Future water-rock interaction in deep repository of spent nuclear fuel
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F17%3A00000003" target="_blank" >RIV/00025798:_____/17:00000003 - isvavai.cz</a>
Result on the web
<a href="http://www.sciencedirect.com/science/journal/22120173" target="_blank" >http://www.sciencedirect.com/science/journal/22120173</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.proeps.2016.12.013" target="_blank" >10.1016/j.proeps.2016.12.013</a>
Alternative languages
Result language
angličtina
Original language name
Future water-rock interaction in deep repository of spent nuclear fuel
Original language description
A deep geological repository of spent nuclear fuel has to be safe for at least 100 thousand years. During this time, water–rock interaction on surface as well as in the rock around the repository will progress. All exogenous processes will depend on future evolution of climate. Based on the research of Quaternary sediments, three limiting scenarios of future climate evolution are considered: Maximum cooling and drying in glacial periods; maximum warming and moistening in interglacial periods and climate evolution affected by elevated concentrations of CO2 in the atmosphere. Formation of permafrost, infiltration of melted water and oxidation will influence chemical composition of ground water. Two analogues of the changes are presented. They are ground waters in two mines in the Bohemian massive: (1) Mine “Svornost” in an abandoned historical uranium deposit Jáchymov (Joachimstahl), (2) underground research facility of “Bukov” near the uranium deposit of Rožná. Ground water was sampled from surface to a depth of 1200 m. The water–rock interaction during the infiltration and flow of ground water is the cause of the observed stratification of the chemical composition. The chemical composition of the collected samples indicate a probable future composition of ground water within the repository.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
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Continuities
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Others
Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Procedia Earth and Planetary Science
ISSN
1878-5220
e-ISSN
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Volume of the periodical
17
Issue of the periodical within the volume
neuveden
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
4
Pages from-to
100-103
UT code for WoS article
000398020400026
EID of the result in the Scopus database
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