XPS study of nitridation of diamond and graphite with a nitrogen ion beam

Citation
I. Kusunoki et al., XPS study of nitridation of diamond and graphite with a nitrogen ion beam, SURF SCI, 492(3), 2001, pp. 315-328
Citations number
38
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
SURFACE SCIENCE
ISSN journal
00396028 → ACNP
Volume
492
Issue
3
Year of publication
2001
Pages
315 - 328
Database
ISI
SICI code
0039-6028(20011020)492:3<315:XSONOD>2.0.ZU;2-E
Abstract
Diamond (CVD.) and graphite (HOPG) samples were nitrided at room temperatur e by irradiation with 300-700 eV N-2(+) ion beams. X-ray photoelectron spec tra (XPS) were recorded in situ during the nitridation. The YPS spectra of Cls and N1s core levels are divided into three (A, B, C) and four (D, E, F, G) components, respectively. The A component at similar to 284.8 eV is ass igned to the non-damaged substrate below the ion penetration depth. The B c omponent at similar to 286.0 eV originates in the damaged phase and the sub -nitride phase (CNx: x < 1). The C component at similar to 287.3 eV is attr ibuted to genuine nitrides such as C3N4. The broad N1s XPS peak at similar to 400 eV splits clearly into the D (similar to 398.4 eV) and F (similar to 401.2 eV) components upon annealing at 600 degreesC in vacuum. The splitti ng is caused by evaporation of the volatile E component (similar to 399.7 e V). The intensity of the D component was always comparable to that of the F component in both diamond and graphite cases. The origins of these compone nts are discussed. The G component may be due to nitrogen trapped at defect s. (C) 2001 Elsevier Science B.V. All rights reserved.