| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4701190 | Chemical Geology | 2007 | 10 Pages |
Abstract
The results show that DFO-B is a very efficient U-desorbent and affects uranium mobility in clay containing soils. Moreover, the ligand-promoted desorption results principally in a stable neutral aqueous species (UO2DFOBH) not likely to re-adsorb on soil particles to a great extent. Hence, the siderophore effect on the bioavailability of U(VI) is not exclusively determined by its desorptive strength but also encompasses the aqueous speciation that follows desorption.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Domenik Wolff-Boenisch, Samuel J. Traina,