Titlebook: Hydrogeological and Environmental Investigations in Karst Systems; Bartolomé Andreo,Francisco Carrasco,James W. LaMor Textbook 2015 Spring

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Role of the Soil-Epikarst-Unsaturated Zone in the Hydrogeological Functioning of Karst Aquifers. Thng variables (PCO. and SI.), together with natural tracers of infiltration (TOC and NO..), monitored in two karst springs of the Sierra Gorda de Villanueva del Trabuco aquifer (Southern Spain), reflect the greater relative importance of the soil-epikarst-unsaturated zone in the hydrogeological funct

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Recharge Processes of Karst Massifs: Examples from Southern Italy,vironments, the infiltration can occur in both concentrated and diffuse forms. In several areas of the Mediterranean, karst massifs are important sources of drinking water. In southern Italy, karst massifs are generally characterized by wide endorheic basins with seasonal lakes, which constitute lar

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Use of Tracing Tests to Study the Impact of Boundary Conditions on the Transfer Function of Karstics acquired in very different hydrologic conditions. Principal components analysis and hierarchical clustering were applied on both environmental variables and karstic system response variables (parameters of the RTD curves). Equations between the RTD parameters and the most relevant variables were e

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A Computer Method for Separating Hard to Separate Dye Tracers,the surface of the earth. Usually, hydrogeologists carry out tracer tests with only one tracer at a time, but sometimes two or more fluorescent substances are simultaneously injected into different spots and collected in a spring. Then, the resulting cocktail is analyzed by optical methods (fluoresc

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