Rapid Mobilization of Noncrystalline U(IV) Coupled with FeS Oxidation
| Autor: | Kim F. Hayes, Yuqiang Bi, Rizlan Bernier-Latmani, Malgorzata Alicja Stylo |
|---|---|
| Rok vydání: | 2016 |
| Předmět: |
Inorganic chemistry
Carbonates chemistry.chemical_element Iron sulfide 010501 environmental sciences engineering.material 010502 geochemistry & geophysics 01 natural sciences Oxygen Redox chemistry.chemical_compound Adsorption Mackinawite Oxidizing agent Environmental Chemistry Ferrous Compounds 0105 earth and related environmental sciences Lability Photoelectron Spectroscopy General Chemistry X-Ray Absorption Spectroscopy chemistry engineering Uranium Carbonate Environmental Pollutants Oxidation-Reduction |
| Zdroj: | Environmental Science & Technology. 50:1403-1411 |
| ISSN: | 1520-5851 0013-936X |
| DOI: | 10.1021/acs.est.5b04281 |
| Popis: | The reactivity of disordered, noncrystalline U(IV) species remains poorly characterized despite their prevalence in biostimulated sediments. Because of the lack of crystalline structure, noncrystalline U(IV) may be susceptible to oxidative mobilization under oxic conditions. The present study investigated the mechanism and rate of oxidation of biogenic noncrystalline U(IV) by dissolved oxygen (DO) in the presence of mackinawite (FeS). Previously recognized as an effective reductant and oxygen scavenger, nanoparticulate FeS was evaluated for its role in influencing U release in a flow-through system as a function of pH and carbonate concentration. The results demonstrated that noncrystalline U(IV) was more susceptible to oxidation than uraninite (UO2) in the presence of dissolved carbonate. A rapid release of U occurred immediately after FeS addition without exhibiting a temporary inhibition stage, as was observed during the oxidation of UO2, although FeS still kept DO levels low. X-ray photoelectron spectroscopy (XPS) characterized a transient surface Fe(III) species during the initial FeS oxidation, which was likely responsible for oxidizing noncrystalline U(IV) in addition to oxygen. In the absence of carbonate, however, the release of dissolved U was significantly hindered as a result of U adsorption by FeS oxidation products. This study illustrates the strong interactions between iron sulfide and U(IV) species during redox transformation and implies the lability of biogenic noncrystalline U(IV) species in the subsurface environment when subjected to redox cycling events. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
|