Adsorption of uranyl ions on kaolinite, montmorillonite, humic acid and composite clay material

被引:45
|
作者
Campos, Bruno [1 ]
Aguilar-Carrillo, Javier [1 ]
Algarra, Manuel [1 ]
Goncalves, Mario A. [2 ,3 ]
Rodriguez-Castellon, Enrique [4 ]
Esteves da Silva, Joaquim C. G. [5 ]
Bobos, Iuliu [1 ]
机构
[1] Univ Porto, Ctr Geol, Fac Ciencias, P-4169007 Oporto, Portugal
[2] Univ Lisbon, Dept Geol, Fac Ciencias CREMINER, P-1749016 Lisbon, Portugal
[3] Univ Lisbon, CeGUL, P-1749016 Lisbon, Portugal
[4] Univ Malaga, Fac Ciencias, Dept Quim Inorgan, E-29071 Malaga, Spain
[5] Univ Porto, Fac Ciencias, Ctr Invest Quim, P-4169007 Oporto, Portugal
关键词
Batch; Flow through reactor; Breakthrough curves; Molecular fluorescence; Infrared and X-ray photoelectron spectroscopy; URANIUM(VI) SORPTION; OPALINUS CLAY; U(VI); COMPLEXES; BINDING; ABSENCE; UO22+; WATER; PORE; SOIL;
D O I
10.1016/j.clay.2013.08.046
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Adsorption of uranyl ions onto kaolinite, montmorillonite, humic acid and composite clay material (both clays and humic acid) was studied by measuring the system response to clay suspensions (pre-equilibrated with or without uranyl) and to perturbations of the solution chemistry. Adsorption behavior of selected materials under the frame of batch experiments was tested at high uranyl concentrations (6-1170 mu g/mL; 2.5 x 10(-2) to 4.9 mu M), whereas that under flow through continuous stirred reactor experiments was tested at low concentrations (1.00 x 10(-4) to 1.18 x 10(-4) M). Both experiments were developed at pH 4.5 and ionic strength 02 mM. The adsorption experiments follow a Langmuir isotherm model with a good correlation coefficient (R-2 > 0.97). The calculated amount of adsorbed and desorbed uranyl was carried out by numeric integration of the experimental data, whereas the desorption rates were determined from the breakthrough curve experiments. Kaolinite with highly disordered structure adsorbed less uranyl (3.86 x 10(-6) mol/g) than well-ordered kaolinite (1.76 x 10(-5) mol/g). Higher amount of uranyl was adsorbed by montmorillonite (3.60 x 10(-5) mol/g) and only half of adsorbed amount was desorbed (1.85 x 10(-5) mol/g). The molecular interactions between kaolinite, montmorillonite, humic acid, composite material and saturated uranyl ion solutions were studied by molecular fluorescence, infrared and X-ray photoelectron spectroscopy. The Stem-Volmer constant obtained for montmorillonite (2.6 x 10(3) M-1) is higher than for kaolinite (0.3 x 10(3) M-1). Molecular vibrations of Si-O stretching and Al-OH bending related to hydroxylated groups ( SiOH or AlOH) of kaolinite and montmorillonite show structural changes when uranyl ions are adsorbed. X-ray photoelectron spectroscopy shows that the U 4f(7/2) core level signals occur at 380.5 eV in either kaolinite or montmorillonite that resulted from the interaction of aluminol surface sites with the (UO2)(3)(OH)(5)(+). (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:53 / 63
页数:11
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