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Updated: Jul 19, 2025

Facile Preparation of Ultrafine Aluminum Hydroxide Particles with or without Mesoporous MCM-41 in Ambient Environments
Published on: May 11, 2017
Anhydrous Aluminum Carbonates and Isostructural Compounds
Lkhamsuren Bayarjargal1, Dominik Spahr1, Victor Milman2
1Institute of Geosciences, Goethe University Frankfurt, Altenhöferallee 1, Frankfurt 60438, Germany.
Researchers synthesized novel aluminum carbonates, Al2[C2O5][CO3]2 and Al2[CO3]3, under high pressure and temperature. These compounds, featuring unique carbonate structures, can be recovered at ambient conditions and offer insights into deep Earth carbon storage.
Area of Science:
- High-pressure mineral physics and inorganic chemistry.
- Investigating the behavior of oxides and carbonates under extreme conditions.
Background:
- Understanding the Earth's deep carbon cycle requires knowledge of carbon's behavior under high pressures and temperatures.
- Aluminum oxides (Al2O3) are relevant to mantle compositions, but their high-pressure carbonate phases are not well-characterized.
Purpose of the Study:
- To synthesize and characterize new anhydrous aluminum carbonate phases.
- To determine the structural properties and formation conditions of these carbonates.
- To explore the potential for similar structures in other metal oxides and their implications for deep Earth carbon storage.
Main Methods:
- High-pressure and high-temperature synthesis of aluminum carbonates from Al2O3 and CO2.
- Characterization using Raman spectroscopy and X-ray diffraction for structural analysis.
- Density functional theory (DFT) calculations to predict reactions with other metal oxides.
Main Results:
- Successfully synthesized two anhydrous aluminum carbonates: Al2[CO3]3 and Al2[C2O5][CO3]2.
- Al2[CO3]3 forms at 24-28 GPa, characterized by isolated carbonate groups.
- Al2[C2O5][CO3]2 forms above 38 GPa, featuring pyrocarbonate and trigonal carbonate groups, and octahedrally coordinated cations.
- Both synthesized aluminum carbonates are recoverable under ambient conditions.
- DFT predicts isostructural compounds for Fe2O3, Ti2O3, Ga2O3, In2O3, and MgSiO3.
- MgSi[C2O5][CO3]2 is predicted stable in the mantle and offers novel carbon speciation for storage.
Conclusions:
- New aluminum carbonate structures, Al2[CO3]3 and Al2[C2O5][CO3]2, have been synthesized and structurally elucidated.
- The pyrocarbonate-bearing Al2[C2O5][CO3]2 structure type is predicted to form in other metal oxides under high pressure.
- This structure type provides a potential mechanism for significant carbon storage in the deep Earth, incorporating abundant mantle elements.
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