Aqueous geochemistry of the Romerike area, southern Norway

dc.contributor.author	Jørgensen, Per
dc.contributor.author	Østmo, Svein Roar
dc.contributor.author	Stuanes, Arne O.
dc.date.accessioned	2020-08-26T09:07:36Z
dc.date.available	2020-08-26T09:07:36Z
dc.date.issued	1990
dc.identifier.uri	https://hdl.handle.net/11250/2674192
dc.description.abstract	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 sillicates. The decalcified zone which formed during postglacial time is about 10 m thick. The acid consumed in weathering processes is mainly CO2 formed in the unsaturated zone. Oxidation of sulphides as well as leaching of old sea salt change the composition of the groundwater.
dc.language.iso	nor
dc.relation.ispartofseries	NGU Bulletin (420)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	GRUNNVANN
dc.title	Aqueous geochemistry of the Romerike area, southern Norway
dc.type	Journal article
dc.description.localcode	36268
dc.source.pagenumber	57-67

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