13 results on '"Kantor I"'
Search Results
2. Electronic state of Fe2+ in (Mg,Fe)(Si,Al)O3 perovskite and (Mg,Fe)SiO3 majorite at pressures up to 81 GPa and temperatures up to 800 K
- Author
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Narygina, Olga V., Kantor, I. Yu., McCammon, C. A., and Dubrovinsky, L. S.
- Published
- 2010
- Full Text
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3. Local structure and spin transition in Fe2O3 hematite at high pressure
- Author
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Sanson A, Kantor I, Cerantola V, Irifune T, Carnera A, Pascarelli S, Sanson, A, Kantor, I, Cerantola, V, Irifune, T, Carnera, A, and Pascarelli, S
- Subjects
EXAFS ,high pressure ,diamond anvil cell ,XAS ,structural transition ,spin transition ,hematite - Abstract
The pressure evolution of the local structure of Fe2O3 hematite has been determined by extended x-ray absorption fine structure up to ∼79 GPa. Below the phase-transition pressure at ∼50 GPa, no increasing of FeO6 octahedra distortion is observed as pressure is applied. Above the phase transition, an abrupt decrease of the nearest-neighbor Fe-O distance is observed concomitantly with a strong reduction in the FeO6 distortion. This information on the local structure, used as a test-bench for the different high-pressure forms proposed in the literature, suggests that the orthorhombic structure with space group Aba2, recently proposed by Bykova [Nat. Commun. 7, 10661 (2016)2041-172310.1038/ncomms10661], is the most probable, but puts into question the presence of the P21/n form in the pressure range 54-67 GPa. Finally, the crossover from Fe high-spin to low-spin states with pressure increase has been monitored from the pre-edge region of the Fe K-edge absorption spectra. Its "simultaneous" comparison with the local structural changes allows us to conclude that it is the electronic transition that drives the structural transition and not vice versa.
- Published
- 2016
4. High pressure atomic structure of Zr–Cu metallic glass via EXAFS spectroscopy and molecular dynamics simulations.
- Author
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Dziegielewski, P., Mathon, O., Kantor, I., Pascarelli, S., Shinmei, T., Irifune, T., and Antonowicz, J.
- Subjects
METALLIC glasses ,EXTENDED X-ray absorption fine structure ,MOLECULAR spectroscopy ,ATOMIC structure ,MOLECULAR dynamics ,AMORPHOUS alloys ,HYDROSTATIC pressure - Abstract
In this work, we use extended X-ray absorption fine structure (EXAFS) data collected using nano-polycrystalline diamond anvil cell to study the atomic arrangement in Zr–Cu metallic glass in high pressure (HP) conditions. To reveal the microscopic details of stress accommodation mechanism, we performed molecular dynamics (MD) simulations of the HP atomic arrangement. By comparing the experimental and the calculated Zr and Cu K-edge EXAFS signal we prove the realistic character of the computer simulations. A detailed geometrical analysis of the simulated atomic configurations shows that with increasing hydrostatic pressure the local structure of Zr–Cu amorphous alloy becomes gradually dominated by Cu-centred icosahedral structural motifs involving fivefold symmetry incompatible with crystalline ordering. The variation of the short-range order is attributed to preferential straining of mechanically soft bonds between zirconium atoms. [ABSTRACT FROM AUTHOR]
- Published
- 2020
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5. Local structure investigation of β-Ni(OH) 2 under pressure using combined Raman and Ni K-edge extended x-ray absorption fine structure studies.
- Author
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Marini, C., Joseph, B., Caramazza, S., Capitani, F., Bendele, M., Kantor, I., Lotti, P., Mathon, O., Pascarelli, S., and Postorino, P.
- Subjects
NICKEL compounds ,CHEMICAL structure ,X-ray absorption ,FINE structure (Physics) ,RAMAN spectroscopy ,HIGH pressure (Technology) ,HYDROGEN bonding - Abstract
We present a combined high pressure Ni K-edge x-ray absorption and Raman spectroscopic investigation of β-Ni(OH). Extended x-ray absorption fine structure analysis reveals a progressive shrinking of the Ni–O and Ni–Ni bond distances with pressure. As pressure is increased, Raman data show a continuous hardening of the phonon modes associated with the vibration of Ni–O sublattice, whereas a systematic frequency softening is displayed by the hydroxyl (O–H) symmetric stretching mode. This contrasting behavior implies a gradual development of a lattice instability with pressure in nickel hydroxide. Under pressure hydrogen bonds become increasingly unstable mainly due to the displacement of H atoms around the Ni–O axis inducing a local-lattice instability may explain the structural, Raman and x-ray absorption results. [ABSTRACT FROM AUTHOR]
- Published
- 2017
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6. High pressure dynamic XAS studies using an energy-dispersive spectrometer.
- Author
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Mathon, O., Occelli, F., Lescoute, E., Sollier, A., Loubeyre, P., Helsby, W., Headspith, J., Torchio, R., Kantor, I., and Pascarelli, S.
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HIGH pressure (Science) ,ENERGY dispersive X-ray spectroscopy ,SYNCHROTRONS ,CHEMICAL stability ,CHEMICAL reactions ,X-ray absorption spectra - Abstract
We present in this paper recent advances in the high pressure domain provided by the introduction of time-resolved energy-dispersive XAS (EDXAS) techniques at synchrotrons. We highlight technical aspects and describe two modes of acquisition: the ‘movie’ mode, where the time resolution is given by the detector acquisition speed and the ‘pump-and-probe’ mode, where the time resolution is given by the delay between the pump and the probe. These two modes define a frontier in the time resolution, respectively above and below the ∼10 μs regime. In the former, examples of applications are chemical stability and reactions at high pressure and high temperature or probing the warm dense matter regime using rapid current ramps. In the latter, an example is given on studies of dynamically compressed matter, by coupling single-bunch EDXAS at high-brilliance synchrotron to a nanosecond high-power laser. [ABSTRACT FROM PUBLISHER]
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- 2016
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7. On-line laser heating setup for ED-XAS at ID24: preliminary optical design and test results.
- Author
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Marini, C., Kantor, I., Mathon, O., and Pascarelli, S.
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LASER heating , *DIAMOND anvil cell , *SYNCHROTRON radiation , *HIGH temperatures , *HIGH pressure (Science) , *IRON compounds - Abstract
Double-sided laser heating (LH) combined with synchrotron X-ray radiation forin situstudies in the diamond anvil cell (DAC) has been the most productive and widely used high-temperature–high pressure technique in the past two decades. In the framework of the UPBL11 project (upgrade of ID24 beamline of European Synchrotron Radiation Facility), we developed a new on-line LH system for DACs. The preliminary optical scheme of the system is presented and discussed. Varying the settings, we are able to shape and to size the beam on the surface of the sample in the DAC. First pilot applications to the Fe case are shown. [ABSTRACT FROM AUTHOR]
- Published
- 2013
- Full Text
- View/download PDF
8. Electronic state of Fe2+ in (Mg,Fe)(Si,Al)O3 perovskite and (Mg,Fe)SiO3 majorite at pressures up to 81 GPa and temperatures up to 800 K.
- Author
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Narygina, Olga V., Kantor, I. Yu., McCammon, C. A., and Dubrovinsky, L. S.
- Subjects
PEROVSKITE ,OXIDE minerals ,MOSSBAUER spectroscopy ,SPECTRUM analysis ,GARNET - Abstract
Despite a large number of studies of iron spin state in silicate perovskite at high pressure and high temperature, there is still disagreement regarding the type and P– T conditions of the transition, and whether Fe
2+ or Fe3+ or both iron cations are involved. Recently, our group published results of a Mössbauer spectroscopy study of the iron behaviour in (Mg,Fe)(Si,Al)O3 perovskite at pressures up to 110 GPa (McCammon et al. ), where we suggested stabilization of the intermediate spin state for 8- to 12-fold coordinated ferrous iron ([8–12] Fe2+ ) in silicate perovskite above 30 GPa. In order to explore the behaviour in related systems, we performed a comparative Mössbauer spectroscopic study of silicate perovskite (Fe0.12 Mg0.88 SiO3 ) and majorite (with two compositions—Fe0.18 Mg0.82 SiO3 and Fe0.11 Mg0.88 SiO3 ) at pressures up to 81 GPa in the temperature range 296–800 K, which was mainly motivated by the fact that the oxygen environment of ferrous iron in majorite is quite similar to that in silicate perovskite. The[8–12] Fe2+ component, dominating the Mössbauer spectra of majorites, shows high quadrupole splitting (QS) values, about 3.6 mm s−1 , in the entire studied P– T region (pressures to 58 GPa and 296–800 K). Decrease of the QS of this component with temperature at constant pressure can be described by the Huggins model with the energy splitting between low-energy eg levels of[8–12] Fe2+ equal to 1,500 (50) cm−1 for Fe0.18 Mg0.82 SiO3 and to 1,680 (70) cm−1 for Fe0.11 Mg0.88 SiO3 . In contrast, for the silicate perovskite dominating Mössbauer component associated with[8–12] Fe2+ suggests the gradual change of the electronic properties. Namely, an additional spectral component with central shift close to that for high-spin[8–12] Fe2+ and QS about 3.7 mm s−1 appeared at ~35 (2) GPa, and the amount of the component increases with both pressure and temperature. The temperature dependence of QS of the component cannot be described in the framework of the Huggins model. Observed differences in the high-pressure high-temperature behaviour of[8–12] Fe2+ in the silicate perovskite and majorite phases provide additional arguments in favour of the gradual high-spin—intermediate-spin crossover in lower mantle perovskite, previously reported by McCammon et al. () and Lin et al. (). [ABSTRACT FROM AUTHOR]- Published
- 2010
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9. Pressure-induced transformations in Ce-Al metallic glasses: The role of stiffness of interatomic pairs.
- Author
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Dziegielewski, P., Antonowicz, J., Pietnoczka, A., Mathon, O., Pascarelli, S., Kantor, I., Shinmei, T., and Irifune, T.
- Subjects
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METALLIC glasses , *STIFFNESS (Mechanics) , *ATOMIC structure , *POLYMORPHISM (Crystallography) , *HIGH pressure (Science) - Abstract
When high pressure is applied to Ce-Al metallic glasses, their disordered atomic structure exhibits some unusual properties like polyamorphism or transformation into a crystalline phase. In this work, we probe the atomic arrangement of Ce 55 Al 45 and Ce 75 Al 25 glasses by X-ray absorption spectroscopy and X-ray diffraction in the pressure range of 0–30 GPa. The pressure-dependent parameters of local environment of cerium atoms are evaluated by extended X-ray absorption fine structure (EXAFS) fitting. We demonstrate that due to compositional dependence of stiffness of Ce-Al pairs, densification of Ce 55 Al 45 is accompanied by an increase of atomic size mismatch between Ce and Al stabilizing the amorphous phase, while a decrease of the mismatch is observed in Ce 75 Al 25 alloy which eventually leads to its devitrification at 25 GPa. [ABSTRACT FROM AUTHOR]
- Published
- 2018
- Full Text
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10. Pressure tuning of charge ordering in iron oxide
- Author
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Alexander Kurnosov, Konstantin Glazyrin, Catherine McCammon, Aleksandr I. Chumakov, Rudolf Rüffer, Rudra Sekhar Manna, Leonid Dubrovinsky, Alexander A. Tsirlin, Ilya Kupenko, Innokenty Kantor, Sergey V. Ovsyannikov, Elena Bykova, Irina Chuvashova, Valerio Cerantola, Maxim Bykov, Anna S. Pakhomova, Bayerisches Geoinstitut (BGI), Universität Bayreuth, Deutsches Elektronen-Synchrotron [Hamburg] (DESY), Center for Electronic Correlations and Magnetism, Universität Augsburg [Augsburg], European Synchrotron Radiation Facility (ESRF), Ovsyannikov, S, Bykov, M, Bykova, E, Glazyrin, K, Manna, R, Tsirlin, A, Cerantola, V, Kupenko, I, Kurnosov, A, Kantor, I, Pakhomova, A, Chuvashova, I, Chumakov, A, Ruffer, R, Mccammon, C, and Dubrovinsky, L
- Subjects
Materials science ,iron oxides ,XRD ,PEROVSKITE ,Science ,[SDV]Life Sciences [q-bio] ,Iron oxide ,General Physics and Astronomy ,LOWER-MANTLE ,02 engineering and technology ,Crystal structure ,low temperature ,01 natural sciences ,Article ,General Biochemistry, Genetics and Molecular Biology ,Condensed Matter::Materials Science ,chemistry.chemical_compound ,Charge ordering ,Oxidation state ,0103 physical sciences ,Pentoxide ,ddc:530 ,Redistribution (chemistry) ,CRYSTAL-STRUCTURE ,FE4O5 ,lcsh:Science ,010306 general physics ,STRUCTURAL BEHAVIOR ,MAGNETITE FE3O4 ,Magnetite ,Multidisciplinary ,VERWEY TRANSITION ,Mössbauer spectroscopy ,General Chemistry ,021001 nanoscience & nanotechnology ,SINGLE-CRYSTAL ,COMPRESSIBILITY ,high pressure ,Crystallography ,diamond anvil cell ,chemistry ,BEAMLINE ,lcsh:Q ,ddc:500 ,0210 nano-technology ,Single crystal - Abstract
Nature Communications 9(1), 4142 (2018). doi:10.1038/s41467-018-06457-x, A Verwey-type charge-ordering transition in magnetite at 120 K leads to the formation of linear units of three iron ions with one shared electron, called trimerons. The recently-discovered iron pentoxide (Fe$_4$O$_5$) comprising mixed-valent iron cations at octahedral chains, demonstrates another unusual charge-ordering transition at 150 K involving competing formation of iron trimerons and dimerons. Here, we experimentally show that applied pressure can tune the charge-ordering pattern in Fe$_4$O$_5$ and strongly affect the ordering temperature. We report two charge-ordered phases, the first of which may comprise both dimeron and trimeron units, whereas, the second exhibits an overall dimerization involving both the octahedral and trigonal-prismatic chains of iron in the crystal structure. We link the dramatic change in the charge-ordering pattern in the second phase to redistribution of electrons between the octahedral and prismatic iron chains, and propose that the average oxidation state of the iron cations can pre-determine a charge-ordering pattern., Published by Nature Publishing Group UK, [London]
- Published
- 2018
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- View/download PDF
11. Pressure-mediated structural transitions in bulk EuTiO 3
- Author
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Dimitrios Bessas, D. S. Ellis, V. Potapkin, Konstantin Glazyrin, S. van Smaalen, Innokenty Kantor, Dániel G. Merkel, Raphaël P. Hermann, Alfred Q. R. Baron, Valerio Cerantola, Bessas, D, Glazyrin, K, Ellis, D, Kantor, I, Merkel, D, Cerantola, V, Potapkin, V, van Smaalen, S, Baron, A, and Hermann, R
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Materials science ,XRD ,02 engineering and technology ,021001 nanoscience & nanotechnology ,01 natural sciences ,Nuclear forward scattering ,high pressure ,diamond anvil cell ,Condensed Matter::Superconductivity ,synchrotron ,0103 physical sciences ,ddc:530 ,010306 general physics ,0210 nano-technology - Abstract
The high pressure structural phase diagram of EuTiO3 is revisited by means of single crystal x-ray diffraction at pressures below 30GPa. We report a transition at about 3GPa with a surprisingly small lattice distortion. At 23GPa we have detected a yet unknown transition into a new orthorhombic phase (space group Ibam). Combining our observations on structures obtained on single crystals and polycrystalline samples with complementary methods, such as electrical resistivity and nuclear forward scattering of synchrotron radiation measured on polycrystalline samples, we address issues relevant to chemistry and disorder.
- Published
- 2018
- Full Text
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12. High-pressure synthesis and properties of iron oxides
- Author
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Irina Chuvashova, Anna S. Pakhomova, Valerio Cerantola, Rudra Sekhar Manna, Sergey V. Ovsyannikov, Leonid Dubrovinsky, Konstantin Glazyrin, Catherine McCammon, Elena Bykova, Alexander Kurnosov, Aleksandr I. Chumakov, Rudolf Rüffer, Alexander A. Tsirlin, Ilya Kupenko, Innokenty Kantor, Maxim Bykov, Ovsyannikov, S, Bykov, M, Bykova, E, Glazyrin, K, Manna, R, Tsirlin, A, Cerantola, V, Kupenko, I, Kurnosov, A, Kantor, I, Pakhomova, A, Chuvashova, I, Chumakov, A, Ruffer, R, Mccammon, C, and Dubrovinsky, L
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iron oxide ,Materials science ,XRD ,Condensed Matter Physics ,Biochemistry ,high temperature ,Inorganic Chemistry ,high pressure ,diamond anvil cell ,Chemical engineering ,Structural Biology ,High pressure ,Mössbauer ,General Materials Science ,synthesi ,Physical and Theoretical Chemistry ,crystallography - Published
- 2019
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13. Stability of iron-bearing carbonates in the deep Earth's interior
- Author
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Volodymyr Svitlyk, Jeroen Jacobs, Sylvain Petitgirard, Michael Hanfland, Clemens Prescher, Catherine McCammon, Mohamed Mezouar, Marco Merlini, Leonid Dubrovinsky, Maxim Bykov, Valerio Cerantola, Ilya Kupenko, Innokenty Kantor, Elena Bykova, A. I. Chumakov, Leyla Ismailova, Rudolf Rüffer, Vitali B. Prakapenka, Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany, European Synchrotron Radiation Facility (ESRF), DESY, Extreme Condit Beamline P02 2, Notkestr 85, D-22607 Hamburg, Germany, Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany, Univ Milan, Dipartimento Sci Terra, Via Botticelli 23, I-20133 Milan, Italy, Skolkovo Innovat Ctr, Skolkovo Inst Sci & Technol, Ctr Hydrocarbon Recovery, Moscow 143026, Russia, Natl Univ Sci & Technol MSIS, Mat Modeling & Dev Lab, Moscow 119049, Russia, MAX IV Lab, Fotongatan 2, S-22594 Lund, Sweden, Univ Cologne, Inst Geol & Mineral, Greinstr 4-6, D-50939 Cologne, Germany, University of Chicago, Cerantola, V, Bykova, E, Kupenko, I, Merlini, M, Ismailova, L, Mccammon, C, Bykov, M, Chumakov, A, Petitgirard, S, Kantor, I, Svitlyk, V, Jacobs, J, Hanfland, M, Mezouar, M, Prescher, C, Ruffer, R, Prakapenka, V, and Dubrovinsky, L
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Materials science ,010504 meteorology & atmospheric sciences ,XRD ,Science ,General Physics and Astronomy ,Mineralogy ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,reaction ,Crystal structure ,engineering.material ,010502 geochemistry & geophysics ,01 natural sciences ,General Biochemistry, Genetics and Molecular Biology ,Diamond anvil cell ,Mantle (geology) ,Article ,high temperature ,Mössbauer spectroscopy ,synchrotron ,14. Life underwater ,Geothermal gradient ,0105 earth and related environmental sciences ,Multidisciplinary ,Iron carbonate ,siderite ,Diamond ,General Chemistry ,laser heating ,phase diagram ,high pressure ,diamond anvil cell ,13. Climate action ,phase transition ,redox ,engineering ,ddc:500 ,tetracarbonate - Abstract
The presence of carbonates in inclusions in diamonds coming from depths exceeding 670 km are obvious evidence that carbonates exist in the Earth’s lower mantle. However, their range of stability, crystal structures and the thermodynamic conditions of the decarbonation processes remain poorly constrained. Here we investigate the behaviour of pure iron carbonate at pressures over 100 GPa and temperatures over 2,500 K using single-crystal X-ray diffraction and Mössbauer spectroscopy in laser-heated diamond anvil cells. On heating to temperatures of the Earth’s geotherm at pressures to ∼50 GPa FeCO3 partially dissociates to form various iron oxides. At higher pressures FeCO3 forms two new structures—tetrairon(III) orthocarbonate Fe43+C3O12, and diiron(II) diiron(III) tetracarbonate Fe22+Fe23+C4O13, both phases containing CO4 tetrahedra. Fe4C4O13 is stable at conditions along the entire geotherm to depths of at least 2,500 km, thus demonstrating that self-oxidation-reduction reactions can preserve carbonates in the Earth’s lower mantle., Carbonates are shown to exist in the lower mantle as seen in diamond inclusions, but thermodynamic constraints are poorly understood. Here, the authors synthesise two new iron carbonate compounds and find that self-oxidation-reduction reactions can preserve carbonates in the mantle.
- Published
- 2017
- Full Text
- View/download PDF
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