Abstract
The statistics of catastrophic slip associated with discontinuous yielding (the Portevin–Le Châtelier effect) is investigated on an Al-Mg alloy. It is shown that a peaked distribution of stress drops changes towards a monotonic one, characterized by a power law with an exponent of 1.1, with increasing temperature and rate of straining. A model describing this behavior is studied, and it is suggested that there exists a formal similarity of the governing equations with those describing instabilities in frictional sliding. The use of discontinuous yielding in a tensile Al-Mg specimen is proposed as a candidate for modeling of earthquake statistics on a crustal fault.
- Received 3 June 1994
DOI:https://doi.org/10.1103/PhysRevLett.74.4758
©1995 American Physical Society