Heterogeneidad del acuífero de la Vega de Granada en el entorno urbano de Granada (España)

  1. Virginia María Robles-Arenas 1
  2. José Benavente Herrera 2
  3. Carmen Almécija Ruiz 2
  1. 1 Departamento de Ingeniería Civil y Minera. Universidad Politécnica de Cartagena. Cartagena
  2. 2 Departamento de Geodinámica. Facultad de Ciencias. Universidad de Granada. Granada
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 2022

Número: 71

Páginas: 47-50

Tipo: Artículo

Otras publicaciones en: Geogaceta

Resumen

Hydrodynamic data in 5 wells located in the city of Granada and in its peri-urban area asses the horizontal and vertical heterogeneity in the hydraulic conductivity of the Vega de Granada alluvial aquifer (AVG) at its eastern part. They also indicate the existence of a perched level in one of the studied points (FC) and characterize its lowering since 2001. It is confirmed that the hydrodynamic response to recharge is more effective in the SE of the studied sector. A conceptual model is proposed that integrates our results in the context of the piezometric evolution linked to the increase in pumping in the eastern half of the AVG since approximately 1970.