2017
DOI: 10.1016/j.jconhyd.2016.12.009
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Investigation of hexavalent chromium sorption in serpentine sediments

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Cited by 23 publications
(7 citation statements)
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“…Hexavalent chromium shows two main forms, i.e., chromate (CrO 4 2− ) and dichromate (Cr 2 O 7 2− ); both forms are highly toxic in nature. 50 According to Mpouras et al 51 chromium removal might be related to two main effects: adsorption and reduction. A reduction of approximately 50% was observed at pH 5.…”
Section: Adsorption Of Metalsmentioning
confidence: 99%
“…Hexavalent chromium shows two main forms, i.e., chromate (CrO 4 2− ) and dichromate (Cr 2 O 7 2− ); both forms are highly toxic in nature. 50 According to Mpouras et al 51 chromium removal might be related to two main effects: adsorption and reduction. A reduction of approximately 50% was observed at pH 5.…”
Section: Adsorption Of Metalsmentioning
confidence: 99%
“…At present, a large amount of low-quality serpentine mining waste has not been effectively utilized. Considering that serpentine is rich in mineral elements such as magnesium ( Galey et al., 2017 ; Mpouras et al., 2017 ; Sakaguchi et al., 2018 ), it may be effective when trying to improve local saline-alkali soil by using an appropriate amount of serpentine instead of sand. In addition, the weathering of serpentine coupled with carbon fixation is also expected to increase the capture of atmospheric CO 2 ( Kojima et al., 1997 ; Liu et al., 2021 ; Lu et al., 2022 ), which may increase more soil carbon sinks while improving saline-alkali land.…”
Section: Introductionmentioning
confidence: 99%
“…Trivalent Cr is undoubtedly the most thermodynamically stable form of Cr in soil, as it readily precipitates as chromium hydroxide [Cr(OH) 3 ] and iron-chromium hydroxide [(Fe,Cr)(OH) 3 ] or becomes immobilised after sorption onto soil colloids (Leita et al, 2009). On the other hand, Cr(VI) is thermodynamically metastable in the pore solution and much more mobile in soil, since Cr(VI) oxyanions (chromate CrO 4 2− , hydrogen chromate HCrO 4 − , and dichromate Cr 2 O 7 2− ) are not adsorbed onto soil colloids under sub-neutral to alkaline conditions (Becquer et al, 2003;Mpouras et al, 2017). At these soil pHs, Cr(VI) can be present in the form of solid minerals in association with different cations characterised by a wide range of solubility: barium, calcium, lead and zinc chromates are the most insoluble (Kotas and Stasicka, 2000;Pettine and Capri, 2005), while alkaline and some alkaline-earth chromates are highly soluble.…”
Section: Introductionmentioning
confidence: 99%