4.5 Article

Determination of high-pressure phase equilibria of Fe2O3 using the Kawai-type apparatus equipped with sintered diamond anvils

期刊

AMERICAN MINERALOGIST
卷 94, 期 2-3, 页码 205-209

出版社

MINERALOGICAL SOC AMER
DOI: 10.2138/am.2009.2913

关键词

High-pressure phase equilibria; Fe2O3; Kawai-cell; sintered diamond; in situ X-ray observation

向作者/读者索取更多资源

Phase equilibria of Fe2O3 have been studied tip to 58 GPa and 1400 K using the Kawai-type multi anvil apparatus equipped with sintered diamond anvils. Identification of phases and pressure determination has been carried out by means of in situ X-ray observation using synchrotron radiation at SPring-8. Hematite (phase I) successively transforms to the Rh2O3(II)-type structure (phase II) and then to an orthorhombic structure (phase III) with increasing pressure. The transformations of hematite into high-pressure phases have been observed only at temperatures higher than 500 K, which is not concordant with previous results obtained by using the diamond anvil cell. Volume changes accompanied by the I-II and II-III transformations are calculated to be 2.8 and -5.0%, respectively. The phase boundary between I and II phases and that between II and III have been proposed to be P (GPa)- 0.015 T(K) + 44.2 and P (GPa) = -0.005 T(K) + 48.7, respectively. Possible correlation between a Mott transition and the phase stabilities may be concealed at room temperature due to Slow reaction kinetics of the structural transformations.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Spectroscopy

High-pressure Raman study of Na-Ca burbankite-A possible CO2 host in deep mantle

Sergey Rashchenko, Anastasia Mikhno, Anton Shatskiy

Summary: This study characterizes the structure and stability of Na-Ca carbonates synthesized under high pressures, particularly in the mantle transition zone. The results demonstrate that Na-Ca burbankite remains structurally stable at pressures up to 24 GPa, suggesting its potential presence in the deep mantle.

JOURNAL OF RAMAN SPECTROSCOPY (2023)

Article Geochemistry & Geophysics

Dissolution mechanisms of water in depolymerized silicate (peridotitic) glasses based on infrared spectroscopy

Dmitry Bondar, Anthony C. Withers, Alan G. Whittington, Hongzhan Fei, Tomoo Katsura

Summary: The dissolution of water in melts and its impact on glass structure were studied using Fourier transform infrared spectroscopy. It was found that the proportion of water molecules in the glass decreases with increasing depolymerization. Additionally, a new peak related to a specific hydroxyl group was identified, and the position of another peak was found to shift with depolymerization. These findings provide insights into the dissolution mechanisms of water in highly depolymerized glasses and their effect on glass structure.

GEOCHIMICA ET COSMOCHIMICA ACTA (2023)

Article Geosciences, Multidisciplinary

Change in carbonate budget and composition during subduction below metal saturation boundary

Anton Shatskiy, Anton V. Arefiev, Konstantin D. Litasov

Summary: The study investigates the reaction kinetics and properties of mantle carbonates with iron metal, revealing the reduction, evolution, and preservation of carbonates in the mantle. This has significant implications for understanding diamond formation and mantle material cycling.

GEOSCIENCE FRONTIERS (2023)

Article Chemistry, Multidisciplinary

Ferric Iron Substitution Mechanism in Bridgmanite under SiO2-Saturated Conditions at 27 GPa

Artem Chanyshev, Hongzhan Fei, Dmitry Bondar, Biao Wang, Zhaodong Liu, Takayuki Ishii, Robert Farla, Catherine McCammon, Tomoo Katsura

Summary: The chemistry of bridgmanite is important for understanding the Earth's lower mantle. Fe3+ can substitute for Mg in bridgmanite, and this substitution affects its physical properties. We investigated the substitution mechanism of Fe3+ and found that only the charge-coupled mechanism takes place, leading to the formation of FeFeO3 component. The absence of vacancies in bridgmanite under SiO2-saturated conditions implies differences in viscosity and electrical conductivity compared to the surrounding mantle, which may affect lower-mantle dynamics.

ACS EARTH AND SPACE CHEMISTRY (2023)

Article Geochemistry & Geophysics

The NaCl-CaCO3 and NaCl-MgCO3 systems at 6 GPa: Link between saline and carbonatitic diamond forming melts

Anton Shatskiy, Ivan V. Podborodnikov, Anastasia S. Fedoraeva, Anton Arefiev, Altyna Bekhtenova, Konstantin D. Litasov

Summary: The phase relations in the NaCl-CaCO3 and NaCl-MgCO3 systems were experimentally studied using a multi-anvil press at 6 GPa and temperatures ranging from 1000 to 1600 degrees C. Both systems were found to have eutectic type phase diagrams, with subsolidus assemblages of halite + aragonite and halite + magnesite. The composition of the halite-aragonite eutectic was determined to be 40 wt% NaCl and 60 wt% CaCO3 at temperatures below 1200 degrees C, while the halite-magnesite eutectic had a composition of 72 wt% NaCl and 28 wt% MgCO3 at 1300 degrees C. Complete miscibility between carbonate and chloride liquids was observed up to 1600 degrees C.

AMERICAN MINERALOGIST (2023)

Article Geochemistry & Geophysics

Iron and aluminum substitution mechanism in the perovskite phase in the system MgSiO3-FeAlO3-MgO

Takayuki Ishii, Catherine McCammon, Tomoo Katsura

Summary: The chemical composition of Fe,Al-bearing MgSiO3 perovskite (bridgmanite) was studied at high temperatures, revealing a decrease in the FeAlO3 content and no change in the Fe2O3 content with increasing temperature. The presence of MgFeO2.5 and Fe2/3SiO3 as charge-coupled components was also observed.

AMERICAN MINERALOGIST (2023)

Article Geosciences, Multidisciplinary

Effect of Iron Content on Thermal Conductivity of Ferropericlase: Implications for Planetary Mantle Dynamics

Youyue Zhang, Takashi Yoshino, Masahiro Osako

Summary: We have measured thermal conductivity and thermal diffusivity for polycrystalline ferropericlase with different Fe contents under high pressure and high temperature conditions. The results show that even small amounts of Fe can significantly reduce the thermal conductivity of ferropericlase at low temperatures. There is a decrease in the pressure and temperature dependence with increasing Fe content. A universal equation was derived to estimate the thermal conductivity of ferropericlase under mantle conditions.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Geosciences, Multidisciplinary

Hadean mantle oxidation inferred from melting of peridotite under lower-mantle conditions

Hideharu Kuwahara, Ryoichi Nakada, Shintaro Kadoya, Takashi Yoshino, Tetsuo Irifune

Summary: The formation of the early Earth's mantle is believed to have been highly reducing, but geological evidence suggests it was oxidized. Experiments melting peridotite under deep mantle conditions show that the Fe3+ content of Earth's magma ocean was significantly higher than that of the present upper mantle, explaining the evidence for a highly oxidized Hadean mantle. This oxidation likely ended with the cessation of huge impacts, and the reduction in Fe3+ content and oxidation state of the upper mantle could be attributed to accretion of reduced materials by small impactors during the late Hadean and early Archaean eons.

NATURE GEOSCIENCE (2023)

Article Physics, Condensed Matter

Investigation of Solid-Solid Transition in Ti and Zr at High Pressure by Electrical Resistivity

Innocent C. Ezenwa, Takashi Yoshino

Summary: This study reports the changes in electrical resistivity of titanium (Ti) and zirconium (Zr) at room temperature under pressures up to 20 GPa using a 4-wire resistivity method. The resistivity slopes of both metals change at different pressures. At 10 GPa, the resistivity of Ti increases with pressure while the resistivity of Zr decreases. This difference is attributed to incoherent scattering in Ti and coherent scattering in Zr during their solid α->ω transition. Furthermore, the study allows constraining the boundaries of the α->ω phase coexistence region in Zr to be 4-8 GPa.

PHYSICA STATUS SOLIDI B-BASIC SOLID STATE PHYSICS (2023)

Article Geochemistry & Geophysics

The System KCl-CaCO3-MgCO3 at 3 GPa

Anton Shatskiy, Ivan V. V. Podborodnikov, Anton V. V. Arefiev, Konstantin D. D. Litasov

Summary: Inclusions in mantle minerals and xenoliths from kimberlites derived from deep depths showed great variations in composition. The stability range of these inclusions remains unclear. New experimental data on the KCl-CaCO3-MgCO3 system obtained at 3 GPa show the eutectic type of phase relations. The melting reactions of KCl-bearing carbonated eclogite at different pressures and depths are also identified.

MINERALS (2023)

Article Geochemistry & Geophysics

Rheology of Hexagonal Close-Packed (hcp) Iron

Yu Nishihara, Shunta Doi, Noriyoshi Tsujino, Daisuke Yamazaki, Kyoko N. Matsukage, Yumiko Tsubokawa, Takashi Yoshino, Andrew R. Thomson, Yuji Higo, Yoshinori Tange

Summary: The viscosity of hcp-Fe is critical for understanding the dynamics of the Earth's inner core. High-pressure and -temperature deformation experiments were conducted to study the rheology of hcp-Fe, revealing a power-law dislocation creep mechanism. The dominant deformation mechanism at high temperatures is power-law dislocation creep, while at lower temperatures, a mechanism with power-law breakdown prevails.

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH (2023)

Article Geosciences, Multidisciplinary

Some new insights about electrical discontinuities in the cratonic lithosphere

Baohua Zhang, Hongzhan Fei, Takashi Yoshino, Qunke Xia

Summary: The thermal structure of Craton plays a crucial role in its internal melting state, electrical conductivity and dynamic evolution. Enhanced conductivity in Craton with high surface heat flow can be explained by the presence of silicate or carbonate melt, while Craton with relatively low surface heat flow may be due to a small amount of carbonate melt or water in nominally anhydrous minerals (NAMs).

EARTH-SCIENCE REVIEWS (2023)

Article Multidisciplinary Sciences

Variation in bridgmanite grain size accounts for the mid-mantle viscosity jump

Hongzhan Fei, Maxim D. Ballmer, Ulrich Faul, Nicolas Walte, Weiwei Cao, Tomoo Katsura

Summary: A substantial viscosity difference is observed in the lower mantle of Earth at a depth of 800-1,200 km, known as the mid-mantle viscosity jump. This viscosity jump plays a crucial role in the dynamics and evolution of the mantle, affecting slab subduction, plume ascent, and chemical mixing. The origin of this viscosity jump has remained unknown, but this study suggests that rocks enriched with bridgmanite in the deep lower mantle have significantly larger grain size and higher viscosity compared to overlying pyrolitic rocks, providing an explanation for the mid-mantle viscosity jump.

NATURE (2023)

Article Multidisciplinary Sciences

Effect of water on seismic attenuation of the upper mantle: The origin of the sharp lithosphere-asthenosphere boundary

Chao Liu, Takashi Yoshino, Daisuke Yamazaki, Noriyoshi Tsujino, Hitoshi Gomi, Moe Sakurai, Youyue Zhang, Ran Wang, Longli Guan, Kayan Lau, Yoshinori Tange, Yuji Higo

Summary: This study investigates the effect of water on the seismic properties of olivine aggregates in the oceanic lithosphere. The results show that water substantially enhances energy dispersion and reduces elastic moduli, with an attenuation peak at higher frequencies. The findings suggest that the sharp seismic changes at the lithosphere-asthenosphere boundary far from mid-ocean ridges could be attributed to the difference in water content between the lithosphere and asthenosphere.

PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2023)

Article Chemistry, Multidisciplinary

Ferric Iron Substitution Mechanism in Bridgmanite under SiO2-Saturated Conditions at 27 GPa

Artem Chanyshev, Hongzhan Fei, Dmitry Bondar, Biao Wang, Zhaodong Liu, Takayuki Ishii, Robert Farla, Catherine McCammon, Tomoo Katsura

Summary: The substitution mechanisms of Fe3+ in bridgmanite and its impact on physical properties were investigated under specific high pressure and temperature conditions. The study found that the fraction of Fe3+ increases with temperature, and the substitution mechanism only takes place under specific conditions. Additionally, the absence of vacancies in bridgmanite under specific conditions has important implications for lower-mantle dynamics.

ACS EARTH AND SPACE CHEMISTRY (2023)

暂无数据