D. Danailov et al., Deduction of the He-Fe interaction potential in eV-range from experimentaldata by computer simulation in grazing ion-surface scattering: Row-model, NUCL INST B, 180, 2001, pp. 265-273
In glancing-angle scattering of keV-ions from a crystal surface, the ion re
flection takes place in the eV-part of the interaction potentials. The elas
tic interactions are determined by the energy transverse to atomic rows, wh
ich can be of the order of 10 eV, A row-model using averaged potentials acc
ording to the Lindhard cylindrical potential has been developed using step-
by-step integration of Newton's equations of motion. Previously [D. Danailo
v, K. Gartner, A. Care, Nucl. Instr. and Math. B 153 (1999) 191; presented
on COSIRES, Okayama, 1998] we reported that zig-zag trajectories within sur
face channels and the corresponding multimode azimuthal angular distributio
ns of reflected ions are very sensitive to the interaction potential used i
n the simulation. Here we simulate the scattering of 15 keV Heatoms from Fe
(1 0 0) surfaces at different angles of incidence comparable with previousl
y published experimental results [D, Danailov, T. Igel, R. Pfandzelter, H.
Winter, Nucl. Instr. and Meth. B 164-165 (2000) 583]. Our results show that
for interaction energies below about 4 eV the well-known "universal" poten
tial works well. However. for energies between 4 and 13 eV the "individual"
He-Fe potential(D. Danailov, K. Gartner, A. Care, Nucl. Instr. and Meth. B
153 (1999) 191, presented on COSIRES, Okayama, 1998) gives a better agreem
ent with the experimental data. For interaction energies above 13 eV both p
otentials are similar. We have constructed a mixed He-Fe potential, which d
escribes the experimental observations well. The row-model enables us to de
duce the He-Fe interaction potential in the eV-range. In addition, a shift
in the experimental angular spectra compared with the calculated spectra in
dicates that the atomistic rows undergo an elastic horizontal bend due to t
he scattering and an order of magnitude smaller vertical displacement. (C)
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