scholarly journals Management of high-level nuclear wastes

1978 ◽  
Author(s):  
A. M. Platt ◽  
J. L. McElroy
Keyword(s):  

1996 ◽  
Vol 451 ◽  
Author(s):  
Guen Nakayama ◽  
Yuichi Fukaya ◽  
Masatsune Akashi

ABSTRACTIn the scheme for geological disposal of high level radioactive nuclear wastes, the burial pit is to be isolated from the sphere of human life by a multiple-barrier system, which consists of an artificial barrier, composed of a canister, an overpack and a bentonite cushioning layer, and a natural barrier, which is essentially the bedrock. As the greatest as well as essentially the sole detriment to its integrity would be corrosion by groundwater. The groundwater comes to it seeping through the bentonite zone, thereby attaining conceivably the pH of transition from general corrosion to passivity, pHd, the behaviors of mild steel in such a groundwater environment have been examined. It has been shown that the pHd is lowered (enlargement of the passivity domain) with rising temperature and carbonate-bicarbonate concentration, while it is raised (enlargement of the general corrosion region) with increasing concentrations of chloride and sulfate ions.



1982 ◽  
Vol 91 (1) ◽  
pp. 22 ◽  
Author(s):  
Fred A. Donath


AIP Advances ◽  
2018 ◽  
Vol 8 (4) ◽  
pp. 045221 ◽  
Author(s):  
Shinta Watanabe ◽  
Toshikazu Sato ◽  
Tomoko Yoshida ◽  
Masato Nakaya ◽  
Masahito Yoshino ◽  
...  


1999 ◽  
Author(s):  
E. Kent Barefield ◽  
Charles L. Liotta ◽  
Henry M. Neumann






2008 ◽  
Vol 28 (1) ◽  
pp. 107-117 ◽  
Author(s):  
Nesrin Demir ◽  
Gamze Genç ◽  
Taner Altunok ◽  
Hüseyin Yapıcı


2016 ◽  
Vol 80 (5) ◽  
pp. 765-780 ◽  
Author(s):  
P. Sengupta ◽  
J. Sanwal ◽  
N. L. Dudwadkar ◽  
S. C. Tripathi ◽  
P. M. Gandhi

AbstractStalagmites and stalactites, as observed within natural caves, may develop inside geological repositories during constructional and post-operational periods. It is therefore important to understand actinide sorption within such materials. Towards this, experimental studies were carried out with 233U, 238Np (VI), 238Np (IV), 239Pu and 241Am radiotracers using natural speleothem samples collected from the Dharamjali cave of the Kumaon Lesser Himalayas, India. Petrological/mineralogical studies showed that natural speleothems have three general domains: (1) columnar calcite; (2) microcrystalline calcite; and (3) botryoidal aragonite – each with ferruginous materials. Results showed that all domains of speleothems can take up >99% actinides, irrespective of valence state and pH (1–6 range) of the solution. However, distribution coefficients were found to be at a maximum in aragonite for most of the actinides. Such data are very important for long-term performance and safety assessments of the deep geological repositories planned for the disposal of high-level nuclear wastes.



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