Volcanic ash particulate matter from the 2010 Eyjafjallajokull eruption in dust deposition at Prague, central Europe

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10173788" target="_blank" >RIV/00216208:11310/13:10173788 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985831:_____/13:00392114

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.aeolia.2012.12.002" target="_blank" >http://dx.doi.org/10.1016/j.aeolia.2012.12.002</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.aeolia.2012.12.002" target="_blank" >10.1016/j.aeolia.2012.12.002</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Volcanic ash particulate matter from the 2010 Eyjafjallajokull eruption in dust deposition at Prague, central Europe

Popis výsledku v původním jazyce

Particles originating from the last major Eyjafjallajökull volcano eruption in April 2010 were subsequently found in settled dust samples collected in a suburban area of Prague, Czech Republic. These dust samples contained predominantly non-volcanic particulate matter of super-regional but mainly local origin. The highest proportion of the Eyjafjallajökull material recorded in the Prague daily dust samples reached 12% of the total lithic component mass. Volcanogenic particles, mostly glasses, were concentrated in particle size classes from 2.5 to 25 ?m, but rare fragments of volcanic glasses up to 50 ?m in diameter were also found. The most effective method for detection and identification of the volcanic ash particles were morpho-textural observationscombined with energy dispersive and wavelength dispersive analysis of individual grains and X-ray powder diffraction. Because of the low percentage of volcanic ash particles in the total samples, the geochemical signal was rather weak al

Název v anglickém jazyce

Volcanic ash particulate matter from the 2010 Eyjafjallajokull eruption in dust deposition at Prague, central Europe

Popis výsledku anglicky

Particles originating from the last major Eyjafjallajökull volcano eruption in April 2010 were subsequently found in settled dust samples collected in a suburban area of Prague, Czech Republic. These dust samples contained predominantly non-volcanic particulate matter of super-regional but mainly local origin. The highest proportion of the Eyjafjallajökull material recorded in the Prague daily dust samples reached 12% of the total lithic component mass. Volcanogenic particles, mostly glasses, were concentrated in particle size classes from 2.5 to 25 ?m, but rare fragments of volcanic glasses up to 50 ?m in diameter were also found. The most effective method for detection and identification of the volcanic ash particles were morpho-textural observationscombined with energy dispersive and wavelength dispersive analysis of individual grains and X-ray powder diffraction. Because of the low percentage of volcanic ash particles in the total samples, the geochemical signal was rather weak al

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DD - Geochemie

OECD FORD obor

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Projekt

<a href="/cs/project/IAAX00130702" target="_blank" >IAAX00130702: Hydrodynamické pojetí tvorby stromataktů v geologii</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Aeolian Research

ISSN

1875-9637

e-ISSN

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Svazek periodika

9

Číslo periodika v rámci svazku

JUNE

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

12

Strana od-do

191-202

Kód UT WoS článku

000319632500016

EID výsledku v databázi Scopus

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