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Enviroscan Ukrainian Institute of Speleology and Karstology

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Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

New publications on hypogene speleogenesis

Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,

The deepest terrestrial animal

Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found: Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...

Caves - landscapes without light

akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum   The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...

Did you know?

That temperature efficiency is an efficiency factor defined by thornthwaite for different climates. see also thornthwaite.?

Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms

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Browse Speleogenesis Issues:

KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
See all featured articles
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;
See all featured articles from other geoscience journals

Journal of Cave and Karst Studies, 2008, Vol 70, Issue 1, p. 62-70
Ground-water storage calculation in karst aquifers with alluvium or no-flow boundaries
The determination of water-budget parameters, such as change in storage and subsurface inflow and outflow, is costly and unreliable due to heterogeneities of karst aquifers. Some karst aquifers may have one or a combination of boundaries such as impermeable formations, alluvial aquifers, and known ground-water divides. Karst water only discharges through springs or flows to the adjacent alluvium. A new procedure is proposed to estimate volume of storage in region during the dry season in these settings. The subsurface inflow and outflow can be measured in the adjacent alluvium using equipotential and flow lines, cross-sectional area, and transmissivity of the alluvial aquifer. The dry season makes it possible to calculate the karst spring recession coefficient and karst aquifer dynamic volume at the beginning and end of the hydrological year. The change of storage is the difference between the dynamic volumes of the karst aquifer at the beginning and end of the hydrological year. The volume of water which flows to the adjacent alluvium or spring is measured by plotting the discharge as a function of time and estimating the recession coefficient at the beginning (or end) of the hydrological year. Known equations are used to calculate the dynamic volume of springs. A general equation is proposed to calculate the dynamic volume of a karst aquifer when there is a combination of springs, and subsurface inflow and outflow from the karst aquifer. The proposed method is applicable to the Zagros Folded Zone in Iran.