Lyon Keenan, Rusz Jan
Department of Physics and Astronomy, Uppsala University, Box 516, S-751 20 Uppsala, Sweden.
Acta Crystallogr A Found Adv. 2021 Nov 1;77(Pt 6):509-518. doi: 10.1107/S2053273321008792. Epub 2021 Oct 29.
The multislice method, which simulates the propagation of the incident electron wavefunction through a crystal, is a well established method for analysing the multiple scattering effects that an electron beam may undergo. The inclusion of magnetic effects into this method proves crucial towards simulating enhanced magnetic interaction of vortex beams with magnetic materials, calculating magnetic Bragg spots or searching for magnon signatures, to name a few examples. Inclusion of magnetism poses novel challenges to the efficiency of the multislice method for larger systems, especially regarding the consistent computation of magnetic vector potentials A and magnetic fields B over large supercells. This work presents a tabulation of parameterized magnetic (PM) values for the first three rows of transition metal elements computed from atomic density functional theory (DFT) calculations, allowing for the efficient computation of approximate A and B across large crystals using only structural and magnetic moment size and direction information. Ferromagnetic b.c.c. (body-centred cubic) Fe and tetragonal FePt are chosen to showcase the performance of PM values versus directly obtaining A and B from the unit-cell spin density by DFT. The magnetic fields of b.c.c. Fe are well described by the PM approach while for FePt the PM approach is less accurate due to deformations in the spin density. Calculations of the magnetic signal, namely the change due to A and B of the intensity of diffraction patterns, show that the PM approach for both b.c.c. Fe and FePt is able to describe the effects of magnetism in these systems to a good degree of accuracy.
多切片方法通过模拟入射电子波函数在晶体中的传播,是一种用于分析电子束可能经历的多重散射效应的成熟方法。将磁效应纳入该方法对于模拟涡旋束与磁性材料的增强磁相互作用、计算磁布拉格点或寻找磁振子特征等至关重要。对于更大的系统,纳入磁性给多切片方法的效率带来了新的挑战,特别是在大超胞上一致计算磁矢势A和磁场B方面。这项工作给出了根据原子密度泛函理论(DFT)计算得出的前三排过渡金属元素的参数化磁(PM)值列表,允许仅使用结构、磁矩大小和方向信息在大晶体上高效计算近似的A和B。选择铁磁体心立方(b.c.c.)的Fe和四方晶系的FePt来展示PM值相对于通过DFT从单胞自旋密度直接获得A和B的性能。b.c.c. Fe的磁场用PM方法能很好地描述,而对于FePt,由于自旋密度的变形,PM方法不太准确。对磁信号的计算,即衍射图案强度因A和B引起的变化,表明b.c.c. Fe和FePt的PM方法都能够在相当高的精度上描述这些系统中的磁性效应。