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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;
Karstologia, 1986, Issue 7, p. 21-24
Utilisation de la méthode des traçages pour l'étude des aquifères fissurés en milieu calcaire
Fourneaux J. C. , Sommeria L.
Abstract:
USE OF THE TRACING METHODS TO STUDY THE FISSURED AQUIFERS IN LIMESTONES - The limestones aquifers study by tracing shows the fissured zones, with or without karstic stream channels. Inversely that happens when the tracer is injected in a place in connection with an important drain, the tracer injected anywhere in the aquifer (wells, drill...) will be dispersed in space and in time. The dispersion will be more important especially as the jointing is developed. Analysis of the relation between concentration and time permit often to separate the open-channels flow from the flow in fissured zone. The results presented here come from different multi-tracing operations in limestone areas, in France.
USE OF THE TRACING METHODS TO STUDY THE FISSURED AQUIFERS IN LIMESTONES - The limestones aquifers study by tracing shows the fissured zones, with or without karstic stream channels. Inversely that happens when the tracer is injected in a place in connection with an important drain, the tracer injected anywhere in the aquifer (wells, drill...) will be dispersed in space and in time. The dispersion will be more important especially as the jointing is developed. Analysis of the relation between concentration and time permit often to separate the open-channels flow from the flow in fissured zone. The results presented here come from different multi-tracing operations in limestone areas, in France.