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model he proposed to explain the origin of friction is still quite modern. According to Amontons, surfaces
are tilted on a microscopic scale. Therefore, when two surfaces are pressed against each other and moved,
a certain lateral force is needed to lift the surfaces against the loading force. Assuming that no friction
occurs between the tilted surfaces, one immediately finds from purely geometric arguments
where
α
is the tilting angle on a microscopic scale. This model relates the friction to the microscopic
structure of the surface. Today we know that this model is too simple to explain the friction on a
macroscopic scale, i.e., everyday friction. In fact, it is well known that surfaces touch each other at many
microasperities and that the shearing of these microasperities is responsible for friction (Bowden and
Tabor, 1950). Within this model the friction coefficient is related to such parameters as shear strength
and hardness of the surfaces. On an atomic scale, however, the mechanism responsible for friction is
different. As will be discussed in more detail in this chapter, the model for explaining energy dissipation
in a scanning force microscope (SFM) is that the tip has to overcome the potential well between adjacent
atoms of the surface. For certain experimental conditions, which are in practice almost always realized,
the tip jumps from one stable equilibrium position on the surface to another. This process is not reversible,
leads to energy dissipation, and, therefore, on average to a friction force. The similarity between Amon-
tons’ model of friction and these modern models for friction on an atomic scale is evident. In both cases
asperities have to be passed, the only difference is the length scale of these asperities, in the first case
assumed to be microscopic, in the second case atomic.
Although tribology is an old science, and in spite of the efforts and progress made by scientists and
engineers, tribology is still far from being a well-understood subject, in fact (Maugis, 1982),
“It is incredible that, all properties being known (surface energy, elastic properties, loss properties), a
friction coefficient cannot be found by an
a priori
calculation.”
This is in contrast to other fields in physics, such as statistical physics, quantum mechanics, relativity,
or gauge field theories, which in spite of being much younger are already well established and serve as
fundamental theories for more complex problems such as solid state physics, astronomy and cosmology,
or particle physics. A fundamental theory of friction does not exist. Moreover, and although recently
considerable progress has been made, the determination of relevant tribological phenomena from first
principles is right now a very complicated task, indeed (Anonymous, 1995):
“What is needed … would be to calculate the results of moving a probe of known Miller surface of a
perfect crystal and calculate how energy is generated in the various phonon modes of the crystal as a
function of time.”
From another point of view, the difficulties encountered in tribology are not so surprising taking into
account the diversity of phenomena which in principle can contribute to the process of friction. In fact,
for a detailed understanding of friction the precise nature of the surfaces and their mutual interaction
have to be known. Adsorbed films which can serve as lubricants, surface roughness, oxide layers, and
maybe even defects and surface reconstructions determine the tribological properties of surfaces. The
essential complexity of friction has been described very accurately by Dowson (1979):
“… If an understanding of the nature of surfaces calls for such sophisticated physical, chemical,
mathematical, materials and engineering studies in both macro and molecular terms, how much more
challenging is the subject of … interacting surfaces in relative motion.”
An additional problem in tribology is that until recently it has not been possible to find a simple
experimental system which would serve as a model system. This contrasts with other fields in physics.
There, complex physical situations can usually be reduced to much simpler and basic ones where theories
can be developed and tested under well-defined experimental conditions. Note that it is not enough if
such a system can be thought of theoretically. For testing the theory this system has to be constructed
FF
lat load
=
()
⋅tan
α