File:Groundwater flow NL.svg

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Nederlands: De lengte, diepte en residentietijd van grondwater varieert veel. Grondwaterstroomlijnen (of -stroompaden) laten de weg van grondwater op een bepaalde plek zien. Het grondwater wordt aangevuld door neerslag, gevolgd door infiltratie en percolatie in de bodem. Hoewel neerslag overal optreedt, vindt percolatie en aanvulling van het grondwater alleen in aanvullingsgebieden (Engels: recharge areas) plaats. Het grondwater stroomt dan langzaam via gekromde stroomlijnen naar de plek waar kwel (Engels: discharge areas) plaatsvindt, normaal gesproken op plekken al beekdalen, waar afvoer via oppervlaktewater (een beek of rivier) plaatsvindt. De stroomlijnen worden afgebogen in slecht-doorlaatbare lagen (aquitards). De residentietijd van grondwater kan variëren van dagen tot millennia, afhankelijk van de lengte van de stroomlijn.
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This is a retouched picture, which means that it has been digitally altered from its original version. Modifications: tranlation into Dutch. The original can be viewed here: Groundwater flow.svg: . Modifications made by Woudloper.

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This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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current08:11, 23 January 2022Thumbnail for version as of 08:11, 23 January 2022645 × 400 (226 KB)Woudloper (talk | contribs)Uploaded own work with UploadWizard

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