Calculation of radionuclides 90Sr and 239Pu releasing amount from melt glass
Description
Assumed the melt glass consists of spheres with uniformly size and nuclides' content, the mathematical expression is deduced to calculate nuclide releasing rates. According to the glass dissolution rate measured by Livermore laboratory, the lower and upper dissolution rates of granitic melt glass are estimated to be 5.04 × 10-7 g/(m2·d) and l.42 × 10-4 g/(m2·d) at 25 ℃. The releasing rates and ratios of 90Sr and 239Pu are calculated and from the result it can be concluded the radionuclide dissolution rate and ratio at high temperature stage is l04∼5 times higher than at normal temperature and that nuclides dissolution largely takes place at high temperature stage. The dissolution ratio of 90Sr might between 0.3% and 65%, the dissolution ratio of 239Pu might between 0.5% and 82%. The key factors affecting nuclides release are temperature, glass dissolution rate and reactive surface area. (authors)
Additional details
Publishing Information
- Journal Title
- Radiation Protection (Taiyuan)
- Journal Volume
- 33
- Journal Issue
- 3
- Journal Page Range
- p. 151-157
- ISSN
- 1000-8187
INIS
- Country of Publication
- China
- Country of Input or Organization
- China
- INIS RN
- 49042677
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- DISSOLUTION; GLASS; PLUTONIUM 239; STRONTIUM 90; SURFACE AREA; TEMPERATURE RANGE 0400-1000 K
- Descriptors DEC
- ACTINIDE NUCLEI; ALKALINE EARTH ISOTOPES; ALPHA DECAY RADIOISOTOPES; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; EVEN-EVEN NUCLEI; EVEN-ODD NUCLEI; HEAVY NUCLEI; INTERMEDIATE MASS NUCLEI; ISOTOPES; NUCLEI; PLUTONIUM ISOTOPES; RADIOISOTOPES; SPONTANEOUS FISSION RADIOISOTOPES; STRONTIUM ISOTOPES; SURFACE PROPERTIES; TEMPERATURE RANGE; YEARS LIVING RADIOISOTOPES
Optional Information
- Notes
- 6 figs., 1 tab., 5 refs.