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Estimating groundwater residence time and recharge patterns in a saline coastal aquifer
Author(s) -
Caschetto M.,
Colombani N.,
Mastrocicco M.,
Petitta M.,
Aravena R.
Publication year - 2016
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.10942
Subject(s) - groundwater recharge , aquifer , groundwater , hydrology (agriculture) , environmental science , environmental isotopes , geology , geotechnical engineering
Abstract A detailed study using environmental tracers such as chloride (Cl − ) and tritium ( 3 H), deuterium ( 2 H) and oxygen ( 18 O) isotopes was performed in an alluvial coastal aquifer in two contrasting environments (urban and agricultural). These environmental tracers combined with a high‐resolution multi‐level sampling approach were used to estimate groundwater residence time and recharge patterns and to validate the hydrogeochemical conceptual model already proposed in previous studies. δ 18 O and δ 2 H combined with Cl − data proved that the hypersaline groundwater present in the deepest part of the aquifer was sourced from the underlying hypersaline aquitard via an upward flux. Both chemical and isotopic data were employed to calibrate a density‐dependent numerical model based on SEAWAT 4.0, where 3 H and Cl − were helped quantifying solutes transport within the modelled aquifer. Model results highlighted the differences on estimated recharge in the two contrasting environments, with the urban one exhibiting concentrated recharge because of preferential infiltration associated to the storm water drains network, while scarce local recharge characterized the agriculture setting. In the urban field site, is still possible to recognize at 9 m b.g.l. the input of the atmospheric anthropogenic 3 H generated by testing of thermonuclear weapons, while in the agricultural field site, the 3 H peak has been washed out at 6 m b.g.l. because the groundwater circulation is restricted only to the upper fresh part of the aquifer, drained by the reclamation system. The presented approach that combined high‐resolution field monitoring, environmental tracers and numerical modelling, resulted effective in validating the conceptual model of the aquifer salinization. Copyright © 2016 John Wiley & Sons, Ltd.