Title of article :
Groundwater salinization in the Saloum (Senegal) delta aquifer:
minor elements and isotopic indicators
Author/Authors :
Serigne Fayea، نويسنده , , Piotr Maloszewskib، نويسنده , , *، نويسنده , , Willibald Stichlerb، نويسنده , , Peter Trimbornb، نويسنده , ,
Seynabou Cisse´ Fayea، نويسنده , , Cheikh Be´caye Gayec، نويسنده ,
Issue Information :
هفته نامه با شماره پیاپی سال 2005
Abstract :
The hydrochemistry of minor elements bromide (Br), boron (B), strontium (Sr), environmental stable isotopes (18O and 2H)
together with major-ion chemistry (chloride, sodium, calcium) has been used to constrain the source(s), relative age, and
processes of salinization in the Continental Terminal (CT) aquifer in the Saloum (mid-west Senegal) region. Seventy-one
groundwater wells which include 24 wells contaminated by saltwater and three sites along the hypersaline Saloum River were
sampled to obtain additional information on the hydrochemical characteristics of the groundwater defined in previous studies.
Use of Br against Cl confirms the Saloum River saline water intrusion up to a contribution of 7% into the aquifer. In addition to
this recent intrusion, a relatively ancient intrusion of the Saloum River water which had reached at least as far as 20 km south
from the source was evidenced. The high molar ratio values of Sr/Cl and Sr/Ca indicate an additional input of strontium
presumably derived from carbonate precipitation/dissolution reactions and also via adsorption reactions. The variable B
concentrations (7–650 Ag/L) found in the groundwater samples were tested against the binary mixing model to evaluate the
processes of salinization which are responsible for the investigated system. Sorption of B and depletion of Na occur as the
Saloum river water intrudes the aquifer (salinization) in the northern part of the region, whereas B desorption and Na
enrichment occur as the fresh groundwater flushing displaces the saline waters in the coastal strip (refreshening). In the central
zone where ancient intrusion prevailed, the process of freshening of the saline groundwater is indicated by the changes in majorion
chemistry as well as B desorption and Na enrichment. In addition to these processes, stable isotopes reveal that mixing with
recently infiltrating waters and evaporation contribute to the changes in isotopic signature.
Keywords :
Minor elements , Salinization , Mixing model , Sorption/desorption , Hydrochemistry
Journal title :
Science of the Total Environment
Journal title :
Science of the Total Environment