|
|
|
|
| LEADER |
02535nmm a2200265 u 4500 |
| 001 |
EB000320411 |
| 003 |
EBX01000000000000000157624 |
| 005 |
00000000000000.0 |
| 007 |
cr||||||||||||||||||||| |
| 008 |
120214 ||| eng |
| 020 |
|
|
|a 9789264060579
|
| 245 |
0 |
0 |
|a Stability and Buffering Capacity of the Geosphere for Long-term Isolation of Radioactive Waste
|h Elektronische Ressource
|b Application to Crystalline Rock
|c Organisation for Economic Co-operation and Development and Nuclear Energy Agency
|
| 260 |
|
|
|a Paris
|b OECD Publishing
|c 2009
|
| 300 |
|
|
|a 302 p.
|c 20 x 27cm
|
| 505 |
0 |
|
|a Examples of Key Processes Affecting the Geosphere for Crystalline Rock -- Conclusions -- Scope and Objectives of the Workshop -- Poster Session -- Arguments to Support Confidence in the Stability of Crystalline Rocks as Potential Host Formations -- Poster Session: Summary of Posters -- General Framework: Crystalline Rocks as Host Formations -- Response and Resilience of Crystalline Rock to Natural Perturbations and Geosphere Evolution (Buffering) -- Synthesis of the Workshop -- Introduction
|
| 653 |
|
|
|a Nuclear Energy
|
| 710 |
2 |
|
|a Organisation for Economic Co-operation and Development
|
| 710 |
2 |
|
|a Nuclear Energy Agency
|
| 041 |
0 |
7 |
|a eng
|2 ISO 639-2
|
| 989 |
|
|
|b OECD
|a OECD Books and Papers
|
| 490 |
0 |
|
|a Radioactive Waste Management
|
| 028 |
5 |
0 |
|a 10.1787/9789264060579-en
|
| 856 |
4 |
0 |
|a oecd-ilibrary.org
|u https://doi.org/10.1787/9789264060579-en
|x Verlag
|3 Volltext
|
| 082 |
0 |
|
|a 333
|
| 520 |
|
|
|a Geological settings selected as potential host formations for the deep geological disposal of radioactive waste are chosen for, among other assets, their long-term stability and buffering capacity against destabilising events and processes. These proceedings present the outcomes of a geosphere stability workshop, held in November 2007, that focused on crystalline and other types of hard, fractured rocks. The workshop underscored the fact that many such rocks are intrinsically stable environments that evolve extremely slowly and provide good buffering against external events and processes. The proceedings show a good understanding of the processes and events that can affect crystalline rocks and, although there is less confidence in predicting exactly when and where such events will occur and the volume of rock that will be affected, the extent of the impacts on a geological repository can be confidently addressed using bounding approaches supported by geological information from similar sites around the world
|