Volume 56, Issue 51 pp. 16202-16206
Communication

High-Magnesium Calcite Mesocrystals: Formation in Aqueous Solution under Ambient Conditions

Dr. Pao-Tao Yu

Dr. Pao-Tao Yu

Department of Chemistry, National (Taiwan) University, No. 1, Section 4, Roosevelt Road, Taipei, 10617 Taiwan

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Chieh Tsao

Chieh Tsao

Department of Chemistry, National (Taiwan) University, No. 1, Section 4, Roosevelt Road, Taipei, 10617 Taiwan

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Dr. Chun-Chieh Wang

Dr. Chun-Chieh Wang

National Synchrotron Radiation Research Center, Hsinchu, 30076 Taiwan

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Chun-Yu Chang

Chun-Yu Chang

Department of Chemistry, National (Taiwan) University, No. 1, Section 4, Roosevelt Road, Taipei, 10617 Taiwan

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Dr. Chia-Hsin Wang

Dr. Chia-Hsin Wang

National Synchrotron Radiation Research Center, Hsinchu, 30076 Taiwan

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Prof. Dr. Jerry Chun Chung Chan

Corresponding Author

Prof. Dr. Jerry Chun Chung Chan

Department of Chemistry, National (Taiwan) University, No. 1, Section 4, Roosevelt Road, Taipei, 10617 Taiwan

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First published: 02 November 2017
Citations: 20

Graphical Abstract

Mesocrystals of high-Mg calcites are prepared in aqueous solution using phospholipids as additives. The dark-field images originating from the (104) diffraction spot indicate that a large collection of the nanocrystallites of Mg-calcites have the same orientation.

Abstract

Mesocrystals of high-magnesian calcites are commonly found in biogenic calcites. Under ambient conditions, it remains challenging to prepare mesocrystals of high-magnesian calcite in aqueous solution. We report that mesocrystals of calcite with magnesium content of about 20 mol % can be obtained from the phase transformation of magnesian amorphous calcium carbonate (Mg-ACC) in lipid solution. The limited water content on the Mg-ACC surface would reduce the extent of the dissolution–reprecipitation process and bias the phase transformation pathway toward solid-state reaction. We infer from the selected area electron diffraction patterns and the dark-field transmission electron microscopic images that the formation of Mg-calcite mesocrystals occurs through solid-state secondary nucleation, for which the phase transformation is initiated near the mineral surface and the crystalline phase propagates gradually toward the interior part of the microspheres of Mg-ACC.

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