Influence of diffusion on W sputtering by carbon

Citation
K. Schmid et al., Influence of diffusion on W sputtering by carbon, J NUCL MAT, 290, 2001, pp. 148-152
Citations number
12
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science","Nuclear Emgineering
Journal title
JOURNAL OF NUCLEAR MATERIALS
ISSN journal
00223115 → ACNP
Volume
290
Year of publication
2001
Pages
148 - 152
Database
ISI
SICI code
0022-3115(200103)290:<148:IODOWS>2.0.ZU;2-T
Abstract
This paper concerns with temperature dependence of tungsten (W) sputtering by carbon (C). Weight loss measurements of W samples during sputtering by 2 .4 keV C ions at different temperatures in the range between 300 and 1000 I t showed a strong temperature dependence. At a certain fluence, which depen ds on the temperature, the probe's weight starts to increase again. This is due to C enrichment in the surface during ion bombardment, which eventuall y leads to the formation of a pure C surface. This C film then shields the underlying W from further sputtering and further growth of this film increa ses the probe's weight. The growth of this him depends critically on the di ffusion of C into the W bulk material since this removes C from the surface and thereby increases the W concentration and W erosion. This in turn resu lts in an increased reflection of the incoming C ions. These two coupled me chanisms hinder the growth of the C film with the diffusion accounting for the temperature dependence of the weight loss. To verify this model, C dept h profiles in W were determined by means of Rutherford backscattering (RBS) with He ions. To increase sensitivity, the increased cross-section at 5715 keV was used. Analysis of depth profiles measured in the temperature range between 300 and 1000 It show that relevant diffusion processes appear at a pproximately 800 K, By performing Boltzmann Matano analysis on the measured depth profiles, a concentration dependant diffusion coefficient for C diff usion in W was deduced. The weight loss measurements were simulated using a combination of the Monte Carlo program TRIDYN and the diffusion code PIDAT . (C) 2001 Elsevier Science B.V. All rights reserved.