By J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)
IV overseas Symposium on Karst Media, Malaga, Spain 2010 The Malaga Symposia sequence offers a global discussion board for medical debate at the growth made in examine into karst environments. The 2010 assembly of the 4th overseas ISKA provides eighty papers in 4 key themes: karst hydrogeology and investigations, karst landscapes and ecosystems, human interplay with karst environments, rather in caves, and engineering geology in karst components. This publication may be an invaluable version to the libraries of experts, scientists, teachers, and coverage makers fascinated about the particular problems with karst terrains.
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References Benn DI (1998) Glaciers and Glaciation. Arnold Publishers, 760 p Chandler D, Hubbard B, Hubbard A, Murray T, Rippin D (2008) Optimising ice flow law parameters using borehole deformation measurements and numerical modelling. Geophysical Research Letters, 35(12) 36 V. Gremaud, N. Goldscheider Goldscheider N (2005) Fold structure and underground drainage pattern in the alpine karst system Hochifen-Gottesacker. Eclogae Geologicae Helvetiae, 98(1): 1–17 Greene AM, Broecker WS, Rind D (1999) Swiss glacier recession since the Little Ice Age: Reconciliation with climate records.
Instead, the fraction of rainfall that results in recharge seems to increase exponentially with the magnitude of the precipitation event. Infiltration coefficients estimated vary widely, between 5 and 36%, and entail that the average yearly infiltration coefficient is less than 10%. Despite the limitations that stem from defining aquifers as equivalent porous media, this model provides an intuitive estimate of the system’s behavior and replicates the observed trends reasonably well. This, together with direct observation of the system, suggests that this approach provides a sufficiently accurate representation of reality.
A. B. Hunt, J. Beery In 1997, a concrete vault was constructed over the entrance to Antioch Cave (Fig. 3). 9-m diameter butterfly valve was installed in the side of the vault. The valve would be manually closed to hold out contaminant-laden stormwater or opened to allow cleaner, baseflow water to enter the cave. In 2008, a second valve was installed in the vault. This valve can be automatically opened and closed depending on turbidity levels of water in the creek. In addition, an intake screen was installed to filter out sediment and debris from stormwater (Fig.
Advances in Research in Karst Media by J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)