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多级 CaCO 成核的电泳和电位特征。

Electrophoretic and potentiometric signatures of multistage CaCO nucleation.

机构信息

Institute of Physical Chemistry, Polish Academy of Sciences, Warsaw, Poland.

Department of Chemistry and Biochemistry, Józef Piłsudski University of Physical Education, Warsaw, Poland.

出版信息

J Colloid Interface Sci. 2019 May 15;544:249-256. doi: 10.1016/j.jcis.2019.03.002. Epub 2019 Mar 2.

Abstract

HYPOTHESIS

Calcium carbonate nucleation is often a complex and multistep process that is difficult to follow in situ. The time-resolved electrochemical and electrophoretic methods can provide a new insight into the nucleation pathway.

EXPERIMENTS

Here, we used a combination of speciation calculations with time-resolved electrophoretic and potentiometric methods to monitor calcium carbonate precipitation from a slightly supersaturated solution.

FINDINGS

After an initial mixing period of three minutes in which metastable CaCO phases may have nucleated and subsequently dissolved due to locally-high supersaturations, bulk solution pH and Ca concentrations stabilize before decreasing in tandem with the precipitation of a CaCO phase. After an hour, the precipitate is dominated by calcite that grows at the expense of dissolving vaterite. The time-dependent electrokinetic potential shows analogous signatures of multistage nucleation process: initial rapid changes in ζ-potential are followed by much slower equilibration starting about one hour after reagents are mixed. The changes in ζ-potential, solution pH, saturation indexes, and particle morphology are consistent with vaterite to calcite transformation via dissolution of the former and recrystallization of the latter. These findings highlight the potential use of ζ-potential measurements for monitoring polymorphic transformations of carbonate phases in-situ.

摘要

假设

碳酸钙成核通常是一个复杂的多步骤过程,难以进行原位跟踪。时间分辨电化学和电泳方法可以为成核途径提供新的见解。

实验

在这里,我们使用了形态分析计算与时间分辨电泳和电位法的组合,从略微过饱和的溶液中监测碳酸钙的沉淀。

发现

在最初的三分钟混合期内,可能会有亚稳 CaCO 相成核,随后由于局部过饱和度较高而溶解,在沉淀 CaCO 相的同时,溶液的 pH 值和 Ca 浓度稳定下来,然后再下降。一个小时后,沉淀物主要由方解石组成,方解石的生长是以溶解文石为代价的。随时间变化的动电电势显示出多阶段成核过程的类似特征:ζ 电位的初始快速变化后,约在试剂混合一小时后,开始进行慢得多的平衡。ζ 电位、溶液 pH 值、饱和度指数和颗粒形态的变化与文石到方解石的转变一致,前者通过溶解,后者通过再结晶。这些发现突出了 ζ 电位测量在原位监测碳酸盐相多晶型转变中的潜在用途。

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