2005
DOI: 10.1016/j.gca.2005.03.044
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CTR diffraction and grazing-incidence EXAFS study of U(VI) adsorption onto α-Al2O3 and α-Fe2O3 (11̄02) surfaces

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Cited by 85 publications
(98 citation statements)
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(99 reference statements)
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“…However, the uranyl-carbonato ternary surface complex was not confined to the alkaline pH range but predominant even down to pH 4.5. Crystal truncation rod diffraction, grazing incidence EXAFS, and bond-valance calculations have also identified the presence of a binuclear, bidentate uranyl-carbonate ternary complex on hematite (Catalano et al, 2005). In contrast, in situ attenuated total reflection-infrared spectroscopy detected a binary, inner-sphere, multidentate surface complex of uranyl on hematite (Lefèvre et al, 2006).…”
Section: Precipitation Speciation and Adsorptionmentioning
confidence: 99%
“…However, the uranyl-carbonato ternary surface complex was not confined to the alkaline pH range but predominant even down to pH 4.5. Crystal truncation rod diffraction, grazing incidence EXAFS, and bond-valance calculations have also identified the presence of a binuclear, bidentate uranyl-carbonate ternary complex on hematite (Catalano et al, 2005). In contrast, in situ attenuated total reflection-infrared spectroscopy detected a binary, inner-sphere, multidentate surface complex of uranyl on hematite (Lefèvre et al, 2006).…”
Section: Precipitation Speciation and Adsorptionmentioning
confidence: 99%
“…In the case of ternary surface complex formation between uranyl and carbonate, the number of CO 3 2À ions present in the UO 2 2+ coordination sphere varies considerably between structural models. For hematite, surface complexes with one (Bargar et al, 1999) and two CO 3 2À ions (Bargar et al, 2000;Catalano et al, 2005) have been suggested. For goethite, the formation of a surface complex with only one CO 3 2À ion in the uranyl coordination sphere has been proposed (Sherman et al, 2008) and this has also been suggested for natural samples (Bostick et al, 2002).…”
Section: Introductionmentioning
confidence: 99%
“…More importantly, U(VI) in air-equilibrated hematite systems is known to form U(VI)-carbonate ternary complexes (Bargar et al, 1999(Bargar et al, , 2000. Recent grazing-incidence X-ray absorption spectroscopic studies indicated the formation of innersphere bidentate and outer-sphere complexes on rutile (TiO 2 ) (1 1 0) and (0 0 1) planes, and inner-sphere surface species on a-A 2 O 3 (1 1 0 2) and (1 1 0) surfaces and aFe 2 O 3 (1 1 0 2) surfaces (Den Auwer et al, 2003;Denecke et al, 2003;Catalano et al, 2005).…”
Section: Introductionmentioning
confidence: 99%