Publications des scientifiques de l'IRD

Ammar F. H., Chkir N., Zouari K., Hamelin Bruno, Deschamps Pierre, Aigoun A. (2014). Hydro-geochemical processes in the Complexe Terminal aquifer of southern Tunisia : an integrated investigation based on geochemical and multivariate statistical methods. Journal of African Earth Sciences, 100, p. 81-95. ISSN 1464-343X.

Titre du document
Hydro-geochemical processes in the Complexe Terminal aquifer of southern Tunisia : an integrated investigation based on geochemical and multivariate statistical methods
Année de publication
2014
Type de document
Article référencé dans le Web of Science WOS:000345473200007
Auteurs
Ammar F. H., Chkir N., Zouari K., Hamelin Bruno, Deschamps Pierre, Aigoun A.
Source
Journal of African Earth Sciences, 2014, 100, p. 81-95 ISSN 1464-343X
Hydrochemical data from a total of 104 groundwater samples were used to investigate the main factors and mechanisms that control the chemistry of groundwaters in the Complexe Terminal (Cl') aquifer of Chott region in southern Tunisia. Multivariate statistical techniques combining Hierarchical Cluster Analysis (HCA) and Principal Component Analysis (PCA) were applied to the dataset of 12 physicochemical parameters (i.e. pH, T degrees, depth, Na+, K+, Ca2+, Mg2+, HCO3- NO3-, Cl-, SO42-, and TDS). The HCA using Ward's method and squared Euclidean distance classified the parameters into four clusters based on their dissimilarities. The application of PCA resulted in two factors explaining 64.25% variance. Geochemical methods combined with HCA and PCA confirm that groundwater chemistry is not controlled by the different lithological fades of the aquifer, but by the presence of evaporates randomly distributed in the basin. Although stable isotope data (H-2 and O-18) of some groundwater are consistent with a slight modern recharge, Cl' groundwaters are mostly depleted bearing witness to the recharge of the aquifer system occurred under different climatic conditions than present. The stable isotopic composition of these paleowaters which all lie to the right of the local meteoric water line also indicates more pronounced evaporation of rainfall during the recharge process than during present-day conditions.
Plan de classement
Hydrologie [062]
Description Géographique
TUNISIE
Localisation
Fonds IRD [F B010063119]
Identifiant IRD
fdi:010063119
Contact