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Elevated erosion surfaces were used as an independent data set in an integrated study of the landscape development in central West Greenland.The study resulted in a time-constrained model describing m...
During the last decades several wells giving yields up to 100,000 llh have been drilled in the reddish Brumunddal Sandstone, which covers an area of approximately 10 km2 near lake Mjosa, Southern No...
Langtjern is an acid lake situated in south-central Norway, 516 m above sea level. The watershed is underlain by biotite gneisses and granites. Coniferous forests cover 63% of the watershed, while 1...
Input of neutral salt, primarily NaCI, from sea spray is an important factor for shortterm acidification of surface water, primarily in already acidified areas, because Na may substitute for H+ and ...
We conducted a 3-year artificial deepening of the thermocline in the dimictic Lake Breisjøen, southern Norway, by means of a large submerged propeller. An adjacent lake served as untreated refe...
Controls of stream water NO3 in mountainous and forested catchments are not thoroughly understood. Long-term trends in stream water NO3 are positive, neutral and negative, often apparently independent...
As part of the national monitoring programme for long-range transported air pollutants, four groundwater aquifers in southern Norway were monitored for acidification trends during the period 1980 – 19...
We compare 5 years of meteorological records from automatic weather stations (AWSs) on Storbreen and Midtdalsbreen, two glaciers in southern Norway, located approximately 120 km apart. The records are...
The acidification model MAGIC was used to predict recovery of small lakes in southernmost Norway to future reduction of acid deposition. A set of 60 small headwater lakes was sampled annually from eit...
Shallow-levelplutonscausedextensivecontactmetamorphismofLowerPaleozoicshaleandcarbonatesequencesinthePermianOsloRift.A500mlongand100mwideshale- limestonexenolithembeddedwithinmonzonitesbelongingtothe...
The Numedal River basin (6000 km2) in central and east Norway contains 3 × 109 m3 of clayey material, corresponding to a clay loam sediment, which contains 2 million tons of absorbed rare earth elemen...

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