FAIMON, Jiří, Monika LIČBINSKÁ, Petr ZAJÍČEK and Ondra ŠRÁČEK. Partial pressures of CO2 in epikarstic zone deduced from hydrogeochemistry of permanent drips, the Moravian Karst, Czech Republic (deduced from hydrogeochemistry of permanent drips, the Moravian Karst, Czech Republic). Acta carsologica. Ljubljana: Slovenska akademia znanosti in umetnosti, 2012, 41/2012, No 1, p. 47-57. ISSN 0583-6050.
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Basic 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
Original language English
Type of outcome Article in a journal
Field of Study Geochemistry
Country of publisher Slovenia
Confidentiality degree is not subject to a state or trade secret
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 AKR, rivok
Tags International impact, Reviewed
Changed by Changed by: Ing. Andrea Mikešková, učo 137293. Changed: 11/4/2013 13:24.
Abstract
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.
Abstract (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 projectName: Recentní krasové procesy: destrukce speleotém
Investor: Czech Science Foundation, Recent karst processes: speleothem destruction
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