R. Schellenberg et al., PHOTOELECTRON DIFFRACTION - A SOURCE FOR MAGNETIC DICHROISM IN ANGLE-RESOLVED PHOTOEMISSION FROM FERROMAGNETS, Physical review. B, Condensed matter, 57(22), 1998, pp. 14310-14319
Magnetic dichroism has been measured in angle-resolved core-level phot
oemission from the Fe 2p and 3p levels in epitaxially grown ultrathin
films of Fe(001) and in an amorphous metallic glass with composition F
e78B13Si9. Unpolarized Al K alpha and Mg K alpha radiation was used fo
r excitation, leading to diffraction patterns that are dominated by fo
rward scattering along low-index crystallographic directions. The Fe(0
01) data for both total intensity and magnetic dichroism are quantitat
ively compared to theoretical calculations at both a two-atom single-s
cattering level and a multiatom multiple-scattering level. Strong effe
cts on the magnetic dichroism due to photoelectron diffraction are fou
nd, and the combined angle and energy dependence of the dichroism show
s a characteristic ''checkered'' pattern that should be generally obse
rvable in all single crystals. Comparing dichroism data obtained for s
ingle-crystal Fe films with those obtained from the amorphous glass an
d from two-atom and multiatom diffraction theory further permits estim
ating the relative contributions of free-atom-like dichroism and of ph
otoelectron diffraction, with the free-atom dichroism (that is dominan
t along low-index directions) being smaller by about a factor of 2 to
4 than the maximum diffraction dichroism (that dominates away from low
-index directions). Such photoelectron-diffraction-produced magnetic d
ichroism thus should provide a useful tool for studying magnetic order
near single-crystal surfaces. The deviation of the zero in the dichro
ic asymmetry from the low-index directions is also found via photoelec
tron diffraction theory to be very sensitive to the s-to-d partial-wav
e phase difference, and the experimental data permit estimating this q
uantity and the solid-state effects on it.