Beilstein Arch. 2025, 202542. https://doi.org/10.3762/bxiv.2025.42.v1
Published 02 Jul 2025
Contact resonance atomic force microscopy (CR-AFM) has been used in many studies to characterize variations in the elastic and viscoelastic constants of materials along a heterogeneous surface. In almost all experimental work, the quantitative modulus of the surface is calculated in reference to a known reference material, rather than calculated directly from the dynamics models of the cantilever. We measure the cantilever displacement with very high sampling frequencies over the course of the experiment and capture its oscillations that result from thermal energy. Using short term Fourier transformations (STFT), it is possible to fit the thermal resonance peak of the normal displacement to track the frequency and Q-factor of the cantilever during an experiment, using a similar process to that used to calibrate the normal bending stiffness of cantilevers. With this quantitive data, we have used the dynamic mechanics models relating the contact stiffness of the tip/cantilever pressing into a surface with the oscillation frequency of the cantilever and show that they do not accurately model the experiment. Several material combinations of tip and sample are examined, as well as tip size and cantilever stiffness demonstrate that existing models cannot capture the physics of this problem.
Keywords: atomic force microscopy; contact resonance; highly oriented pyrolytic graphite (HOPG); mechanical property measurements; surface science
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Mathias, T.; Bennewitz, R.; Egberts, P. Beilstein Arch. 2025, 202542. doi:10.3762/bxiv.2025.42.v1
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