Detailed Information on Publication Record
2012
Partial pressures of CO2 in epikarstic zone deduced from hydrogeochemistry of permanent drips, the Moravian Karst, Czech Republic
FAIMON, Jiří, Monika LIČBINSKÁ, Petr ZAJÍČEK and Ondra ŠRÁČEKBasic information
Original name
Partial pressures of CO2 in epikarstic zone deduced from hydrogeochemistry of permanent drips, the Moravian Karst, Czech Republic
Name in Czech
Paciální tlaky CO2 v epikrasu dedukované z hydrogeochemie permanentních skapů, Moravský kras, Česká republika
Authors
FAIMON, Jiří (203 Czech Republic, guarantor, belonging to the institution), Monika LIČBINSKÁ (203 Czech Republic, belonging to the institution), Petr ZAJÍČEK (203 Czech Republic) and Ondra ŠRÁČEK (203 Czech Republic)
Edition
Acta carsologica, Ljubljana, Slovenska akademia znanosti in umetnosti, 2012, 0583-6050
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
Geochemistry
Country of publisher
Slovenia
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 0.542
RIV identification code
RIV/00216224:14310/12:00057407
Organization unit
Faculty of Science
UT WoS
000315422300004
Keywords (in Czech)
cave; carbon dioxide; dripwater; hydrogeochemistry; hypothetical partial pressure; karst processes; karstification model
Keywords in English
cave; carbon dioxide; dripwater; hydrogeochemistry; hypothetical partial pressure; karst processes; karstification model
Tags
International impact, Reviewed
Změněno: 11/4/2013 13:24, Ing. Andrea Mikešková
V originále
Permanent drips from straw stalactites of selected caves of the Moravian Karst were studied during one-year period. A hypothetical partial pressure of CO2 that has participated in limestone dissolution, PCO2(H)=10^-1.53+-0.04, was calculated from the dripwater chemistry. The value significantly exceeds the partial pressures generally measured in relevant shallow karst soils, PCO2(soil)=10-2.72+-0.02. This finding may have important implications for karst/cave conservation and paleoenvironmental reconstructions.
In Czech
Permanent drips from straw stalactites of selected caves of the Moravian Karst were studied during one-year period. A hypothetical partial pressure of CO2 that has participated in limestone dissolution, PCO2(H)=10^-1.53+-0.04, was calculated from the dripwater chemistry. The value significantly exceeds the partial pressures generally measured in relevant shallow karst soils, PCO2(soil)=10-2.72+-0.02. This finding may have important implications for karst/cave conservation and paleoenvironmental reconstructions.
Links
| GA205/03/1128, research and development project |
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