Comportamiento de los elementos conservativos en las aguas de infiltración de la cueva del Canelobre (Busot, Alicante)

  1. J. Cuevas-González 1
  2. A. Fernández-Cortes 2
  3. M.C. Muñoz Cervera 1
  4. J.M. Andreu 1
  5. M.A. García del Cura 1
  6. D. Benavente 1
  7. J.C. Cañaveras 1
  1. 1 Universitat d'Alacant
    info

    Universitat d'Alacant

    Alicante, España

    ROR https://ror.org/05t8bcz72

  2. 2 Museo Nacional de Ciencias Naturales (CSIC)
Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Any de publicació: 2012

Títol de l'exemplar: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Número: 13

Pàgines: 856-859

Tipus: Article

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Altres publicacions en: Geotemas (Madrid)

Resum

Abstract: The analysis of dripping waters at Canelobre Cave for two years with a very different rainfall pattern was carried out. The study of concentration of conservative element Clestablished the marine influence on the different dripping waters. Sulphate ion concentration showed a linear relationship with the chloride, indicating its conservative behaviour during percolation processes. Variations in chloride concentrations were related to infiltration paths and type of drip, and also to the annual clime regime. These paths are controlled by the epikarst structure which is shaped by the type and geometrical position of their structural discontinuities (fractures, dding). Results showed the relationship between Cland rainfall events, which allowed better understanding and classification for different drip types

Fuente de los datos: Dialnet