Self radiolysis of tritiated water
Description
The mechanism of water radiolysis implies several reactions and depends on many parameters such as the radiation characteristics (type of radiation, energy ...), the temperature and the chemical composition of irradiate water. Thus it is very difficult to foresee, without experimental data, the overall effect of these parameters. If radiolysis of pure water under γ rays or α particles has been widely studied, it is not the case for self radiolysis of tritiated water (low energy β- particles radiation). In order to fill this lack of experimental knowledge and to understand the radiolysis of stored tritiated water produced in tritium plants, we studied the evolution of hydrogen and oxygen concentrations in the gaseous phase above chemically pure tritiated water. The simulation of pure water radiolysis has been carried out and the results are compared with experimental data
Additional details
Identifiers
- DOI
- 10.1016/S0920-3796(03)00236-9;
- arXiv
- arXiv:chao-dyn/9605006v1;
- PII
- S0920379603002369;
Publishing Information
- Journal Title
- Fusion Engineering and Design
- Journal Volume
- 69
- Journal Issue
- 1-4
- Journal Page Range
- p. 57-60
- ISSN
- 0920-3796
- CODEN
- FEDEEE
Conference
- Title
- 22. symposium on fusion technology
- Dates
- 9-13 Sep 2002
- Place
- Helsinki (Finland)
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 35045674
- Subject category
- S38: RADIATION CHEMISTRY, RADIOCHEMISTRY AND NUCLEAR CHEMISTRY; S70: PLASMA PHYSICS AND FUSION TECHNOLOGY;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- BETA PARTICLES; CONCENTRATION RATIO; HYDROGEN; OXYGEN; RADIOLYSIS; TRITIUM OXIDES
- Descriptors DEC
- CHALCOGENIDES; CHARGED PARTICLES; CHEMICAL RADIATION EFFECTS; CHEMICAL REACTIONS; DECOMPOSITION; ELEMENTS; HYDROGEN COMPOUNDS; IONIZING RADIATIONS; NONMETALS; OXIDES; OXYGEN COMPOUNDS; RADIATION EFFECTS; RADIATIONS; TRITIUM COMPOUNDS; WATER
Optional Information
- Copyright
- Copyright (c) 2003 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.