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Published online 6 January 2006
Published in Soil Sci Soc Am J 70:192-203 (2006)
DOI: 10.2136/sssaj2005.0054
© 2006 Soil Science Society of America
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Right arrow Soil Chemistry

Selenite Adsorption Mechanisms on Pure and Coated Montmorillonite: An EXAFS and XANES Spectroscopic Study

Derek Peak*, U. K. Saha and P. M. Huang

Dep. of Soil Science, Univ. of Saskatchewan, 51 Campus Dr., Saskatoon SK S7N 5A8 Canada



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Fig. 1. Se K-Edge EXAFS results for aqueous selenite solutions. Solid lines denote the raw data, and open squares are the fit to theoretical standards.

 


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Fig. 2. Se K-Edge EXAFS results for selenite adsorbed on a range of sorbents at pH 4.5 and 0.01 M I. Solid lines denote the raw data, and open squares are the fit to theoretical standards. Arrows denote spectral features consistent with Se-Al backscattering due to inner-sphere complexation.

 


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Fig. 3. Relationship between protonation state, molecular symmetry, and bond delocalization for selenite species.

 


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Figure 4. (a) XANES spectra of H2SeO3, HSeO3, and SeO32– (b) 12.665 to 12.69 keV energy range expanded to more clearly show differences in the near edge spectra.

 


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Fig. 5. Linear combination XANES fits of aqueous samples where more than one selenite protonation state is present. LC-XANES predicted distributions are within 0.5% of actual speciation values, and the estimated error of the LC-XANES fitting was 3%.

 


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Fig. 6. (a):Se K-Edge XANES spectra of selenite sorbed onto Mt, HYA,HAS, HYA-Mt, and HAS-Mt samples. HSeO3 and H2SeO3 solutions are included for comparison. (b) 12.665 to 12.69 keV energy range expanded to more clearly show differences in the near edge spectra for HAS, HYA, HYA-Mt, and Mt samples.

 


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Fig. 7. Selenite adsorption mechanisms for pH 4.5 samples consistent with EXAFS and XANES spectroscopy.

 


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Fig. 8. Linear combination XANES fits of selenite on HYA and HAS coated montmorillonite. Estimated error for the fitting is ± 5%.

 





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