Noordplas Polder - Netherlands

Noordplas Polder drainage area after de Louw et al. 2011, modified

Location

latitude 52°04' N, longitude 04°34' E

Catchment size

37 km²

Climate

Maritime

long-term mean annual precipitation 916 mm

potential evapotranspiration after Makkink 615 mm

Geology

The geohydrological situation is characterized by two (semi-) confined aquifers of Pleistocene sands. The upper aquifer is covered by a 6–9 m thick, confining layer of Holocene peat, loam and clay of low permeability. At various locations, the compacted peat and overlying loam and clay deposits have been eroded by streams and tidal channels during the Holocene. The groundwater in the Pleistocene aquifers is brackish to saline and shows an increasing trend of chloride concentrations with depth.

Topography

average soil surface level is 5 m below mean sea level

Vegetation/Land use

86% is used for agriculture (arable farming 62%; pasture 24%)
14% is urban area

Context of investigation

hydrologic processes including water quality, salinisation and water management

Measurements/Equipment

Meteorological station dating from 1996 to the present are available
Runoff/ Water level monitoring
Piezometers
Soil moisture

Links to project webpages

References

de Louw,P.G.B., Vandenbohede, A., Werner, A.D., Oude Essink, G.H.P. 2013.Natural saltwater upconing by preferential groundwater discharge through boils. Journal of Hydrology, 490, 74–87, DOI: 10.1016/j.jhydrol.2013.03.025.
de Louw,P.G.B., van der Velde, Y., van der Zee, S.E.A.T.M. 2011. Quantifying water and salt fluxes in a lowland polder catchment dominated by boil seepage: a probabilistic end-member mixing approach. Hydrol. Earth Syst. Sci., 15, 2101–2117, DOI: 10.5194/hess-15-2101-2011.
de Louw,P.G.B., Oude Essink, G.H.P., Stuyfzand, P.J., van der Zee, S.E.A.T.M. 2010.Upward groundwater flow in boils as the dominant mechanism of salinization in deep polders, The Netherlands. Journal of Hydrology, 394, 494–506, DOI: 10.1016/j.jhydrol.2010.10.009.