Resumen de Consideraciones sobre el funcionamiento hidrogeológico y la vulnerabilidad a la contaminación de la Sierra de las Nieves (Málaga) a partir de un ensayo de trazador en condiciones de estiaje

Nico Goldscheider, Pablo Jiménez Gavilán, A. Cobos Rodríguez, Jesús María Vías Martínez, Christoph Neukum, N. Göppert, Francisco Carrasco Cantos, R. Ferrer, Damián Sánchez García, Bartolomé Andreo Navarro, Iñaki Vadillo, H. Hotzl, L del Campo, Cristina Liñán Baena, Isaac Pérez Ramos

• A tracer test during low-flow conditions was carried out in the karstic aquifer of Sierra de las Nieves (Málaga) in order to assess its hydrogeological functioning and vulnerability to contamination. Two kilogrammes of Eosine were injected in an active siphon located in the Sima del Aire cave shaft (-640 m) at the end of August 2003. The springs were sampled until November 2003. For more than 50 days, the tracer was not detected at any of the springs. After several rainfall events in October 2003, a signal was observed in the two Río Grande springs. The first arrival of Eosine appears before the increase of spring discharge and the dilution effect of the most important rainfalls (86 mm, October 25th). The calculated groundwater velocities (below 4 m/hour) are not representative of the dry period because rainfall forced the Eosine transport. However, they give an idea about the long residence time if a contamination event occurs during low-flow conditions.