X-ray diffraction study of high pressure transition in InOOH

スポンサーリンク

概要

• 論文の詳細を見る

• We performed high-pressure and high-temperature X-ray diffraction experiments on InOOH using laser heated diamond anvil cells. After heating at 1300 K, pyrite-type InOOH was formed at 14 GPa and it was stable up to at least 30 GPa. Pyrite-type InOOH partially transformed back to distorted rutile-type InOOH after recovery. The lattice constant and unit-cell volume of pyrite-type InOOH were determined to be a0 = 5.3151(8) Å and V0 = 150.15 (7) Å3 at ambient conditions, respectively. The density difference between pyrite-type and distorted rutile-type InOOH was 5% at ambient condition.

• 日本鉱物科学会の論文
• 2008-04-01

著者

• YAGI Takehiko

  Institute for Solid State Physics, University of Tokyo

• Yagi Takehiko

  Institute For Solid State Physics The University Of Tokyo

• Gotou Hirotada

  Institute For Solid State Physics The University Of Tokyo

• SANO Asami

  Institute for Solid State Physics, The University of Tokyo

• OKADA Taku

  Institute for Solid State Physics, The University of Tokyo

• OHTANI Eiji

  Institute of Mineralogy, Petrology, and Economic Geology, Faculty of Science, Tohoku University

• TSUCHIYA Jun

  Geodynamic Research Center, Ehime University

• KIKEGAWA Takumi

  Photon Factory, High Energy Accelerator Research Organization

• Tsuchiya Jun

  Geodynamics Research Center Ehime University

• Okada Taku

  Institute For Solid State Physics The University Of Tokyo

• Sano Asami

  Institute For Solid State Physics University Of Tokyo

• Ohtani Eiji

  Inst. Of Mineralogy Petrology And Economic Geology Graduate School Of Sci. Tohoku Univ.

• Ohtani Eiji

  Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University

• Kikegawa Takumi

  Photon Factory High Energy Accelerator Res. Organization

関連論文

• Superconducting Properties of Pr-Based Filled Skutterudite PrRu_4As_(Condensed matter: electronic structure and electrical, magnetic, and optical properties)
• First principles prediction of new high-pressure phase of InOOH
• New Polymorph of SiO_2 Formed under Quasi-Hydrostatic Compression of Cristobalite
• Microscopic Brillouin Scatterirng Study in TeO_2 : Pressure Dependence of Acoustic Modes
• X-ray diffraction study of high pressure transition in InOOH
• High-Pressure Phase Transformation of Cobalt Monoxide Due to Electronic Transition
• Type-I-Type-II Transition in GaAs/AlAs Short Period Superlattices Studied under Pulsed High Magnetic Fields and High Pressures
• Analysis of Powder X-ray Diffraction Data Obtained under Uniaxial Stress Field
• Pressure Effect on Optical Absorption Coefficients for Amorphous Silicon-Germanium Alloys
• Highly Coplanar Polythiophenes with -C≡CR Side Chains : Self-Assembly, Linear and Nonlinear Optical Properties, and Piezochromism
• Pressure dependence of u parameter in ringwoodite up to 7.9GPa
• Brillouin Scattering Study of Pressure-Induced Phase Transition in MnF_2
• Cation vacancies and possible hydrogen atom positions in Fe-bearing hydrous forsterite, Mg_Fe_Si_H_O_4, synthesized at 13.5GPa and 1400℃
• Time-resolved X-ray diffraction analysis of the experimental dehydration of serpentine at high pressure
• Stability of dense hydrous magnesium silicate phase G in the transition zone and the lower mantle
• Raman spectroscopic study of a garnetite xenolith from Malaita, Southwest Pacific
• Application of FIB system to ultra-high-pressure Earth science
• Pressure-Induced Rhombohedral-Simple Cubic Structural Phase Transition in As
• New Stishovite-like Phase of Silica formed by Hydrostatic Compression of Cristobalite
• Pressure-induced phase changes of argon hydrate and methane hydrate at room temperature
• Compressibility of Mg0.9Al0.2Si0.9O3 perovskite
• In situ X-ray Observation of Iron Hydride under High Pressure and High Temperature
• Magnetic Properties of New Filled Skutterudite Compounds Eu$T_{4}$As12 ($T=\text{Fe}$, Ru, and Os) Synthesized under High Pressure
• Space Efficient Opposed-Anvil High-Pressure Cell and Its Application to Optical and NMR Measurements up to 9 GPa
• Synthesis, Structure, and Electromagnetic Properties of Manganese Hollandite, KxMnO
• Pressure dependence of u parameter in ringwoodite up to 7.9 GPa
• Flotation of Olivine in the Peridotite Melt at High Pressure.
• Stability of Magnesite under the Lower Mantle Conditions.
• Pressure Effect on the Structure and Superconducting Transition Temperature of Filled Skutterudites LaT_{4}P
• Formation of Hexagonal Diamond by Room Temperature Compression of Graphite.
• Pressure Effect on the Structure and Superconducting Transition Temperature of Filled Skutterudites LaT₄P₁₂ (T=Fe, Ru)
• Isothermal compression and stability of perovskite-type CaSiO3.
• Origin of Cratonic Peridotite and Komatiite: Evidence for Melting in the Wet Archean Mantle.:Evidence for Melting in the Wet Archean Mantle
• Pressure Effect on Mn, Co and Ni Partitioning between Iron Hydride and Mantle Minerals.

もっと見る 閉じる

スポンサーリンク