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Macro- to nanoscale study of the effect of aqueous sulphate on calcite growth

机译:硫酸盐水溶液对方解石生长影响的宏观到纳米研究

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Calcite growth rates were measured in the presence of sulphate using mixed-flow reactors and in situ Atomic Force Microscopy. Preliminary observations reveal that the kinetics and mechanism of the calcite growth was altered by the presence of sulphate. Calcite growth rates in the presence of sulphate (>= 5 mM) were decreased and two-dimensional nuclei tend to grow on top of existing nuclei, rather than spreading. The height of new nuclei was approx 4 A, 1 A greater than that of pure calcite growth. This difference reflects the incorporation of tetrahedral SO_4~(2-) anions into the calcite lattice.
机译:使用混合流反应器和原位原子力显微镜在硫酸盐存在下测量方解石的生长速率。初步观察表明,硫酸盐的存在改变了方解石生长的动力学和机理。存在硫酸盐(> = 5 mM)时方解石的生长速率降低,并且二维原子核倾向于在现有原子核的顶部生长,而不是扩散。新核的高度约为4 A,比纯方解石生长的高度大1A。这种差异反映了四面体SO_4〜(2-)阴离子掺入方解石晶格中。

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