Cave Rock Surface Temperature Evaluation Using Non-Contact Measurement Methods
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F14%3A33152494" target="_blank" >RIV/61989592:15310/14:33152494 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/62156489:43210/14:00230785
Výsledek na webu
<a href="http://dx.doi.org/10.3986/ac.v43i2.646" target="_blank" >http://dx.doi.org/10.3986/ac.v43i2.646</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3986/ac.v43i2.646" target="_blank" >10.3986/ac.v43i2.646</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Cave Rock Surface Temperature Evaluation Using Non-Contact Measurement Methods
Popis výsledku v původním jazyce
The aim of this study was to evaluate the rock surface temperature (RST) regime in Kateřinská Cave in the Moravian Karst (Czech Republic, South Moravia) using nondestructive infrared methods. Air temperature monitoring was also included to quantify the dominant factors affecting the RST. Measurements were taken during the period covering January, 2010 to March, 2012. HOBO air temperature sensors with data loggers were placed in front of the cave entrance, in the entrance corridor and on selected sites in the cave interior. An infrared (IR) the solid rock. The RST in the cave interior during each season was also recorded by IR camera. The average temperature of the rock surface over the two year period was 6.95 °C. The longterm average of the RST was always 0.01 to 0.79 °C lower than the air temperature. The dynamics of the RST are most obvious at the entrance corridor to the cave, with temperature variability up to 17.34 °C. The dynamism of both the RST and air temperature decrease as
Název v anglickém jazyce
Cave Rock Surface Temperature Evaluation Using Non-Contact Measurement Methods
Popis výsledku anglicky
The aim of this study was to evaluate the rock surface temperature (RST) regime in Kateřinská Cave in the Moravian Karst (Czech Republic, South Moravia) using nondestructive infrared methods. Air temperature monitoring was also included to quantify the dominant factors affecting the RST. Measurements were taken during the period covering January, 2010 to March, 2012. HOBO air temperature sensors with data loggers were placed in front of the cave entrance, in the entrance corridor and on selected sites in the cave interior. An infrared (IR) the solid rock. The RST in the cave interior during each season was also recorded by IR camera. The average temperature of the rock surface over the two year period was 6.95 °C. The longterm average of the RST was always 0.01 to 0.79 °C lower than the air temperature. The dynamics of the RST are most obvious at the entrance corridor to the cave, with temperature variability up to 17.34 °C. The dynamism of both the RST and air temperature decrease as
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Acta Carsologica
ISSN
0583-6050
e-ISSN
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Svazek periodika
43
Číslo periodika v rámci svazku
2-3
Stát vydavatele periodika
SI - Slovinská republika
Počet stran výsledku
12
Strana od-do
257-268
Kód UT WoS článku
000348504700005
EID výsledku v databázi Scopus
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