A radioisotope technique was used for the determination of the rate of movement of Ca
2+ and Fe
3+ ions in MgO added with or without a small amount of SiO
2, Al
2O
3, etc. As the tracers RI
45Ca and RI
59Fe were used. The relationship between the rate of movement of these ions and the sintering behaviors of the mixtures were also studied.
The results obtained were summarized as follows:
(1) The movement of these ions is caused by thermal diffusion and draining. In MgO added with CaO and SiO
2, the rate of movement of Ca
2+ ion increased with increasing the molar ratio CaO/SiO
2, reached to a maximum when CaO/SiO
2≅1, and then decreared; no movement was observed when CaO/SiO
2_??_2. Additions of Al
2O
3 and Fe
2O
3 to MgO together with CaO and SiO
2, however, produced different results, i.e., the rate of movement of Ca
2+ in this mixture increased with increasing the ratio (CaO/SiO
2) without having a maximum.
(2) Additions of oxides such as TiO
2, Cr
2O
3, MnO
2, B
2O
3, etc., which were found, by the author's previous works, to be effective in promoting sintering of MgO and the growth of periclase crystals, always increased the rate of movement of Ca
2+.
(3) Comparing with Ca
2+ ions, Fe
3+ ions in MgO had a low rate of diffusion. Draining occured only when Ca
2+ coexisted in MgO.
(4) X-ray analysis showed that the compounds, CaO⋅MgO⋅SiO
2, 2CaO⋅Fe
2O
3, 4CaO⋅Al
2O
3⋅Fe
2O
3, etc., were produced in MgO by the movement of Ca
2+ and Fe
3+ ions.
(5) It was suggested that when the above compounds melt at high temperatures producing the liquid phase, the loard-bearing capacity of MgO is lowered.
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