Hydraulic Conductivity - Issues, Determination and Applications 2011
DOI: 10.5772/22093
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Contribution of Tracers for Understanding the Hydrodynamics of Karstic Aquifers Crossed by Allogenic Rivers, Spain

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Cited by 4 publications
(3 citation statements)
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“…The hydrograph of Fuentetoba Spring was analyzed. Tracer tests can be done (for example, Käss, W, 1998;Geyer et al, 2007;Benischke et al, 2007;Perrin and Luetscher, 2008;Goldscheider et al, 2008;Segovia et al, 2011) to characterize local hydrogeological properties, such as the possible effect of siphoning or lags in flow. In the case of Fuentetoba Spring, three tracer tests were performed in 2012 and 2013 during low-water periods that were followed by recharge events, using uranine, together with point injections of NaCl.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The hydrograph of Fuentetoba Spring was analyzed. Tracer tests can be done (for example, Käss, W, 1998;Geyer et al, 2007;Benischke et al, 2007;Perrin and Luetscher, 2008;Goldscheider et al, 2008;Segovia et al, 2011) to characterize local hydrogeological properties, such as the possible effect of siphoning or lags in flow. In the case of Fuentetoba Spring, three tracer tests were performed in 2012 and 2013 during low-water periods that were followed by recharge events, using uranine, together with point injections of NaCl.…”
Section: Methodsmentioning
confidence: 99%
“…3). A characteristic of the large springs of the Upper Cretaceous aquifers in this zone is the presence of phreatic conduits associated with them; the spring at Fuentona de Muriel emerges from a conduit that is more than 110 m deep and 400 m long (Sanz Pérez and Medina Ferrer, 1987), the spring at La Galiana flows from a conduit with some 400 m exploredlength (Segovia et al, 2011), and the Fuente Azul de San Pedro de Arlanza in Burgos emerges from a vertical phreatic conduit more than 100 m deep.…”
Section: Caves Submerged Conduits and Subterranean Riversmentioning
confidence: 99%
“…It was not known if it behaved only as a losing stream along its entire length, nor what the infiltration capacity of its river bed was. Tracing studies were required to elucidate the hydraulic connection between the rivers and the aquifer (Segovia et al, 2011) [11].…”
Section: Open Accessmentioning
confidence: 99%