钙矾石-偏钙矾石转换中的可逆有序-无序转变

Tulio Honoro, S. A. Dandachli, Alexandra Bourdot
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引用次数: 0

摘要

. 采用大正则蒙特卡罗(GCMC)和(经典)分子动力学(MD)混合模拟方法对渗透系综进行采样,研究了钙矾石在吸附下的稳定性和向偏钙矾石转化的过程。模拟得到的解吸分支及相应的体积变化与实验结果一致。我们特别关注低相对湿度下的结构变化,这与偏钙矾石转化有关,这被认为是一种结构未知的无序多晶钙矾石。我们证明了钙矾石向偏钙矾石的转化与熵的增加有关。模拟得到的吸附分支在钙矾石区域是可逆的,与实验结果一致。偏钙矾石转化为钙矾石的可逆性是实验观察到的,但所采用的模拟方法没有捕捉到。与钙矾石解吸有关的大变形使得用渗透集合的直接采样很难捕获可逆性。进一步,我们讨论了氢键在钙矾石吸附循环中观察到的滞回效应中的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reversible Order-Disorder Transition in Ettringite-Metaettringite Conversion
. The stability of ettringite under sorption and the conversion into metaettringite are studied using hybrid Grand Canonical Monte Carlo (GCMC) and (classical) Molecular Dynamics (MD) simulations sampling the osmotic ensemble. The desorption branch obtained from simulation and the associated volume changes are in agreement with the experimental evidence. We pay special attention to the structural changes at low RH, which is associated with metaettringite conversion, which is recognized as a disordered polymorph of ettringite with an unknown structure to date. We show that the conversion of ettringite into metaettringite is associated with an increase in entropy. The adsorption branch obtained from simulations is reversible in the ettringite domain in agreement with experiments. The reversibility in the conversion of metaettringite into ettringite, which is observed experimentally, is not captured by the simulation approach adopted. The large deformations associated with ettringite desorption make it difficult to capture reversibility with a direct sampling of the osmotic ensemble. Further, we discuss the role of hydrogen bonds on the hysteresis observed in sorption cycles in ettringite.
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