Laboratoire de Thermodynamique et Physico-chimie d'Hydrures et Oxydes, Université de Paris-Sud, F-91405 Orsay, France.
J Phys Condens Matter. 2013 Oct 16;25(41):415502. doi: 10.1088/0953-8984/25/41/415502. Epub 2013 Sep 18.
The segregation of Cr in Fe is known to be anomalous since the barrier for surface segregation of Cr is not determined by the topmost surface layer, as one would expect, but rather by the subsurface layer where the energy of segregation is much larger and endothermic. This has been attributed to a complex interaction involving the antiferromagnetism of Cr and the ferromagnetism of Fe. We report in this paper the results of our ab initio electronic structure calculations on the segregation behaviour of all the 3d elements on the (1 0 0) surface of ferromagnetic iron in the hope of better understanding this phenomenon. We find a similar behaviour for the segregation of the next antiferromagnetic 3d element Mn in Fe, where the subsurface layer is also found to block the segregation of Mn to the surface. On the other hand, ferromagnetic Co exhibits a normal segregation behaviour. The elements Sc, Cu and Ni do not form solid solutions with ferromagnetic iron. The early elements Ti and V are non-magnetic in their metallic states, but are strongly polarized by Fe, and develop magnetic moments which are aligned antiferromagnetically to those of Fe atoms. While the subsurface layer blocks the segregation of Ti to the surface, no blocking behaviour is found for the segregation of V. The segregation behaviour of all these elements is strongly correlated with the displacement of the solute atoms on the surface of Fe. The elements showing anomalous segregation behaviour are all displaced upwards on the surface, while those showing normal segregation are pulled inwards. These results indicate that the antiferromagnetism of the segregating element plays the key role in the anomalous segregation behaviour in Fe.
铬在铁中的偏析是反常的,因为铬的表面偏析势垒不是由最表层决定的,而不是像人们预期的那样,而是由能量较大的次表层决定的,这是一个吸热过程。这归因于涉及 Cr 的反铁磁性和 Fe 的铁磁性的复杂相互作用。我们在本文中报告了我们对所有 3d 元素在铁的铁磁 (100) 表面上偏析行为的从头算电子结构计算的结果,希望能更好地理解这一现象。我们发现 Fe 中相邻的反铁磁 3d 元素 Mn 的偏析行为也相似,次表层也阻止 Mn 向表面偏析。另一方面,铁磁 Co 表现出正常的偏析行为。元素 Sc、Cu 和 Ni 与铁不形成固溶体。早期元素 Ti 和 V 在其金属状态下是非磁性的,但被 Fe 强烈极化,并发展出与 Fe 原子反铁磁排列的磁矩。虽然次表层阻止了 Ti 向表面的偏析,但 V 的偏析行为并没有被阻止。所有这些元素的偏析行为都与溶质原子在 Fe 表面的位移强烈相关。表现出反常偏析行为的元素都在表面向上移动,而表现出正常偏析行为的元素则向内移动。这些结果表明,偏析元素的反铁磁性在 Fe 中的反常偏析行为中起着关键作用。