Caspersen Kyle J, Lew Adrian, Ortiz Michael, Carter Emily A
Department of Chemistry and Biochemistry, University of California, Los Angeles, California 90095-1569, USA.
Phys Rev Lett. 2004 Sep 10;93(11):115501. doi: 10.1103/PhysRevLett.93.115501.
Iron shows a pressure-induced martensitic phase transformation from the ground state ferromagnetic bcc phase to a nonmagnetic hcp phase at approximately 13 GPa. The exact transformation pressure (TP) and pathway are not known. Here we present a multiscale model containing a quantum-mechanics-based multiwell energy function accounting for the bcc and hcp phases of Fe and a construction of kinematically compatible and equilibrated mixed phases. This model suggests that shear stresses have a significant influence on the bcc<-->hcp transformation. In particular, the presence of modest shear accounts for the scatter in measured TPs. The formation of mixed phases also provides an explanation for the observed hysteresis in TP.
铁在约13吉帕斯卡的压力下会发生从基态铁磁体心立方相到非磁性六方密堆积相的压力诱导马氏体相变。确切的转变压力(TP)和转变路径尚不清楚。在此,我们提出了一个多尺度模型,该模型包含一个基于量子力学的多阱能量函数,用于描述铁的体心立方相和面心立方相,以及一个运动学兼容且平衡的混合相结构。该模型表明,剪应力对体心立方相<-->面心立方相的转变有显著影响。特别是,适度剪应力的存在解释了测量得到的转变压力的离散性。混合相的形成也为观察到的转变压力滞后现象提供了解释。