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Dissolution and hydration kinetics of MgO

Surface Technology
Publication Date
DOI: 10.1016/0376-4583(85)90080-9
  • Earth Science
  • Physics


Abstract The dissolution and hydration kinetics of MgO single crystals and powder samples were investigated with regard to the H + and Mg 2+ concentrations and the temperature. The rate of dissolution of rotating MgO discs in buffered solutions was determined from measurements of [Mg 2+] and those of the crystals and powder fractions were determined by pH and conductivity analysis. The degree of hydration was analysed by means of a thermogravimetric method. Several rate-controlling processes depending on pH were present at room temperature. (1) At pH < 5 the rate-controlling step was proton attack followed by desorption of Mg 2+ of OH - depending on the value of [Mg 2+]. The rate was proportional to either -pH or pMg-pH. These processes are part of the overall neutralization reaction. MgO + 2H +→Mg 2+ + H 2 O (2) At pH ≈ 5 the rate-controlling step was a diffusion-limitation process due to protons. The rate was proportional to the proton concentration. (3) At pH > 7 the rate-controlling step was OH - adsorption followed by Mg 2+ and OH - desorption leading to a rate maximum. These processes are part of the overall dissolution reaction. MgO + H 2 O→Mg 2+ + 2OH - The neutralization processes are interpreted in terms of irreversible thermodynamics yielding a linear dependence of the rate on pH or pMg-pH. It is concluded from conductivity and scanning electron microscopy measurements during and after hydration experiments that the hydration rate is controlled by the dissolution rate under given conditions. After a supersaturation period Mg(OH) 2 precipitates preferentially at the MgO surface, so that an MgO lattice reaction can be excluded. All processes undergo an Arrhenius acceleration with increasing temperature (activation energy, 70 kJ mol -1) and the overall reactions are then limited by proton and OH - diffusion.

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