Abstract
Maximum friction coefficients of common minerals can be characterized by empirical Byerlee's rule, however, some important fault-forming minerals such as mica and clay minerals have ultimately low friction coefficient. The layered structure and high affinity to water should be related to the low friction coefficient. We have investigated the interlayer bonding energy, adsorption energy of water molecules, and physical properties of adsorbed water by using molecular simulations, surface x-ray scattering, and surface forces measurements. These results were used for interpreting the weak friction coefficients of layered minerals.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Japanese Magazine of Mineralogical and Petrological Sciences
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
