1 / 12

Fresh water lenses on saline groundwater

Fresh water lenses on saline groundwater. Dispersive Behavior of the Mixing Zone between a Shallow Freshwater Lens and Upward Seeping Saline Groundwater S.Eeman, A. Leijnse, S.E.A.T.M. van der Zee Wageningen UR, Sub-department of Soil Physics, Ecohydrology and Groundwater management.

Download Presentation

Fresh water lenses on saline groundwater

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Fresh water lenses on saline groundwater Dispersive Behavior of the Mixing Zone between a Shallow Freshwater Lens and Upward Seeping Saline Groundwater S.Eeman, A. Leijnse, S.E.A.T.M. van der Zee Wageningen UR, Sub-department of Soil Physics, Ecohydrology and Groundwater management

  2. Background • Low lying areas • Changing climate • Non-equilibrium of ground water system • Influence on land use options? • Characterization of small scale system Source: G. Oude Essink, Deltares

  3. Lens on field Scale • Most relevant for users • Mixing zone not negligible • Boundary conditions well defined

  4. δc/δz Z Methods • Numerical modeling using SUTRA • Density dependent • Unsaturated zone • Analysis of results using spatial moments of concentration change with depth

  5. Results • Comparison to the analytical solution by Maas (2007) • Analyses of dispersion and diffusion

  6. Numerical vs Maas(2007) • First vertical moment dC/dy • From initially saline towards steady state Steady state Max. thickness in time

  7. Processes contributing to mixing • Longitudinal dispersion • Transverse dispersion • Molecular diffusion • Different processes • Different circumstances • Phase • Location • Num. calculations • Local coordinate system • Parallel to “interface” • Less accurate near ditch

  8. Contributions to mixing I Moving ‘interface’ Steady state conditions

  9. 5m 15m 25m Contributions to mixing II

  10. Conclusions • Steady conditions: analytical model of Maas (2007) is a very good approximation • Contribution of dispersion and diffusion to mixing depend on phase and location • Developing lens: longitudinal dispersion • Steady state: transverse dispersion / diffusion • Mid field: BC prohibits transverse dispersion • Near ditch: transverse dispersivity

  11. Current work • Start of fieldwork in Zeeland with P. de Louw, Deltares (thanks!) • Sensitivity of a fresh water lens for different climatic conditions

  12. Thank You!

More Related