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• W2113444974 abstract "The thermodynamic analysis of the thermal decomposition reaction of carbonates showed that the temperatures of thermal stability of dolomite and magnesium carbonate are very similar. Kinetics of isothermal and non-isothermal decompositions of natural dolomite in air atmosphere were investigated. Under the examined conditions, dolomite decomposed in a one-stage process. The final solid products of dolomite’s decomposition were calcium and magnesium oxides. The average value of isoconversional apparent activation energy of non-isothermal decomposition was 205.60 kJ mol−1. The kinetics of decomposition can be described by the power-law model P2/3 with ln(A) = 20.98 for the extent of reaction α < 0.77 and by two-dimensional diffusion model D2 with ln(A) = 21.12 for α > 0.77." @default.
• W2113444974 created "2016-06-24" @default.
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• W2113444974 date "2014-12-03" @default.
• W2113444974 modified "2023-10-04" @default.
• W2113444974 title "Thermal behavior of natural dolomite" @default.
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• W2113444974 doi "https://doi.org/10.1007/s10973-014-4301-6" @default.
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