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Title: Thermally activated diffusion of copper into amorphous carbon

Journal Article · · Journal of Vacuum Science and Technology A
DOI:https://doi.org/10.1116/1.4991519· OSTI ID:1411175
 [1];  [2];  [1];  [3];  [1];  [4];  [1]
  1. Ames Lab. and Iowa State Univ., Ames, IA (United States)
  2. Ames Lab., Ames, IA (United States); Mantis Deposition, Inc., Denver, CO (United States)
  3. Ames Lab., Ames, IA (United States)
  4. Max Planck Institute for Intelligent Systems, Stuttgart (Germany)

Using x-ray photoelectron spectroscopy, the authors characterize the thermally activated changes that occur when Cu is deposited on amorphous carbon supported on Si at 300 K, then heated to 800 K. The authors compare data for Cu on the basal plane of graphite with pinning defects, where scanning tunneling microscopy reveals that coarsening is the main process in this temperature range. Coarsening begins at 500–600 K and causes moderate attenuation of the Cu photoelectron signal. For Cu on amorphous carbon, heating to 800 K causes Cu to diffuse into the bulk of the film, based on the strong attenuation of the Cu signal. Diffusion into the bulk of the amorphous carbon film is confirmed by changes in the shape of the Cu 2p inelastic tail, and by comparison of attenuation between Cu 2p and Cu 3p lines. The magnitude of the photoelectron signal attenuation is compatible with Cu distributed homogeneously throughout the amorphous carbon film, and is not compatible with Cu at or below the C–Si interface under the conditions of our experiments. As a result, desorption is not significant at temperatures up to 800 K.

Research Organization:
Ames Lab., Ames, IA (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
AC02-07CH11358
OSTI ID:
1411175
Report Number(s):
IS-J-9513
Journal Information:
Journal of Vacuum Science and Technology A, Vol. 35, Issue 6; ISSN 0734-2101
Publisher:
American Vacuum SocietyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 4 works
Citation information provided by
Web of Science

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