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In situ observation of step dynamics on gypsum crystals

机译:石膏晶体阶跃动力学的原位观察

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In this work we studied the kinetics of gypsum crystals growing from aqueous solutions as a function of temperature and supersaturation. Laser confocal differential interference contrast microscopy (LCM-DIM) and atomic force microscopy (AFM) were used to observe in situ the step advancement and the evolution of the surface morphology of the {010} face. We found that, for the experimental conditions used in this study, 2D nucleation is the main step generation mechanism, even at low supersaturations, and only a few spiral hillocks were observed. Due to the elongated morphology of 2D islands along the c-axis and the frequent nucleation of multilayer 2D islands, {010} faces growing from a supersatured solution developed a "hill and valley" topography. This type of surface topography is observed at all temperatures. The step kinetic coefficient, βst, was determined in the temperature range 20-80 °C, and a steep increment in the kinetic coefficient is found with increasing temperature. From these data, the activation barrier for incorporation of building units in the {010} face was determined to be 70.7 ± 5.0 kJ/mol. Analysis of the kinetic data shows that at low temperatures (≤40 °C) growth of the {010} face is dominated by a mixed regime and at higher temperatures (>40 °C) growth is controlled solely by diffusion.
机译:在这项工作中,我们研究了从水溶液中生长的石膏晶体随温度和过饱和度变化的动力学。使用激光共聚焦微分干涉对比显微镜(LCM-DIM)和原子力显微镜(AFM)来原位观察{010}面的台阶进展和表面形态演变。我们发现,对于本研究中使用的实验条件,即使在低过饱和度下,二维成核也是主要的台阶生成机理,并且仅观察到了几个螺旋形小丘。由于二维岛沿c轴的拉长形态以及多层二维岛的频繁成核,{010}由超解决方案生成的面发展为“丘陵和山谷”形貌。在所有温度下都可以观察到这种类型的表面形貌。在20-80°C的温度范围内确定阶跃动力学系数βst,并且发现随着温度的升高,动力学系数会急剧增加。根据这些数据,确定在{010}面中掺入建筑单元的活化势垒为70.7±5.0 kJ / mol。动力学数据分析表明,在低温(≤40°C)下,{010}面的生长受混合态的控制,而在较高温度(> 40°C)下,生长仅受扩散的控制。

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