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Thermal decomposition of synthesised layered double hydroxides based upon Mg/(Fe,Cr) and carbonate

2008; Elsevier BV; Volume: 479; Issue: 1-2 Linguagem: Inglês

10.1016/j.tca.2008.08.016

1872-762X

Henry J. Spratt, Sara J. Palmer, Ray L. Frost,

Inorganic Chemistry and Materials

Thermal analysis complimented with evolved gas mass spectrometry has been applied to hydrotalcites of the pyroaurite–stitchtite series containing the carbonate anion prepared by co-precipitation and with varying Fe3+, Cr3+ trivalent cation ratio. The resulting materials were characterised by XRD, and TGA/DTG to determine the stability of the hydrotalcites synthesised. Hydrotalcites of formula Mg6(Cr0.8,Fe0.2)2(OH)16(CO3)·xH2O, Mg6(Cr0.6,Fe0.4)2(OH)16(CO3)·xH2O, Mg6(Cr0.4,Fe0.6)2(OH)16(CO3)·xH2O and Mg6(Cr0.2,Fe0.8)2(OH)16(CO3)·xH2O formed by intercalation with the carbonate anion as a function of Fe3+, Cr3+ trivalent cationic ratio show variation in the d-spacing attributed to the size of the cation. The thermal decomposition of stitchtite–pyroaurite solid solution follows the following steps: removal of adsorbed water (<100 °C), elimination of the interlayer structural water (100–150 °C), and the simultaneous dehydroxylation and decarbonation of the hydrotalcite framework (300–400 °C). The effect of replacement of Cr3+ by Fe3+ has no effect on the dehydroxylation temperature. The ion current curves provide evidence for the formation of Fe3+ and Cr3+ carbonates during dehydroxylation. Dehydroxylation results in the collapse of the hydrotalcite structure to that of its corresponding metal oxides, and results in the formation of spinels, including MgO, MgFe2O4, MgCr2O4, and MgFeAlO4.