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21.
The mineralogy adopted by a depleted harzburgite composition has been studied over the pressure interval 5–26 GPa at temperatures of 1300–1400°C. The pyroxene-garnet component of the harzburgite composition (harzburgite minus 82 wt.% olivine) transforms to majorite garnet by 18–19 GPa, and further disproportionates to the assemblage of garnet + stishovite + Mg2SiO4 spinel above 20 GPa. At still higher pressures, first ilmenite (22–24 GPa) and then perovskite MgSiO3 (24–26 GPa) are found to coexist with garnet. Garnet disappears at 26 GPa and almost complete transition to perovskite is achieved at this pressure. The mineral proportions and density profiles in the subducting oceanic lithosphere, modelled by a combination of 80% harzburgite + 20% primitive MORB compositions are calculated as a function of depth under conditions isothermal with surrounding pyrolite mantle, and also for a temperature distribution in which the slab is substantially cooler than surrounding mantle to below 700 km. Under isothermal conditions, the slab has a density similar to surrounding mantle to a depth of 600 km. However, between 600 and 700 km, the slab is up to 0.08 g/cm3 denser than surrounding mantle. This is caused primarily by the higher alumina content in pyrolite as compared to harzburgite, which causes the transition to perovskite in pyrolite to occur at substantially higher pressures than in harzburgite. The presence of alumina also smears out the garnet-perovskite transition in pyrolite over a depth interval of 50 km, whereas this transformation is much sharper in the harzburgite composition. Calculations based on the observed phase equilibria also show that a subducted cool slab remains much denser (by 0.1–0.3 g/cm3) than surrounding mantle to a depth of 700 km but possesses a density similar to surrounding mantle below this depth. These results have important implications for the dynamical behaviour of slabs possessing different thermal regimes when they encounter the 670 km discontinuity and also for the nature of this discontinuity. 相似文献
22.
23.
Shigeto Hirai Yohei Kojima Hiroaki Ohfuji Norimasa Nishiyama Tetsuo Irifune Stephan Klemme Geoffrey Bromiley J. Paul Attfield 《Physics and Chemistry of Minerals》2011,38(8):631-637
Raman spectroscopy and heat capacity measurements have been used to study the post-perovskite phase of CaIr0.5Pt0.5O3, recovered from synthesis at a pressure of 15 GPa. Laser heating CaIr0.5Pt0.5O3 to 1,900 K at 60 GPa produces a new perovskite phase which is not recoverable and reverts to the post-perovskite polymorph
between 20 and 9 GPa on decompression. This implies that Pt-rich CaIr1−xPtxO3 perovskites including the end member CaPtO3 cannot easily be recovered to ambient pressure from high P–T synthesis. We estimate an increase in the thermodynamic Grüneisen
parameter across the post-perovskite to perovskite transition of 34%, of similar magnitude to those for (Mg,Fe)SiO3 and MgGeO3, suggesting that CaIr0.5Pt0.5O3 is a promising analogue for experimental studies of the competition in energetics between perovskite and post-perovskite
phases of magnesium silicates in Earth’s lowermost mantle. Low-temperature heat capacity measurements show that CaIrO3 has a significant Sommerfeld coefficient of 11.7 mJ/mol K2 and an entropy change of only 1.1% of Rln2 at the 108 K Curie transition, consistent with the near-itinerant electron magnetism. Heat capacity results for post-perovskite
CaIr0.5Rh0.5O3 are also reported. 相似文献
24.
Variations of Raman spectra of hydroxyl-clinohumite were studied up to ∼370 kbar at room temperature, and in the range 81–873 K
at atmospheric pressure. With the exception of the symmetric OH-stretch bands, the Raman frequencies of all bands were observed
to increase monotonically with increasing pressure, and decrease with increasing temperature. This behavior is in line with
those observed for other humite members (norbergite and chondrodite) so far studied. The symmetric OH-stretching band shows
a mode softening with increasing pressure, and splits into two bands at either high pressure or low temperature. In the quasihydrostatic
experiment, the compression and decompression paths of one of the asymmetric OH-stretch bands form a hysteresis loop, but
the same behavior was not observed in the nonhydrostatic experiment. These results indicate that the two kinds of OH groups
in hydroxyl-clinohumite have nonequivalent movement paths on compression, and with one OH group experiencing a release of
spatial hindrance during compression. This behavior appears to be modified by shear stress. The same complication of the OH
groups was not observed in the temperature variation study. The pressure and temperature variations of the Raman frequencies
for the various vibrations involving the SiO4 tetrahedra and MgO6 octahedra below ∼1000 cm−1 for clinohumite behave similarly to other hydrous magnesium silicates. On the basis of the relationship between isothermal
bulk modulus and Raman data, it is suggested that the linear pressure dependences of vibrational frequencies of various Raman
bands reported in the literature are inadequate.
Received: 20 March 1999 / Revised, accepted: 24 August 1999 相似文献
25.
Fe-Mg interdiffusivities in (Fe,Mg)O magnesiowüstite have been measured in experiments conducted at pressures of 7-35 GPa and temperatures of 1573-1973 K using a Kawai-type high-pressure apparatus. The diffusion profiles were measured across the interface between MgO and (Fe0.5,Mg0.5)O samples by electron microprobe analysis, and the Fe-Mg interdiffusivities were determined as DFe-Mg=D0exp{−E*(1+PV*Mg/E*Mg)/RT}, where D0=4.1(+16.1−3.3)×10−7 m2/s, E*=(1−CMg)E*Fe+CMgE*Mg (activation energy for the concentration of Mg, where E*Fe=113(±74) kJ/mol and E*Mg=226(±32) kJ/mol), the activation volume V*Mg=1.8(±1.2)×10−6 m3/mol. By extrapolating these results to the P-T conditions of the core-mantle boundary, we conclude that the interdiffusivity of Fe-Mg in magnesiowüstite at the bottom of the lower mantle is at least one order of magnitude larger than that at the top of the lower mantle. 相似文献
26.
Variation of Raman spectra of both natural (F-bearing) and synthetic (F-free) chondrodite samples were studied up to 400 kbar
at room temperature. Ambient Raman frequencies for the synthetic sample are in general lower than those for the natural one.
This is correlated with a slight expansion of the volume of the synthetic sample due to substitution of OH for F. The frequencies
of all Raman bands for both samples increase monotonically with increasing pressure. The positive pressure dependences in
the O−H stretch frequencies for both F-free and F-bearing samples are contrary to those for other dense hydrous magnesium
silicates. A mechanism involving both the hydrogen-hydrogen repulsion and hydrogen bondings is proposed to explain the abnormal
behavior. The effects of substitution of F for OH on both the ambient and high-pressure Raman spectra of chondrodite are also
discussed.
Received: 19 February 1998 / Revised accepted: 26 June 1998 相似文献
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28.
Variations of Raman spectra of MgSiO3·10% Al2O3-perovskite were investigated up to about 270 kbar at room temperature and in the range 108–425 °K at atmospheric pressure. Like MgSiO3-perovskite, the Raman frequencies of MgSiO3·10% Al2O3-perovskite increase nonlinearly with increasing pressure and decrease linearly with increasing temperature within the experimental uncertainties and the range investigated. A comparison of these data with those of MgSiO3-perovskite suggests that MgSiO3·10% Al2O3-perovskite is slightly more compressible than MgSiO3-perovskite, and that the volume thermal expansion for MgSiO3·10% Al2O3-perovskite is also slightly greater than that for MgSiO3-perovskite. 相似文献
29.
Mina Yutani Takehiko Yagi Hitoshi Yusa Tetsuo Irifune 《Physics and Chemistry of Minerals》1997,24(5):340-344
In situ X-ray diffraction experiments of calcium ferrite-type MgAl2O4 have been carried out using a diamond anvil cell combined with synchrotron radiation and an imaging plate X-ray detector
under hydrostatic pressures up to 9 GPa. The observed unit-cell volumes at various pressures were fitted to the Birch-Murnaghan
equation of state, yielding a bulk modulus of K
T
0= 241(3) GPa when K′
T
0=4 is assumed. This relatively large bulk modulus of calcium ferrite-type MgAl2O4 is consistent with that expected from the systematic relation between bulk modulus and molar volume for the most compounds
possessing fcc oxygen packing.
Received March 5, 1996/Revised, accepted October 15, 1996 相似文献
30.
T. Inoue T. Irifune Y. Higo T. Sanehira Y. Sueda A. Yamada T. Shinmei D. Yamazaki J. Ando K. Funakoshi W. Utsumi 《Physics and Chemistry of Minerals》2006,33(2):106-114
The phase boundary between wadsleyite and ringwoodite in Mg2SiO4 has been determined in situ using a multi-anvil apparatus and synchrotron X-rays radiation at SPring-8. In spite of the similar X-ray diffraction profiles of these high-pressure phases with closely related structures, we were able to identify the occurrence of the mutual phase transformations based on the change in the difference profile by utilizing a newly introduced press-oscillation system. The boundary was located at ~18.9 GPa and 1,400°C when we used Shim’s gold pressure scale (Shim et al. in Earth Planet Sci Lett 203:729–739, 2002), which was slightly (~0.8 GPa) lower than the pressure as determined from the quench experiments of Katsura and Ito (J Geophys Res 94:15663–15670, 1989). Although it was difficult to constrain the Clapeyron slope based solely on the present data due to the kinetic problem, the phase boundary [P (GPa)=13.1+4.11×10−3×T (K)] calculated by a combination of a P–T position well constrained by the present experiment and the calorimetric data of Akaogi et al. (J Geophys Res 94:15671–15685, 1989) reasonably explains all the present data within the experimental error. When we used Anderson’s gold pressure scale (Anderson et al. in J Appl Phys 65:1535–1543, 1989), our phase boundary was located in ~18.1 GPa and 1,400°C, and the extrapolation boundary was consistent with that of Kuroda et al. (Phys Chem Miner 27:523–532, 2000), which was determined at high temperature (1,800–2,000°C) using a calibration based on the same pressure scale. Our new phase boundary is marginally consistent with that of Suzuki et al. (Geophys Res Lett 27:803–806, 2000) based on in situ X-ray experiments at lower temperatures (<1,000°C) using Brown’s and Decker’s NaCl pressure scales. 相似文献