dc.contributor.author | Hongve, Dag | |
dc.contributor.author | Jørgensen, Per | |
dc.contributor.author | Englund, Jens-Olaf | |
dc.contributor.author | Haldorsen, Sylvi | |
dc.contributor.author | Kirkhusmo, Lars A. | |
dc.date.accessioned | 2020-08-26T09:14:18Z | |
dc.date.available | 2020-08-26T09:14:18Z | |
dc.date.issued | 1992 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674298 | |
dc.description.abstract | Forkortet: 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.language.iso | nor | |
dc.relation.ispartofseries | NGU Bulletin (422) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | GRUNNVANN | |
dc.title | Groundwater contribution to a mountain stream channel, Hedmark, Norway | |
dc.type | Journal article | |
dc.description.localcode | 36276 | |
dc.source.pagenumber | 3-14 | |