2014
DOI: 10.1017/s0885715614000888
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Calcite V: a hundred-year-old mystery has been solved

Abstract: Since Boeke's finding of a reversible phase transition of calcite (calcium carbonate, CaCO 3 ) at elevated temperatures [Boeke, H. E. (1912). Neues Jahrb. Mineral. 1, 91-121], and following W. L. Bragg's determination of the structure of the room-temperature Phase I [Bragg, W. L. (1914). Proc. R. Soc. Lond. A 89,, the high-temperature Phase V of calcite has been an enduring mystery. Here, we summarize a paper on the structure of Phase V [Ishizawa, N., Setoguchi, H. and Yanagisawa, K. (2013). Sci. Rep. 3, 2832… Show more

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Cited by 17 publications
(13 citation statements)
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“…Carbonate rotational disorder at high temperatures is common. Calcite (R 3c) undergoes a second-order phase transition to 'carbonate disordered' calcite IV approaching a critical temperature of T c ¼ 970 C. 33,34 This transition is characterized by the rotation of carbonates by 60 about their threefold axes, effectively inverting about the carbon center. Above 970 C calcite IV becomes further disordered into a 'carbonate-melted' calcite V with R 3m symmetry.…”
Section: Carbonate Orderingmentioning
confidence: 99%
“…Carbonate rotational disorder at high temperatures is common. Calcite (R 3c) undergoes a second-order phase transition to 'carbonate disordered' calcite IV approaching a critical temperature of T c ¼ 970 C. 33,34 This transition is characterized by the rotation of carbonates by 60 about their threefold axes, effectively inverting about the carbon center. Above 970 C calcite IV becomes further disordered into a 'carbonate-melted' calcite V with R 3m symmetry.…”
Section: Carbonate Orderingmentioning
confidence: 99%
“…Although the mentioned “calcite-I → calcite-II → calcite-IIIb → calcite-III” phase transitions in CaCO 3 were thoroughly studied both structurally and spectroscopically and the aragonite equation of state (EoS) was constrained throughout its stability field up to 29 GPa and 1673 K, there is a wide gap between the high-temperature boundary of the aragonite stability field and CaCO 3 melting line (Figure ) where neither structures nor properties of thermodynamically stable phases have ever been reported. In a few experimental works, the high-temperature transition of aragonite into a previously unknown phase was studied; the latter was described as “disordered calcite” , “disordered phase” , or “new phase” , , or associated with a low-pressure calcite-V polymorph ( R 3̅ m space group) known to be stable above ∼1240 K at ambient pressure, , and no attempts to reveal any crystal structures, symmetries, or even unit cells have been reported.…”
Section: Introductionmentioning
confidence: 99%
“…Dynamic disorder is a well-known phenomenon observed upon heating of organic crystals. It is also quite widespread in inorganic compounds with rigid triangular anionic groups such as carbonates and nitrates, 1 for example, NaNO 3 , 2-5 KNO 3 , 6,7 AgNO 3 8,9 and alkaline earth metal carbonates such as CaCO 3 , [10][11][12][13][14] SrCO 3 14,15 and BaCO 3 . 14,15 For the listed compounds, the transition to the dynamically disordered state is realized at high temperatures, usually close to the temperature of melting or decomposition.…”
mentioning
confidence: 99%
“…With a further increase in the temperature, CaCO 3 -IV transforms into a ''fully'' disordered state, CaCO 3 -V, in which [CO 3 ] groups rotate continuously and do not remain for a long time at any position. [11][12][13] Similarly, this is applicable to [BO 3 ] groups in cube cages in Ba 3 (BO 3 ) 2 . The transition of CaCO 3 to a disordered state begins when the angle of librations of the [CO 3 ] groups around the axis perpendicular to the threefold molecular axis exceeds the critical value of B451.…”
mentioning
confidence: 99%