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Balderer, Werner (1985) The NAGRA investigation project for the assessment of repositories for high-level radioactive waste in geological formations. Mineralogical Magazine, 49 (351) 281-288 doi:10.1180/minmag.1985.049.351.15

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Reference TypeJournal (article/letter/editorial)
TitleThe NAGRA investigation project for the assessment of repositories for high-level radioactive waste in geological formations
JournalMineralogical MagazineISSN0026-461X
AuthorsBalderer, WernerAuthor
Year1985 (April)Volume49
Issue351
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_49/49-351-281.pdf+
DOIdoi:10.1180/minmag.1985.049.351.15Search in ResearchGate
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Mindat Ref. ID3733Long-form Identifiermindat:1:5:3733:8
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Full ReferenceBalderer, Werner (1985) The NAGRA investigation project for the assessment of repositories for high-level radioactive waste in geological formations. Mineralogical Magazine, 49 (351) 281-288 doi:10.1180/minmag.1985.049.351.15
Plain TextBalderer, Werner (1985) The NAGRA investigation project for the assessment of repositories for high-level radioactive waste in geological formations. Mineralogical Magazine, 49 (351) 281-288 doi:10.1180/minmag.1985.049.351.15
In(1985, April) Mineralogical Magazine Vol. 49 (351) Mineralogical Society
Abstract/NotesAbstractThe first results of isotopic investigations as a part of the hydrogeological study of northern Switzerland are presented. This study is part of the global geological research project of the NAGRA (National Co-operative for the Storage of Radioactive Waste) which is intended to provide the scientific knowledge required for the assessment of the feasibility of safe disposal of highly radioactive waste in the geological formations of the area. The aim of the hydrogeological research programme is to assess the natural conditions in the sedimentary sequence and the underlying granite basement, by regional investigation of hydraulic parameters, isotopic composition, and hydrogeochemistry at all existing wells (boreholes and natural thermal springs) and in 11 to 12 deep-drilled boreholes (to final depth of 1500–2500 m).


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