Amorphous and crystalline iron oxides are prevalent in subsurface systems and are important surfaces for metal contaminant sorption. While discrete amorphous iron oxide is microporous with particles ranging from 1 to 100 µm resulting in significant contributions from intraparticle diffusion, the deg
An Analysis of Zinc Sorption to Amorphous versus Crystalline Iron Oxides Using XAS
✍ Scribed by Paras Trivedi; Lisa Axe; Trevor A. Tyson
- Book ID
- 102583239
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 152 KB
- Volume
- 244
- Category
- Article
- ISSN
- 0021-9797
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✦ Synopsis
This research probes the mechanisms of Zn adsorption on hydrated oxides of iron (HFO and goethite) using XAS. A systematic investigation reveals that Zn 2+ upon sorption to HFO retains its hydration shell (N ∼ 6 oxygens, R ∼ 2.18 Å), irrespective of pH and adsorbate loading. Furthermore, the absence of second-shell contributions in combination with the temperature dependence of the structural parameters confirms outer-sphere adsorption complexes with HFO. In a coprecipitation study, the local coordination environment was consistent with Zn adsorption to HFO. On the other hand, Zn 2+ strongly adsorbs to goethite forming a tetragonal structure (N ∼ 4 oxygens and R ∼ 1.97 Å). Evidence of two Fe 3+ ions in the second shell at approximately 3.51 Å suggests an innersphere adsorption complex with goethite. Results demonstrate that even though the local structures of HFO and goethite are similar, the surface sites available to transition metals like zinc are vastly different. Overall, these spectroscopic analyses are consistent with macroscopic observations.
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