Transfer of climatic variables by dripwater: a case study from Kateřinská Cave (Moravian Karst)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F16%3A00090876" target="_blank" >RIV/00216224:14310/16:00090876 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/61989592:15310/16:33160210
Výsledek na webu
<a href="http://doi.org/10.1007/s12665-016-5982-x" target="_blank" >http://doi.org/10.1007/s12665-016-5982-x</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s12665-016-5982-x" target="_blank" >10.1007/s12665-016-5982-x</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Transfer of climatic variables by dripwater: a case study from Kateřinská Cave (Moravian Karst)
Popis výsledku v původním jazyce
Hydrogeochemical properties of drips in Kateřinská Cave (Moravian Karst) were studied with focus on their relation to climatic variables, especially rainfall and temperature. The discharges of two drips (marked as meteorologically sensitive drips) showed statistically significant positive correlations with rainfalls with lag of -5 and -2 days. In addition, the discharges showed statistically significant positive correlations with specific electrical conductivity, pH, and supersaturation with respect to calcite. Other drips in the same cave (marked as meteorologically insensitive drips) did not show this correlation. Because the climatic conditions are identical, the drip types must differ in their reaction/flow paths. It indicates that the paths may control some proxies possibly preserved in speleothems, which should be taken into consideration for paleoenvironmental reconstructions.
Název v anglickém jazyce
Transfer of climatic variables by dripwater: a case study from Kateřinská Cave (Moravian Karst)
Popis výsledku anglicky
Hydrogeochemical properties of drips in Kateřinská Cave (Moravian Karst) were studied with focus on their relation to climatic variables, especially rainfall and temperature. The discharges of two drips (marked as meteorologically sensitive drips) showed statistically significant positive correlations with rainfalls with lag of -5 and -2 days. In addition, the discharges showed statistically significant positive correlations with specific electrical conductivity, pH, and supersaturation with respect to calcite. Other drips in the same cave (marked as meteorologically insensitive drips) did not show this correlation. Because the climatic conditions are identical, the drip types must differ in their reaction/flow paths. It indicates that the paths may control some proxies possibly preserved in speleothems, which should be taken into consideration for paleoenvironmental reconstructions.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DD - Geochemie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Environmental Geology (Environmental Earth Sciences)
ISSN
1866-6280
e-ISSN
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Svazek periodika
75
Číslo periodika v rámci svazku
16
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
16
Strana od-do
"nestrankovano"
Kód UT WoS článku
000381986800001
EID výsledku v databázi Scopus
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