By J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)
IV foreign Symposium on Karst Media, Malaga, Spain 2010 The Malaga Symposia sequence offers a global discussion board for medical debate at the development made in study into karst environments. The 2010 assembly of the 4th overseas 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 parts. This e-book could be an invaluable variation to the libraries of experts, scientists, teachers, and coverage makers desirous about the precise problems with karst terrains.
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The glacier’s geometry was investigated by geophysical surveys, using radiomagnetotelluric (RMT): The estimated ice volume is 1:0 108 m3 , corresponding to 0:92 108 m3 freshwater. Meltwater production displays diurnal and seasonal variability influencing the shape of tracer breakthrough curves and, thus, flow and transport in the aquifer. A preliminary prognosis of water availability when the glacier will have disappeared has been established, predicting more available water in winter, but shortages in long dry summer and autumn periods, due to the absence of meltwater and less estival rainfall.
Chandler et al. 2008; Hubbard 2002; Hubbard and Hubbard 1998; Hubbard et al. 2000; Sharp et al. 1989). More recent studies investigate the relations between the geological structure and the drainage pattern in the karst aquifer (Gremaud et al. 2009) and glacier-aquifer relations (Gremaud and Goldscheider 2010). Fig. 1 Location and general overview of the Tsanfleuron-Sanetsch glacier and karst aquifer system in the Western Swiss Alps. 22 tracer tests made it possible to delineate the recharge area of the Glarey spring (modified from Gremaud and Goldscheider 2010) Climate Change Effects on Aquifer Recharge in a Glacierised Karst Aquifer System 33 This article focuses on climate change impacts on the glacier and aquifer dynamics, and also presents estimations on glacier volume and meltwater availability in the near future.
With extended periods of flow, the amount of recharge to the aquifer through Antioch Cave could be significant enough to increase the amount of water in storage which will help maintain water levels in wells and springflow at Barton Springs during periods of drought. A. B. Hunt, J. Beery rainfall. This additional water going into storage can reduce the impact of drought on wells and the endangered species at Barton Springs. References Hauwert, NM (2009) Groundwater Flow and Recharge within the Barton Springs Segment of the Edwards Aquifer, Southern Travis County and Northern Hays Counties, Texas: PhD Dissertation, University of Texas at Austin, Texas.
Advances in Research in Karst Media by J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)