Mineralogy of a natural As-rich hydrous ferric oxide coprecipitate formed by mixing of hydrothermal fluid and seawater: Implications regarding surface complexation and color banding in ferrihydrite deposits

2001 ◽  
Vol 86 (7-8) ◽  
pp. 834-851 ◽  
Author(s):  
Denis G. Rancourt ◽  
Danielle Fortin ◽  
Thomas Pichler ◽  
Pierre-Jean Thibault ◽  
Gilles Lamarche ◽  
...  
2010 ◽  
Vol 275 (3-4) ◽  
pp. 262-271 ◽  
Author(s):  
Thomas J. Reich ◽  
Soumya Das ◽  
Carla M. Koretsky ◽  
Tracy J. Lund ◽  
Christopher J. Landry

2009 ◽  
Vol 339 (2) ◽  
pp. 302-309 ◽  
Author(s):  
Melinda S. Schaller ◽  
Carla M. Koretsky ◽  
Tracy J. Lund ◽  
Christopher J. Landry

2009 ◽  
Vol 73 (13) ◽  
pp. 3723-3737 ◽  
Author(s):  
Christopher J. Landry ◽  
Carla M. Koretsky ◽  
Tracy J. Lund ◽  
Melinda Schaller ◽  
Soumya Das

2007 ◽  
Vol 95 (5) ◽  
Author(s):  
Maria R. Romero-González ◽  
Tao Cheng ◽  
Mark O. Barnett ◽  
Eric E. Roden

Previous published data for the adsorption of U(VI) and/or phosphate onto amorphous Fe(III) oxides (hydrous ferric oxide, HFO) and crystalline Fe(III) oxides (goethite) was examined. These data were then used to test the ability of a commonly-used surface complexation model (SCM) to describe the adsorption of U(VI) and phosphate onto pure amorphous and crystalline Fe(III) oxides and synthetic goethite-coated sand, a surrogate for a natural Fe(III)-coated material, using the component additivity (CA) approach. Our modeling results show that this model was able to describe U(VI) adsorption onto both amorphous and crystalline Fe(III) oxides and also goethite-coated sand quite well in the absence of phosphate. However, because phosphate adsorption exhibits a stronger dependence on Fe(III) oxide type than U(VI) adsorption, we could not use this model to consistently describe phosphate adsorption onto both amorphous and crystalline Fe(III) oxides and goethite-coated sand. However, the effects of phosphate on U(VI) adsorption could be incorporated into the model to describe U(VI) adsorption to both amorphous and crystalline Fe(III) oxides and goethite-coated sand, at least for an initial approximation. These results illustrate both the potential and limitations of using surface complexation models developed from pure systems to describe metal/radionuclide adsorption under more complex conditions.


2008 ◽  
Vol 9 (1) ◽  
Author(s):  
Tracy J Lund ◽  
Carla M Koretsky ◽  
Christopher J Landry ◽  
Melinda S Schaller ◽  
Soumya Das

Water SA ◽  
2015 ◽  
Vol 41 (1) ◽  
pp. 157 ◽  
Author(s):  
HA Mengistu ◽  
A Tessema ◽  
MB Demlie ◽  
TA Abiye ◽  
O Roeyset

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