Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)

Groundwater resources are facing increasing pressure especially in semi-arid regions where they often represent the main freshwater resource to sustain human needs. Several aquifers in the Mediterranean basin suffer from salinization and quality degradation. This study provides an assessment of Grom...

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Main Authors: Siwar Kammoun, Rim Trabelsi, Viviana Re, Kamel Zouari
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/2/129
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spelling doaj-4777470bed7847f0aeae880764595dd82021-01-09T00:00:35ZengMDPI AGWater2073-44412021-01-011312912910.3390/w13020129Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)Siwar Kammoun0Rim Trabelsi1Viviana Re2Kamel Zouari3Laboratory of Radio-Analyses and Environment, National School of Engineers of Sfax, BP1173, Sfax 3038, TunisiaLaboratory of Radio-Analyses and Environment, National School of Engineers of Sfax, BP1173, Sfax 3038, TunisiaLaboratory of Radio-Analyses and Environment, National School of Engineers of Sfax, BP1173, Sfax 3038, TunisiaLaboratory of Radio-Analyses and Environment, National School of Engineers of Sfax, BP1173, Sfax 3038, TunisiaGroundwater resources are facing increasing pressure especially in semi-arid regions where they often represent the main freshwater resource to sustain human needs. Several aquifers in the Mediterranean basin suffer from salinization and quality degradation. This study provides an assessment of Grombalia coastal aquifer (Tunisia) based on multidisciplinary approach that combines chemical and isotopic (δ<sup>2</sup>H, δ<sup>18</sup>O, <sup>3</sup>H, <sup>14</sup>C and δ<sup>13</sup>C) methods to characterize the relation between groundwater quality variation and aquifer recharge. The results indicate that total dissolved solids exceed 1000 mg/L in the most of samples excepting the recharge area. In addition to water–rock interaction, evaporation and nitrate pollution contributing to groundwater mineralization, the reverse cation exchange process constitute an important mechanism controlling groundwater mineralization with enhancing risk of saltwater intrusion. Environmental isotope tracers reveal that groundwater is evolving within an open system to close system. A significant component of recent water that is recharging Grombalia aquifer system is confirmed by applying correction models based on the δ<sup>13</sup>C values and <sup>14</sup>C activities and tritium contents. However, this recharge, which is mainly associated to the return flow of irrigation water, contributes to the groundwater salinization, especially for the shallow aquifer.https://www.mdpi.com/2073-4441/13/2/129groundwatermineralizationwater–rock interactionscation exchange processisotopesaquifer recharge
collection DOAJ
language English
format Article
sources DOAJ
author Siwar Kammoun
Rim Trabelsi
Viviana Re
Kamel Zouari
spellingShingle Siwar Kammoun
Rim Trabelsi
Viviana Re
Kamel Zouari
Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
Water
groundwater
mineralization
water–rock interactions
cation exchange process
isotopes
aquifer recharge
author_facet Siwar Kammoun
Rim Trabelsi
Viviana Re
Kamel Zouari
author_sort Siwar Kammoun
title Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
title_short Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
title_full Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
title_fullStr Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
title_full_unstemmed Coastal Aquifer Salinization in Semi-Arid Regions: The Case of Grombalia (Tunisia)
title_sort coastal aquifer salinization in semi-arid regions: the case of grombalia (tunisia)
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-01-01
description Groundwater resources are facing increasing pressure especially in semi-arid regions where they often represent the main freshwater resource to sustain human needs. Several aquifers in the Mediterranean basin suffer from salinization and quality degradation. This study provides an assessment of Grombalia coastal aquifer (Tunisia) based on multidisciplinary approach that combines chemical and isotopic (δ<sup>2</sup>H, δ<sup>18</sup>O, <sup>3</sup>H, <sup>14</sup>C and δ<sup>13</sup>C) methods to characterize the relation between groundwater quality variation and aquifer recharge. The results indicate that total dissolved solids exceed 1000 mg/L in the most of samples excepting the recharge area. In addition to water–rock interaction, evaporation and nitrate pollution contributing to groundwater mineralization, the reverse cation exchange process constitute an important mechanism controlling groundwater mineralization with enhancing risk of saltwater intrusion. Environmental isotope tracers reveal that groundwater is evolving within an open system to close system. A significant component of recent water that is recharging Grombalia aquifer system is confirmed by applying correction models based on the δ<sup>13</sup>C values and <sup>14</sup>C activities and tritium contents. However, this recharge, which is mainly associated to the return flow of irrigation water, contributes to the groundwater salinization, especially for the shallow aquifer.
topic groundwater
mineralization
water–rock interactions
cation exchange process
isotopes
aquifer recharge
url https://www.mdpi.com/2073-4441/13/2/129
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AT rimtrabelsi coastalaquifersalinizationinsemiaridregionsthecaseofgrombaliatunisia
AT vivianare coastalaquifersalinizationinsemiaridregionsthecaseofgrombaliatunisia
AT kamelzouari coastalaquifersalinizationinsemiaridregionsthecaseofgrombaliatunisia
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