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2015
DOI: 10.1007/s10967-014-3893-4
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Sorption of U(VI) on magnetic illite: effects of pH, ions, humic substances and temperature

Abstract: The sorption of U(VI) on magnetic illite as a function of pH, ionic strength, solid-to-liquid ratio, shaking time, humic acid (HA) and temperature was investigated through batch experiments. The results showed that the sorption process had a strong dependent on the changes of pH, temperature and HA in solution. And at below pH 6.5, with decreasing of the valences of anions such as Cl -, SO 2À 4 and PO 3À 4 ; the sorption amount increased obviously, but that was almost not influenced by cations. This experiment… Show more

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Cited by 27 publications
(2 citation statements)
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“…In addition, the adsorption capacities of U when the adsorption equilibrium was reached after 24 h in the experiments showed a slight difference from those obtained through tting. These results indicate that the U adsorption by sandstones outside a mining area is more consistent with the pseudo-second-order kinetic equation and that its adsorption rate is controlled by chemical adsorption (Du et al 2015). In addition, the tting of data on different cores yielded similar Q e values, suggesting that the cores at different distances from the mining area had similar saturated adsorption capacities of U in groundwater.…”
Section: )supporting
confidence: 60%
“…In addition, the adsorption capacities of U when the adsorption equilibrium was reached after 24 h in the experiments showed a slight difference from those obtained through tting. These results indicate that the U adsorption by sandstones outside a mining area is more consistent with the pseudo-second-order kinetic equation and that its adsorption rate is controlled by chemical adsorption (Du et al 2015). In addition, the tting of data on different cores yielded similar Q e values, suggesting that the cores at different distances from the mining area had similar saturated adsorption capacities of U in groundwater.…”
Section: )supporting
confidence: 60%
“…Sorption is more widely used for heavy metal pollution remediation than membrane separation, precipitation, ion exchange and extraction (Michard et al 1996;Ganesh et al 1999;Vaaramaa et al 2000;Kulkarni 2003;Singh et al 2010). At present, research on the sorption of uranium onto silicate minerals is chiefly concentrated on clay minerals such as kaolinite, illite, montmorillonite and bentonite (Chisholm-Brause et al 2001;Ren et al 2010;Du et al 2015;Reinoso-Maset and Ly 2016). However, the sorption characteristics of uranium onto mullite have not been commonly studied.…”
Section: Introductionmentioning
confidence: 99%