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Groundwater ages in coastal aquifers
Post, V.E.A.; Vandenbohede, A.; Werner, A.D.; Maimun; Teubner, M.D. (2013). Groundwater ages in coastal aquifers. Adv. Water Resour. 57: 1-11. dx.doi.org/10.1016/j.advwatres.2013.03.011
In: Advances in Water Resources. Elsevier: Southampton. ISSN 0309-1708, more
Peer reviewed article  

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Author keywords
    Coastal aquifer; Groundwater age; Numerical model; Seawater intrusion

Authors  Top 
  • Post, V.E.A.
  • Vandenbohede, A., more
  • Werner, A.D.
  • Maimun
  • Teubner, M.D.

Abstract
    The interpretation of groundwater ages in coastal aquifers requires an improved understanding of relationships between age distributions and the processes accompanying dispersive, density-dependent flow and transport. This study uses numerical modeling to examine the influence of mixing and a selection of other hydrogeological factors on steady-state age distributions in coastal aquifers. Three methods of age estimation are compared: the piston flow age, the direct age, and the tracer-based age. These are applied to various forms of the Henry problem, as well as to three variants of a larger, hypothetical coastal aquifer. Circulation of water within the seawater wedge results in markedly higher ages in the transition zone than in the underlying saltwater or overlying freshwater. Piston flow ages show a sharp increase where the freshwater and saltwater systems meet, whereas direct- and tracer-based simulations result in a smoother age distribution, as expected. Greater degrees of mixing result in larger differences between piston flow and direct or tracer-based ages, and bring about lower ages in the saltwater wedge. Tracer-based ages are preferred over direct-and piston flow ages for comparison with field data, especially in cases with wide transition zones. Despite the relatively simple conditions used for the simulations, complex age distributions with depth were obtained. Hence, the assessment of ages in field cases will be difficult, particularly where accurate ages in the transition zone are sought.

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