Abstract
Calcite, CaCO3, is a common carbon-bearing mineral found on the Earth.s surface. As carbon dioxide in the atmosphere can be sequestered in carbon-bearing minerals (carbonates), the stability of carbonate minerals is of great interest to earth science. In our study, in-situ X-ray diffraction observations indicate that calcium carbonate (CaCO3) transforms to an orthopyroxene-type structure that has fourfold coordination of carbon cations, when heated to temperatures >1500 K at pressures >130 GPa, which is in agreement with theoretical predictions from ab initio calculations. The volume reduction of this transition is ~0.5%, and the high-pressure phase did not quench on decompression to ambient pressure. Although the post-aragonite phase, which has threefold coordination of carbon cations, shows strongly anisotropic compressibility of each axis of the unit-cell parameter, no obvious anisotropy in the pyroxene-type phase was observed. The stability of this new calcium carbonate implies that the carbon dioxide could be storable at the base of the lower mantle.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- Experimental evidence of sixfold oxygen coordination for phosphorus
- Dehydration of Ca-montmorillonite at the crystal scale. Part I: Structure evolution
- Dehydration of Ca-montmorillonite at the crystal scale. Part 2. Mechanisms and kinetics
- The high-pressure crystal structure of potassium hydrogen carbonate (KHCO3)
- Effect of Al3+ and H+ on the elastic properties of stishovite
- Investigation of synthetic Mg1.3V1.7O4 spinel with MgO inclusions: Case study of a spinel with an apparently occupied interstitial site
- Thermal expansion of deuterated hopeite, Zn3(PO4)2·4D2O
- Compression, thermal expansion, structure, and instability of CaIrO3, the structure model of MgSiO3 post-perovskite
- Crystal chemical relationships in the tourmaline group: Structural constraints on chemical variability
- The energetics of hematite dissolution in iron-oxide-rich melts: In situ high-temperature calorimetric studies
- A simple model of oscillatory zoning in magmatic plagioclase: Development of an isothermal undercooling model
- TEM investigation of Ca-rich plagioclase: Structural β uctuations related to the I1-P1 phase transition
- Crystal-chemistry of Ni in marine ferromanganese crusts and nodules
- Effect of structural transitions on properties of high-pressure silicate melts: 27Al NMR, glass densities, and melt viscosities
- Material conversion from paper-sludge ash in NaOH, KOH, and LiOH solutions
- High-pressure phase relations and crystal chemistry of calcium ferrite-type solid solutions in the system MgAl2O4-Mg2SiO4
- Origin of atoll garnets in eclogites and implications for the redistribution of trace elements during slab exhumation in a continental subduction zone
- Determination of the refractive index of particles in the clay and sub-micrometer size range
- Crystal chemistry of synthetic Ca2Al3Si3O12OH–Sr2Al3Si3O12OH solid-solution series of zoisite and clinozoisite
- Thermal infrared spectroscopy and modeling of experimentally shocked basalts
- P-V and T-V Equations of State of natural biotite: An in-situ high-pressure and high-temperature powder diffraction study, combined with Mössbauer spectroscopy
- Cation ordering in MgTi2O5 (karrooite): Probing temperature dependent effects with neutrons
- An order-disorder model for omphacitic pyroxenes in the system jadeite-diopsidehedenbergite- acmite, with applications to eclogitic rocks
- The high-pressure structural configurations of Ca0.2Sr0.8Al2Si2O8 feldspar: The I1̅-I2/c and I2/c-P21/c phase transitions
- Mechanisms of diamond oxidation and their bearing on the fluid composition in kimberlite magmas
- Brittle fracturing and fracture healing of zircon: An integrated cathodoluminescence, EBSD, U-Th-Pb, and REE study
- Galaxite, MnAl2O4, a spectroscopic standard for tetrahedrally coordinated Mn2+ in oxygen-based mineral structures
- Magmatic paragonite in trondhjemites from the Sierra del Convento mélange, Cuba
- Valence state partitioning of Cr and V between pyroxene-melt: Estimates of oxygen fugacity for martian basalt QUE 94201
- Crystal-structure refinement of Na-bearing clinopyroxenes from mantle-derived eclogite xenoliths
- High-pressure transition of CaCO3
Articles in the same Issue
- Experimental evidence of sixfold oxygen coordination for phosphorus
- Dehydration of Ca-montmorillonite at the crystal scale. Part I: Structure evolution
- Dehydration of Ca-montmorillonite at the crystal scale. Part 2. Mechanisms and kinetics
- The high-pressure crystal structure of potassium hydrogen carbonate (KHCO3)
- Effect of Al3+ and H+ on the elastic properties of stishovite
- Investigation of synthetic Mg1.3V1.7O4 spinel with MgO inclusions: Case study of a spinel with an apparently occupied interstitial site
- Thermal expansion of deuterated hopeite, Zn3(PO4)2·4D2O
- Compression, thermal expansion, structure, and instability of CaIrO3, the structure model of MgSiO3 post-perovskite
- Crystal chemical relationships in the tourmaline group: Structural constraints on chemical variability
- The energetics of hematite dissolution in iron-oxide-rich melts: In situ high-temperature calorimetric studies
- A simple model of oscillatory zoning in magmatic plagioclase: Development of an isothermal undercooling model
- TEM investigation of Ca-rich plagioclase: Structural β uctuations related to the I1-P1 phase transition
- Crystal-chemistry of Ni in marine ferromanganese crusts and nodules
- Effect of structural transitions on properties of high-pressure silicate melts: 27Al NMR, glass densities, and melt viscosities
- Material conversion from paper-sludge ash in NaOH, KOH, and LiOH solutions
- High-pressure phase relations and crystal chemistry of calcium ferrite-type solid solutions in the system MgAl2O4-Mg2SiO4
- Origin of atoll garnets in eclogites and implications for the redistribution of trace elements during slab exhumation in a continental subduction zone
- Determination of the refractive index of particles in the clay and sub-micrometer size range
- Crystal chemistry of synthetic Ca2Al3Si3O12OH–Sr2Al3Si3O12OH solid-solution series of zoisite and clinozoisite
- Thermal infrared spectroscopy and modeling of experimentally shocked basalts
- P-V and T-V Equations of State of natural biotite: An in-situ high-pressure and high-temperature powder diffraction study, combined with Mössbauer spectroscopy
- Cation ordering in MgTi2O5 (karrooite): Probing temperature dependent effects with neutrons
- An order-disorder model for omphacitic pyroxenes in the system jadeite-diopsidehedenbergite- acmite, with applications to eclogitic rocks
- The high-pressure structural configurations of Ca0.2Sr0.8Al2Si2O8 feldspar: The I1̅-I2/c and I2/c-P21/c phase transitions
- Mechanisms of diamond oxidation and their bearing on the fluid composition in kimberlite magmas
- Brittle fracturing and fracture healing of zircon: An integrated cathodoluminescence, EBSD, U-Th-Pb, and REE study
- Galaxite, MnAl2O4, a spectroscopic standard for tetrahedrally coordinated Mn2+ in oxygen-based mineral structures
- Magmatic paragonite in trondhjemites from the Sierra del Convento mélange, Cuba
- Valence state partitioning of Cr and V between pyroxene-melt: Estimates of oxygen fugacity for martian basalt QUE 94201
- Crystal-structure refinement of Na-bearing clinopyroxenes from mantle-derived eclogite xenoliths
- High-pressure transition of CaCO3