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Groundwater Contamination of Wadi Haliy Area, Southwestern Arabian Shield, Saudi Arabia

  • Saleh A. BajabaaEmail author
Chapter
Part of the Regional Geology Reviews book series (RGR)

Abstract

Contamination of surface water, groundwater, sediment, and atmosphere by heavy metals and radionuclide is among the most significant issues facing the Kingdom. Wadi Haliy is considered as important source of water to the Red Sea coastal plain. Copper, zinc and other base-metals mineralization occur in the Precambrian Arabian shield rocks that dominate the water catchments area of this wadi. The water samples were analyzed for major, trace elements and heavy metals using collaborative techniques. The groundwaters in Wadi Haliy are of Cl–SO–Na–Ca type. The variation in water type indicates variation in natural processes such as evaporation, differences in rock units and mineralization, water rock interactions and water residence time. The data analyses showed some samples are of high heavy metals and uranium contents. Pollution by heavy metals and uranium arises mainly from neighboring rocks and also from emissions from mining activities. Generally, the uranium and heavy metal contents are higher in samples collected from the upstream area of the wadi where the crystalline rocks are exposed and in direct contact with the runoff. The Elevated heavy metal and uranium contents suggests that these mining areas are considered as potential sources for these natural pollutants and likely affecting the water quality in these wadis. The attenuation of heavy metals and uranium is reported in this study along the flow path, from the mining area to downstream. The processes governing the evolution of the leachates plume and its heavy metals budget are modeled in two steps: (1) Neutralization of acidic mine drainage water; (2) Heavy metal attenuation by adsorption, evaporation and co-precipitation with Fe oxides.

Keywords

Wadi Halyi Groundwater of Saudi Arabia Groundwater contamination Water pollution 

References

  1. Al-Hageri FY (1977) Groundwater studies of Wadi Qudaid. Institute of Applied Geology, King Abdulaziz University, Jeddah, Saudi Arabia. Research series no. 2. 132–178Google Scholar
  2. Al-Jarash MA (1989) The climatic water balance in Saudi Arabia 1970–1986. Scientific Publishing Centre, King Abdulaziz University, Jeddah, Saudi Arabia, 441 ppGoogle Scholar
  3. Al-Turki AL (2010) Assessment of well drinking water quality in Hail Region of North Central Saudi Arabia. J Agric Vet Sci 2(2):101–110Google Scholar
  4. Camp VE (1984) Island arcs and their role in the evolution of the western Arabian Shield. Geol Soc Am Bull 95:913–921CrossRefGoogle Scholar
  5. Dames and Moore (1978) Representative basin study for wadis. Yiba, Habonah, Tabalah, Liyyah and Lith, Saudi Arabia 52Google Scholar
  6. Giese U, Moller P, Munzberg S (1991) Mobilization of metals in granitoids. In: Pagel M, Leory JL (eds) Source, transport and deposition of metals. Balkema, Rotterdam, pp 49–52Google Scholar
  7. Heidmann I (2004) Influence of fulvic acid on ion binding and colloidal stability of kaolinite particles, Ph.D. thesis unpublished, University of Kiel, Germany, 117 ppGoogle Scholar
  8. Hua MS, Huang CC, Yang YJ (1996) Chronic elemental mercury intoxication: neuropsychological follow-up case study. Brain Inj 10:377–384CrossRefGoogle Scholar
  9. Huet PM, Guillaume E, Cote J, Légaré A, Lavoie P, Noncirrhotic Viallet A (1975) Presinusoidal portal hypertension associated with chronic arsenical intoxication. Gastroenterology 68(5):1270–1277Google Scholar
  10. Hussain G, Alquwaizany A, Al-Zarah A (2010) Guidelines for irrigation water quality and water management in the Kingdom of Saudi Arabia: an overview. J Appl Sci 10(2):79–96CrossRefGoogle Scholar
  11. Johnson PR (2000) Proterozoic geology of Saudi Arabia: current concepts and issues. In: Contribution to a workshop on the geology of the Arabian Peninsula, 6th meeting of the Saudi Society for earth science, King Abdulaziz City for Science and Technology, Riyadh, Saudi Arabia, 32 ppGoogle Scholar
  12. Johnson PR (2006) Explanatory notes to the map of proterozoic geology of western Saudi Arabia. Technical report SGS-Tr-2006-4Google Scholar
  13. Koçak M, Akçil E (2006) The effects of chronic cadmium toxicity on the hemostatic system. Pathophysiol Haemost Thromb 35(6):411–416CrossRefGoogle Scholar
  14. Levy DB, Barbarick KA, Siemer EG, Sommers LE (1992) Distribution and partitioning of trace metals in contaminated soils near Leadville, Colorado. J Environ Qual 21:185–195CrossRefGoogle Scholar
  15. Nwankwo EA, Ibrahim U (2006) Environmental lead intoxication and chronic kidney disease: a review. Internet J Nephrol 3(1)Google Scholar
  16. Pierzynski GM, Schnoor JL, Banks MK, Tracy JC, Licht LA, Erickson LE (1994) Vegetative remediation at superfund sites, mining and its environmental impact. In: Hester RE, Harrison RM (eds) Issues in environmental science and technology. Royal Society of Chemistry, vol 1, pp 49–69Google Scholar
  17. Prinz WC (1983) Geologic map of the Al Qunfudhah quadrangle, sheet 19E, Kingdom of Saudi Arabia: Saudi Arabian Deputy Ministry of Mineral Resources Geoscience Map GM-70 A, C, scale 1:250,000; text, 19pGoogle Scholar
  18. Rechcigl JE (1995) Soil amendments and environmental quality. Soil and Water Science Department, Research and Education Center, Ona, FloridaGoogle Scholar
  19. Stoeser DB (1986) Distribution and tectonic setting of plutonic rocks of the Arabian Shield. J Afr Earth Sci 4:21–46Google Scholar
  20. Stoeser DB, Camp VE (1985) Pan-African microplate accretion of the Arabian Shield. Bull Geol Soc Am 6:817–826CrossRefGoogle Scholar
  21. Stoeser DB, Whitehouse MJ, Stacey JS (2001) The Khida terrane-geology of Paleoproterozoic rocks in the Muhayil area, Eastern Arabian Shield, Saudi Arabia (Abstract). Int Geosci J Gondwana Res 4(2):192–194CrossRefGoogle Scholar
  22. Thornton I (1983) Applied environmental geochemistry. Academic Press, London, 501p. Research volume 2, no 7, pp 1–17, July 2011Google Scholar
  23. Taha M, Harb S, Nagib M, Tantawy A (1981) The climate of the Near East. In: Climates of southern and western Asia, vol 9. Elsevier, New York, pp 183–229Google Scholar
  24. Zaidi FK, Nazzal Y, Jafri MK, Naeem M, Ahmed I (2015) Reverse ion exchange as a major process controlling the ground-water chemistry in an arid environment: a case study from northwestern Saudi Arabia. Environ Monit Assess 187:607CrossRefGoogle Scholar

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© Springer Nature Switzerland AG 2020

Authors and Affiliations

  1. 1.Faculty of Earth Sciences, Hydrogeology DepartmentKing Abdulaziz UniversityJeddahSaudi Arabia

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