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• W4253085688 abstract "This chapter describes fragmentation. Upon the sudden introduction of a sufficient strong external energy source, an object can break into smaller fragments, whose distribution is the primary observational evidence for the nature of the breakup process. For brittle materials, breaking occurs when the applied stress exceeds the fracture stress, which is often close to the point where linear response breaks down. According to the Griffith theory, the magnitude of this fracture stress depends on the distribution of preexisting flaws, or cracks, in the material. Owing to the concentration of stress at a crack tip, the fracture stress of a flawed material is typically much smaller than the stress needed to break atomic bonds. There is considerable well-documented data for the distribution of fragment sizes in a variety of realizations of instantaneous fracture, ranging from the over-compression of glass spheres to high-velocity impacts of small projectiles onto fixed rock targets. On the basis of these experiments, the possible outcomes for the fracture event are often classified into three broad regimes of behavior depending on the energy input and on the geometrical features of the experiment. While the terminology is not universal, the three regimes may be written as (1) abrasion (or surface erosion), (2) cleavage (transition behavior), and (3) destructive breaking (or shattering)." @default.
• W4253085688 created "2022-05-12" @default.
• W4253085688 creator A5011256345 @default.
• W4253085688 date "1990-01-01" @default.
• W4253085688 modified "2023-09-26" @default.
• W4253085688 title "Fragmentation" @default.
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• W4253085688 doi "https://doi.org/10.1016/b978-0-444-88551-7.50021-5" @default.
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