2013
DOI: 10.1002/ejic.201300735
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Oxidation of Dodecanoate Intercalated Iron(II)–Iron(III) Layered Double Hydroxide to Form 2D Iron(III) (Hydr)oxide Layers

Abstract: A planar trioctahedral iron(II)-iron(III) hydroxide (green rust, GR) intercalated with dodecanoate (GR C12 ) has been oxidized by dioxygen to produce the corresponding planar iron(III) (hydr)oxide. The formulae of GR C12 and the final iron(III) product (oxGR C12 ) were determined to be Fe II 2.00 Fe III 1.00 (OH) 5.31 (C 12 H 23 O 2 ) 0.66 (SO 4 ) 0.51 and Fe III 3 O 2.18 -(OH) 3.13 (C 12 H 23 O 2 ) 0.56 (SO 4 ) 0.47 , respectively. oxGR C12 has the same planar layer structure as GR C12 , as revealed by identi… Show more

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Cited by 24 publications
(16 citation statements)
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“…3a) shows platelets with a lateral dimension of 50-200 nm similar to its parent layered iron(III) oxyhydroxide compound. 15 The suspension of nano-sized TBA dispersed SSI colloids shows a high optical absorption with a peak centred at 275 nm and a strong shoulder at 341 nm which are not observed in the bulk iron oxides (Fig. 4a).…”
Section: Ssi Lm Fabrication and Characterizationmentioning
confidence: 92%
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“…3a) shows platelets with a lateral dimension of 50-200 nm similar to its parent layered iron(III) oxyhydroxide compound. 15 The suspension of nano-sized TBA dispersed SSI colloids shows a high optical absorption with a peak centred at 275 nm and a strong shoulder at 341 nm which are not observed in the bulk iron oxides (Fig. 4a).…”
Section: Ssi Lm Fabrication and Characterizationmentioning
confidence: 92%
“…Interestingly, the reverse reaction, oxidation of iron(II) to iron(III), then should take place with dehydroxylation as a consequence. 15 The n th PDDA/SSI lm is as electroactive as the rst one (Fig. 10b), and all the SSI fragments in one PDDA/SSI lm stay in electronic contact with each other due to close packing with possible water layers between them.…”
Section: Fast Charge Transfer and Electrochemical Active Fractionmentioning
confidence: 99%
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“…Indeed, the expectation is that the ferrous–ferric oxyhydroxide fougerite, along with FeS, comprised the first barrier that kept the disequilibria between the alkaline hydrothermal solutions and the early carbonic ocean at bay, necessary for driving life’s onset ( 8 , 17 , 18 ). It is worth remarking here that fougerite can absorb and host long-chain carboxylic acids in its interlayers, acids that could be released to the alkaline vent on delamination ( 19 ).…”
Section: Emergence Of Lifementioning
confidence: 99%