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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.;
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;
SAZU, Ljubljana
Acta carsologica, 1999, Vol 28, Issue 2, p. 241-253
Water tracing test in the Tianshengan region, China at low water level in November 1998
Kogovš, Ek Janja, Hong Liu
Abstract:
In 1998 a water tracing test at low water level was carried out within the international scientific co-operation between Slovenia and China in the Tianshengan region, Yunnan. This water tracing completed the knowledge achieved by water tracing during middle and high water level that was reached by water tracing tests in 1996 and 1997. From the injection point d towards the final Dalongtan spring the water drainage at low water level was three times slower than at middle water level. The water tracing also showed that water does not flow towards the spring 11 south-west from the injection point near the Shibanshou fault which remained an open question from previous water tracing tests.
In 1998 a water tracing test at low water level was carried out within the international scientific co-operation between Slovenia and China in the Tianshengan region, Yunnan. This water tracing completed the knowledge achieved by water tracing during middle and high water level that was reached by water tracing tests in 1996 and 1997. From the injection point d towards the final Dalongtan spring the water drainage at low water level was three times slower than at middle water level. The water tracing also showed that water does not flow towards the spring 11 south-west from the injection point near the Shibanshou fault which remained an open question from previous water tracing tests.