2005
DOI: 10.1016/j.jcis.2004.08.019
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Competitive sorption of protons and metal cations onto kaolinite: experiments and modeling

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Cited by 98 publications
(110 citation statements)
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“…5,7,14,16,17 The strong adsorption by goethite at pH > 4.0 is consistent with many observations in the literature, where iron (oxy)hydroxides such as amorphous iron hydroxide, ferrihydrite and goethite in aquifer sediments have been identified as major sinks for U(VI). 6,13,15,18−20 Compared to the fine fractions (Figure 2c,d), kaolinite exhibits stronger U(VI) adsorption at pH < 4.0 and a similar adsorption extent at pH > 4.0 (up to 7.0), and goethite shows a similar adsorption extent at pH < 4.0 and stronger adsorption at pH > 4.0 (up to 8.0).…”
Section: +supporting
confidence: 79%
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“…5,7,14,16,17 The strong adsorption by goethite at pH > 4.0 is consistent with many observations in the literature, where iron (oxy)hydroxides such as amorphous iron hydroxide, ferrihydrite and goethite in aquifer sediments have been identified as major sinks for U(VI). 6,13,15,18−20 Compared to the fine fractions (Figure 2c,d), kaolinite exhibits stronger U(VI) adsorption at pH < 4.0 and a similar adsorption extent at pH > 4.0 (up to 7.0), and goethite shows a similar adsorption extent at pH < 4.0 and stronger adsorption at pH > 4.0 (up to 8.0).…”
Section: +supporting
confidence: 79%
“…Our modeling approach is summarized by the following points: (i) U(VI) is adsorbed via formation of bidentate surface complexes; (ii) in addition to the UO 2 2+ surface species ternary uranyl-carbonato surface complexes are formed. In agreement with our goethite system, we assumed that similar surface complexes ( Table 2, i.e., (>SOH) 2 UO 2 + , (>SOH) 2 UO 2 CO 3 − ) are formed on the kaolinite amphoteric edge sites; (iii) for kaolinite, cation exchange sites (>X − ) and amphoteric edge sites (>SOH) with a 1-pK model were chosen based on the data of Heidmann et al 14,35 The >SOH sites simply represent both silanol (>SiOH) and aluminol (>AlOH) sites on kaolinite surfaces. The treatment of amphoteric edge sites as a single surface site is generally recognized as a convenient modeling framework rather than a precise representation of actual functional groups existing at clay edge sites.…”
Section: +mentioning
confidence: 97%
“…The sorption of trace elements on kaolin depends on several physico-chemical parameters (pH, ionic strength, ion competition, and surface modification) (Heidmann et al 2005;Sarkar et al 2000;Srivastava et al 2005). Concerning OTC, it was previously shown that tin compounds are sorbed on suspended clay and sand particles following two processes: (a) by electrostatic interaction and/or (b) by hydrophobic binding (Bueno et al 1998;Weidenhaupt et al 1997).…”
mentioning
confidence: 99%
“…The sorption capacity of kaolin clay is pH dependent because its surface charge is more negative for pH values higher than its point of zero charge PZC [90]. Studies of Heidmann et al [31,32], Alkan et al [2] and Jiang et al [34,35] confirmed that the adsorption of lead, copper, nickel and cadmium on kaolinite increases with increasing pH. Hence, the adsorption decrease noticed here at higher concentrations, which was most distinct for the adsorption of copper on the untreated kaolinite (Fig.…”
Section: Batch Sorption Tests Resultsmentioning
confidence: 99%