Here, a kinetic study of the thermal decomposition of synthesized hydrotalcite, Mg-6 Al-2 CO3(OH)(16)center dot H2O, has been carried out using thermogravimetric experiments in air atmosphere. It is shown that the thermal decomposition occurs in two well differentiated stages. The first one is a single-step dehydration process that comprises the release of four water molecules. On the other hand, the second stage is complex and corresponds to both dehydroxylation and decarbonation processes which occur simultaneously. The kinetic parameters describing all processes were calculated by means of a combined approach comprising isoconversional, model-fitting and deconvolution methods. It was concluded that dehydroxilation and decarbonization cannot be separated by TG experiments and the two stages contributing to the complex process do not apparently match the expected stoichiometry of the process. Therefore, it is proposed that such stages mark a change on the reaction mechanism due to the structural collapse of the laminar double hydroxide.
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St Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, RussiaSt Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, Russia
Zhitova, Elena S.
Kriyoyichev, Sergey, V
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St Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, Russia
Russian Acad Sci, Nanomat Res Ctr, Kola Sci Ctr, Apatity, RussiaSt Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, Russia
Kriyoyichev, Sergey, V
Pekov, Igor
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Moscow MV Lomonosov State Univ, Fac Geol, Dept Mineral, Moscow, RussiaSt Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, Russia
Pekov, Igor
Greenwell, H. Christopher
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Univ Durham, Dept Earth Sci, Durham DH1 3LE, EnglandSt Petersburg State Univ, Inst Earth Sci, Dept Crystallog, St Petersburg, Russia