Surface and buried interface layer studies on challenging structures as studied by ARXPS
Previous extensive studies were performed at Surface Science Western on the treatment of III‐V semiconductors to produce surfaces suitable for subsequent epitaxial growth. X‐ray photoelectron spectroscopy (XPS) was used to study oxide formation and capping techniques, and to monitor changes that wou...
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Veröffentlicht in: | Surface and interface analysis 2017-12, Vol.49 (13), p.1309-1315 |
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Sprache: | eng |
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Zusammenfassung: | Previous extensive studies were performed at Surface Science Western on the treatment of III‐V semiconductors to produce surfaces suitable for subsequent epitaxial growth. X‐ray photoelectron spectroscopy (XPS) was used to study oxide formation and capping techniques, and to monitor changes that would occur upon thermal desorption. The effects of a remote plasma on these surfaces were studied as well as to apply thin dielectric films of Si3N4 in order to study interfacial properties. Angle‐resolved XPS (ARXPS) was performed in many cases to ascertain oxide layer thickness, uniformity, and structure. For the types of surfaces studied—mirror finished semiconductors, ARXPS is straightforward, and the angular dependence is obtained by physically altering the surface orientation with respect to the analyser. While the sample can be repositioned with care to analyse the same spot, changing the angle will effectively change the sampling area, further, surface topography can preclude the use of ARXPS. Use of parallel PARXPS, now available on recent instrumentation, can alleviate these problems. In this case, photoelectrons are collected simultaneously from a large angle. A multichannel detector allows this to be split into smaller angles thereby giving the PARXPS spectra without physically tilting the sample. Further, because the sample is not tilted, topographical effects are minimised allowing meaningful data to be extracted from not so perfect samples. To illustrate this, a detailed PARXPS study on a gallium Indium eutectic (EGaIn) will be presented. Various methods of extracting the depth information from these spectra will be discussed. Finally, the application of using PARXPS to study buried interfaces will be briefly discussed. Copyright © 2017 John Wiley & Sons, Ltd. |
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ISSN: | 0142-2421 1096-9918 |
DOI: | 10.1002/sia.6270 |