• Aqueous geochemistry of the Romerike area, southern Norway 

      Jørgensen, Per; Østmo, Svein Roar; Stuanes, Arne O. (NGU Bulletin (420), Journal article, 1990)
      Groundwater flowing through the sandy glaciofluvial deposits at Romerike has an average residence time of 30 years. The most important processes taking place along its flowpaths are dissolution of low-Mg calcite and ...
    • Groundwater contribution to a mountain stream channel, Hedmark, Norway 

      Hongve, Dag; Jørgensen, Per; Englund, Jens-Olaf; Haldorsen, Sylvi; Kirkhusmo, Lars A. (NGU Bulletin (422), Journal article, 1992)
      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 ...
    • Hydrogeology in the Romerike area, southern Norway 

      Jørgensen, Per; Østmo, Svein Roar (NGU Bulletin (418), Journal article, 1990)
      A hydrogeological model has been developed on the basis of field observat- ions and data collected during the International Hydrological Decade. From water balance studies it was found that half the annual precipitation ...
    • Kvartærgeologiske undersøkelser i Randsverkområdet, Jotunheimen. 

      Jørgensen, Per (NGU (228), Journal article, 1964)
      A short account is given of the Late Pleistocene deglaciation and drainage in an area of Jotunheimen (fig. 2). Already at the beginning the mountain tops emerges through the ice sheet, and it is possible to follow the ...