corner
corner

Phys. Rev. B 61, 14968–14974 (2000)

Origin of mist and hackle patterns in brittle fracture

Download: PDF (363 kB) Buy this article Export: BibTeX or EndNote (RIS)

A. Rabinovitch and G. Belizovsky
Department of Physics, Ben-Gurion University, Beer Sheva 84105, Israel

D. Bahat
Department of Geology & Environmental Sciences, The Deichmann, Rock Mechanics Laboratory of the Negev, Ben Gurion University, Beer Sheva 84105, Israel

Received 8 April 1999; revised 29 November 1999; published in the issue dated 1 June 2000

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.

© 2000 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevB.61.14968
DOI:
10.1103/PhysRevB.61.14968
PACS:
62.20.Mk