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dc.contributor.authorHenriksen, Helge
dc.contributor.authorSoldal, Oddmund
dc.contributor.authorRye, Noralf
dc.coverage.spatial13173 Kvamsøy
dc.date.accessioned2020-08-26T09:14:52Z
dc.date.available2020-08-26T09:14:52Z
dc.date.issued1996
dc.identifier.urihttps://hdl.handle.net/11250/2674310
dc.description.abstractA shallow alluvial aquifer in Esebotn, Sogn og Fjordane, Norway has been investigated from a hydrological standpoint in order to obtain estimates of groundwater transit times. Water levels, oxygen isotopes, water temperatures and precipitation were monitored over a one-year period. Groundwater transit times were calculated applying a traditional Darcyan approach and by using oxygen isotopes and temperaturee as tracers. All methods give transit times of 60-90 days. The oxygen isotopes indicate that groundwater recharge due to infil tration from the river Ygleelvi makes up about 80% of the total groundwater recharge in the central parts of the aquifer during the summer season.
dc.language.isoeng
dc.relation.ispartofseriesNGU Bulletin (431)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectVANNKVALITET
dc.subjectGRUNNVANN
dc.titleGroundwater transit times in a small coastal aquifer at Esebotn, Sogn og Fjordane, western Norway
dc.typeJournal article
dc.description.localcode49104
dc.source.pagenumber5-17


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    Artikler fra seriene NGU, NGU Bulletin og NGU Skrifter

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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal