Salinidad del recurso hidrico subterraneo del Altiplano central

Translated title of the contribution: Salinity of the groundwater on the central Altiplano

A. Coudrain-Ribstein, B. Pratx, J. Quintanilla, G. M. Zuppi, D. Cahuaya

Research output: Contribution to journalArticlepeer-review

10 Scopus citations

Abstract

Close to the piedmont, groundwater is fresh and depleted in heavy isotopes like the rain during the humid season (<0.5 mS cm-1; δ18 < -14‰). Close to the recharge zone by the Desaguadero, groundwater has similar characteristics to the mean values of the Rio (2 mS cm-1 and δ180 ≃-10‰). Downstream, a more saline zone (3-6 mS cm-1) presents an isotopic signal of evaporated water and an age of around 3500 BP (14C and hydraulic model).

Translated title of the contributionSalinity of the groundwater on the central Altiplano
Original languageSpanish
Pages (from-to)483-493
Number of pages11
JournalBulletin - Institut Francais d'Etudes Andines
Volume24
Issue number3
StatePublished - 1996
Externally publishedYes

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