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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 7
Hydrol. Earth Syst. Sci., 15, 2101–2117, 2011
https://doi.org/10.5194/hess-15-2101-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 15, 2101–2117, 2011
https://doi.org/10.5194/hess-15-2101-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 07 Jul 2011

Research article | 07 Jul 2011

Quantifying water and salt fluxes in a lowland polder catchment dominated by boil seepage: a probabilistic end-member mixing approach

P. G. B. de Louw1, Y. van der Velde2,3, and S. E. A. T. M. van der Zee2 P. G. B. de Louw et al.
  • 1Deltares, Department Soil and Groundwater, P.O. Box 85467, 3508 AL Utrecht, The Netherlands
  • 2Wageningen University, Environmental Sciences Group, Soil Physics, Ecohydrology and Groundwater Management, P.O. Box 47, 6700 AA Wageningen, The Netherlands
  • 3Wageningen University, Environmental Sciences Group, Hydrology and quantitative water management, P.O. Box 47, 6700 AA Wageningen, The Netherlands

Abstract. Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in the Netherlands. Identifying measures to reduce the salt content requires a thorough understanding and quantification of the dominant sources of water and salt on a daily basis. However, as in most balance studies, there are large uncertainties in the contribution from groundwater seepage. Taking these into account, we applied a probabilistic (GLUE) end-member mixing approach to simulate two years of daily to weekly observations of discharge, salt loads and salt concentration of water pumped out of an artificially drained polder catchment area. We were then able to assess the contribution from the different sources to the water and salt balance of the polder and uncertainties in their quantification. Our modelling approach demonstrates the need to distinguish preferential from diffuse seepage. Preferential seepage via boils contributes, on average, 66 % to the total salt load and only about 15 % to the total water flux into the polder and therefore forms the main salinization pathway. With the model we were able to calculate the effect of future changes on surface water salinity and to assess the uncertainty in our predictions. Furthermore, we analyzed the parameter sensitivity and uncertainty to determine for which parameter the quality of field measurements should be improved to reduce model input and output uncertainty. High frequency measurements of polder water discharge and weighted concentration at the outlet of the catchment area appear to be essential for obtaining reliable simulations of water and salt fluxes and for allotting these to the different sources.

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