Abstract (EN):
Radiocaesium (Cs-137) dispersion and Cs+ fixation were studied in the sediments collected from the lagoon systems of "Ria de Aveiro". The Cs+ sorption was tested for the fine mica grains and for the < 2 mu m clay fractions extracted from silty clays. The Cs+ exchange is found strongly onto mica-rich fractions than smectite-rich fractions. The distribution coefficient increases if the silty material is constituted by rich-mica clay fractions or if the non-clay minerals are removed from the silty-clay material. The samples studied behave as multisite ion exchange, where Cs+ engages in ion-exchange reactions with hydrated cations on planar sites on expansible layer silicates. Higher concentrations of the Cs-137 were found associated with mica-rich silty clays. The 137Cs ranges from 3.2 to 3.9 Bq kg(-1) in the < 38 mu m fractions and from 2.9 to 3.3 Bq kg(-1) in the < 64 mu m fractions.
Language:
English
Type (Professor's evaluation):
Scientific
Contact:
ibobos@fc.up.pt
No. of pages:
6