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

Result code in 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>
Alternative codes found
RIV/67985831:_____/13:00392114
Result on the web
<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>

Result language
angličtina
Original language name
Volcanic ash particulate matter from the 2010 Eyjafjallajokull eruption in dust deposition at Prague, central Europe
Original language description
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
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DD - Geochemistry
OECD FORD branch
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Project
<a href="/en/project/IAAX00130702" target="_blank" >IAAX00130702: Hydrodynamic concept of stromatactis formation in geology</a><br>
Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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