2021
DOI: 10.1021/acs.inorgchem.1c01243
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Retention of Iodide and Chloride by Formation of a Green Rust Solid Solution GR-Cl1–xIx: A Multiscale Approach

Abstract: The uptake of iodide and chloride during the synthesis of green rust (GR), the Fe endmember of the layered double hydroxide (LDH) group, was investigated. GR compounds were prepared by aerial oxidation of Fe­(OH)2 in suspension, considering various I/Cl ratios at constant ionic strength. Only GR compounds formed in all experiments, and the associated I/Cl ratio increased with that of the starting suspension. No preferential uptake of any halide could be detected, and all compounds had comparable morphology. Fu… Show more

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Cited by 5 publications
(9 citation statements)
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“…According to these results, there is no significant preference for one anion over the other (chloride or iodide) for uptake. These results compare well with previously reported solid solution experiments, where the Cl – /I – ratio in the GR interlayer was the same as in the contacting aqueous phase. , Data from this study further show that the absence of selective uptake of one of these two anions is also valid at higher ionic strength up to 5 mol/kg (Figure ). This experimental finding is also well captured by the solid solution model.…”
Section: Resultssupporting
confidence: 93%
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“…According to these results, there is no significant preference for one anion over the other (chloride or iodide) for uptake. These results compare well with previously reported solid solution experiments, where the Cl – /I – ratio in the GR interlayer was the same as in the contacting aqueous phase. , Data from this study further show that the absence of selective uptake of one of these two anions is also valid at higher ionic strength up to 5 mol/kg (Figure ). This experimental finding is also well captured by the solid solution model.…”
Section: Resultssupporting
confidence: 93%
“…X-ray diffractograms of the synthesized GR compounds (Figure S1) evidence the presence of only green rust minerals, and electron micrographs show that samples are made of thin hexagonal platelets (Figure S3). These results compare well with reported findings for GR-Cl samples prepared by precipitation from ferric and ferrous ions or by oxidation of Fe­(OH) 2 . , The synthesized magnetite is made of octahedral crystals of 100–200 nm, and the crystal structure was assessed by XRD analysis (Figures S2 and S4).…”
Section: Resultssupporting
confidence: 90%
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