2017
DOI: 10.1016/j.gca.2017.08.003
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Effects of surface structural disorder and surface coverage on isotopic fractionation during Zn(II) adsorption onto quartz and amorphous silica surfaces

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Cited by 45 publications
(72 citation statements)
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“…These trends, similar but less strong compared to the impacts on the kinetics, again show that siliceous composition—which enhances the formation of high-surface-area three-dimensional geopolymer gel—is vital for enhanced Pb sorption performance. 57 , 58 Also, high Na content is expected to enhance the formation of the three-dimensional geopolymer gel, 59 and on the account of the high exchangeability of Na, thought to also improve the ion-exchange properties of the resulting geopolymer sorbent.…”
Section: Results and Discussionmentioning
confidence: 99%
“…These trends, similar but less strong compared to the impacts on the kinetics, again show that siliceous composition—which enhances the formation of high-surface-area three-dimensional geopolymer gel—is vital for enhanced Pb sorption performance. 57 , 58 Also, high Na content is expected to enhance the formation of the three-dimensional geopolymer gel, 59 and on the account of the high exchangeability of Na, thought to also improve the ion-exchange properties of the resulting geopolymer sorbent.…”
Section: Results and Discussionmentioning
confidence: 99%
“…The Zn-bearing mineral standards presented here were previously characterized by EXAFS and X-ray diffraction analysis to establish purity and homogeneity of the phases as detailed by Nelson et al (2017). The adsorption samples of Zn on silica presented here were also previously characterized by EXAFS analysis to establish the coordination environment as detailed by Nelson et al (2017).…”
Section: Methodsmentioning
confidence: 99%
“…The Zn-bearing mineral standards presented here were previously characterized by EXAFS and X-ray diffraction analysis to establish purity and homogeneity of the phases as detailed by Nelson et al (2017). The adsorption samples of Zn on silica presented here were also previously characterized by EXAFS analysis to establish the coordination environment as detailed by Nelson et al (2017). The specific silica substrates were purchased as 0.5-10 mm conchoidally fractured quartz particles and 74-125 mm conchoidally fractured SiO 2(am) particles with measured specific surface areas of 5.92 AE 0.06 m 2 g À1 (2) and 9.76 AE 0.29 m 2 g À1 (2), respectively (Nelson et al, 2017).…”
Section: Methodsmentioning
confidence: 99%
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