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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

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

  • 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

  • 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