Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5786919 | Russian Geology and Geophysics | 2017 | 6 Pages |
Abstract
The kinetics of fracture in stressed heterogeneous materials is investigated in a differentiated way using the parameter Ît, the interval between single or multiple (cooperative) microfracture events recorded by acoustic emission (AE) responses. The patterns of fracture nucleation and growth, which is a statistic process, are controlled by the heterogeneity of deforming material. There are two important aspects revealed by the study: 1) structural heterogeneity of materials causes uneven distribution of stress in loaded solids and thus creates local zones of microstress and ensuing microfracture in the overstressed zones; 2) AE measurements and microseismic monitoring are applicable to prediction of fracture by locating its source and thus allows predicting related hazard in mines, tunnels, bridges, nuclear-power plants, and other important engineering objects.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
V.S. Kuksenko, Kh.F. Makhmudov,