2005
DOI: 10.1016/j.gca.2004.12.029
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Surface complexation model for multisite adsorption of copper(II) onto kaolinite

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Cited by 84 publications
(54 citation statements)
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“…At pH < 5.0 the cationic form Cip + dominates, whereas at pH values between 5.0 and 9.0 the zwitterionic form Cip ( is the most important species and at pH > 10.0 the anionic form Cip -is the most abundant (SI Figure S1a). Consistent with Peacock and Sherman (22), Cu(II) was present as free cation between pH 2.0 and 6.6 (SI Figure S1b). Above pH 6.6, Cu precipitation as Cu(OH) 2 (s) as the major Cu(II) species would limit the concentration of aqueous Cu(II).…”
Section: Species Of Cip Cu(ii) and Cip-cu(ii) Complexes In Solutionsupporting
confidence: 86%
“…At pH < 5.0 the cationic form Cip + dominates, whereas at pH values between 5.0 and 9.0 the zwitterionic form Cip ( is the most important species and at pH > 10.0 the anionic form Cip -is the most abundant (SI Figure S1a). Consistent with Peacock and Sherman (22), Cu(II) was present as free cation between pH 2.0 and 6.6 (SI Figure S1b). Above pH 6.6, Cu precipitation as Cu(OH) 2 (s) as the major Cu(II) species would limit the concentration of aqueous Cu(II).…”
Section: Species Of Cip Cu(ii) and Cip-cu(ii) Complexes In Solutionsupporting
confidence: 86%
“…So, cations adsorption on siloxane basal surfaces is relatively weak compared with the cases of 2:1 type phyllosilicates (Vasconcelos et al, 2007). In contrast, metal cations can form strong chemical bonds with dangling sites on broken surfaces (Peacock and Sherman, 2005;Gu and Evans, 2008).…”
Section: Introductionmentioning
confidence: 98%
“…In contrast, there are much fewer studies on edge surfaces of kaolinite. For example, Peacock and Sherman (2005) investigated the complexing of Cu 2+ cations on broken surfaces. In the study of Kremleva et al (2011), they looked into uranyl complexing on the edge surfaces with static quantum mechanical methods.…”
Section: Introductionmentioning
confidence: 99%
“…Using EXAFS, Peacock and Sherman (2004) showed that under acidic conditions Cu sorption to goethite occurs as inner-sphere complex binding of CuO 4 H n n-6 and binuclear Cu 2 O 6 H n n-8 . Sorption experiments of Cu binding to kaolinite at low pH suggest binding is a non-specific ion exchange on the permanently charged basal surface sites, whereas with increasing pH the variably charged edge sites become the major adsorption sites (Gu and Evans, 2008).…”
Section: Sorption Of Cu In Lateritementioning
confidence: 99%