Testing the cation-hydration effect on the crystallization of Ca–Mg–CO 3 systems
Open accessAbstract
Significance: Magnesium-bearing carbonate minerals play critical roles in the health and function of the Earth system because they constitute a significant fraction of lithosphere carbon reservoir and build skeletal structures for the majority of marine invertebrate organisms. Despite wide occurrence, high-Mg and sole-Mg phases such as dolomite ([Ca,Mg]CO 3 ) and magnesite (MgCO 3 ) prove virtually impossible to be crystallized under ambient conditions. It has long been believed that Mg 2+ hydration is the cause for such a geological mystery. Here, we probe this hypothesis by investigating Ca–Mg–CO 3 precipitation in the absence of water and find direct proof suggesting the existence of a more intrinsic crystallization barrier. These findings provide a perspective augmenting our understanding in carbonate mineralogy, biomineralization, and mineral-carbonation processes.
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The dehydration of the Mg-water complex is considered the most critical barrier for dolomite nucleation and growth.
“Therefore, the dehydration of the Mg–water complex is considered the most critical barrier for dolomite nucleation and growth.21,27,32”
From Low-Temperature Synthesis of Disordered Dolomite and High-Magnesium Calcite in Ethanol–Water Solutions: The Solvation Effect and Implications (2022) · cites this paper as [32]
The Aqueous-phase reactions section describes Mg hydration as a long-standing explanation for difficulty forming dolomite, but the paper tests that explanation rather than endorsing it as the most critical barrier. The Conclusion (page not available) reports a fundamental barrier other than cation hydration that prevents ordered Mg-carbonate structures from forming, while acknowledging a hydration effect. (LLM, conf=0.88)
Checked by a reasoning model — may be wrong.
Experimental — accuracy not yet measuredAnhydrous amorphous Mg carbonates have been formed in aprotic solvents.
“but anhydrous amorphous Mg carbonates have been formed in aprotic solvents.17”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
The Results and Discussion report producing anhydrous amorphous magnesium carbonate. The paper says the experiments used dry formamide, described in the introduction as a hydrogen-bonding organic solvent (O=CH–NH₂); it does not support describing the solvent as aprotic. (LLM, conf=0.87)
Experimental — accuracy not yet measuredThe hydration problem is not the only limiting factor in inhibiting dolomite growth in a low-temperature environment; other factors are lattice limitation, difference in cation properties, and reduced surface energy from cation disordering.
“We recognize that the hydration problem is not the only limiting factor in inhibiting dolomite growth in a low-temperature environment. Other factors are lattice limitation,32 difference in cation properties,39 and reduced surface energy from cation disordering.40”
From Low-Temperature Synthesis of Disordered Dolomite and High-Magnesium Calcite in Ethanol–Water Solutions: The Solvation Effect and Implications (2022) · cites this paper as [32]
A significantly slower water-exchange rate of Mg2+ compared to that of Ca2+ resulted in a more stable hydration shell around Mg2+.
“On the other hand, a significantly slower water-exchange rate of Mg2+ compared to that of Ca2+ resulted in a more stable hydration shell around Mg2+.32”
From Low-Temperature Synthesis of Disordered Dolomite and High-Magnesium Calcite in Ethanol–Water Solutions: The Solvation Effect and Implications (2022) · cites this paper as [32]
Few works in the last decade have demonstrated precipitation of amorphous magnesium carbonates employing variable precursors (MgCl2•6H2O, MgO, and anhydrous MgCl2).
“As a matter of fact, few works produced in the last decade have demonstrated the precipitation of amorphous magnesium carbonates employing variable precursors (MgCl 2 •6H 2 O, 85 MgO, 86,87 and anhydrous MgCl 2 17,88 ).”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
The problem of synthesizing magnesite and dolomite at ambient conditions shares the same root.
“Considering that magnesite and dolomite belong to the same mineral class and space group of anhydrous carbonates, it is plausible to infer that the problem of synthesizing these minerals at ambient conditions share the same root.17”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
An intrinsic structural/spatial barrier of the CO3 2- groups in the magnesite symmetry group hinders the kinetics of magnesite precipitation at room temperature.
“and/or (ii) to the intrinsic structural/spatial barrier of the CO 3 2-groups 17 in the magnesite symmetry group.”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
In systems with high Mg contents, the main product was anhydrous amorphous Mg carbonate.
“It was observed that in systems with high Mg contents the main product was anhydrous amorphous Mg carbonate.”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
The product of the reaction shifted towards protodolomite at Mg/Ca = 1, and in systems with Mg/Ca < 1, the reaction shifted towards precipitation of crystalline calcite.
“The product of the reaction shifted towards protodolomite at Mg/Ca = 1, and in the systems with Mg/Ca < 1, the reaction shifted towards the precipitation of crystalline calcite.”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
The tight cage arrangement in the R3̄C geometry of the magnesite structure reduces the degrees of freedom of the carbonate groups, which also hampers the precipitation step.
“Moreover, the tight cage arrangement in the R3 ˉC geometry of the magnesite structure reduces the degrees of freedom of the carbonate groups, which also hampers the precipitation step.17,20”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
Disorder among the CO3 2- groups due to their limited degrees of freedom around the small Mg2+ cations may mean that the dolomite/magnesite problem is a stereochemical issue: strong electrostatic attraction to Mg2+ prevents rotation and tilting of the carbonate groups, hindering crystalline ordering in the precipitation step.
“The observations were associated to the disorder among the CO 3 2groups due to their limited degrees of freedom around the small Mg 2+ cations (radii of Mg 2+ is ca.30% smaller than Ca 2+ ), which may mean that the dolomite/magnesite problem is a stereochemical issue: the strong electrostatic attraction to the Mg 2+ cations prevents the rotation and tilting of the carbonate groups, hindering the”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
High Mg contents hinder long-range order in the Mg-CO3 system, implying an intrinsic difficulty in obtaining the rhombohedral arrangement of magnesite.
“These findings demonstrated that high Mg contents hinders the long-range orders in the Mg-CO 3 system, implying that there is an intrinsic difficulty in obtaining the rhombohedral arrangement of magnesite.”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [17]
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- Authors
- Xu, J., Yan, C., Zhang, F., Konishi, H., Xu, H., & Teng, H. H.
- Affiliations
- George Washington University (US)
- University of Wisconsin–Madison (US)
- Venue
- Proceedings of the National Academy of Sciences
- Publisher
- National Academy of Sciences
- Published
- 2013-10-14
- Volume
- 110
- Issue
- 44
- Pages
- 17750-17755
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- PMC
- PMC3816432
- OpenAlex
- W1998776045
- Semantic Scholar
- 81844e40b0725ca95f815f1a25f77a0422167b58
- Cited by
- 181
- References
- 77
- Citations by year
- 2026: 27 · 2025: 11 · 2024: 14 · 2023: 14 · 2022: 15 · 2021: 18 · 2020: 10 · 2019: 17 · 2018: 13 · 2017: 10 · 2016: 13 · 2015: 12 · 2014: 7
- FWCI
- 4.07
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Proceedings of the National Academy of Sciences (publishedVersion)
- Europe PMC (PubMed Central) (publishedVersion)
- PubMed Central (publishedVersion)
- PubMed (publishedVersion)
- Funders
- U.S. Department of Energy (DE‐FG02‐, FG02-02ER15366, DEFG0202ER15366)
- Topics
- Physical Sciences › Materials Science › Biomaterials › Calcium Carbonate Crystallization and Inhibition
- Physical Sciences › Environmental Science › Environmental Engineering › CO2 Sequestration and Geologic Interactions
- Physical Sciences › Materials Science › Materials Chemistry › Crystallization and Solubility Studies
- Keywords
- dolomite problem, magnesite, dolomite, magnesian calcite, amorphous carbonates, protodolomite, nanocrystals, calcium carbonate, biomineralization, CO2 mineralization
- MeSH terms
- Calcium Carbonate, Crystallization, Image Processing, Computer-Assisted, Magnesium, Microscopy, Electron, Scanning, Chemical Precipitation, Spectrophotometry, Infrared, Water, X-Ray Diffraction, Microscopy, Electron, Transmission
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