首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >High-pressure elasticity of calcium oxide: A comparison between Brillouin spectroscopy and radial X-ray diffraction
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High-pressure elasticity of calcium oxide: A comparison between Brillouin spectroscopy and radial X-ray diffraction

机译:氧化钙的高压弹性:布里渊光谱与径向X射线衍射的比较

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Single-crystal Brillouin scattering to 25.2 GPa and powder X-ray diffraction to 65.2 GPa in a radial geometry were carried out on CaO (lime) at ambient temperature in a diamond cell. From Brillouin scattering measurements the isentropic elastic constants of CaO at ambient conditions are C 11 = 219.4 (7), C 12 = 58.1 (7), C 44 = 80.0 (2) GPa, where the numbers in parentheses are 1σ uncertainties on the last digit. The pressure derivatives of the compressional and off-diagonal constants at ambient pressure are ?C 11/?P = 9.9 (1), ?C 12/?P = 2.2 (1), respectively. The pressure derivative of the shear constant is ?C 44/?P = 0.25 (3), and it becomes negative at pressures above 5.9 GPa. Aggregate bulk and shear moduli are K S0 = 112.0 (2) and G 0 = 80.05 (9) GPa, and their pressure derivatives are 4.72 (6) and 1.69 (5), respectively. The radial X-ray diffraction data allow us to estimate the yield strength and the elastic constants of CaO using a phenomenological lattice strain model. The calculated strength of CaO increases from 0.3 to 1.9 GPa in the pressure range between 5.6 and 57.8 GPa. The estimated elastic constants are in good agreement with the extrapolation of the Brillouin data up to 36.6 GPa. At higher pressures, C 11 appears softer and C 12 appears stiffer than the extrapolation of Brillouin results. The value of C 44 from radial diffraction is in agreement with the Brillouin data through the entire experimental pressure range. The discrepancies between Brillouin and radial diffraction data for C 11 and C 12 can be reconciled if α, the parameter which describes degree of stress/strain continuity across the sample's grains boundary, is allowed to vary from 1 at 36.6 GPa to 0.82 at 65.2 GPa. The “hydrostatic” cell volumes determined by applying lattice strain theory were fitted to the third-order Birch-Murnaghan equation. The fitted bulk modulus and its pressure derivative are K T0 = 110 (5) GPa and (?K T /?P) T0 = 4.5 (4), consistent with the Brillouin results, although possible softening of the equation of state at high pressure has been identified. The general agreement between the results of the two methods indicates that radial diffraction with lattice strain theory is a valid probe of the mechanical properties of a moderately soft cubic solid as CaO at ultrahigh pressures. However, more tests are required to quantify the effect of plasticity and texturing on the results of this method.
机译:在室温下在金刚石池中的CaO(石灰)上进行径向几何形状的单晶布里渊散射至25.2 GPa和粉末X射线衍射至65.2 GPa。根据布里渊散射测量,环境条件下CaO的等熵弹性常数为C 11 = 219.4(7),C 12 = 58.1(7),C 44 = 80.0(2)GPa,其中括号中的数字为最后的1σ不确定性数字。在环境压力下的压缩常数和对角线常数的压力导数分别为ΔC11 /ΔP= 9.9(1),ΔC12 /ΔP= 2.2(1)。剪切常数的压力导数为ΔC44 /ΔP= 0.25(3),并且在高于5.9 GPa的压力下为负。骨料的总体积模量和剪切模量为K S0 = 112.0(2)和G 0 = 80.05(9)GPa,它们的压力导数分别为4.72(6)和1.69(5)。径向X射线衍射数据使我们能够使用现象学的晶格应变模型估算CaO的屈服强度和弹性常数。在5.6和57.8 GPa之间的压力范围内,CaO的计算强度从0.3 GPa增加到1.9 GPa。估计的弹性常数与高达36.6 GPa的布里渊数据外推非常吻合。在较高的压力下,比布里渊结果外推,C 11看起来更软,C 12看起来更坚硬。在整个实验压力范围内,径向衍射得到的C 44值与布里渊数据一致。如果允许将描述样品晶界上应力/应变连续性程度的参数α从36.6 GPa的1更改为65.2 GPa的0.82,则可以调节C 11和C 12的布里渊与径向衍射数据之间的差异。 。通过应用晶格应变理论确定的“静水”细胞体积被拟合到三阶Birch-Murnaghan方程。拟合的体积模量及其压力导数为K T0 = 110(5)GPa和(ΔKT/ΔP)T0 = 4.5(4),与布里渊结果一致,尽管在高压下状态方程可能会变软被确定。两种方法的结果之间的总体一致性表明,采用晶格应变理论的径向衍射是对中软立方固体如CaO在超高压下的力学性能的有效探究。但是,需要更多测试来量化可塑性和纹理化对该方法结果的影响。

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