Abstract
Hydrochemistry of groundwater is largely determined by both natural processes, such as dissolution, cation exchange, mixing, evaporation; and anthropogenic activities, which can affect the aquifer systems by contaminating them or by modifying their hydrological cycle. Both natural and anthropogenic processes vary in time and space; which is reflected in groundwater hydrochemistry variation. The objective of this study is the determination of the main hydrogeochemical processes that affect the quality of shallow groundwaters in the Grombalia basin, located in the Cap Bon Peninsula, north-eastern Tunisia. In this area, the chemical composition of groundwater is mostly characterized by Na–Cl–NO3–Ca water type which reveals the implication of natural and anthropogenic major factors. Natural factors are dissolution of evaporatic minerals, i.e. halite and gypsum and cation exchange with clays, while anthropogenic factors are pollution with industrial Sr-rich waste water and return flow of irrigation water, highly contaminated by MgSO4 and methyl-bromide fertilizers.
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References
Adams S, Tredoux G, Harris C, Titus R, Pietersen K (2001) Hydrochemical characteristics of aquifers near Sutherland in the Western Karoo, South Africa. J Hydrol 241:91–103
Ben Ayed N (1993) Évolution tectonique de l’avant-pays de la chaîne alpine de la Tunisie du début du Mésozoïque à l’Actuel. Ph.D. thesis, University of Paris 11, Orsay
Ben Salem H (1995) Évolution de la péninsule du Cap Bon (Tunisie orientale) au cours du Néogène. Notes Serv Geol Tunis 61:73–84
Castany G (1948) Les fossés d’effondrement de Tunisie. Ann Min Geol Tunis, p 3
Castany G (1967) Traité pratique des eaux souterraines, 2nd edn edn. Ed Dunod, Paris, p 471
Chihi L (1995) Les fossés néogènes à quaternaires de la Tunisie et de la mer Pélagienne: une étude structurale et une signification dans le cadre géodynamique de la Méditerranée centrale. Ph.D. thesis, University of Tunis II
Garcia MG, Del Hidalgo M, Blesa MA (2001) Geochemistry of groundwater in the alluvial plain of Tucuman province, Argentina. J Hydrol 9:597–610
Gi-Tak C, Kangjoo K, Seong T, Kyoung H, Soon O, Byoung Y, Hyoung S, Chul W (2004) Hydrogeochemistry of alluvial groundwaters in an agricultural area: an implication for groundwater contamination susceptibility. Chemosphere 55:369–378
Hitchon B, Perkins EH, Gunter D (1999) Introduction to groundwater geochemistry. Geoscience Publishing Ltd, Sherwood Park, p 310
Mc Lean W, Jankowski J, Lavitt N (2000) Groundwater quality and sustainability in alluvial aquifer, Australia. In: Sililo O et al (eds) Groundwater, past achievement and future challenges. Bolkema, Rotterdam, pp 567–573
Piper AM (1944) A graphic procedure in the geochemical interpretation of water-analyses. Trans Am Geophys Union 25:914–923
Richer BC, Kreitler CW (1993) Geochemical techniques for identifying sources of groundwater salinization. CRC, Boca Raton
Stigter TY, Carvalho AM, Ribeiro L, Reis E (2006) A impact of the shift from groundwater to surface water irrigation on aquifer dynamics and hydrochemistry in a semi-arid region in the south of Portugal. Agric Water Manage 85:121–132
Zhu GF, Li ZZ, Su YH, Ma JZ, Zhang YY (2007) Hydrogeochemical and isotope evidence of groundwater evolution and recharge in Minqin Basin, Northwest China. J Hydrol 333:239–251
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Ben Moussa, A., Zouari, K. & Oueslati, N. Geochemical study of groundwater mineralization in the Grombalia shallow aquifer, north-eastern Tunisia: implication of irrigation and industrial waste water accounting. Environ Geol 58, 555–566 (2009). https://doi.org/10.1007/s00254-008-1530-7
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DOI: https://doi.org/10.1007/s00254-008-1530-7