Cryogenic Cave Pearls In the Periglacial Zones of Ice Caves
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61389005%3A_____%2F13%3A00390419" target="_blank" >RIV/61389005:_____/13:00390419 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985831:_____/13:00390419
Výsledek na webu
<a href="http://dx.doi.org/10.2110/jsr.2013.16" target="_blank" >http://dx.doi.org/10.2110/jsr.2013.16</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2110/jsr.2013.16" target="_blank" >10.2110/jsr.2013.16</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Cryogenic Cave Pearls In the Periglacial Zones of Ice Caves
Popis výsledku v původním jazyce
The Carpathian Mountains across Slovakia and Romania are home of several ice caves located at elevations between 700 and 1,200 m above sea level (asl). Although the mean surface annual temperature is above the freezing point, perennial ice deposits are common in caves and shafts with certain morphologies (large entrances followed by steep vertical or downward-sloping passages), into which the dense cold winter air sinks and remains trapped all year round. A particular type of cave pearls (cryogenic cavepearls, CCPs) occur in spatially restricted accumulations or extensive pearl fields (layers locally up to 0.5 m in thickness) within the scree covering the cave floor in the periglacial zone of these caves. The temperature in the periglacial zone oscillates around the freezing point, promoting seasonal ice formation. A similar type of pearl is observed in the entrance section of other caves that experience temporary freezing conditions during the cold season. When compared to pearls of
Název v anglickém jazyce
Cryogenic Cave Pearls In the Periglacial Zones of Ice Caves
Popis výsledku anglicky
The Carpathian Mountains across Slovakia and Romania are home of several ice caves located at elevations between 700 and 1,200 m above sea level (asl). Although the mean surface annual temperature is above the freezing point, perennial ice deposits are common in caves and shafts with certain morphologies (large entrances followed by steep vertical or downward-sloping passages), into which the dense cold winter air sinks and remains trapped all year round. A particular type of cave pearls (cryogenic cavepearls, CCPs) occur in spatially restricted accumulations or extensive pearl fields (layers locally up to 0.5 m in thickness) within the scree covering the cave floor in the periglacial zone of these caves. The temperature in the periglacial zone oscillates around the freezing point, promoting seasonal ice formation. A similar type of pearl is observed in the entrance section of other caves that experience temporary freezing conditions during the cold season. When compared to pearls of
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GAP210%2F10%2F1760" target="_blank" >GAP210/10/1760: Kryogenní jeskynní karbonáty: mechanismy vzniku a vztah k hloubkovému dosahu permafrostu</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Sedimentary Research
ISSN
1527-1404
e-ISSN
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Svazek periodika
83
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
14
Strana od-do
207-220
Kód UT WoS článku
000317703200014
EID výsledku v databázi Scopus
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