@article{10272/8381,
year = {2007},
url = {http://hdl.handle.net/10272/8381},
abstract = {From may/2006 to april/2007 a monthly sampling of the recharge conditions and main hydrogeochemical
parameters was conducted at a network of dripping points within Canelobre cave (Alicante). Speleothems
are fed by a combination of seepage and fracture water, indicating that the system consists of a matrix with
a network of discontinuities (fractures or conduits) with different characteristics. Control of Mg/Ca and Sr/
Ca indexes has provided data to identify several water infiltration processes into the vadose zone under
arid conditions: ranges of flow-through times to drips, prior calcite precipitation and dissolution of Mg
and Sr. Both indexes depend on the discharge intensity, though their variability adjust to a spatial framework
determined by cave geomorphology (grade of karst development, stratigraphic contacts and fractures)},
title = {Variación espacio-temporal de Ca-Mg-Sr en el agua de goteo de la Cueva del Canelobre (Alicante): ejemplo de procesos de infiltración en ambientes kársticos semiáridos},
title = {Space-time variations of Ca-Mg-Sr on drip water of Canelobre Cave (Alicante): example of infiltration processes on
semiarid karstic areas},
author = {Fernández Cortés, A. and Cuevas González, Jaime and Cañaveras, J.C. and Andreu Rodes, José Miguel and Sánchez Moral, S. and García del Cura, María Angeles and Hernández Bravo, J. A.},
}