High-pressure spectroscopic study of siderite (FeCO3) with a focus on spin crossover
-
Valerio Cerantola
, Catherine McCammon
Abstract
Fe-bearing carbonates have been proposed as possible candidate host minerals for carbon inside the Earth’s interior and hence their spectroscopic properties can provide constraints on the deep carbon cycle. Here we investigate high-pressure spin crossover in synthetic FeCO3 (siderite) using a combination of Mössbauer, Raman, and X-ray absorption near edge structure spectroscopy in diamond-anvil cells. These techniques sensitive to the short-range atomic environment show that at room temperature and under quasi-hydrostatic conditions, spin crossover in siderite takes place over a broad pressure range, between 40 and 47 GPa, in contrast to previous X-ray diffraction data that described the transition as a sharp volume collapse at approximately 43 GPa. Based on these observations we consider electron spin pairing in siderite to be a dynamic process, where Fe atoms can be either high spin or low spin in the crossover region. Mode Grüneisen parameters extracted from Raman spectra collected at pressures below and above spin crossover show a drastic change in stiffness of the Fe-O octahedra after the transition, where they become more compact and hence less compressible. Mössbauer experiments performed on siderite single crystals as well as powder samples demonstrate the effect of differential stress on the local structure of siderite Fe atoms in a diamond-anvil cell. Differences in quadrupole splitting values between powder and single crystals show that local distortions of the Fe site in powder samples cause spin crossover to start at higher pressure and broaden the spin crossover pressure range.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- On understanding the structure and composition of crystals
- Stable and metastable silicate liquid immiscibility in ferrobasalts
- When was the Earth’s conveyor belt set in motion?
- Trace element partitioning into sulfide: How lithophile elements become chalcophile and vice versa
- Petrology on Mars
- Hf and Nd isotope systematics of early Archean komatiites from surface sampling and ICDP drilling in the Barberton Greenstone Belt, South Africa
- Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13 at high temperature
- Tracking the thermal decomposition of plasma-sprayed hydroxylapatite
- Experimental constraints on bubble formation and growth during magma ascent: A review
- Ankerite grains with dolomite cores: A diffusion chronometer for low- to medium-grade regionally metamorphosed clastic sediments
- Crystal structure, high-pressure, and high-temperature behavior of carbonates in the K2Mg(CO3)2–Na2Mg(CO3)2 join
- Temperature micro-mapping in oscillatory-zoned chlorite: Application to study of a green-schist facies fault zone in the Pyrenean Axial Zone (Spain)
- Micro- and nano-characterization of Zn-clays in nonsulfide supergene ores of southern Peru
- Mineralogical characterization of individual growth structures of Mn-nodules with different Ni+Cu content from the central Pacific Ocean
- The magma plumbing system of the Emeishan large igneous province and its role in basaltic magma differentiation in a continental setting
- Weathering of the Ethiopian volcanic province: A new weathering index to characterize and compare soils
- Recommended mineral-melt partition coefficients for FRTEs (Cu), Ga, and Ge during mantle melting
- Tetrahedral plot diagram: A geometrical solution for quaternary systems
- Investigations on alunogen under Mars-relevant temperature conditions: An example for a single-crystal-to-single-crystal phase transition
- Crystallization of calcium oxalate hydrates by interaction of calcite marble with fungus Aspergillus niger
- Direct and indirect evidence for free oxygen (O2–) in MO-silicate glasses and melts (M = Mg, Ca, Pb)
- Effect of fluid composition on growth rate of monazite in quartzite at 1.0 GPa and 1000 °C
- Determination of the full elastic tensor of single crystals using shear wave velocities by Brillouin spectroscopy
- Temperature dependence of the velocity-density relation for liquid metals under high pressure: Implications for the Earth’s outer core
- Thermal, compositional, and compressional demagnetization of cementite
- The MnCO3-II high-pressure polymorph of rhodocrosite
- Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China
- Hydrogrossular, Ca3Al2(SiO4)3–x(H4O4)x: An ab initio investigation of its structural and energetic properties
- High-pressure synthesis of skiagite-majorite garnet and investigation of its crystal structure
- Mineralogical evolution of Fe–Si-rich layers at the olivine-water interface during carbonation reactions
- High-pressure spectroscopic study of siderite (FeCO3) with a focus on spin crossover
- Exploring the potential of Raman spectroscopy for crystallochemical analyses of complex hydrous silicates: I. Amphiboles
- Apexite, NaMg(PO4)·9H2O, a new struvite-type phase with a heteropolyhedral cluster
- The mechanism of infiltration of metamorphic fluids recorded by hydration and carbonation of epidote-amphibolite facies metabasaltic sills in the SW Scottish Highlands
- The axial ratio of hcp Fe and Fe–Ni–Si alloys to the conditions of Earth’s inner core
- Shock-induced mobilization of metal and sulfide in planetesimals: Evidence from the Buck Mountains 005 (L6 S4) dike-bearing chondrite
- The accretion and differentiation of Earth under oxidizing conditions
- Dislocation microstructures in simple-shear-deformed wadsleyite at transition-zone conditions: Weak-beam dark-field TEM characterization of dislocations on the (010) plane
- Chemical composition and crystal structure of merrillite from the Suizhou meteorite
Articles in the same Issue
- On understanding the structure and composition of crystals
- Stable and metastable silicate liquid immiscibility in ferrobasalts
- When was the Earth’s conveyor belt set in motion?
- Trace element partitioning into sulfide: How lithophile elements become chalcophile and vice versa
- Petrology on Mars
- Hf and Nd isotope systematics of early Archean komatiites from surface sampling and ICDP drilling in the Barberton Greenstone Belt, South Africa
- Quasicrystals at extreme conditions: The role of pressure in stabilizing icosahedral Al63Cu24Fe13 at high temperature
- Tracking the thermal decomposition of plasma-sprayed hydroxylapatite
- Experimental constraints on bubble formation and growth during magma ascent: A review
- Ankerite grains with dolomite cores: A diffusion chronometer for low- to medium-grade regionally metamorphosed clastic sediments
- Crystal structure, high-pressure, and high-temperature behavior of carbonates in the K2Mg(CO3)2–Na2Mg(CO3)2 join
- Temperature micro-mapping in oscillatory-zoned chlorite: Application to study of a green-schist facies fault zone in the Pyrenean Axial Zone (Spain)
- Micro- and nano-characterization of Zn-clays in nonsulfide supergene ores of southern Peru
- Mineralogical characterization of individual growth structures of Mn-nodules with different Ni+Cu content from the central Pacific Ocean
- The magma plumbing system of the Emeishan large igneous province and its role in basaltic magma differentiation in a continental setting
- Weathering of the Ethiopian volcanic province: A new weathering index to characterize and compare soils
- Recommended mineral-melt partition coefficients for FRTEs (Cu), Ga, and Ge during mantle melting
- Tetrahedral plot diagram: A geometrical solution for quaternary systems
- Investigations on alunogen under Mars-relevant temperature conditions: An example for a single-crystal-to-single-crystal phase transition
- Crystallization of calcium oxalate hydrates by interaction of calcite marble with fungus Aspergillus niger
- Direct and indirect evidence for free oxygen (O2–) in MO-silicate glasses and melts (M = Mg, Ca, Pb)
- Effect of fluid composition on growth rate of monazite in quartzite at 1.0 GPa and 1000 °C
- Determination of the full elastic tensor of single crystals using shear wave velocities by Brillouin spectroscopy
- Temperature dependence of the velocity-density relation for liquid metals under high pressure: Implications for the Earth’s outer core
- Thermal, compositional, and compressional demagnetization of cementite
- The MnCO3-II high-pressure polymorph of rhodocrosite
- Lanthanide tetrads in normalized rare element patterns of zircon from the Koktokay No. 3 granitic pegmatite, Altay, NW China
- Hydrogrossular, Ca3Al2(SiO4)3–x(H4O4)x: An ab initio investigation of its structural and energetic properties
- High-pressure synthesis of skiagite-majorite garnet and investigation of its crystal structure
- Mineralogical evolution of Fe–Si-rich layers at the olivine-water interface during carbonation reactions
- High-pressure spectroscopic study of siderite (FeCO3) with a focus on spin crossover
- Exploring the potential of Raman spectroscopy for crystallochemical analyses of complex hydrous silicates: I. Amphiboles
- Apexite, NaMg(PO4)·9H2O, a new struvite-type phase with a heteropolyhedral cluster
- The mechanism of infiltration of metamorphic fluids recorded by hydration and carbonation of epidote-amphibolite facies metabasaltic sills in the SW Scottish Highlands
- The axial ratio of hcp Fe and Fe–Ni–Si alloys to the conditions of Earth’s inner core
- Shock-induced mobilization of metal and sulfide in planetesimals: Evidence from the Buck Mountains 005 (L6 S4) dike-bearing chondrite
- The accretion and differentiation of Earth under oxidizing conditions
- Dislocation microstructures in simple-shear-deformed wadsleyite at transition-zone conditions: Weak-beam dark-field TEM characterization of dislocations on the (010) plane
- Chemical composition and crystal structure of merrillite from the Suizhou meteorite