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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.;
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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;
SAZU, Ljubljana
Acta carsologica, 1999, Vol 28, Issue 1, p. 161-198
New knowledge about the underground water drainage in the Northern part of Javorniki Mountains (High Karst)
Kogovš, Ek Janja
Abstract:
In spring 1997 during low waters the water tracing test on PoËek, NE part of Javorniki, established directions, velocities and rates of fluorescent dye Uranin. The most direct connections were shown to be towards MalenźËica spring (0.72 cm/s in the first tracing pulse) and seasonal Škratovka spring (0.76 cm/s), both on Planinsko Polje, and towards Vipava spring (0.72 cm/s). The appearance of Uranin in the underground Pivka in Planinska Jama was recorded as well as in Rak, Prunkovec and KotliËi springs in Rakov Škocjan. The drainage velocities of these directions were slightly lower. The slowest drainage (0.29 cm/s) appeared in the direction to Strćen spring near Stara Vas. The MalenźËica drained 55%, and the Vipava 26% of injected tracer from PoËek. The total quantity of returned Uranin is estimated to be near 100%.
In spring 1997 during low waters the water tracing test on PoËek, NE part of Javorniki, established directions, velocities and rates of fluorescent dye Uranin. The most direct connections were shown to be towards MalenźËica spring (0.72 cm/s in the first tracing pulse) and seasonal Škratovka spring (0.76 cm/s), both on Planinsko Polje, and towards Vipava spring (0.72 cm/s). The appearance of Uranin in the underground Pivka in Planinska Jama was recorded as well as in Rak, Prunkovec and KotliËi springs in Rakov Škocjan. The drainage velocities of these directions were slightly lower. The slowest drainage (0.29 cm/s) appeared in the direction to Strćen spring near Stara Vas. The MalenźËica drained 55%, and the Vipava 26% of injected tracer from PoËek. The total quantity of returned Uranin is estimated to be near 100%.