Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface
The fracture behaviour of a specific material, a semi-crystalline biobased polymer, was here studied. Dynamic fracture tests on strip band specimens were carried out. Fracture surfaces were observed at different scales by optical and electron microscopy to describe cracking scenarios. Crack initiati...
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2021-01-01
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doaj-3ed300aca20c45dca05c71a54bdfc2fd2021-09-21T15:17:01ZengEDP SciencesEPJ Web of Conferences2100-014X2021-01-012500601210.1051/epjconf/202125006012epjconf_dymat2021_06012Dynamice fracture in a semicristalline polymer: an analysis of the fracture surfaceKopp Jean-Benoît0Girardot Jérémie1Arts et Metiers Institute of Technology, Univ. of Bordeaux, CNRS, Bordeaux INP, INRAE, HESAM Université, I2M BordeauxArts et Metiers Institute of Technology, Univ. of Bordeaux, CNRS, Bordeaux INP, INRAE, HESAM Université, I2M BordeauxThe fracture behaviour of a specific material, a semi-crystalline biobased polymer, was here studied. Dynamic fracture tests on strip band specimens were carried out. Fracture surfaces were observed at different scales by optical and electron microscopy to describe cracking scenarios. Crack initiation, propagation and arrest zones were described. Three distinct zones are highlighted in the initiation and propagation zone: a zone with conical markings, a mist zone and a hackle zone. The conical mark zone shows a variation in the size and density of the conical marks along the propagation path. This is synonymous with local speed variation. Microcracks at the origin of the conical marks in the initiation zone seem to develop from the nucleus of the spherulites. In the propagation zone with complex roughness, the direction of the microcracks and their cracking planes are highly variable. Their propagation directions are disturbed by the heterogeneities of the material. They branch or bifurcate at the level of the spherulites. In the arrest zone, the microcracks developed upstream continue to propagate in different directions. The surface created is increasingly smoother as the energy release rate decreases. It is shown that the local velocity of the crack varies in contrast to the macroscopic speed.https://www.epj-conferences.org/articles/epjconf/pdf/2021/04/epjconf_dymat2021_06012.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Kopp Jean-Benoît Girardot Jérémie |
spellingShingle |
Kopp Jean-Benoît Girardot Jérémie Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface EPJ Web of Conferences |
author_facet |
Kopp Jean-Benoît Girardot Jérémie |
author_sort |
Kopp Jean-Benoît |
title |
Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
title_short |
Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
title_full |
Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
title_fullStr |
Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
title_full_unstemmed |
Dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
title_sort |
dynamice fracture in a semicristalline polymer: an analysis of the fracture surface |
publisher |
EDP Sciences |
series |
EPJ Web of Conferences |
issn |
2100-014X |
publishDate |
2021-01-01 |
description |
The fracture behaviour of a specific material, a semi-crystalline biobased polymer, was here studied. Dynamic fracture tests on strip band specimens were carried out. Fracture surfaces were observed at different scales by optical and electron microscopy to describe cracking scenarios. Crack initiation, propagation and arrest zones were described. Three distinct zones are highlighted in the initiation and propagation zone: a zone with conical markings, a mist zone and a hackle zone. The conical mark zone shows a variation in the size and density of the conical marks along the propagation path. This is synonymous with local speed variation. Microcracks at the origin of the conical marks in the initiation zone seem to develop from the nucleus of the spherulites. In the propagation zone with complex roughness, the direction of the microcracks and their cracking planes are highly variable. Their propagation directions are disturbed by the heterogeneities of the material. They branch or bifurcate at the level of the spherulites. In the arrest zone, the microcracks developed upstream continue to propagate in different directions. The surface created is increasingly smoother as the energy release rate decreases. It is shown that the local velocity of the crack varies in contrast to the macroscopic speed. |
url |
https://www.epj-conferences.org/articles/epjconf/pdf/2021/04/epjconf_dymat2021_06012.pdf |
work_keys_str_mv |
AT koppjeanbenoit dynamicefractureinasemicristallinepolymerananalysisofthefracturesurface AT girardotjeremie dynamicefractureinasemicristallinepolymerananalysisofthefracturesurface |
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