dc.contributor.author | Vogel, Andreas | |
dc.contributor.author | Diplas, Spyridon | |
dc.contributor.author | Durant, Adam | |
dc.contributor.author | Azar, Amin Shahrestani | |
dc.contributor.author | Sunding, Martin Fleissner | |
dc.contributor.author | Rose, William I. | |
dc.contributor.author | Sytchkova, Anna Krasilnikova | |
dc.contributor.author | Bonadonna, Costanza | |
dc.contributor.author | Krüger, Kirstin | |
dc.contributor.author | Stohl, Andreas | |
dc.date.accessioned | 2020-12-14T12:41:03Z | |
dc.date.available | 2020-12-14T12:41:03Z | |
dc.date.created | 2017-11-29T12:29:12Z | |
dc.date.issued | 2017 | |
dc.identifier.citation | Journal of Geophysical Research - Atmospheres. 2017, 122 9485-9514. | en_US |
dc.identifier.issn | 2169-897X | |
dc.identifier.uri | https://hdl.handle.net/11250/2719194 | |
dc.description.abstract | Uncertainty in the physicochemical and optical properties of volcanic ash particles creates errors in the detection and modeling of volcanic ash clouds and in quantification of their potential impacts. In this study, we provide a data set that describes the physicochemical and optical properties of a representative selection of volcanic ash samples from nine different volcanic eruptions covering a wide range of silica contents (50–80 wt % SiO2). We measured and calculated parameters describing the physical (size distribution, complex shape, and dense‐rock equivalent mass density), chemical (bulk and surface composition), and optical (complex refractive index from ultraviolet to near‐infrared wavelengths) properties of the volcanic ash and classified the samples according to their SiO2 and total alkali contents into the common igneous rock types basalt to rhyolite. We found that the mass density ranges between ρ = 2.49 and 2.98 g/cm3 for rhyolitic to basaltic ash types and that the particle shape varies with changing particle size (d < 100 μm). The complex refractive indices in the wavelength range between λ = 300 nm and 1500 nm depend systematically on the composition of the samples. The real part values vary from n = 1.38 to 1.66 depending on ash type and wavelength and the imaginary part values from k = 0.00027 to 0.00268. We place our results into the context of existing data and thus provide a comprehensive data set that can be used for future and historic eruptions, when only basic information about the magma type producing the ash is known. | en_US |
dc.language.iso | eng | en_US |
dc.publisher | Wiley | en_US |
dc.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/deed.no | * |
dc.subject | complex shape | en_US |
dc.subject | dense‐rock equivalent mass density | en_US |
dc.subject | chemical composition | en_US |
dc.subject | complex refractive index | en_US |
dc.subject | volcanic ash properties | en_US |
dc.title | Reference data set of volcanic ash physicochemical and optical properties | en_US |
dc.type | Peer reviewed | en_US |
dc.type | Journal article | en_US |
dc.description.version | publishedVersion | en_US |
dc.rights.holder | ©2017. The Authors.This is an open access article under the terms of the Creative Commons Attribution-NonCommercial NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. | en_US |
dc.source.pagenumber | 9485-9514 | en_US |
dc.source.volume | 122 | en_US |
dc.source.journal | Journal of Geophysical Research - Atmospheres | en_US |
dc.source.issue | 17 | en_US |
dc.identifier.doi | 10.1002/2016JD026328 | |
dc.identifier.cristin | 1520167 | |
dc.relation.project | EC/FP7/607905 | en_US |
dc.relation.project | Nordforsk: 57001 | en_US |
cristin.unitcode | 7401,80,6,2 | |
cristin.unitname | Materialfysikk. Oslo | |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 2 | |