arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2402.04036cond-mat.mtrl-sci
收藏

MgSiO3在高温高压下的电导率:对地幔的启示

Electrical conductivity of MgSiO3 at high temperatures and pressures: implications for the Earth's mantle

Samuel S. M. Santos, Lucy V. C. Assali, João F. Justo

AI总结:

本文通过第一性原理和玻尔兹曼输运理论计算,发现MgSiO3电导率随压力、温度和结构相变化,相变及带隙转变影响地幔电导率。

摘要:

本文利用第一性原理密度泛函理论和玻尔兹曼输运理论,在地球下地幔的热力学条件下研究了硅酸镁MgSiO3的电导率。我们发现,纯净MgSiO3的电导率强烈依赖于材料的结构相,以及温度和压力。钙钛矿相的电导率随压力(下地幔深度)增加而增大,直至90 GPa,随后由于材料的带隙从直接带隙转变为间接带隙,电导率在更高压力下下降。最后,MgSiO3在下地幔底部附近经历从钙钛矿到后钙钛矿的结构相变,导致MgSiO3电导率增加,这应有助于地球D"层热力学条件下地幔电导率的增加。

英文摘要:

The electrical conductivity of magnesium silicate MgSiO3 has been studied, using the framework of the first-principles density functional theory and the Boltzmann transport theory, under the thermodynamic conditions of the Earth's lower mantle. We find that the conductivity of pristine MgSiO3 depends strongly on the structural phase of the material, as well as on temperature and pressure. The conductivity of the perovskite phase increases with increasing pressure (depth of the lower mantle) up to 90 GPa, then decreases at higher pressures due to a change in the material's band gap transition from direct to indirect. Finally, the structural phase transition that MgSiO3 undergoes near the bottom of the lower mantle, from perovskite to post-perovskite, causes an increase in the conductivity of MgSiO3, which should contribute to the increase in the electrical conductivity of the Earth's mantle under the thermodynamic conditions of the Earth's D" layer.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑