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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F04%3A00103874%21RIV%2F2005%2FGA0%2FA09005%2FN
rdf:type
n7:Vysledek skos:Concept
dcterms:description
Cryogenic cave calcite (CCC), formed by segregation of solutes during water freezing, was found in three Central European caves. This calcite type forms accumulation of loose calcite grains on cave floor. Detailed C and O stable isotope study of CCC samples revealed that slow water freezing under isotope equilibrium was the dominant formational process in the studied Polish and Czech caves. Significantly higher ?13C values of CCC in the Stratenská Jaskyňa Cave indicate either water freezing in a more opened systém with continuous CO 2 escape (Rayleigh fractional separation(, or partipation of another CO 2 source. The model of slow water freezing under isotope equilibrium is supported by isolated character of the caves having limited ventilation. Cryogenic cave calcite (CCC), formed by segregation of solutes during water freezing, was found in three Central European caves. This calcite type forms accumulation of loose calcite grains on cave floor. Detailed C and O stable isotope study of CCC samples revealed that slow water freezing under isotope equilibrium was the dominant formational process in the studied Polish and Czech caves. Significantly higher ?13C values of CCC in the Stratenská Jaskyňa Cave indicate either water freezing in a more opened systém with continuous CO 2 escape (Rayleigh fractional separation(, or partipation of another CO 2 source. The model of slow water freezing under isotope equilibrium is supported by isolated character of the caves having limited ventilation. V několika jeskyních byly objeveny neobvyklé formy kalcitu, který vzniká vymrzáním z krasových roztoků v podmínkách poslední ledové doby. Nálezy indikují klimatické změny v posledních 100 tisíci letech
dcterms:title
Cryogenic cave calcite from several Central European caves: age, carbon and a genetic model Cryogenic cave calcite from several Central European caves: age, carbon and a genetic model Kryogenní formy kalcitu z několika středoevropských jeskyní: původ, stáří a genetický model
skos:prefLabel
Cryogenic cave calcite from several Central European caves: age, carbon and a genetic model Cryogenic cave calcite from several Central European caves: age, carbon and a genetic model Kryogenní formy kalcitu z několika středoevropských jeskyní: původ, stáří a genetický model
skos:notation
RIV/67985831:_____/04:00103874!RIV/2005/GA0/A09005/N
n3:strany
119;136
n3:aktivita
n16:P
n3:aktivity
P(GA205/02/0449)
n3:cisloPeriodika
-
n3:dodaniDat
n12:2005
n3:domaciTvurceVysledku
n13:5557585
n3:druhVysledku
n17:J
n3:duvernostUdaju
n11:S
n3:entitaPredkladatele
n10:predkladatel
n3:idSjednocenehoVysledku
559024
n3:idVysledku
RIV/67985831:_____/04:00103874
n3:jazykVysledku
n4:eng
n3:klicovaSlova
cryogenic calcite;periglacial zone
n3:klicoveSlovo
n14:cryogenic%20calcite n14:periglacial%20zone
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[B8E74486D628]
n3:nazevZdroje
Chemical Geology
n3:obor
n5:DB
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
4
n3:projekt
n15:GA205%2F02%2F0449
n3:rokUplatneniVysledku
n12:2004
n3:svazekPeriodika
206
n3:tvurceVysledku
Žák, K. Urban, J. Cílek, Václav Hercman, H.
s:issn
0009-2541
s:numberOfPages
18