Published May 1989 | Version v1
Report

Quito Valley: General behaviour and problems of natural aquifer recharge

  • 1. International Atomic Energy Agency, Vienna (Austria)
  • 2. Institut Francais de Recherche Scientifique pour le Developpement en Cooperation, Quito (Ecuador)
  • 3. Instituto Ecuatoriano de Recursos Hidraulicos, Quito (Ecuador)

Description

The environmental isotopic study of the Quito aquifer system, performed to complement the conventional hydrogeological survey, led us to the identification of two different recharge processes: (1) In the north, the water circulation is of ''hypodermic'' type on the flank of the volcano Pichincha and the recharge of the aquifer is mainly due to direct infiltration of rainwater and surface water; (2) In the south, the infiltration is more effective in the highest part of the mountain and the aquifer recharge derives from deep groundwater circulation. (author). 5 refs, 6 figs, 2 tabs

Part of:
Isotope hydrology investigations in Latin America

Additional details

Additional titles

Original title (Spanish)
Cubeta de Quito: Comportamiento general y problematica de la recarga natural del acuifero

Publishing Information

Imprint Title
Isotope hydrology investigations in Latin America
Imprint Pagination
482 p.
Journal Page Range
p. 305-317.
Report number
IAEA-TECDOC--502

Conference

Title
Regional seminar for Latin America on the use of isotope techniques in hydrology.
Dates
28 Sep - 2 Oct 1987.
Place
Salazar (Mexico).

Optional Information

Notes
Imprint:Estudios de hidrologia isotopica en America Latina.;Actas de un seminario regional para America Latina sobre el empleo de tecnicas isotopicas en hidrologia celebrado en el Centro de Investigaciones Nucleares de Salazar, Mexico, 28 de Septiembre a 2 de Octubre de 1987.