| Programme annuel & rapport de suivi technique |
-
Programmes Techniques 2025
-
Rapport d'activités 2023
|
| Géocatalogue |
|
| Appels d'Offres |
-
DESIGNATION D’UN REVISEUR COMPTABLE POUR LES EXERCICES 2025-2026-2027
-
ACQUISITION DE MATERIEL INFORMATIQUE ET EQUIPEMENTS RESEAUX
|
|
Investir en Tunisie |
|
|
|
|
|
::
Documentation and Editions
>>
Research library
|
| |
|
[
Search by author
]
[
Search keyword
]
[
Search by index
]
[
Search by category
]
|
title of the reference :
|
Geochemistry of brines of the chott el Jerid in Southern Tunisia - Application of Pitzer's equations.
|
|
Publication Date:
|
1983
|
|
Author :
|
Gueddari Moncef, Monnin Christophe, Perret-Gentil Christophe, Fritz Bertrand, Tardy Yves
|
|
Catalogue type :
|
Livre
|
|
Catalogue reference :
|
T. 39 (NLD) Chem. Geol. T. 39 Geochemistry of brines of the chott el Jerid in Southern Tunisia - Application of Pitzer's equations. Géochimie des saumures du chott el Jerid au Sud de la Tunisie. Application des équations de Pitzer. In the chott El Jerid in southern Tunisia, waters are strongly concentrated by evaporation under an arid climate. The diluted waters are of the Ca-Mg-SO4 type whereas the brines are of the Na-Cl type, relatively concentrated in K and Mg. In concentrated waters, Ca and silica concentrations remain at a very low level. The use of Pitzer's equations for calculating the ion activities has permitted accurate saturation tests and a fairly good evaluation of the mineral sequences controlling the geochemistry of the basin.
bibliogr. saumure ; sebkha ; évaporation ; milieu aride ; thermodynamique ; sâturation ; équation Pitzer ; activité ionique ; Tunisie ; Chott el Jerid Monnin Christophe Perret-Gentil Christophe Fritz Bertrand Tardy Yves Gueddari Moncef Géochimie
|
|
Indexation decimale :
|
Géochimie
|
|
Keywords :
|
saumure ; sebkha ; évaporation ; milieu aride ; thermodynamique ; sâturation ; équation Pitzer ; activité ionique ; Tunisie ; Chott el Jerid
|
|
Summary :
|
In the chott El Jerid in southern Tunisia, waters are strongly concentrated by evaporation under an arid climate. The diluted waters are of the Ca-Mg-SO4 type whereas the brines are of the Na-Cl type, relatively concentrated in K and Mg. In concentrated waters, Ca and silica concentrations remain at a very low level. The use of Pitzer's equations for calculating the ion activities has permitted accurate saturation tests and a fairly good evaluation of the mineral sequences controlling the geochemistry of the basin.
|
|
Exemplaries :
|
TU660
|
|
|
|
|
|
|
|
