Abstract
The evolution of the vertical distribution of Cs134 from Chernobyl in two soils of north-west Italy has been investigated to highlight the factors controlling its mobility. In one of the site only a poor control from the amount of fine fraction appears. In the other site a significant mineralogical control is shown, the amount of smectite being the parameter correlated with mobility.
| Original language | English |
|---|---|
| Pages (from-to) | 701-705 |
| Number of pages | 5 |
| Journal | Fresenius Environmental Bulletin |
| Volume | 4 |
| Issue number | 11 |
| Publication status | Published - 1995 |
| Externally published | Yes |
Keywords
- radiocaesium
- mobility
- soil