I-131(-) sorption by thermally treated hydrotalcites

Citation
Mt. Olguin et al., I-131(-) sorption by thermally treated hydrotalcites, CLAY CLAY M, 46(5), 1998, pp. 567-573
Citations number
24
Categorie Soggetti
Environment/Ecology,"Earth Sciences
Journal title
CLAYS AND CLAY MINERALS
ISSN journal
00098604 → ACNP
Volume
46
Issue
5
Year of publication
1998
Pages
567 - 573
Database
ISI
SICI code
0009-8604(199810)46:5<567:ISBTTH>2.0.ZU;2-G
Abstract
The sorption capacity of hydrotalcite (HT) and its calcined product (CHT) w as evaluated for I-131(-) sorption from water solution and it was determine d as a function of the calcining temperature. The radionuclide content was determined by gamma-spectrometry. Solids were characterized by thermal anal ysis, X-ray diffraction (XRD), electron microscopy and Brunauer-Emmett-Tell er (BET) analysis. For 0.1 M Na I solution, labeled with I-131(-), sorption capacity was found to be 0.24 meg g(-1) (7.2% of the anion exchange capaci ty, AEC). But, if the sample was previously calcined at 773 K and the HT st ructure destroyed, the sorption of I- increased considerably, up to 2.08 me g g(-1) (63% of the AEC) and the HT structure was reconstructed. The I-131( -) sorption at very low concentrations (10(-14) M) was 0.04 x 10(-14) meg o f I-131(-) g(-1) in the noncalcined HT, but for calcined samples at 773 K, the sorption increased to circa 0.97 X 10(-14) meg g(-1). Calcination tempe rature determines the surface area of the resulting mixed oxides, and that property seems to be the most important factor controlling the I- sorption. If the calcination temperature was increased to 873 K, the specific surfac e area of the oxide mixture increased and I- sorption increased as well, wh ereas calcination of HT at 973-1073 K resulted in a low surface area and a low I- retention.