Origin of mist and hackle patterns in brittle fracture

A. Rabinovitch, G. Belizovsky, D. Bahat

Research output: Contribution to journalArticlepeer-review

17 Scopus citations

Abstract

A velocity growth rule for secondary cracks in brittle materials is suggested. This rule agrees with the assumption that the mist-hackle transition originates from the inability of the primary crack to overtake secondary cracks. The geometrical shapes of the secondary cracks in the mist and hackle zones change gradually with distance from the fracture origin. The velocity rule is used to calculate these shapes across the mist and at the beginning of the hackle zone. These calculations are shown to be in agreement with experimental results.

Original languageEnglish
Pages (from-to)14968-14974
Number of pages7
JournalPhysical Review B - Condensed Matter and Materials Physics
Volume61
Issue number22
DOIs
StatePublished - 1 Jan 2000

Fingerprint

Dive into the research topics of 'Origin of mist and hackle patterns in brittle fracture'. Together they form a unique fingerprint.

Cite this