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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F06%3A00015855%21RIV08-GA0-14310___
rdf:type
skos:Concept n17:Vysledek
dcterms:description
Comparing the CO2-peaks at staying of persons in cave with cave drip water chemistry suggests that cave CO2 do not reach the concentrations, at which both the carbonate species in drip water and in cave air are in equilibrium. Under given conditions, the drip waters will continue (1) in further CO2-degassing and (2) in increasing of the current supersaturation. The threshold values, at which water would became aggressive with respect to calcite, log pCO2[soil] about -2, were not reached. Generally, a reversion of speleothem growth into speleothem dissolution by human breath impact is highly improbable; it would need really extreme conditions. Comparing the CO2-peaks at staying of persons in cave with cave drip water chemistry suggests that cave CO2 do not reach the concentrations, at which both the carbonate species in drip water and in cave air are in equilibrium. Under given conditions, the drip waters will continue (1) in further CO2-degassing and (2) in increasing of the current supersaturation. The threshold values, at which water would became aggressive with respect to calcite, log pCO2[soil] about -2, were not reached. Generally, a reversion of speleothem growth into speleothem dissolution by human breath impact is highly improbable; it would need really extreme conditions. Comparing the CO2-peaks at staying of persons in cave with cave drip water chemistry suggests that cave CO2 do not reach the concentrations, at which both the carbonate species in drip water and in cave air are in equilibrium. Under given conditions, the drip waters will continue (1) in further CO2-degassing and (2) in increasing of the current supersaturation. The threshold values, at which water would became aggressive with respect to calcite, log pCO2[soil] about -2, were not reached. Generally, a reversion of speleothem growth into speleothem dissolution by human breath impact is highly improbable; it would need really extreme conditions.
dcterms:title
Environmentální vlivy antropogenních toků CO2 v Císařské jeskyni (Moravský kras, Česká republika) Environmentální vlivy antropogenních toků CO2 v Císařské jeskyni (Moravský kras, Česká republika) An environmental impact of antropogennic CO2-fluxes in the Císařská Cave (Moravian Karst, Czech Republic)
skos:prefLabel
Environmentální vlivy antropogenních toků CO2 v Císařské jeskyni (Moravský kras, Česká republika) Environmentální vlivy antropogenních toků CO2 v Císařské jeskyni (Moravský kras, Česká republika) An environmental impact of antropogennic CO2-fluxes in the Císařská Cave (Moravian Karst, Czech Republic)
skos:notation
RIV/00216224:14310/06:00015855!RIV08-GA0-14310___
n4:strany
151-155
n4:aktivita
n9:P
n4:aktivity
P(GA205/03/1128)
n4:dodaniDat
n19:2008
n4:domaciTvurceVysledku
n5:1131664 n5:6717373 n5:1742167
n4:druhVysledku
n13:D
n4:duvernostUdaju
n20:S
n4:entitaPredkladatele
n7:predkladatel
n4:idSjednocenehoVysledku
474312
n4:idVysledku
RIV/00216224:14310/06:00015855
n4:jazykVysledku
n16:cze
n4:klicovaSlova
atmosphere; carbon dioxide; cave; dissolution; dripwater; flux; growth; speleothem
n4:klicoveSlovo
n8:flux n8:dissolution n8:speleothem n8:dripwater n8:atmosphere n8:growth n8:cave n8:carbon%20dioxide
n4:kontrolniKodProRIV
[3DFE19ED0011]
n4:mistoKonaniAkce
Demänovská Dolina
n4:mistoVydani
Liptovský Mikuláš
n4:nazevZdroje
Výskum, využívanie a ochrana jaskýň. 5. vedecká konferencia s medzinárodnou účsťou, zborník referátov
n4:obor
n18:DD
n4:pocetDomacichTvurcuVysledku
3
n4:pocetTvurcuVysledku
3
n4:projekt
n21:GA205%2F03%2F1128
n4:rokUplatneniVysledku
n19:2006
n4:tvurceVysledku
Faimon, Jiří Štelcl, Jindřich Sas, Daniel
n4:typAkce
n15:EUR
n4:zahajeniAkce
2005-09-26+02:00
s:numberOfPages
5
n10:hasPublisher
Správa slovenský jaskýň, Slovenské múzeum ochrany prírody, Slovenská speleologická společnosť, Asociácia slovenských geomorfológov pri SAV
n14:isbn
80-8064-263-X
n6:organizacniJednotka
14310