Pressure dependence of u parameter in ringwoodite up to 7.9 GPa
スポンサーリンク
概要
- 論文の詳細を見る
X-ray diffraction intensities were measured for single-crystal, spinel structure ringwoodite (γ-Mg1.97SiH0.03O4) at pressures up to 7.9 GPa in the BL-10A synchrotron beam line of the Photon Factory. The isothermal bulk modulus calculated using the Birch-Murnaghan equation of state assuming KT' = 4 was KT = 184(6) GPa. The difference between this result and the value for anhydrous ringwoodite is not significant within the limit of experimental error due to a minimal H2O content. The oxygen positional parameter u was revealed to increase significantly with pressure, approaching the ideal value of 1/4 for cubic closest packing. The mean Si-O distance remained almost constant up to 7.9 GPa, with compression of the unit cell occurring in proportion to that of the MO6 octahedron.
- 日本鉱物科学会の論文
著者
-
Tanaka Masahiko
Institute Of Materials Structure Science High Energy Accelerator Research Organization
-
Ohtani Eiji
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
-
Kudoh Yasuhiro
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
-
Mizobata Hiroki
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
-
Kuribayashi Takahiro
Institute Of Mineralogy Petrology And Economic Geology Faculty Of Science Tohoku University
-
Sasaki Satoshi
Materials and Structure Laboratory, Tokyo Institute of Technology, Nagatsuta 4259, Midori, Yokohama 226-8503, Japan
-
TANAKA Masahiko
Institute of Materials Structure Science, High Energy Accelerator Reasearch Organization
関連論文
- Observation of Soft Phonon Modes in 1T-TaS_2 by means of X-ray Thermal Diffuse Scattering(Condensed Matter : Structure, Mechanical and Thermal Properties)
- Site-Specific Studies on X-Ray Magnetic Circular Dichroism at Fe K Edge for Transition-Metal Ferrites
- X-Ray Diffuse Scattering Study of Magnetite by the Valence-Difference Contrast Method
- X-ray diffraction study of high pressure transition in InOOH
- X-Ray Magnetic Circular Dichroism and Structural Model for Co-Doped TiO_2 (Anatase) Thin Film (Condensed Matter : Structure, Mechanical and Thermal Properties)
- Determination of the Stokes-Poincare Parameters for a Synchrotron X-Ray Beam by Multiple Bragg Scattering
- Pressure dependence of u parameter in ringwoodite up to 7.9GPa
- High-pressure single crystal X-ray diffraction and FT-IR observation of natural chondrodite and synthetic OH-chondrodite
- Cation vacancies and possible hydrogen atom positions in Fe-bearing hydrous forsterite, Mg_Fe_Si_H_O_4, synthesized at 13.5GPa and 1400℃
- Cation vacancy and possible hydrogen positions in hydrous forsterite, Mg_Si_H_O_4, synthesized at 13.5GPa and 1300℃
- Orientational ordering of three SiO_4 tetrahedra in α'_L-Ca_Sr_SiO_4 that satisfies bond-valence requirements and avoids O-O repulsion
- The partially dehydrated structure of natural heulandite : An in situ high temperature single crystal X-ray diffraction study
- Compressibility of phase A, Mg_7Si_2H_6O_ up to 11.2 GPa
- Effect of temperature and pressure on the crystal structure of topaz, Al_2Sio_4(OH,F)_2
- Stability of dense hydrous magnesium silicate phase G in the transition zone and the lower mantle
- Crystal structural features of hydrous forsterite : Effect of Fe on the M-site vacancies, possible hydrogen positions and variation of the unit cell dimensions
- High-Temperature Thermoelectric Property of Layered La2-2xCa1+2xMn2O7 Manganites ($0.75 \leq x \leq 1.0$)
- Raman spectroscopic study of a garnetite xenolith from Malaita, Southwest Pacific
- Application of FIB system to ultra-high-pressure Earth science
- Local structure of Zn in Cretaceous-Tertiary boundary clay from Stevns Klint
- Calculation of X-ray Magnetic Circular Dichroism for Sr-Substituted LaCoO3 by Discrete-Variational Hartree–Fock–Slater Method
- Determination of Cation Distribution in Mn–Zn–Fe Ferrite by X-Ray Anomalous Scattering
- Compositional Dependence of X-Ray Absorption Spectra on Magnetic Circular Dichroism and Near-Edge Structure at Co $K$ Edge in La1-xSrxCoO3 ($0\leq x\leq 0.6$)
- Observation of Soft Phonon Modes in 1T-TaS_2 by means of X-ray Thermal Diffuse Scattering(Condensed Matter : Structure, Mechanical and Thermal Properties)
- Local structure of Zn in Cretaceous-Tertiary boundary clay from Stevns Klint
- Pressure dependence of u parameter in ringwoodite up to 7.9 GPa
- Flotation of Olivine in the Peridotite Melt at High Pressure.
- Origin of Cratonic Peridotite and Komatiite: Evidence for Melting in the Wet Archean Mantle.:Evidence for Melting in the Wet Archean Mantle