Brittle-quasibrittle transition in dynamic fracture: an energetic signature

Autor: Julien Scheibert, F. Celarie, Claudia Guerra, Davy Dalmas, Daniel Bonamy
Přispěvatelé: Service de Physique et de Chimie des Surfaces et Interfaces (SPCSI), Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Surface du Verre et Interfaces (SVI), Centre National de la Recherche Scientifique (CNRS), Facultad de Ingeniería Mecánica y Eléctrica, Universidad Autonoma de Nuevo Leon [Mexique] (UANL)
Rok vydání: 2009
Předmět:
Materials science
fracture energy
Nucleation
General Physics and Astronomy
FOS: Physical sciences
02 engineering and technology
Physics - Classical Physics
[SPI.MECA.SOLID]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Solid mechanics [physics.class-ph]
01 natural sciences
Instability
amorphous materials
Physics::Geophysics
Fracture toughness
Brittleness
brittle
0103 physical sciences
[PHYS.MECA.SOLID]Physics [physics]/Mechanics [physics]/Solid mechanics [physics.class-ph]
Composite material
010306 general physics
roughness
Strain energy release rate
Condensed Matter - Materials Science
dynamic fracture
Classical Physics (physics.class-ph)
Materials Science (cond-mat.mtrl-sci)
Fracture mechanics
021001 nanoscience & nanotechnology
Critical ionization velocity
PMMA
Fracture (geology)
[PHYS.COND.CM-MS]Physics [physics]/Condensed Matter [cond-mat]/Materials Science [cond-mat.mtrl-sci]
0210 nano-technology
62.20.M
46.50.+a
61.43.-j
fracture surface
Zdroj: Physical Review Letters
Physical Review Letters, 2010, 104 (4), pp.045501. ⟨10.1103/PhysRevLett.104.045501⟩
Physical Review Letters, American Physical Society, 2010, 104 (4), pp.045501. ⟨10.1103/PhysRevLett.104.045501⟩
ISSN: 1079-7114
0031-9007
DOI: 10.1103/PhysRevLett.104.045501⟩
Popis: Dynamic fracture experiments were performed in PMMA over a wide range of velocities and reveal that the fracture energy exhibits an abrupt 3-folds increase from its value at crack initiation at a well-defined critical velocity, below the one associated to the onset of micro-branching instability. This transition is associated with the appearance of conics patterns on fracture surfaces that, in many materials, are the signature of damage spreading through the nucleation and growth of microcracks. A simple model allows to relate both the energetic and fractographic measurements. These results suggest that dynamic fracture at low velocities in amorphous materials is controlled by the brittle/quasi-brittle transition studied here.
5 pages, 4 figures, published version, Article highlighted in Physical Review Focus (February 12th, 2010)
Databáze: OpenAIRE