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

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Figure

Fig. 1. The geohydrology and water and salt fluxes in a lowland polder catchment area. Upward groundwater seepage from the upper aquifercan be divided into three different types according to De Louw et al
Fig. 2. Set up of the monitoring network of the Noordplas Polder and the location of the sandy paleochannel belts and boils (adapted fromDe Louw et al., 2010).
Table 1. Summary of monitoring data of Noordplas Polder for period 1 August 1999 up to 1 August 2001.
Table 3. “Goodness-of-fit” criteria (likelihoods) and cut-off criteria. Model runs are only assigned as behavioural when they satisfy all theindividual goodness-of-fit criteria.
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