Structural transitions of calcium carbonate by molecular dynamics simulation

Elizaveta Sidler, Raffaela Cabriolu
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Abstract

Calcium carbonate plays a crucial role in the global carbon cycle, and its phase diagram has always been of significant scientific interest. In this study, we used molecular dynamics (MD) to investigate several structural phase transitions of calcium carbonate. Using the Raiteri potential model, we explored the structural transitions occurring at a constant pressure of 1 bar with temperatures ranging from 300 K to 2500 K, and at a constant temperature of 1600 K with pressures ranging from 0 to 13 GPa. At increasing temperatures, the transitions calcite, CaCO$_3$-IV, and CaCO$_3$-V are observed and characterized. Within the calcite structure, CO$_3^{2-}$ ions are ordered between layers. As temperature increases, the calcite to CaCO$_3$-IV transition occurs, determining the partial disordering of CO$_3^{2-}$ ions. At a higher temperature, CaCO$_3$-IV transforms into CaCO$_3$-V. By applying free energy analysis, we have classified the last transition as a continuous order-disorder phase transition. At a temperature of 2000 K, it appears a `disordered CaCO$_3$' structure, characterized by low order within the calcium and carbonate sublattices and the free rotation of CO$_3^{2-}$ ions. At increasing pressures, two calcium carbonate transformations were observed. At $P=$ 2 GPa, the CaCO$_3$-IV phase undergoes a phase transition into CaCO$_3$-V, demonstrating that the model can describe the transition between these two phases as pressure and temperature-driven. Another phase transition was detected at $P=$ 4.25 GPa -- CaCO$_3$-V transits into the recently discovered CaCO$_3$-Vb phase. This transition is classified as a first-order phase transition by structural analysis and free energy-based arguments.
分子动力学模拟碳酸钙的结构转变
碳酸钙在全球碳循环中起着至关重要的作用,其相图一直备受科学界关注。在这项研究中,我们利用分子动力学(MD)研究了碳酸钙的几种结构相变。利用 Raiteri 势能模型,我们探索了在恒压 1 bar、温度介于 300 K 至 2500 K 之间,以及恒温 1600 K、压力介于 0 至 13 GPa 之间发生的结构转变。在温度升高时,观察到方解石、CaCO$_3$-IV 和 CaCO$_3$-V 的转变,并对其进行了描述。在方解石结构中,CO$_3^{2-}$ 离子在各层之间有序排列。随着温度的升高,方解石向 CaCO$_3$-IV 过渡,决定了 CO$_3^{2-}$ 离子的部分无序化。在高温下,CaCO$_3$-IV 转变为 CaCO$_3$-V。通过自由能分析,我们将最后一种转变归类为连续有序-无序相变。在 2000 K 的温度下,出现了 "无序 CaCO$_3$"结构,其特点是钙和碳酸亚晶格内的有序度较低,CO$_3^{2-}$ 离子自由旋转。在压力增加时,观察到两种碳酸钙转化。在 $P=$ 2 GPa 时,CaCO$_3$-IV 相转变为 CaCO$_3$-V,这表明该模型可以描述这两种相之间的转变是由压力和温度驱动的。在 $P=$ 4.25 GPa 时检测到了另一个相变--CaCO$_3$-V 转变为最近发现的 CaCO$_3$-Vb 相。通过结构分析和基于自由能的论证,这一转变被归类为一阶相变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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