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dc.contributor.authorPastoors MJH
dc.date.accessioned2012-12-12T16:54:22Z
dc.date.available2012-12-12T16:54:22Z
dc.date.issued1992-11-30
dc.identifier714305005
dc.identifier.isbn90-6960-025-0
dc.identifier.urihttp://hdl.handle.net/10029/258322
dc.description.abstractAbstract niet beschikbaar
dc.description.abstractThis report describes the average change in the phreatic groundwater level and to the increase or decrease of the seepage for eight scenarios. The scenarios are composed within the framework of the National Policy Plan for Drinking and Industrial Water Supply for the Netherlands. Several types of groundwater abstractions are distinguished, namely abstractions from phreatic and semi-confined aquifers and riverbank infiltration. In the scenarios the yearly amount of groundwater is increased or decreased, related to the abstracted quantity in 1988. The calculations are carried out with the "Groundwater Model for the Netherlands (LGM)".
dc.description.sponsorshipDGM/DWL
dc.format.extent77 p
dc.language.isonl
dc.relation.ispartofRIVM Rapport 714305005
dc.relation.urlhttp://www.rivm.nl/bibliotheek/rapporten/714305005.html
dc.subject13nl
dc.subjectwiskundig modelnl
dc.subjectsimulatienl
dc.subjectgrondwaternl
dc.subjectwaterstandnl
dc.subjectnederlandnl
dc.subjectgeografisch informatiesysteemnl
dc.subjectmodellingen
dc.subjectsimulationen
dc.subjectfinite elementsen
dc.subjectgisen
dc.subjectgroundwateren
dc.subjectwater levelsen
dc.subjectnetherlandsen
dc.subjecteindige elementen methodeen
dc.titleLandelijk Grondwater Model; berekeningsresultatennl
dc.title.alternativeGroundwater Model for the Netherlands (LGM); resultsen
dc.typeOnderzoeksrapport
dc.date.updated2012-12-12T16:54:22Z
html.description.abstractAbstract niet beschikbaar
html.description.abstractThis report describes the average change in the phreatic groundwater level and to the increase or decrease of the seepage for eight scenarios. The scenarios are composed within the framework of the National Policy Plan for Drinking and Industrial Water Supply for the Netherlands. Several types of groundwater abstractions are distinguished, namely abstractions from phreatic and semi-confined aquifers and riverbank infiltration. In the scenarios the yearly amount of groundwater is increased or decreased, related to the abstracted quantity in 1988. The calculations are carried out with the "Groundwater Model for the Netherlands (LGM)".


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