Abstract
Wadi El-Natrun area has recently undergone extensive urban and agricultural expansion. Due to the absence of natural surface irrigation supplies, the only source of water in the area is the Pliocene groundwater aquifer. As a result, secondary salinization from increased abstractions is the major threat to the groundwater aquifer. There is a dire need for efficient strategies to ensure long-term sustainability of the area’s productive agriculture. These strategies should be based on scientific spatio-temporal monitoring and analysis of the groundwater conditions that is also lacking. To capture the spatio-temporal variability in groundwater conditions, field measurements of total dissolved solids, electrical conductivity, pH, temperature, and water level as well as lab-based ionic composition were performed on 47 groundwater samples collected during 2006 and 2007. Determinations of the hydrochemical characteristics, water types, salt assemblages, and the sodium adsorption ratio were carried out on the samples. Reference data sets recorded in 1973 and 1997 were available for the area and were used to monitor the changes occurred in these periods. Geographic information system (GIS) was appraised for mapping and for integrated analysis of the different layers. Remotely sensed change detection techniques were applied to the Landsat TM and the ETM + imageries and used to highlight the extensive reclamation and urbanization and to find key trends for the alterations in the groundwater conditions and their spatial association with land covers. Results revealed a topographic depression-induced flow pattern, predominance of leaching and dissolution processes, the presence of saline lakes, over-pumping from the Pliocene aquifer, and temporal changes in land uses are the main factors combined to control the spatio-temporal variability in the groundwater. Results also clarified the presence of two: northwestern and southeastern zones that varied distinctively in their hydrodynamic and hydrochemical characteristics. The northwestern zone showed an average water level decline of 15 m, the water of which is brackish (av. 2,037 mg/l) with dominant Na+, Cl− and SO4 2− ions. The groundwater of this zone is characterized by high to very high salinity hazard and high to very high alkali hazard and is not recommended for irrigation on soils with poor drainage and without proper management for salinity control. The southeastern zone showed water level decline less than 2 m, the water of which is fresh (av. 424 mg/l) with major Na+, HCO3 −, Cl−, and SO4 2− ions, and quality suitable for irrigation with medium to high salinity and low to medium alkali hazards. The article represents the first step towards an integrated management of Wadi El-Natrun groundwater resources within a GIS framework.
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References
Abdel-Baki AA (1983) Hydrogeological and hydrogeochemical studies on the area west of Rosetta branch and south of El Nasr canal. PhD Thesis, Faculty of Science, Ain Shams University
Abu Zeid KA (1984) Contribution to the geology of Wadi El-Natrun area and its surroundings. MSc Thesis, Faculty of Science, Cairo University
APHA (1989) Standard methods for the examination of water and wastewater, 7th edn. American Public Health Association, Washington
Atia AKM, Hilmy ME, Bolous SN (1970) Mineralogy of the incrustation deposits of Wadi El-Natrun. Desert Inst Bull 20(2):301–325
Atwia MG, Hassan AA, Ibrahim ShA (1997) Hydrogeology, log analysis, and hydrochemistry of unconsolidated aquifers south of El-Sadat City, Egypt. Hydrogeol J 5(2):27–38
Awad MA, Sallouma MK, Gomaa MA, Ezz El-Din MR (1997) Comparative hydrogeochemical and isotopic studies on groundwater in Wadi El-Farigh and Wadi El-Natrun at the fringes of Western Nile Delta, Egypt. El-Minia Sci Bull 10(1):1–22
Bishay NZ (1977) Contribution to the hydrogeology and hydrochemistry of the area to the west of the Nile Delta. Desert Inst Bull 27(2):1–23
Dassi L (2010) Use of chloride mass balance and tritium data for estimation of groundwater recharge and renewal rate in an unconfined aquifer from North Africa: a case study from Tunisia. Environ Earth Sci 60:861–871
Dassi L, Zouari K, Seiler KP, Faye S, Kamel S (2005) Flow exchange between the deep and shallow groundwaters in the Sbeitla synclinal basin (Tunisia): an isotopic approach. Environ Geol 47(4):501–511
Edmunds WM (2009) Geochemistry’s vital contribution to solving water resource problems. Appl Geochem 24(6):1058–1073
El-Awady MM, Atwia MG, El-Nikhely AH, Hamouda AZ (1997) Chemistry of groundwater in wadi El-Natrun area, Western Desert, Egypt, vol 3. The Third Conference on Geochemistry, September 3–4, Alexandria University, Faculty of Science, pp 57–67
El-Hinnawi EE, Atwa SM (1973) Geochemistry of ground waters from some localities west of the Nile Delta. Geol Rundsch 62:225–245
El-Shahat A, Ayyad SN, Abdalla MA (1997) Pliocene facies and fossil contents of Qaret El-Muluk Formation at Wadi El-Natrun Depression, Western Desert, Egypt. Facies 37:211–224
Fehdi Ch, Rouabhia A, Baali F, Boudoukha A (2009) The hydrogeochemical characterization of Morsott-El Aouinet aquifer, Northeastern Algeria. Environ Geol 58:1611–1620
Fekry AM (1993) Hydrogeological studies of the southern region west of the Nile Delta. PhD Thesis, Faculty of Science, Ain Shams University
Foster SSD, Chilton PJ (2003) Groundwater: the processes and global significance of aquifer degradation. Philos Trans R Soc Lond B 358:1957–1972
Furquim SAC, Graham RC, Barbiero L, Queiroz Neto JP, Vidal-Torrado P (2010) Soil mineral genesis and distribution in a saline lake landscape of the Pantanal Wetland, Brazil. Geoderma 154(3–4):518–528
Gaame OM (2005) Evaluation of well design west of the Nile Delta region with emphasis on Wadi El-Natrun and Wadi El-Farigh areas, vol 1. GRMENA, pp 333–343
Geirnaert W, Laeven MP (1992) Composition and history of ground water in the western Nile Delta. J Hydrol 138(1–2):169–189
General Petroleum Company (GPC) (1978) The groundwater resources of Wadi El-Natrun area. Western Desert, Egypt (unpublished report p 82)
Gomaa MAA (1995) Comparative hydrogeological and hydrogeochemical study on some aquifer west of Nile Delta, Egypt. PhD Thesis, Faculty of Science, Ain Shams University
Hantar G (1990) North Western Desert. In: Said R (ed) Geology of Egypt. A. A. Balkema, Rotterdam, pp 293–327
Howari FM, Banat KM (2002) Hydrochemical characteristics of Jordan and Yarmouk river waters: effect of natural and human activities. J Hydrol Hydromech 50(1):50
Jianhua S, Qi F, Xiaohu W, Yonghong S, Haiyang X, Zongqiang C (2008) Major ion chemistry of groundwater in the extreme arid region northwest China. Environ Geol 57:1079–1087
Khalifa MA, Abu Zeid K (1984) Sedimentological history of the Pliocene sediments in and around Wadi El-Natrun, Western Desert, Egypt. Ann Geol Surv Egypt 14:243–255
Liu C, Yu J, Kendy E (2001) Groundwater exploitation and its impact on the environment in the North China Plain. Water Int 26(2):265–272
Piper AM (1944) A graphic procedure in the geochemical interpretation of water analysis. Trans Am Geophys Union 25:914–923
Rashed MA (1991) Engineering–geological properties of Pliocene argillaceous sediments of the wadi El-Natrun Area (Egypt). Bull Int Assoc Eng Geol 44:69–77
RIGW (1992) Hydrogeological map for the Nile Delta area, Scale 1: 500000. Research Institute for Groundwater, El Kanter El Khairia, Egypt
RIGW (2004) Groundwater Inventory in western Nile Delta. Internal report. Research Institute for Groundwater, El Kanter El Khairia, Egypt
Sanad S (1973) Geology of the area between Wadi El-Natrun and the Moghra depression. PhD Thesis, Assuit University, Egypt, p 184
Shata A, El-Fayoumi I (1967) Geomorphological and morphopedological aspects of the region west of the Nile Delta with special reference to Wadi El-Natrun area. Desert Inst Bull 17:1–28
Shata AA, Pavlov M, Saad KF (1962) Preliminary report on the geology, hydrogeology, and groundwater hydrology of Wadi El-Natrun and adjacent areas. Internal Report. Desert Institute, Cairo, p 159
Shortland AJ (2004) Evaporites of the Wadi Natrun: seasonal and annual variation and its implication for ancient exploitation. Archaeometry 46:497–516
Sulin VA (1946) Waters of petroleum formations in the system of natural water. Gostoptekhiz-dat, Moscow (in Russian), pp 35–96
U.S. Salinity Laboratory Staff (1954) Diagnosis and improvement of saline and alkali soils. U.S. Department of Agriculture, Handbook 60, p 160
Zagonari F (2010) Sustainable, just, equal, and optimal groundwater management strategies to cope with climate change: insights from Brazil. Water Resour Manage. doi:10.1007/s11269-010-9630-z
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Masoud, A.A., Atwia, M.G. Spatio-temporal characterization of the Pliocene aquifer conditions in Wadi El-Natrun area, Egypt. Environ Earth Sci 62, 1361–1374 (2011). https://doi.org/10.1007/s12665-010-0623-2
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DOI: https://doi.org/10.1007/s12665-010-0623-2