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在超临界二氧化碳中进行水镁石碳酸化过程中无定形中间体的原位成像

In situ imaging of amorphous intermediates during brucite carbonation in supercritical CO.

作者信息

Zhang Xin, Lea Alan S, Chaka Anne M, Loring John S, Mergelsberg Sebastian T, Nakouzi Elias, Qafoku Odeta, De Yoreo James J, Schaef Herbert T, Rosso Kevin M

机构信息

Physical and Computational Sciences Directorate, Pacific Northwest National Laboratory, Richland, WA, USA.

Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, Richland, WA, USA.

出版信息

Nat Mater. 2022 Mar;21(3):345-351. doi: 10.1038/s41563-021-01154-5. Epub 2021 Nov 29.

Abstract

Progress in understanding crystallization pathways depends on the ability to unravel relationships between intermediates and final crystalline products at the nanoscale, which is a particular challenge at elevated pressure and temperature. Here we exploit a high-pressure atomic force microscope to directly visualize brucite carbonation in water-bearing supercritical carbon dioxide (scCO) at 90 bar and 50 °C. On introduction of water-saturated scCO, in situ visualization revealed initial dissolution followed by nanoparticle nucleation consistent with amorphous magnesium carbonate (AMC) on the surface. This is followed by growth of nesquehonite (MgCO·3HO) crystallites. In situ imaging provided direct evidence that the AMC intermediate acts as a seed for crystallization of nesquehonite. In situ infrared and thermogravimetric-mass spectrometry indicate that the stoichiometry of AMC is MgCO·xHO (x = 0.5-1.0), while its structure is indicated to be hydromagnesite-like according to density functional theory and X-ray pair distribution function analysis. Our findings thus provide insight for understanding the stability, lifetime and role of amorphous intermediates in natural and synthetic systems.

摘要

在理解结晶途径方面取得的进展取决于在纳米尺度上揭示中间体与最终结晶产物之间关系的能力,这在高压和高温下是一项特殊挑战。在此,我们利用高压原子力显微镜直接观察了在90巴和50°C的含水超临界二氧化碳(scCO₂)中菱镁矿的碳酸化过程。引入水饱和的scCO₂后,原位观察显示先是发生初始溶解,随后在表面形成与无定形碳酸镁(AMC)一致的纳米颗粒成核现象。接着是三水碳镁石(MgCO₃·3H₂O)微晶的生长。原位成像提供了直接证据,表明AMC中间体充当了三水碳镁石结晶的晶种。原位红外光谱和热重-质谱分析表明,AMC的化学计量比为MgCO₃·xH₂O(x = 0.5 - 1.0),而根据密度泛函理论和X射线对分布函数分析,其结构类似于水菱镁矿。因此我们的研究结果为理解无定形中间体在天然和合成体系中的稳定性、寿命及作用提供了见解。

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