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dc.contributor.authorHongve, Dag
dc.contributor.authorJørgensen, Per
dc.contributor.authorEnglund, Jens-Olaf
dc.contributor.authorHaldorsen, Sylvi
dc.contributor.authorKirkhusmo, Lars A.
dc.description.abstractForkortet: The Skvaldra stream in Hedmark, Southern Norway is characterized by a stable baseflow. This baseflow is controlled by a significant groundwater supply from Quaternary deposits. The area was chosen for an attempt at quantification of the baseflow's three groundwater components; (i) groundwater from numerous springs on a spring-horizon at the boundary between permeable sediment-flow deposits in the upper valley side and compact basal till deposited along the lower part of the valley sides and the valley bottom; (ii) groundwater from aquifers in compact basal till, topographically lower than the spring horizon; (iii) deep groundwater from till or underlying bedrock. Flood events in the Skvaldra are due to surface run-off, usually confined to the valley bottom along the stream channel, or due to very shallow subsurface interflow, with very little or no groundwater component.
dc.relation.ispartofseriesNGU Bulletin (422)
dc.rightsNavngivelse 4.0 Internasjonal
dc.titleGroundwater contribution to a mountain stream channel, Hedmark, Norway
dc.typeJournal article

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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