COMPUTATIONAL COMPARISONS BETWEEN THE CONVENTIONAL MULTISLICE METHOD AND THE 3RD-ORDER MULTISLICE METHOD FOR CALCULATING HIGH-ENERGY ELECTRON-DIFFRACTION AND IMAGING
Jh. Chen et al., COMPUTATIONAL COMPARISONS BETWEEN THE CONVENTIONAL MULTISLICE METHOD AND THE 3RD-ORDER MULTISLICE METHOD FOR CALCULATING HIGH-ENERGY ELECTRON-DIFFRACTION AND IMAGING, Ultramicroscopy, 69(4), 1997, pp. 219-240
The third-order multislice method (TOMS) for the calculation of high-e
nergy electron microscopic diffraction patterns and images, as propose
d by Van Dyck, is tested by detailed computations. Results calculated
by the TOMS and the conventional multislice method (CMS) with differen
t slice thicknesses and dynamical apertures (g(max) values) are compar
ed with the accurate results. It is pointed out that for both the TOMS
and the CMS there are basically two types of errors. One is the intri
nsic error imposed by the order of the method in slice thickness, whic
h appears as the pseudo HOLZ (high-order Laue zone) effect in the diff
raction patterns, Another is the numerical error caused by the finite
dynamical aperture, such as the aliasing error and the intensity-loss
error. For zero-order Laue zone (ZOLZ) calculations, it is shown that
the intrinsic errors are the dominant errors for both the TOMS and the
CMS since the elimination of the intrinsic error leads to the disappe
arance of the numerical error, as long as the dynamical aperture is la
rge enough to cover all the ZOLZ reflections. It is also shown that th
e TOMS has much smaller intrinsic error than the CMS for a large slice
thickness and therefore is superior to the CMS with respect to accura
cy vs. computational time for ZOLZ calculations. Nevertheless, the nor
malisation of the total intensity, as an error criterion, is more reli
able for the TOMS than for the CMS. Hence, TOMS is a feasible and comp
etitive procedure for dynamical calculations in high-energy electron d
iffraction (HEED). Possible error sources of practical multislice proc
edures are thoroughly discussed.