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Equation of state of CaIrO3-type MgSiO3 up to 144 GPa

机译:高达144 GPa的CaIrO3型MgSiO3的状态方程

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摘要

The structure and equation of state for CaIrO3-type MgSiO3 were determined using high-pressure powder X-ray diffraction from 116 to 144 GPa. The CaIr-O-3-type phase remained stable over this entire pressure range. At each pressure increment, the sample was heated with a laser to relax the deviatoric stress in the sample. Pressure-volume data could be fitted to the Birch-Murnaghan equation of state with K-0 = 237(1) GPa using Anderson's gold pressure standard, when K-0(1) and V-0 were set to 4 and 162.86 angstrom(3), respectively. This indicates that the bulk modulus of MgSiO3 decreases when the phase transition occurs, because the bulk modulus of perovskite-type MgSiO3 is 250-260 GPa. The b axis of the Unit-cell parameter was more compressive than the a and c axes. The unit-cell volumes at high pressures, observed in high-pressure experiments, were slightly smaller than those predicted by theoretical studies.
机译:CaIrO3型MgSiO3的结构和状态方程是使用116至144 GPa的高压粉末X射线衍射确定的。 CaIr-O-3-型相在整个压力范围内保持稳定。在每个压力增量下,用激光加热样品以缓解样品中的偏应力。当K-0(1)和V-0分别设置为4和162.86埃时,可以使用安德森的金压力标准将压力-体积数据拟合为K-0 = 237(1)GPa的Birch-Murnaghan状态方程。 3)。这表明,由于钙钛矿型MgSiO3的体积模量为250-260 GPa,当发生相变时,MgSiO3的体积模量降低。单元像元参数的b轴比a和c轴更具压缩性。在高压实验中观察到的高压下的晶胞体积比理论研究预测的要小一些。

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