Hidrogeología del entorno de las lagunas del Oso (Ávila)

  1. Pedro Huerta 1
  2. Álvaro Inthirat 1
  3. Pedro Carrasco 1
  4. Ildefonso Armenteros 1
  5. Clemente Recio 1
  6. Esther Rodríguez-Jiménez 1
  7. Javier Carrasco García 2
  1. 1 Universidad de Salamanca
    info
    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

    Geographic location of the organization Universidad de Salamanca
  2. 2 Técnicas Geofísicas, S.L. (Ávila)
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 2022

Issue: 72

Pages: 15-18

Type: Article

DOI: 10.55407/GEOGACETA98432 DIALNET GOOGLE SCHOLAR lock_openOpen access editor

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SDG classification obtained using Aurora SDG artificial intelligence model.

Abstract

In the surroundings of the locality of El Oso in the region of the Moraña (Ávila), there are many wetlands. The most important is El Hoyo lake. The Miocene and Quaternary sands constitute good aquifers with northward groundwater flow. In the vicinity of El Oso the groundwater table is very shallow and groundwater shows an ascendant vertical component. Groundwaters are fresh and have a bicarbonate-calcium-sodic composition. The natural regime of El Hoyo lake has been modified by the groundwater inputs from nearby boreholes. El Hoyo is a recharge lake during the winter, fed mainly by direct precipitation, but during the summer it can receive groundwater inputs.