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Modeling of Groundwater Pollution by Former Seawater in Submarine Groundwater Discharge Driven by Saltwater Intrusion

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Coastal aquifers are usually vulnerable to contamination by saltwater intrusion. The degree of contamination depends on the amount of former seawater intruding the aquifer as submarine groundwater discharge (SGD). A three-dimensional numerical SEAWAT model was developed to provide insights to the responses of saltwater intrusion and amount of seawater portion of SGD, to groundwater withdrawal from four wells at different spatial locations. The results showed that saltwater wedge encroachment varies with a withdrawal rate and well location. Increasing withdrawal rates from 0.165 m3/s to 0.53166 m3/s resulted in a noticeable increase in wedge encroachment into the aquifer from 589 m to 1319 m, respectively, regardless of the distance from the coastline. However, higher withdrawals from the wells closer to the coastline caused the hydraulic head near the seaside to drop below the terrestrial head, causing the saltwater wedge to be pushed back toward the sea. Simulations also showed that a coastal well might act as a hydraulic barrier that prevents the brackish zone from moving further inland, which is critically important in terms of groundwater management. Seawater contributed from 5% to above 33% in SGD. Although the withdrawal rates from Well 3 were 10 to 20 times larger than the Well 2 rates, the seawater contribution associated with Well 3 was about the same. This is attributed to the horizontal vicinity of Well 2 to the seacoast boundary compared to Well 3 even though Well 3 is deeper than Well 2, demonstrating that it is the horizontal location that governs the amount of abstracted former seawater.
Rocznik
Strony
166--175
Opis fizyczny
Bibliogr. 32 poz., rys., tab.
Twórcy
  • Department of Environmental Engineering, College of Engineering, University of Babylon, Babylon 51001, Iraq
autor
  • Housing, Municipalities and Public Works, Soil Investigation Section, Construction Laboratories, Ministry of Construction, Babylon 51001, Iraq
Bibliografia
  • 1. Al-Taliby W., Pandit A. 2017. Comparison of solutions of coupled and uncoupled models for the Henry problem. World Environmental and Water Resources Congress, 89–102.
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  • 4. Bear J., Cheng A.H., Sorek S., Ouazar D., Herrera I. 1999. Seawater intrusion in coastal aquifers: concepts, methods and practices Springer Science & Business Media. The Netherlands: Kluwer Academic Publishers, 14.
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  • 6. Crusius J., Koopmans D., Bratton J.F., Charette M.A., Kroeger K., Henderson P., Colman J.A. 2005. Submarine groundwater discharge to a small estuary estimated from radon and salinity measurements and a box model. Biogeosciences, 2(2), 141–157.
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  • 8. Diersch H.J. 2002. FEFLOW finite element subsurface flow and transport simulation system: DHI-WASY Software. reference manual, DHI-WASY GmbH. Institute for Water Resources Planning and Systems Research, Berlin, Germany, 3, 42.
  • 9. Guo W., Langevin C.D. 2002. User’s Guide to SEAWAT: A Computer Program for Simulation of Three-Dimensional Variable-Density Ground-Water Flow. Techniques of Water-Resources Investigations 6-A7, USGS, Tallahassee, Florida.
  • 10. Hem J.D. 1989. Study and interpretation of the chemical characteristics of natural water (3d ed.): Department of The Interior William P. Clark, Secretary, U.S. Geological Survey Water-Supply Paper 2254, Dallas L. Peck, Director, 272.
  • 11. Henry H.R. 1964. Effects of dispersion on salt encroachment in coastal aquifers, sea water in coastal aquifers. U.S. Geological Survey Water-Supply Paper 1613-C, 70–84, United States Government Printing Office, Washington, 95.
  • 12. Langevin C.D., Thorne D.T., Dausman A.M., Sukop M.C., Guo W., 2008. SEAWAT Version 4: A Computer Program for Simulation of Multi-Species Solute and Heat Transport: U.S. Geological Survey Techniques and Methods Book, 6, 44.
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  • 17. NOAA (National Oceanic and Atmospheric Administration). 1998. Pressures on coastal environments: Population: Distribution, density and growth, in State of the Coast Report, 33.
  • 18. NOAA’s State of the Coast. 2013. National Coastal Population Report: Population Trends from 1970 to 2020. National Oceanic and Atmospheric Administration, Department of Commerce, developed in partnership with the U.S. Census Burea, 22.
  • 19. Pinder G.F., Cooper Jr. H. 1970.Anumerical technique for calculating the transient position of the saltwater front. Water Resources Research, 6(3), 875–882.
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  • 28. Valiela I., Bowen J.L., Kroeger K.D. 2002. Assessment of models for estimation of land-derived nitrogen loads to shallow estuaries. Applied Geochemistry, 17(7), 935–953.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-dd4c294f-5057-4589-91ca-31b2dea8fbd7
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