The thermal and hydrothermal behavior of silica-adsorbed magnesium hydroxide.
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Silica-adsorbed Mg(OH)<SUB>2</SUB> was treated thermally and hydrothermally. The resulting change in the adsorption layer was followed, and the effects of the adsorbed silica on the change in the bulk (Mg(OH)<SUB>2</SUB>, MgO) were examined. (1) Thermal treatment: The dehydration temperature of Mg(OH)<SUB>2</SUB> increased with an increase in the amount of silica adsorbed, and it was higher by 25 °C for Mg(OH)<SUB>2</SUB> adsorbing silica above 0.4 mmol/g than for pure Mg(OH)<SUB>2</SUB>. The amorphous silicate of the adsorption layer on the Mg(OH)<SUB>2</SUB> surface was transformed into forsterite (Mg<SUB>2</SUB>SiO<SUB>4</SUB>) and chain or sheet-like silicate over the temperature range of 870–1100 °C, and the presence of the silica inhibited the sintering and crystallite growth of the MgO grains. At 1400 °C, these products were all transformed into forsterite, and the presence of the silica had little effect on the crystallite growth. (2) Hydrothermal treatment: Below 360 °C, the amorphous silicate on the surface crystallized as serpentine (Mg<SUB>3</SUB>Si<SUB>2</SUB>O<SUB>5</SUB>(OH)<SUB>4</SUB>), and the crystallite growth of Mg(OH)<SUB>2</SUB> was inhibited. Above 420 °C, on the other hand, the silicate was transformed into forsterite through serpentine-like silicate, and the crystallite growth of Mg(OH)<SUB>2</SUB> was promoted. The change in the crystallite size of the bulk by the treatment was interpreted mainly in terms of the behavior of the silicate on the surface.
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