Surface physics with low-energy ion scattering

Authors
Citation
Do. Boerma, Surface physics with low-energy ion scattering, NUCL INST B, 183(1-2), 2001, pp. 73-87
Citations number
58
Categorie Soggetti
Spectroscopy /Instrumentation/Analytical Sciences","Instrumentation & Measurement
Journal title
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS
ISSN journal
0168583X → ACNP
Volume
183
Issue
1-2
Year of publication
2001
Pages
73 - 87
Database
ISI
SICI code
0168-583X(200107)183:1-2<73:SPWLIS>2.0.ZU;2-T
Abstract
Four versions of low-energy ion scattering (LEIS) measurements are briefly reviewed. In the first version discussed here the charged fraction of scatt ered noble-gas ions is detected with an electrostatic analyser. The composi tion of exclusively the outermost layer is probed in this way, even when th e surface of the sample is not smooth. The second method probes the surface step density, and thereby growth oscillations, with grazing-angle specular scattering, whereby the scattered particles are measured without energy re solution. An example is given of the observation of oscillations during the growth of Ag on Ag (0 0 1) at several temperatures. The oscillations are c ompared with oscillations obtained from simulations of the growth process, combined with LEIS simulations. This second method is also sensitive to the structure of the outermost layer. There is no sensitivity to the compositi on of the surface. In the third method either the beam direction, or the di rection of the detector, makes a grazing angle with the surface, and atoms scattered over a large (non-specular) angle are detected with time-of-fligh t (TOF) resolution. This provides sensitivity only to atoms protruding from the surface, like adatoms, or atoms at step edges. An example is presented whereby this method is used to measure adatom mobilities. Finally the conv entional method of measuring with TOF resolution azimuth scans of scattered or recoiled particles in a shadowing or blocking geometry is described. Th e scans are compared with the results of computer simulations carried out f or trial structures. The properties of the program MATCH that can be used e fficiently for these simulations are summarised. As an example of the appli cation of this method the determination of the surface structure of Fe3O4 ( 0 0 1) is presented. The features of the LEIS versions presented are compar ed with MEIS and HEIS features. with emphasis on the possibility to obtain information on the composition and structure, separately for the first few layers of a sample. (C) 2001 Elsevier Science B.V. All rights reserved.