Abstract
The solubility of amorphous silica in sea water is about 85 mg·SiO'; 1 at 20°C, which is less than that in distilled water Cabout 113 mg·SiO,/ l). The dissolution rate seems to be controlled by the amount of silica gel present and its soluhility. Si lica gel in sea water is transformed to dissolved silica at a much faster rate than in distilled water. A maximum value of dissolved silica is observed during the process of dissolution under no abrasion condition, when the dissolution rate is very large. The differences in the solubility and in the dissolution rate of amorphous silica in dist illed and in sea water cannot be explained by the difference in pH values of the waters hut Reem to be due to the salts present: in sea water.
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CITATION STYLE
KATO, K., & KITANO, Y. (1968). Solubility and Dissolution Rate of Amorphous Silica in Distilled and Sea Water at 20°C. Journal of the Oceanographical Society of Japan, 24(4), 147–152. https://doi.org/10.5928/kaiyou1942.24.147
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