The dissipation mechanism of nanoscale kinetic friction between an atomic force microscopy tip and a surface of amorphous glassy polystyrene has been studied as a function of two parameters: the scanning velocity and the temperature. Superposition of the friction results using the method of reduced variables revealed the dissipative behavior as an activated relaxation process with a potential barrier height of 7.0 kcal/mol, corresponding to the hindered rotation of phenyl groups around the C-C bond with the backbone. The velocity relationship with friction F(v) was found to satisfy simple fluctuation surface potential models with F proportional to const-ln(v) and F proportional to const-ln(v)2/3.
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http://dx.doi.org/10.1103/PhysRevLett.91.095501 | DOI Listing |
Nature
January 2025
The Racah Institute of Physics, The Hebrew University of Jerusalem, Jerusalem, Israel.
Frictional motion is mediated by rapidly propagating ruptures that detach the ensemble of contacts forming the frictional interface between contacting bodies. These ruptures are similar to shear cracks. When this process takes place in natural faults, these rapid ruptures are essentially earthquakes.
View Article and Find Full Text PDFACS Nano
December 2024
State Key Laboratory of Solid Lubrication, Lanzhou Institute of Chemical Physics, Chinese Academy of Sciences, Lanzhou 730000, China.
J Biomech Eng
January 2025
Department of Mathematics, COMSATS University Islamabad, Park Road Tarlai Kalan, Islamabad 45550, Pakistan.
The dynamics of electro-osmotically generated flow of biological viscoelastic fluid in a cylindrical geometry are investigated in this paper. This flux is the result of walls contracting and relaxing sinusoidally in a magnetic environment. The blood's viscoelasticity and shear-thinning viscosity are the primary causes of its non-Newtonian characteristics.
View Article and Find Full Text PDFSci Adv
October 2024
Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA.
Whether Earth materials exhibit frictional creep or catastrophic failure is a crucial but unresolved problem in predicting landslide and earthquake hazards. Here, we show that field-scale observations of sliding velocity and pore water pressure at two creeping landslides are explained by velocity-strengthening friction, in close agreement with laboratory measurements on similar materials. This suggests that the rate-strengthening friction commonly measured in clay-rich materials may govern episodic slow slip in landslides, in addition to tectonic faults.
View Article and Find Full Text PDFNature
July 2024
Nevada Seismological Laboratory, University of Nevada, Reno, NY, USA.
Understanding the factors governing the stability of fault slip is a crucial problem in fault mechanics. The importance of fault geometry and roughness on fault-slip behaviour has been highlighted in recent lab experiments and numerical models, and emerging evidence suggests that large-scale complexities in fault networks have a vital role in the fault-rupture process. Here we present a new perspective on fault creep by investigating the link between fault-network geometry and surface creep rates in California, USA.
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