Depth-concentration profile of hydrogen in niobium

1982 ◽  
Vol 26 (6) ◽  
pp. 2900-2906 ◽  
Author(s):  
M. A. Pick ◽  
A. Hanson ◽  
K. W. Jones ◽  
A. N. Goland
1977 ◽  
Vol 32 (2) ◽  
pp. 144-146
Author(s):  
P. A. Büger ◽  
F. Blum ◽  
J. H. Schilling

Results of the depth profiling of a laser mirror are reported and discussed. The sample was bombarded with 40Ar+, 32O2+ and 16O- in order to establish optimum conditions. It was found that the bombardement by means of 16O- results in the best depth concentration profile


1994 ◽  
Vol 01 (04) ◽  
pp. 577-579 ◽  
Author(s):  
V.I. BUKHTIYAROV ◽  
A.I. BORONIN ◽  
O.A. BASCHENKO

Atomic oxygen states adsorbed at silver surface have been studied by angle-resolved XPS. It has been shown that all states have different structure of adsorbed layers. This allowed us to conclude that ARXPS followed by depth concentration profile restoration is useful technique for analysis of the adsorbate location with respect to upper substrate layers.


Author(s):  
G. Remond ◽  
R.H. Packwood ◽  
C. Gilles ◽  
S. Chryssoulis

Merits and limitations of layered and ion implanted specimens as possible reference materials to calibrate spatially resolved analytical techniques are discussed and illustrated for the case of gold analysis in minerals by means of x-ray spectrometry with the EPMA. To overcome the random heterogeneities of minerals, thin film deposition and ion implantation may offer an original approach to the manufacture of controlled concentration/ distribution reference materials for quantification of trace elements with the same matrix as the unknown.In order to evaluate the accuracy of data obtained by EPMA we have compared measured and calculated x-ray intensities for homogeneous and heterogeneous specimens. Au Lα and Au Mα x-ray intensities were recorded at various electron beam energies, and hence at various sampling depths, for gold coated and gold implanted specimens. X-ray intensity calculations are based on the use of analytical expressions for both the depth ionization Φ (ρz) and the depth concentration C (ρz) distributions respectively.


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