Abstract:
Cross-sections of erosion craters formed by vacuum arc discharges on
graphite cathodes are examined using electron microscopy. These reveal
erosion craters that are covered with a growth layer forming a continuous
film on the arced surface. The film surface is composed of sphere-like
structures similar to cauliflower diamond and to the emitted macro-particles
(MPs) observed in coating experiments using graphite vacuum arc sources.
The film thickness within the cathode erosion craters evolves with the mean
values of the MP diameter and mean crater depth for four graphite material
morphologies. These two parameters increase with a decrease in arc spot
velocity. The growth layer shows a relatively porous columnar structure,
with micro-Raman spectroscopy indicating an evolution from amorphous
carbon (cathode base), to graphitic (middle), to diamond dominating the top
layer.