A Li
2O⋅2SiO
2 melt was unidirectionally solidified in a clay crucible from its bottom with a constant temperature gradient of 80°C/cm. When the solidification rate was higher than 3mm/h, many bubbles developed in the melt near the solid-melt interface. Mass spectroscopic analysis of the gas extracted from the bubbles showed that the main component of the gas was H
2O. Infrared spectroscopic analyses of the quenched melt (glass) and the solidified ingot (crystals) showed that the H
2O contents of the melt before and after solidification were 0.025 and 0.003mol/l, respectively. The developement of bubbles was thus attributed to the big difference in solubility of H
2O between the melts before and after solidification; the H
2O gas expelled from the melt on its solidification was concentrated in the melt near the solid-melt interface, supersaturated and finally developed as the bubbles. When the solidification rate was less than 1mm/h, no bubble was observed in the melt throughout the solidification process. In this case the H
2O gas expelled from the solidified melt would not have been concentrated heavily enough to form the bubbles but moved away from the interface by diffusion upward through the melt. Mathematical analysis of the H
2O distribution in the solidifying melt indicated that an upper limit of supersaturation of H
2O in the melt, over which the H
2O gas formed bubbles in the melt, was about 15 times the equilibrium saturated H
2O concentration of the melt.
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