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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >The effect of temperature on the seismic anisotropy of the perovskite and post-perovskite polymorphs of MgSiO3
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The effect of temperature on the seismic anisotropy of the perovskite and post-perovskite polymorphs of MgSiO3

机译:温度对MgSiO3钙钛矿和钙钛矿后多晶型物地震各向异性的影响

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摘要

Using elastic constants determined by ab initio molecular dynamics over a range of temperatures, we show that the seismic anisotropy Of MgSiO3 perovskite is significantly temperature dependent. At 90 GPa, the direction of greatest shear wave splitting changes from [001] at 0 K to [010] at 3500 K. In addition, there is no shear wave splitting in the [100] direction at 0 K, but a significant amount of splitting is exhibited at 3500 K. We have also calculated the first set of high-temperature elastic (constants of the new post-perovskite phase by ab initio molecular dynamics methods. We find that, in contrast to MgSiO3 perovskite, temperature has little effect on the acoustic anisotropy of this phase. We determine partial derivativeln V-S/partial derivativeln V-P for the post-perovskite phase and find it to be very low, about 0.9. This may be an important parameter for mapping out the post-perovskite phase in the lowermost mantle. (C) 2004 Elsevier B.V. All rights reserved.
机译:使用从头算分子动力学在一定温度范围内确定的弹性常数,我们表明MgSiO3钙钛矿的地震各向异性与温度密切相关。在90 GPa时,最大剪切波分裂的方向从0 K的[001]变为3500 K时的[010]。此外,在0 K时[100]方向上没有剪切波分裂,但数量很大我们还计算了第一组高温弹性(通过从头算分子动力学方法得出的新的钙钛矿后常数)。我们发现,与MgSiO3钙钛矿相比,温度影响很小在该相的声各向异性上,我们确定了钙钛矿后相的偏导数VS /偏导数VP,发现它很低,约为0.9,这可能是在图中绘制钙钛矿后相的重要参数。 (C)2004 Elsevier BV保留所有权利。

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