永磁场对碳酸盐水溶液中碳酸钙结晶的影响

IF 0.9 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY Physics and Chemistry of Solid State Pub Date : 2023-11-20 DOI:10.15330/pcss.24.4.616-622
V. Gayevskii, B. Nechyporuk, S. G. Gayevska
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引用次数: 0

摘要

研究了永久磁场对碳酸盐水溶液中碳酸钙结晶的影响。根据碳酸的一阶和二阶解离常数方程、NaCO3- 和 NaHCO30 复合物的稳定常数、质量平衡方程和电中性方程,确定了系统组分的值和碳酸盐子系统组分之间的比率、确定了实验条件下的主要物种为СО32-、NaСО3- 和 HСО3-,碳酸盐子系统的主要成分为СО32-(86.7%)和 HСО3-(13.19%)。研究表明,在温度为 18-20˚C 的溶液中,当 CO32- 离子明显多于 HCO3- 离子时,最有可能形成方解石和辉石。在 125-250 mT 的磁场中,碳酸钙从碳酸盐水溶液中结晶出来,结晶体的尺寸比没有磁场时明显增大。
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The influence of a permanent magnetic field on the crystallization of calcium carbonate from carbonate aqueous solutions
The effect of a permanent magnetic field on the crystallization of calcium carbonate from carbonate aqueous solutions was studied. Based on the equations for the first- and second-order dissociation constants of carbonic acid, the stability constants of NaCO3- and NaHCO30 complexes, the mass balance and electroneutrality equations, the values of the system components and the ratio between the components of the carbonate subsystem were determined, and it was established that the main species in experimental conditions are СО32-, NaСО3- and HСО3- and the main components of the carbonate subsystem are СО32- (86.7%) and HСО3- (13.19%). Studies have shown that with a significant excess of CO32- over HCO3- ions in the solution at temperatures of 18-20˚C, calcite and vaterite are most likely formed. During the crystallization of calcium carbonate from an aqueous carbonate solution in a magnetic field of 125-250 mT, the size of the crystallites increases significantly compared to the absence of a magnetic field.
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来源期刊
CiteScore
1.70
自引率
14.30%
发文量
83
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