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Upward groundwater flow in boils as the dominant mechanism of salinization in deep polders, The Netherlands \ Journal of hydrologic engineering [Wetenschappelijk artikel]
Louw, P.G.B. de \ Oude Essink, G.H.P. \ Stuyfzand, P.J. \ Zee, S.E.A.T.M. van der \ 2010
As upward seepage of saline groundwater from the upper aquifer is leading to surface water salinization of deep polders in the Netherlands, we monitored the processes involved in the Noordplas Polder, a typical deep polder. Our results show three typ ...
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Low-resolution modeling of dense drainage networks in confining layers \ Ground water : journal of the National Water Well Association [Wetenschappelijk artikel]
Pauw, P.S. \ Zee, S.E.A.T.M. van der \ Leijnse, A. \ Delsman, J.R. \ Louw, P.G.B. de \ Lange, W.J. de \ Oude Essink, G.H.P. \ 2014
The results indicate that the conductance expression of De Lange (1999) should be used in similar hydrogeological conditions as considered in this paper, as it is better taking into account the resistance to flow below the surface water bed. For the ...
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Regional scale impact of tidal forcing on groundwater flow in unconfined coastal aquifers \ Journal of hydrology [Wetenschappelijk artikel]
Pauw, P.S. \ Oude Essink, G.H.P. \ Leijnse, A. \ Vandenbohede, A. \ Groen, J. \ Zee, S.E.A.T.M. van der \ 2014
This paper considers the impact of tidal forcing on regional groundwater flow in an unconfined coastal aquifer. Numerical models are used to quantify this impact for a wide range of hydrogeological conditions. Both a shallow and a deep aquifer are in ...
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Fresh water lens persistence and root zone salinization hazard under temperate climate : climate proof fresh water supply in coastal areas and deltas in Europe \ Water resources management : an international journal [Wetenschappelijk artikel]
Stofberg, S.F. \ Oude Essink, G.H.P. \ Pauw, P.S. \ Louw, P.G.B. de \ Leijnse, A. \ Zee, S.E.A.T.M. van der \ 2017
In low lying deltaic areas in temperate climates, groundwater can be brackish to saline at shallow depth, even with a yearly rainfall excess. For primary production in horticulture, agriculture, and terrestrial nature areas, the fresh water availabil ...
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