Mineralogical and Chemical Records of Icelandic Dust Sources upon Ny-Alesund (Svalbard Islands)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F18%3A77032" target="_blank" >RIV/60460709:41330/18:77032 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.3389/feart.2018.00187" target="_blank" >http://dx.doi.org/10.3389/feart.2018.00187</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3389/feart.2018.00187" target="_blank" >10.3389/feart.2018.00187</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Mineralogical and Chemical Records of Icelandic Dust Sources upon Ny-Alesund (Svalbard Islands)
Popis výsledku v původním jazyce
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-Alesund station. We characterized representative sediment samples from Iceland and Svalbard and compared them to a set of aerosol samples collected in Ny-Alesund 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 magne
Název v anglickém jazyce
Mineralogical and Chemical Records of Icelandic Dust Sources upon Ny-Alesund (Svalbard Islands)
Popis výsledku anglicky
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-Alesund station. We characterized representative sediment samples from Iceland and Svalbard and compared them to a set of aerosol samples collected in Ny-Alesund 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 magne
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Frontiers in Earth Sciences
ISSN
1863-4621
e-ISSN
—
Svazek periodika
6
Číslo periodika v rámci svazku
UNSP 187
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
29
Strana od-do
1-29
Kód UT WoS článku
000454082700001
EID výsledku v databázi Scopus
2-s2.0-85057087359