| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6438976 | Geochimica et Cosmochimica Acta | 2013 | 18 Pages |
Abstract
In conclusion, geochemical models used for simulating trace element behavior in acidic environments seem to require ternary metal-phosphate surface complexes to properly describe partitioning of metals between solution and the solid phase.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Charlotta Tiberg, Carin Sjöstedt, Ingmar Persson, Jon Petter Gustafsson,