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Magneto-structural transformations via a solid-state nudged elastic band method: Application to iron under pressure

机译:通过固态微动弹性带方法进行的磁-结构转换:在压力下应用于铁

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摘要

We extend the solid-state nudged elastic band method to handle a non-conserved order parameter, in particular, magnetization, that couples to volume and leads to many observed effects in magnetic systems. We apply this formalism to the well-studied magneto-volume collapse during the pressure-induced transformation in iron-from ferromagnetic body-centered cubic (bcc) austenite to hexagonal close-packed (hcp) martensite. We find a bcc-hcp equilibrium coexistence pressure of 8.4 GPa, with the transition-state enthalpy of 156 meV/Fe at this pressure. A discontinuity in magnetization and coherent stress occurs at the transition state, which has a form of a cusp on the potential-energy surface (yet all the atomic and cell degrees of freedom are continuous); the calculated pressure jump of 25 GPa is related to the observed 25 GPa spread in measured coexistence pressures arising from martensitic and coherency stresses in samples. Our results agree with experiments, but necessarily differ from those arising from drag and restricted parametrization methods having improperly constrained or uncontrolled degrees of freedom. (C) 2015 AIP Publishing LLC.
机译:我们扩展了固态微动弹性带方法,以处理非保守的阶跃参数,特别是磁化强度,该参数耦合到体积并导致在磁系统中观察到许多影响。我们将这种形式主义应用于对铁(从铁磁性体心立方(bcc)奥氏体到六方密堆积(hcp)马氏体)的压力诱导转变过程中经过充分研究的磁体积塌陷。我们发现bcc-hcp平衡共存压力为8.4 GPa,在该压力下的过渡态焓为156 meV / Fe。在过渡态时会发生磁化强度和相干应力的不连续性,这在势能表面上具有尖峰的形式(但原子和单元的所有自由度都是连续的)。计算出的25 GPa的压力跃变与在样品中由马氏体和相干应力产生的共存压力中观察到的25 GPa展宽有关。我们的结果与实验相吻合,但必然不同于因阻力和自由度受到不适当约束或控制而受到限制的参数化方法所产生的结果。 (C)2015 AIP Publishing LLC。

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