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KarstBase a bibliography database in karst and cave science.
Featured articles from Cave & Karst Science Journals
Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo
Chemistry and Karst, White, William B.
The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander
Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo
The use of damaged speleothems and in situ fault displacement monitoring to characterise active tectonic structures: an example from Zapadni Cave, Czech Republic , Briestensky, Milos; Stemberk, Josef; Rowberry, Matt D.;
Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
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Simferopol
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Speleology and Karstology, 2011, Issue 7, p. 15-25
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Spatial-dynamic peculiarities of CO2 distribution in the air of Zoloushka Cave
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Andreychouk V. , Teleshman I. , Kouprich P.
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Abstract:
Zoloushka Cave is characterized by relatively high (1-5%) content of ÑÎ2 in its underground atmosphere. The source of ÑÎ2 is the oxidation of organic matter and methane by ammonifying and methane-oxidizing bacteria. The accumulation of carbon dioxide in the cave air is caused by slow air exchange with the surface. The distribution of ÑÎ2 through the cave space has been investigated in August 2008 and 2009 and compared with the CO2 distribution in 1982. The main regularities of ÑÎ2 distribution in the cave are region-by-region increase in CO2 concentrations in the direction from the entrance into depth of cave and the vertical stratification – increase of carbon dioxide content in depressions of cave bottom and shafts. The influence of ÑÎ2 on the working conditions in the cave, on the human body and his mind, is also analyzed. The integral table of safety precautions is proposed, which should be followed when doing of research in the cave
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Keywords: cave microclimate, underground atmosphere, gas composition of air, co2 content
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Link to the original publication
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