Song Yalan, He Kaihua, Sun Jian, Ma Chaojie, Wan Miao, Wang Qingbo, Chen Qili
Faculty of Maths and Physics, China University of Geosciences, Wuhan, 430074, China.
Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan, 430074, China.
Sci Rep. 2019 Mar 12;9(1):4172. doi: 10.1038/s41598-019-40454-4.
The effects of the spin transition on the electronic structure, thermal expansivity and lattice thermal conductivity of ferropericlase are studied by first principles calculations at high pressures. The electronic structures indicate that ferropericlase is an insulator for high-spin and low-spin states. Combined with the quasiharmonic approximation, our calculations show that the thermal expansivity is larger in the high-spin state than in the low-spin state at ambient pressure, while the magnitude exhibits a crossover between high-spin and low-spin with increasing pressure. The calculated lattice thermal conductivity exhibits a drastic reduction upon the inclusion of ferrous iron, which is consistent with previous experimental studies. However, a subsequent enhancement in the thermal conductivity is obtained, which is associated with the spin transition. Mechanisms are discussed for the variation in thermal conductivity by the inclusion of ferrous iron and the spin transition.
通过高压下的第一性原理计算,研究了自旋转变对铁方镁石电子结构、热膨胀系数和晶格热导率的影响。电子结构表明,铁方镁石在高自旋和低自旋状态下均为绝缘体。结合准谐近似,我们的计算表明,在常压下,高自旋状态的热膨胀系数大于低自旋状态,而随着压力增加,热膨胀系数在高自旋和低自旋之间呈现交叉变化。计算得到的晶格热导率在加入亚铁后急剧降低,这与之前的实验研究一致。然而,随后热导率出现增强,这与自旋转变有关。文中讨论了加入亚铁和自旋转变导致热导率变化的机制。