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  • Anthropogenic CO2-flux in The Nagel Dome (Císařská Cave) was determined to be +8.5 ppm per man and hour. Relaxation rate of the cave was found to be -21 ppm per hour. In the Moravian Karts caves opened to public, huge accumulation of CO2 was observed in summer months. This accumulation as if related to increasing number of cave visitors. However, CO2-concentrations were not distributed uniformly across the caves. They fluctuated depending on cave specific sites. Moreover, extremely high CO2-accumulation was found in the Amatérská Cave. This cave, however, was not opened to public. Based on these findings, natural CO2-fluxes into speleoatmosphere were estimated as dominant.
  • Anthropogenic CO2-flux in The Nagel Dome (Císařská Cave) was determined to be +8.5 ppm per man and hour. Relaxation rate of the cave was found to be -21 ppm per hour. In the Moravian Karts caves opened to public, huge accumulation of CO2 was observed in summer months. This accumulation as if related to increasing number of cave visitors. However, CO2-concentrations were not distributed uniformly across the caves. They fluctuated depending on cave specific sites. Moreover, extremely high CO2-accumulation was found in the Amatérská Cave. This cave, however, was not opened to public. Based on these findings, natural CO2-fluxes into speleoatmosphere were estimated as dominant. (en)
  • Anthropogenic CO2-flux in The Nagel Dome (Císařská Cave) was determined to be +8.5 ppm per man and hour. Relaxation rate of the cave was found to be -21 ppm per hour. In the Moravian Karts caves opened to public, huge accumulation of CO2 was observed in summer months. This accumulation as if related to increasing number of cave visitors. However, CO2-concentrations were not distributed uniformly across the caves. They fluctuated depending on cave specific sites. Moreover, extremely high CO2-accumulation was found in the Amatérská Cave. This cave, however, was not opened to public. Based on these findings, natural CO2-fluxes into speleoatmosphere were estimated as dominant. (cs)
Title
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere (en)
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere (cs)
skos:prefLabel
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere (en)
  • Natural and anthropogenic impacts of CO2 into speleoatmosphere (cs)
skos:notation
  • RIV/00216224:14310/04:00019774!RIV08-GA0-14310___
http://linked.open.../vavai/riv/strany
  • 110-112
http://linked.open...avai/riv/aktivita
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  • P(GA205/03/1128)
http://linked.open...vai/riv/dodaniDat
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  • 575467
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  • RIV/00216224:14310/04:00019774
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  • carbon dioxide; fluxes; speleoatmosphere; cave; Moravian Karst (en)
http://linked.open.../riv/klicoveSlovo
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  • [5DA93B94D661]
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  • Tále
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  • Liptovský Mikuláš
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  • Výskum, využívanie a ochrana jaskýň
http://linked.open...in/vavai/riv/obor
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Faimon, Jiří
  • Štelcl, Jindřich
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
number of pages
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  • Správa slov. jaskýň
https://schema.org/isbn
  • 80-8064-201-X
http://localhost/t...ganizacniJednotka
  • 14310
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