsson-Waldhauserova, Pavla
dc.contributor.author Crocchianti, Stefano
dc.contributor.author Vivani, Riccardo
dc.contributor.author Cappelletti, David
dc.date.accessioned 2019-01-15T11:50:37Z
dc.date.available 2019-01-15T11:50:37Z
dc.date.issued 2018-11-05
dc.identifier.citation Moroni, B., Arnalds, O., Dagsson-Waldhauserova, P., Crocchianti, S., Vivani, R., & Cappelletti, D. (2018). Mineralogical and Chemical Records of Icelandic Dust Sources upon Ny-Ålesund (Svalbard Islands). Frontiers in Earth Science, 6, 187.
dc.identifier.issn 2296-6463
dc.identifier.uri https://hdl.handle.net/20.500.11815/979
dc.description.abstract This work aims to identify the geochemical and mineralogical markers of Icelandic dust and to differentiate it from the dust of local origin deposited at the Ny-Ålesund station. We characterized representative sediment samples from Iceland and Svalbard and compared them to a set of aerosol samples collected in Ny-Ålesund to check the existence and type of the mineralogical markers. The sediment samples were analyzed by X-ray diffraction (XRD) to detect the mineralogical constrain of the geochemical markers. Both aerosol and sediment samples were examined by scanning electron microscopy coupled with EDS microanalysis (SEM-EDS) and image analysis to detect and to provide a morpho-chemical characterization of the mineralogical markers of dust provenance. Comparison between local and Icelandic sediments reveals the metal oxide particles as the most representative and distinguishing mineralogical/phase markers for Iceland dust sources. In particular, we have considered the magnetite-chromite and the magnetite-ülvospinel associations as marker facies of the tholeiitic magmatic series and the presence of volcanic glass as a further indicator of provenance from Iceland. The morphochemical characteristics of the metal oxide particles in the aerosol samples compared to those of the sediment samples have proved to be a powerful tool to separate Icelandic dust from other sources for dust. In particular, the small size, higher grain boundary complexity and lower Fe/Cr ratios suggest the influence of anthropogenic sources, well in accordance with the results of air mass backward trajectories which reveal a main contribution from industrialized areas in Eurasia. This study shows the reliability of the geochemical characterization of the metal oxide particles for the identification of the source regions of dust. In addition it provides an evidence that Icelandic dust can be transported long range to Svalbard confirming the importance of High Latitude Dust sources. © 2018 Moroni, Arnalds, Dagsson-Waldhauserová, Crocchianti, Vivani and Cappelletti.
dc.description.sponsorship OA and PD-W was funded by the Icelandic Research Fund (Rannis) Grant No. 152248-051 and supported by Vinir Vatnajokuls. DC, BM, and SC was funded by the project SIDDARTA (CUP project id: I52F17001230001).
dc.format.extent 6:187
dc.language.iso en
dc.publisher Frontiers Media SA
dc.relation.ispartofseries Frontiers in Earth Science;2018(6)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Arctic region
dc.subject Atmospheric aerosol
dc.subject Mineral chemistry
dc.subject Soil erosion
dc.subject Jarðvegseyðing
dc.subject Veðrun
dc.title Mineralogical and Chemical Records of Icelandic Dust Sources Upon Ny-Ålesund (Svalbard Islands)
dc.type info:eu-repo/semantics/article
dc.description.version Peer Reviewed
dc.identifier.journal Frontiers in Earth Science
dc.identifier.doi 10.3389/feart.2018.00187
dc.relation.url https://www.frontiersin.org/article/10.3389/feart.2018.00187/full
dc.contributor.department Auðlinda- og umhverfisdeild (LBHÍ)
dc.contributor.department Faculty of Natural Resources and Environmental Sciences (AUI)


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