Geological Disposal of Radioactive Waste in Clay

被引:75
作者
Grambow, Bernd [1 ]
机构
[1] Univ Nantes, CNRS IN2P3, SUBATECH Lab, UMR 6457,Mines Nantes, BP 20722, F-44307 Nantes 3, France
关键词
clay rock; geological disposal; nuclear waste; long term safety; radionuclides; TRACER DIFFUSION; RETENTION; FIELD; ROCK;
D O I
10.2113/gselements.12.4.239
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Keeping future generations safe from today's nuclear waste relies on this waste being effectively isolated for all time. Clay rocks, or rocks with a high clay content, offer promising isolation properties over time periods that are as long as the age of their host geological formations. Constructing a repository in such material does not significantly change the clay's isolation properties, which is a great advantage. Isolation is a function of the interplay between the slow release of radionuclides from the waste, the diffusion-controlled radionuclide migration, the establishment of a reducing geochemical environment, and the weak solubility and strong retention of the most toxic radionuclides on clay minerals and on additional engineered barrier materials.
引用
收藏
页码:239 / 245
页数:7
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