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However, real contact clusters are much more complicated.
The displacement fields generated by the contact clusters are continuous all over the surface area.
As the contact area increases, both summits and valleys can form as contact clusters.
However, in the GFMD model, the contact clusters influence each other.
This can be explained by the RMS slope of the contact clusters.
This suggests that the contact clusters in GFMD model are more discrete than those in the asperity model.
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b A typical contact cluster comprising of six independent asperities.
Fig. 2 Contact cluster detecting algorithm: the labeling technique.
Most of the contact cluster locations are coincident with the surface summits/valleys.
Figure 10 shows the contact cluster's RMS slopes for the three models.
The contact cluster merging effect has been observed in both the asperity model and the GFMD model.
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