Abstract
Although the science of fracture mechanics has had considerable success in using continuum mechanics to predict fracture stress distributions and the approximate fracture path in groups of identical samples, a great amount of uncertainty is always present in the behavior of a single sample. It has been generally accepted that this lack of predictability is the result of an incomplete knowledge of the state of flaws on a sample surface coupled with limitations in fracture mechanics models. In the simulation of fracture in amorphous silica, the stress-strain behavior during fracture and the structure of the fracture paths are ultimately dependent on individual atomic motions and all aspects of the structure. This is a hallmark of chaotic behavior, indicating that the characteristics of fracture in materials can be predicted only in general terms, regardless of the precision used to define the initial configurations.
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