Solid products and rate-limiting step in the thermal half decomposition of natural dolomite in a CO2 (g) atmosphere

Natural dolomite powders obtained from caves which give unusual high resistance building materials, have been decomposed in a Knudsen cell at high CO₂ pressures in the temperature range of 913-973 K. XRD traces for the final solid products, after the first half thermal decomposition, have shown, that beside the XRD patterns for the calcite and MgO, the existence of a new structure with major peaks at 2θ equal to 38.5 and 65°. This finding has been ascribed to a solid solution of MgO in calcite. The kinetic analysis of the TG curves yield a total apparent enthalpy (ΔH^∗) for the decomposition equal to 440±10 kJ mol⁻¹ for a range of fraction decomposed (α) varying between 0.2 and 0.7. This value is much closer to the theoretical expected at 950 K value ΔH=486 kJ mol⁻¹ for the dolomite decomposition in CO₂ environment, where CaO, MgO and oxides of solid solution can be the solid reaction products. The rate determining step is the transport of CO₂ across the reacting interface through an high activated thermal process due to solid state diffusion of CO₃²⁻ in the bulk and/or the grain boundaries phases of CaCO₃ and/or of the solid solution. The microstructure evolution of the solid products follows a shear-transformation mechanism. At temperatures below 943 K, porous product particles are characterized by a monomodal narrow pore size distribution around 0.05 μm. At higher temperatures, a critical level of tensions inside the particles is reached and a bimodal pore size distribution around 1 and 0.05 μm is formed.