[M-IS18] 結晶成⻑、溶解における界⾯・ナノ現象

[MIS18-P01] pHおよびカルシウムイオン濃度分布の同時可視化による炭酸カルシウム溶解反応の解析

三木 康誠²、*川野 潤¹、矢崎 誠²、豊福 高志^3,4、長井 裕季子³、永井 隆哉¹ (1.北海道大学大学院 理学研究院、2.北海道大学大学院 理学院、3.海洋研究開発機構、4.東京海洋大学)

キーワード：イメージング、炭酸カルシウム、pH、溶解

Recent developments in experimental and simulation techniques have revealed that the growth or dissolution mechanism of minerals in an aqueous solution is more complicated than we had imagined. To understand these mechanisms, the analysis of local conditions of the solution around the dissolving or forming minerals is critical. Recently, we succeeded in simultaneously visualizing the distribution of pH and calcium concentration around a calcium carbonate crystal dissolving in an aqueous solution using a fluorescent probe. In the present study, more precise calibration between pH/calcium ion concentration and the intensity of fluorescence which probes emitted at these conditions was performed, and the dissolution reaction of calcium carbonate crystal in aqueous solution was analyzed based on it.
pH and calcium ion concentration could be measured and their distributions around calcite dissolving in an aqueous solution were successfully visualized by simultaneously using HPTS (8-hydroxypyrene-1,3,6-trisulfonic acid) and Rhod-5N as pH and calcium concentration probes, respectively. Tendencies of change in calcium ion concentration could be explained by the diffusion equation with the reasonable values of the dissolution rate of calcite and the diffusion constant of calcium ion. When considered simultaneously with changes in pH, bicarbonate ions are suggested to play an important role in the dissolution of calcium carbonate.