Abstract
The chemical composition of groundwater from wells tapping the Continental Intercalaire (CI) aquifer in the Grand Erg Oriental basin and the detailed analysis of saturation indices enable identification of the mineralization origin. CI groundwater is characterized by a Ca–SO4/Cl abundant water type and a Na–Cl second type. Chemical pattern is controlled by evaporites dissolution (halite, anhydrite and gypsum). Recently, the decrease in these CI geothermal water wells performance is explained by an incrustation in the well screen. To study the scaling process, we used the degree of calcite saturation, hardness and Langelier Saturation Index (LSI). It has been demonstrated that scaling potential is the most important in the basin axis, around El Oued region (southern Algeria) and in the south-east of Tunisia and the Chott Djerid borders (El Hamma of Gabes, Tozeur and Kebili) corresponding to the discharge zones. However, the scaling potential decreases towards Algerian reliefs (Tademait and Tinrhert) representing aquifer recharge zones.
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References
Agoun A (2010) Hydrogeological characteristics of the geothermal transboundary aquifer reservoir case study of the Continental Intercalaire aquifer system in North Sahara Aquifer System (NSAS) in southern Tunisian field. In: Proceedings world geothermal congress, Bali, pp 25–29
Baghvand A, Nasrabadi T, Bidhendi GN, Vosoogh A, Karbassi A, Mehrdadi N (2010) Groundwater quality degradation of an aquifer in Iran central desert. Desalination 260:264–275. https://doi.org/10.1016/j.desal.2010.02.038
Busson G (1970) Le Mésozoïque saharien, 2eme partie: essai de synthèse des données des sondages algéro-tunisiens. Publications du Centre de Recherches sur la Zone Aride, Série Géologie, vol 11a–b. CNRS, Paris, pp 1–812. https://scholar.google.fr/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Busson+G+%281970b%29+Le+M%C3%A9sozo%C3%AFque+saharien%2C+2eme+partie%3A+essai+de+synth%C3%A8se+des+donn%C3%A9es+des+sondages+alg%C3%A9ro-tunisiens%2C+2+tomes+Edition+CNRS%2C+Paris.+France%2C+pp+811.&btnG=
Chadha DKA (1999) Proposed new diagram for geochemical classification of natural waters and interpretation of chemical data. Hydrogeol J 7:431–439. https://doi.org/10.1007/s100400050216
Clark PD, Hyne JB, Tyrer JD (1983) Chemistry of organosulphur compound types occurring in heavy oil sands: 1. High temperature hydrolysis and thermolysis of tetrahydrothiophene in relation to steam stimulation processes. Fuel 62:959–962. https://doi.org/10.1016/0016-2361(83)90170-9
Czerewko MA, Cripps JC (2006) Sulfate and sulfide minerals in the UK and their implications for the built environment. Int Assoc Eng Geol. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=.%EF%82%A7%09Czerewko%2C+M.A.+%26+Cripps%2C+J.C.+2006.+Sulfate+and+sulfide+minerals+in+the+UK+and+their+implications+for+the+built+environment.+International+Association+for+Engineering+Geology&btnG=
Edmunds WM, Guendouz A, Mamou A, Moulla A, Shand P, Zouari K (2003) Groundwater evolution in the Continental Intercalaire aquifer of southern Algeria and Tunisia: trace element and isotopic indicators. Appl Geochem 18:805–822
El Guedri M (1999) Assessment of scaling and corrosion problems in the Kebili geothermal field, Tunisia. Report 1 in: geothermal training in Iceland 1999. UNU G.T.P., Iceland, pp 1–40. https://scholar.google.com/scholar?q=El%20Guedri%20M%20%281999%29%20Assessment%20of%20scaling%20and%20corrosion%20problems%20in%20the%20Kebili%20geothermal%20field%2C%20Tunisia.%20Report%201%20in%3A%20Geothermal%20Training%20in%20Iceland%201999%2C%20UNU%20G.T.P.%20Iceland%2C%20pp%201%E2%80%9340
Garcia GM, Hidalgo MDV, Blesa MA (2001) Geochemistry of groundwater in the alluvial plain of Tucuman province, Argentina. Hydrogeol J 9:597–610. https://doi.org/10.1007/s10040-001-0166-4
Gemici U, Filiz S (2001) Hydrogeochemistry of the gesme geothermal field, western Turkey. J Volcanol Geotherm Res 110:171–187
Gueddari M, Besbes M, Mammou A, Bouhlila R (2005) Recharge et paléorecharge du Système Aquifère du Sahara Septentrional-hydrologie.org. http://hydrologie.org/THE/OULD_BABA_SY.pdf
Guendouz A (1985) Contribution à l’étude géochimique et isotopique des nappes profondes du Sahara nord-est septentrional, Algerie. Dissertation, University of Paris-Sud, Orsay. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Guendouz+A+%281985%29+Contribution+%C3%A0+l%E2%80%99%C3%A9tude+g%C3%A9ochimique+et+isotopique+des+nappes+profondes+du+Sahara+nord-est+septentrional%2C+Algerie.+Dissertation%2C+University+of++Paris-Sud%2C+Orsay+++&btnG=
Houari IM (2012) Contribution to the study of the geochemical evolution of water from the table of complex terminal of the northern Sahara. Dissertation, University Kasdi Merbah, Algeria
Houben G (2003) Iron oxide incrustations in wells, parts: genesis, mineralogy and geochemistry. Appl Geochem 18:927–939
Kamel S (2011) Application of selected geothermometers to Continental Intercalaire thermal water in southern Tunisia. Geothermics 41:63–73. https://doi.org/10.1016/j.geothermics.2011.10.003
Langelier WF (1936) The analytical control of anti-corrosion water treatment. Am Water Works Assoc 28:1500–1521. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=Langelier+W.+F+%281936%29+The+Analytical+Control+of+Anti-Corrosion+Water+Treatment.+J.Am.Water+Works+Assoc+28+%3A1500-1521.&btnG=
Larroque F, Franceschi M (2011) Impact of chemical clogging on de-watering well productivity: numerical assessment. J Environ Earth Sci 64:119–131. https://doi.org/10.1007/s12665-010-0823-9
McLean W, Jankowski J, Lavitt N (2000) Groundwater quality and sustainability in an alluvial aquifer, Australia. In: Sililo O et al (eds) Groundwater, past achievements and future challenges. A Balkema, Rotterdam, pp 567–573 http://scholar.google.com/scholar_lookup?title=Groundwater%20quality%20and%20sustainability%20in%20an%20alluvial%20aquifer%2C%20Australia&author=W.%20McLean&author=J.%20Jankowski&author=N.%20Lavitt&pages=567-573&publication_year=2000
Nordstorm DK (1977) Thermochemical redox equilibrium of ZoBell’s solution. Geochim Cosmochim Acta 41:1835–1841. https://doi.org/10.1016/0016-7037(77)90215-0
Olasehinde A, Ashano EC, Oragun I (2012) Mineralogical study of gypsum occurrence from the Mutwe plain, Chad basin, North east Nigeria, using the X-ray diffraction techniques. Open Access Scientific Reports. https://doi.org/10.4172/scientificreports.546. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Olasehinde+A%2C+Ashano+EC%2C+Oragun+I+%282012%29+Mineralogical+study+of+gypsum+occurrence+from+the+Mutwe+plain%2C+Chad+basin%2C+North+east+Nigeria%2C+using+the+X-ray+diffraction+techniques.+Open+Access+Scientific+Reports.+doi+%3A10.4172%2Fscientificreports.546&btnG=
OSS (2003). Système Aquifère du Sahara Septentrional.Volume 2: Hydrogéologie, Projet SASS, Rapport interne, Direction Génerale des Ressources en Eau, Tunis, p 275. http://www.oss-online.org/sites/default/files/fichier/rapport_de_synthese_0.pdf
Papic P (1991) Scaling and corrosion potential of selected geothermal waters in Serbia. The United Nations University. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Papic+P+%281991%29+Scaling+and+corrosion+potential+of+selected+geothermal+waters+in+Serbia.+The+united+nations+university%2C+geothermal+training+programme%2C+Iceland.+&btnG=
PE UNESCO (1972) Etude des ressources en eau de Sahara septentrional. Rapport sur les résultats du projet, Paris. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=PE+UNESCO+%281972%29+Etude+des+ressources+en+eau+de+Sahara+septentrional.+Rapport+sur+les+r%C3%A9sultats+du+projet%2C+Paris%2C+1972&btnG=
Plummer LN, Jones BF, Truesdell AH (1976) WATEQF—A Fortran IV of WATEQ, a computer program for calculating chemical equilibrium of natural water. U.S Geological Survey, Washington. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Plummer+L.N%2C+Jones+BF%2C+Truesdell+AH+%281976%29+WATEQF-+A+Fortran++IV+of+WATEQ%2C++A+computer+program+for+calculating++chemical+equilibrium++of+natural+water.+Washington%2C+U.S.+Geological+Survey&btnG=
Rafferty K (1999) Scaling in geothermal heat pump systems. Prepared for: U.S. Department of Energy, Idaho Operations Office and 785 DOE Place, Idaho Falls, ID 83401. https://scholar.google.com/scholar?hl=fr&as_sdt=0%2C5&q=%EF%82%A7%09Rafferty+K+%281999%29+Scaling+in+geothermal+heat+pump+systems.+U.S.+Department+of+Energy%2C+Idaho+Operations+Office.+&btnG=
Saharawat YS, Malik RS, Jhorar BS, Streck T, Chaudhary N, Jat ML (2009) Changes in the recoverable fractions during successive cycles of aquifer storage and recovery system in North-West India. Curr Sci 97:1369–1374
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The authors wish to thank the anonymous reviewers for their constructive comments that improved the paper. We thank Jennifer and Charlie BLACK and Jemaa ESSEMINE for proofreading the manuscript.
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Essamin, R., Kamel, S. Incrustation ability of geothermal waters of the Continental Intercalaire aquifer in the Grand Erg Oriental basin (Algeria and South Tunisia). Environ Earth Sci 77, 235 (2018). https://doi.org/10.1007/s12665-018-7398-2
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DOI: https://doi.org/10.1007/s12665-018-7398-2