Seasonal variations of water condensation in cave environment: A case study from the Výpustek Cave (Moravian Karst)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F25%3A00142989" target="_blank" >RIV/00216224:14310/25:00142989 - isvavai.cz</a>

Výsledek na webu

<a href="https://journals.muni.cz/gvms/article/view/40916" target="_blank" >https://journals.muni.cz/gvms/article/view/40916</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5817/GVMS2025-40916" target="_blank" >10.5817/GVMS2025-40916</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Seasonal variations of water condensation in cave environment: A case study from the Výpustek Cave (Moravian Karst)

Popis výsledku v původním jazyce

Seasonal variations of water condensation were studied in the Výpustek Cave (Moravian Karst). Microclimatic data such as cave/external air temperatures and visitor numbers were monitored in the Škrapový Dome and exterior of the cave with one-hour step during an almost season-long monitoring campaign. Water condensation data were recorded at monthly intervals using a polished limestone tablet located in a dome near the thermometers. Long-term monitoring showed that the temperature of the cave air was controlled by cave airflow driven by the temperature difference between the exterior and the cave, DTAF. Anthropogenic temperature influence appeared as peaks superimposed onto natural cave air temperatures curves and corresponded to the number of visitors. Seasonality of wate condensation based on cave airflow was identified: no condensation during the UAF mode and drops of condensed water on the tablet surface in the DAF mode. Traces of calcite recrystallization were found on the tablet surface as a consequence of dissolution by the condensed water.

Název v anglickém jazyce

Seasonal variations of water condensation in cave environment: A case study from the Výpustek Cave (Moravian Karst)

Popis výsledku anglicky

Seasonal variations of water condensation were studied in the Výpustek Cave (Moravian Karst). Microclimatic data such as cave/external air temperatures and visitor numbers were monitored in the Škrapový Dome and exterior of the cave with one-hour step during an almost season-long monitoring campaign. Water condensation data were recorded at monthly intervals using a polished limestone tablet located in a dome near the thermometers. Long-term monitoring showed that the temperature of the cave air was controlled by cave airflow driven by the temperature difference between the exterior and the cave, DTAF. Anthropogenic temperature influence appeared as peaks superimposed onto natural cave air temperatures curves and corresponded to the number of visitors. Seasonality of wate condensation based on cave airflow was identified: no condensation during the UAF mode and drops of condensed water on the tablet surface in the DAF mode. Traces of calcite recrystallization were found on the tablet surface as a consequence of dissolution by the condensed water.

Druh

J_SC - Článek v periodiku v databázi SCOPUS

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2025

Kód důvěrnosti údajů

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

Název periodika

Geologické výzkumy na Moravě a ve Slezsku

ISSN

1212-6209

e-ISSN

2336-4378

Svazek periodika

32

Číslo periodika v rámci svazku

1-2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

8

Strana od-do

70-77

Kód UT WoS článku

—

EID výsledku v databázi Scopus

2-s2.0-105028884171