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Chemistry of the waters in the Canelobre Cave (Alicante)

dc.contributor.authorCuevas González, Jaime
dc.contributor.authorAndreu Rodes, José Miguel
dc.contributor.authorCañaveras, J.C.
dc.contributor.authorHernández Bravo, J. A.
dc.contributor.authorSánchez Moral, S.
dc.contributor.authorGarcía del Cura, María Angeles
dc.date.accessioned2014-07-11T11:46:19Z
dc.date.available2014-07-11T11:46:19Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8524
dc.description.abstractThe 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 rainwateren_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherHydrogeochemistryen_US
dc.subject.otherDrip watersen_US
dc.subject.otherKarstic caveen_US
dc.subject.otherCanelobreen_US
dc.titleQuímica de las aguas de goteo en la Cueva de Canelobre (Alicante)en_US
dc.titleChemistry of the waters in the Canelobre Cave (Alicante)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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