Advances in Research in Karst Media by J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco PDF

By J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)

ISBN-10: 3642124852

ISBN-13: 9783642124853

ISBN-10: 3642124860

ISBN-13: 9783642124860

IV foreign Symposium on Karst Media, Malaga, Spain 2010 The Malaga Symposia sequence presents a global discussion board for clinical debate at the development made in study into karst environments. The 2010 assembly of the 4th foreign ISKA offers eighty papers in 4 key subject matters: karst hydrogeology and investigations, karst landscapes and ecosystems, human interplay with karst environments, quite in caves, and engineering geology in karst components. This booklet could be an invaluable variation to the libraries of experts, scientists, teachers, and coverage makers keen on the precise problems with karst terrains.

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This suggests radial flow from a groundwater mound developed when large amounts of water enter an aquifer in a limited area. A potentiometric surface map shows a significant groundwater mound that developed beneath Antioch Cave during wet conditions in 2002 (Fig. 2). Fig. 2 Potentiometric surface map in the vicinity of Antioch Cave (star symbol) and flow paths documented by tracer testing. A. B. Hunt, J. Beery In 1997, a concrete vault was constructed over the entrance to Antioch Cave (Fig. 3).

The biggest deviation has been noticed for the catchment area of Crnojevica springs, where earlier obtained result was Rch D 76:1 while newly calculated average value First Outcomes from New Approach in Assessing Recharge of Highly Karstified Terrains 29 Fig. 0% (Radulovic 2009). 10%. Figure 2 shows final maps of spatial distribution of recharge obtained by KARSTLOP method. 5 Conclusions Method KARSTLOP has been applied and calibrated at catchments of several large karst springs of Montenegro. This method is aimed at mapping the spatial distribution of mean annual recharge of karstic aquifer in specific highly karstified terrains.

1). Its entire territory belongs to Alpine geo structure, to the Dinarides branch. com Z. me B. Andreo et al. 1007/978-3-642-12486-0, © Springer 2010 25 26 M. Radulovic, Z. Stevanovic, M. Radulovic Fig. 1 Geographical location of Montenegro and the four tested catchment areas: a Podgor springs; b Crnojevica springs; c Karuc springs; d Slatina springs territory is highland. Carbonate rocks (limestone and dolomites) cover large parts of the area (over 60%) and are characterized by a very high degree of karstification.

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Advances in Research in Karst Media by J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)

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