Titlebook: Advances in Research in Karst Media; Bartolomé Andreo,Francisco Carrasco,James W. LaMor Book 2010 Springer-Verlag Berlin Heidelberg 2010 E

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https://doi.org/10.1007/978-3-319-41827-8e overlain by the karstic Upper Trinity and Edwards Aquifers, the degree of karstification is not known, but groundwater in certain units of the Middle Trinity Aquifer is chemically similar to shallow groundwater in this area. Geochemical, potentiometric, and hydraulic conductivity data suggest that

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https://doi.org/10.1007/978-3-319-74113-0n a high water discharge period recorded during December 2008 at Port-Miou spring. During this one week event, the discharge in the 20 m diameter saturated conduit had probably been in the range of 50 to 100 m./s. In spite of this huge spring water discharge, the salinity remained persistently above

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https://doi.org/10.1007/978-3-030-11166-3The Lower Karst Subsystem developing at the base of the series is formed by small to medium size conduits with a circular cross section, organized in mazes and cut off by the canyons. It constitutes the earliest cave development, earlier than the canyons cutting the plateaus. Confined conditions acc

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Stephen F. Previs,Daniel P. Downes. Previous studies have examined the model through classical spectral analysis and system identification techniques under a linearity hypothesis. Since a karst area is generally accepted as a non-linear and dynamic system, different approaches, from wavelet paradigmto high order statistically stable

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Yogita Singh Kardam,Kamal Srivastavats. Due to a Mediterranean climate and hydrogeological conditions of the aquifers, spring hydrographs are characterised generally by one annual smoothed peak during spring season and a negligible quick flow component. Insufficient recharge due to poor annual rainfall can cause continuous decreasing

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S. E. Ramberg,C. L. Bartholomewlný vrch/Alsóhegy, several karstic springs occur. Hydrograph recession curves from nine gauged springs on the Slovak part of the transboundary aquifer were analyzed. Individual springs were classified by typical groundwater depletion hydrograph into categories by typical depletion equations. These w