Early stages of diamond-film formation on cobalt-cemented tungsten carbide

被引:17
作者
Polini, R [1 ]
Le Normand, F
Marcheselli, G
Traversa, E
机构
[1] Univ Roma Tor Vergata, Dipartimento Sci & Tecnol Chim, I-00133 Rome, Italy
[2] IPCMS, Grp Surfaces Interfaces, F-67037 Strasbourg, France
[3] Fabbrica Italiana Leghe Met Sinterizzate SPA, I-28877 Anzola Ossola, Italy
关键词
D O I
10.1111/j.1151-2916.1999.tb01935.x
中图分类号
TQ174 [陶瓷工业]; TB3 [工程材料学];
学科分类号
0805 ; 080502 ;
摘要
The surface composition of cemented tungsten carbide (WC-5.8 wt% Co) was studied by X-ray photoelectron spectroscopy (XPS), during the early stages of diamond-film deposition, by hot-filament chemical vapor deposition (HFCVD), The nucleated diamond films were analyzed by scanning electron microscopy (SEM), energy-dispersive spectroscopy (EDS),and automatic image analysis (AIA). The evolution of the surface composition of cemented tungsten carbide during the early stages of diamond-film deposition was strongly dependent on the substrate temperature, At relatively Low temperature (750 degrees C), cobalt-rich particles started to segregate at the substrate surface after a few minutes of diamond deposition. The conspicuous seg regation of the binder partly inhibited the formation of stable diamond nuclei, through intense carbon dissolution or carbon segregation at the binder surface, but did not affect nucleic growth. At higher temperatures (940 degrees C), no cobalt-rich particles formed at the substrate surface, even after 2 h of deposition. However, XPS results demonstrated the presence of cobalt in a surface layer, although in a lower amount than at 750 degrees C. Nevertheless, the nucleation density of diamond at 940 degrees C was much lower than at 750 degrees C, Gaps between WC grains formed within 10 mins. Therefore, intergranular cobalt was removed at 940 degrees C, a finding attributed to the etching performed by monohydrogen, rather than to binder evaporation. The time evolution of the substrate area fraction covered by diamond islands, S(t), was well described by Avrami kinetics for two-dimensional phase transformations, suggesting that dia mend formation took place via a heterogeneous nucleation process. The S(t) functions exhibited a similar trend at 750 degrees and 940 degrees C, because the higher growth rate of diamond crystallites at higher temperature counteracted the slower nucleation rate at the higher temperature.
引用
收藏
页码:1429 / 1435
页数:7
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