Groundwater flow paths in a glacially affected flat area in the Netherlands

R. Dijksma; S.H. Menkveld; G. Bier; A.T. Osterhof

Groundwater flow paths in a glacially affected flat area in the Netherlands

R. Dijksma, S.H. Menkveld, G. Bier, A.T. Osterhof

Research output: Contribution to journal › Article › Academic › peer-review

Abstract

Well field Garyp is abstracting deep groundwater from fluvioglacial sediments, which are covered by glacio-lacustrine clay. This drinking water abstraction is hampered by rapid salinization of the abstraction wells. A detailed ground-water modelling study was done, to reveal the water pathways and the groundwater-surface water interaction. It was concluded that shutting down wells, nor reducing abstraction rates or reduction of well screen depth would result in significantly less abstracted water from brackish layers.

Original language	English
Journal	Bodenkultur
Volume	65
Issue number	3-4
Publication status	Published - 2015

Keywords

Groundwater hydrology
Groundwater-surface water interaction
MODFLOW modeling
Salinity

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http://www.boku.ac.at/en/fos/themen/die-bodenkultur/inhalte/band-65-2014/band-65-heft-3-4/dijksma/

Cite this

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title = "Groundwater flow paths in a glacially affected flat area in the Netherlands",

abstract = "Well field Garyp is abstracting deep groundwater from fluvioglacial sediments, which are covered by glacio-lacustrine clay. This drinking water abstraction is hampered by rapid salinization of the abstraction wells. A detailed ground-water modelling study was done, to reveal the water pathways and the groundwater-surface water interaction. It was concluded that shutting down wells, nor reducing abstraction rates or reduction of well screen depth would result in significantly less abstracted water from brackish layers.",

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year = "2015",

language = "English",

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journal = "Bodenkultur",

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T1 - Groundwater flow paths in a glacially affected flat area in the Netherlands

AU - Dijksma, R.

AU - Menkveld, S.H.

AU - Bier, G.

AU - Osterhof, A.T.

PY - 2015

Y1 - 2015

N2 - Well field Garyp is abstracting deep groundwater from fluvioglacial sediments, which are covered by glacio-lacustrine clay. This drinking water abstraction is hampered by rapid salinization of the abstraction wells. A detailed ground-water modelling study was done, to reveal the water pathways and the groundwater-surface water interaction. It was concluded that shutting down wells, nor reducing abstraction rates or reduction of well screen depth would result in significantly less abstracted water from brackish layers.

AB - Well field Garyp is abstracting deep groundwater from fluvioglacial sediments, which are covered by glacio-lacustrine clay. This drinking water abstraction is hampered by rapid salinization of the abstraction wells. A detailed ground-water modelling study was done, to reveal the water pathways and the groundwater-surface water interaction. It was concluded that shutting down wells, nor reducing abstraction rates or reduction of well screen depth would result in significantly less abstracted water from brackish layers.

KW - Groundwater hydrology

KW - Groundwater-surface water interaction

KW - MODFLOW modeling

KW - Salinity

M3 - Article

VL - 65

JO - Bodenkultur

JF - Bodenkultur

SN - 0006-5471

IS - 3-4

ER -

Groundwater flow paths in a glacially affected flat area in the Netherlands

Abstract

Keywords

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