Angle-resolved X-ray Photoelectron Spectroscopy
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The
effective sampling depth in XPS can be varied (for flat
samples) by changing the angle of the sample with respect to the
detector. The
actual depth sampled, d, is given by the equation: d
= 3λ
sin θ,
where
λ
is the
inelastic mean free path of the photoelectron and
θ is the angle between the sample surface and the analyzer acceptance plane. |
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| http://www.uccs.edu/~tchriste/courses/PHYS549/549lectures/element.html |
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By comparing the relative intensities of peaks at the same kinetic energy over a number of different takeoff angles it is possible to calculate layer thickness. Alternately, comparing relative intensities at low and high take off angles indicates whether a species is enriched or depleted in the surface region. This is useful for the analysis of thin films on surfaces where it is possible to determine the molecular orientation to the surface.
References:
•
P.J.
Cumpson, in D. Briggs and
J.T. Grant (Eds.),
Surface
Analysis
by Auger and X-ray Photoelectron Spectroscopy, IM publications and
SurfaceSpectra Limited: Chichester: Manchester, 2003,
Chapter Angle-Resolved
X-Ray
Photoelectron Spectroscopy.
•
Angle-resolved
X-ray Photoelectron Spectroscopy (ARXPS) by Royston Paynter
For more details, please contact us (kartyush@unm.edu).
