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U-isotopes and (226)Ra as tracers of hydrogeochemical processes in carbonated karst aquifers from arid areas.

José Luis Guerrero,Ángela Vallejos,Juan Carlos Cerón,Francisco Sánchez-Martos,Antonio Pulido-Bosch,Juan Pedro Bolívar

Journal of Environmental Radioactivity（2016）

Cited 24|Views12
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Abstract
Sierra de Gádor is a karst macrosystem with a highly complex geometry, located in southeastern Spain. In this arid environment, the main economic activities, agriculture and tourism, are supported by water resources from the Sierra de Gádor aquifer system.
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Key words
Arid areas,Karst aquifer,Uranium isotopes,226Ra,Radioactive disequilibrium,Sierra de Gádor
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