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Regardless of the source of drift, the relative differences in the friction between the different layers remained constant.
Shallow structures (d: 1.5 μm) showed only slight differences in the friction coefficient, while deeper structures (d: 4.5 μm) led to a significant reduction.
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However, at low velocities, there is a significant difference in the friction coefficient between the two cores.
In addition, the difference in the friction coefficient between clay-rich and siliceous sedimentary rocks is not very large as the smectite-illite transition proceeds at this depth.
Nevertheless, it is necessary to question whether such a minor difference in the average friction forces would yield a clear perceptual difference if the deviation in the friction were to be considerable.
Although the differences in the skin friction, intermittency and turbulent kinetic energy prediction appear to be very limited between (a) and (b), these differences are more than sufficient in obtaining a correct separation prediction.
As shown in Fig. 10 (top), the differences in the average friction forces can be a maximum of 0.1 N among the five types of stimuli, which was shown to be discernible by a fingertip in a previous psychophysical study [44].
There is a noticeable difference in the skin friction coefficient at different values of the velocity slip factor.
Results from experiment Cd.11 corroborate the differences in the load-dependent friction for the two contacts.
Because of the small differences in friction between the presence and absence of a movable target, it is unlikely that participants used the amount of friction to perform the search task.
Specifically, the observations of friction contrast reversal, arising from differences in the load dependence of friction for calcian-otavite films and calcite, demonstrated a need for additional chemical and mechanical considerations beyond a simple friction-strain relationship.
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