Brittle Fracture Theory Describes the Onset of Frictional Motion
| العنوان: | Brittle Fracture Theory Describes the Onset of Frictional Motion |
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| المؤلفون: | Ilya Svetlizky, Jay Fineberg, Elsa Bayart |
| المساهمون: | Racah Institute of Physics, The Hebrew University of Jerusalem (HUJ), Laboratoire de Physique de l'ENS Lyon (Phys-ENS), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Centre National de la Recherche Scientifique (CNRS), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL) |
| المصدر: | Annual Review of Condensed Matter Physics Annual Review of Condensed Matter Physics, Annual Reviews 2019, 10 (1), pp.253-273. ⟨10.1146/annurev-conmatphys-031218-013327⟩ Annual Review of Condensed Matter Physics, 2019, 10 (1), pp.253-273. ⟨10.1146/annurev-conmatphys-031218-013327⟩ |
| بيانات النشر: | HAL CCSD, 2019. |
| سنة النشر: | 2019 |
| مصطلحات موضوعية: | 010504 meteorology & atmospheric sciences, [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph], friction, Fracture mechanics, Mechanics, Condensed Matter Physics, 01 natural sciences, Physics::Geophysics, rupture fronts, [PHYS.MECA.MEMA]Physics [physics]/Mechanics [physics]/Mechanics of materials [physics.class-ph], Shear (geology), fracture mechanics, 0103 physical sciences, General Materials Science, 010306 general physics, [PHYS.COND.CM-SCM]Physics [physics]/Condensed Matter [cond-mat]/Soft Condensed Matter [cond-mat.soft], Geology, Brittle fracture, 0105 earth and related environmental sciences |
| الوصف: | International audience; Contacting bodies subjected to sufficiently large applied shear will undergo frictional sliding. The onset of this motion is mediated by dynamically propagating fronts, akin to earthquakes, that rupture the discrete contacts that form the interface separating the bodies. Macroscopic motion commences only after these ruptures have traversed the entire interface. Comparison of measured rupture dynamics with the detailed predictions of fracture mechanics reveals that the propagation dynamics, dissipative properties, radiation, and arrest of these "laboratory earthquakes" are in excellent quantitative agreement with the predictions of the theory of brittle fracture. Thus, interface fracture replaces the idea of a characteristic static friction coefficient as a description of the onset of friction. This fracture-based description of friction additionally provides a fundamental description of earthquake dynamics and arrest. 253 Review in Advance first posted on December 10, 2018. (Changes may still occur before final publication. |
| اللغة: | English |
| تدمد: | 1947-5454 1947-5462 |
| URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8932e50f9272b990eee469efca5fcc5e https://hal.archives-ouvertes.fr/hal-03026026 |
| حقوق: | OPEN |
| رقم الأكسشن: | edsair.doi.dedup.....8932e50f9272b990eee469efca5fcc5e |
| قاعدة البيانات: | OpenAIRE |
| تدمد: | 19475454 19475462 |
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