Filtered generated 485 hits.
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Bilaga 3 - Kärnkraftverken.pdf
2186 kB...
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Bilaga 4 - Bränslefabriken i Västerås.pdf
2486 kB...
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2016:37 PARTRIDGE project: Review and evaluation of the probabilistic fracture mechanics code PRO-LOCA
2858 kB...
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2016:40 Analys av signalsvar från simulerade bindfel
13459 kB...
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2016:36 Säker kraftförsörjning i svenska kärnkraftanläggningar? – En historisk betraktelse
1436 kB...
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2016:33 Technical Note, Översikt över mättekniker för verifiering av atypiska bränsleobjekt på Clab
1169 kB...
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2016:38 Kartläggning av värdefull natur kring Sveriges kärntekniska anläggningar
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2012:17 Technical Note, Corrosion of copper canister
It is expected that the inflow of ground water to the deposition holes and tunnels in the Forsmark repository will be very slow. Thus, it might take some few hundred years up to thousand years before the deposition holes are filled with ground water and it might take 6000 years or more before the bentonite buffer is fully water saturated and pressurized. The copper canisters will therefore...
Content type: Publications -
2011:10e Review and evaluation of the Swedish Nuclear Fuel and Waste Management Company’s RD&D Programme 2010. Statement to the Government and summary of the review report
In accordance with Section 25 of the Ordinance (1984:14) on Nuclear Activities (Nuclear Activities Ordinance), the Swedish Radiation Safety Authority (SSM) shall review and assess the research, development and demonstration programme (RD&D programme) that the reactor licensees are obligated to establish in accordance with the Act (1984:3) on Nuclear Activities (Nuclear Activities Act).
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2010:43 Displacement along extensive deformation zones at the two SKB sites: Forsmark and Laxemar
The Fennoscandian shield is distinguished by that the exposed bedrock is mainly composed of Precambrian metamorphic and igneous rocks older than a billion or one and a half billion years with few easily distinguished testimonies for the younger history. Large parts of the present ground surface closely coincides with a late Precambrian denudation surface; the sub-Cambrian peneplain.
Content type: Publications