Salinidad del recurso hidrico subterraneo del Altiplano central

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

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 journal › Article › peer-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 contribution	Salinity of the groundwater on the central Altiplano
Original language	Spanish
Pages (from-to)	483-493
Number of pages	11
Journal	Bulletin - Institut Francais d'Etudes Andines
Volume	24
Issue number	3
State	Published - 1996
Externally published	Yes

Cite this

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title = "Salinidad del recurso hidrico subterraneo del Altiplano central",

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).",

author = "A. Coudrain-Ribstein and B. Pratx and J. Quintanilla and Zuppi, {G. M.} and D. Cahuaya",

year = "1996",

language = "Espa{\~n}ol",

volume = "24",

pages = "483--493",

journal = "Bulletin de L'Institut Francais d'Etudes Andines",

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number = "3",

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TY - JOUR

T1 - Salinidad del recurso hidrico subterraneo del Altiplano central

AU - Coudrain-Ribstein, A.

AU - Pratx, B.

AU - Quintanilla, J.

AU - Zuppi, G. M.

AU - Cahuaya, D.

PY - 1996

Y1 - 1996

N2 - 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).

AB - 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).

UR - http://www.scopus.com/inward/record.url?scp=0030434136&partnerID=8YFLogxK

M3 - Artículo

AN - SCOPUS:0030434136

VL - 24

SP - 483

EP - 493

JO - Bulletin de L'Institut Francais d'Etudes Andines

JF - Bulletin de L'Institut Francais d'Etudes Andines

SN - 0303-7495

IS - 3

ER -

Salinidad del recurso hidrico subterraneo del Altiplano central

Abstract

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