Química de las aguas de goteo en la Cueva de Canelobre (Alicante)
The Cave of Canalobre, located in the west middle of the Alicante province, is one of the most visited cave in Comunidad Valenciana. During the last years some drip water samples have been collected. The analytical results have allowed us the physico-chemical characterization of the waters. Use of p...
| Autores: | , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2006 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/8524 |
| Acceso en línea: | http://hdl.handle.net/10272/8524 |
| Access Level: | acceso abierto |
| Palabra clave: | Hydrogeochemistry Drip waters Karstic cave Canelobre |
| Sumario: | The Cave of Canalobre, located in the west middle of the Alicante province, is one of the most visited cave in Comunidad Valenciana. During the last years some drip water samples have been collected. The analytical results have allowed us the physico-chemical characterization of the waters. Use of principal components analysis (PCA) and a study of hydrodynamic equilibria have allowed us to stablish that the proper ties and composition of these waters depend on both dissolution proccess of the rock during the downward passage and climatic concentration in the soil of the components dissolved in the rainwater |
|---|