Titlebook: Deformation Processes in Minerals, Ceramics and Rocks; David J. Barber,Philip G. Meredith Book 1990 D. J. Barber, P. G. Meredith & contrib

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外星人

BANAL

Single-crack behaviour and crack statistics,f cracks, not necessarily isotropic and homogeneous, more or less interacting, so that the physical properties are those of a complex structure. In such a situation, understanding of the behaviour of a single crack may appear to be irrelevant. It should be looked at rather as a necessary, although n

Concomitant

Fracture of polycrystalline ceramics, critical flaw dimensions increase in size from a scale less than characteristic micro-structure dimensions to a size which encompasses many grain diameters, the resistance to fracture increases, in certain polycrystals, by a factor of 5–10. This increase represents the difference between the fractu

松馳

Compressive brittle fracture and the construction of multi-axial failure maps,these cracks extend to the sample surface, or if they interact with each other so that they grow in an unstable manner, then a macroscopic failure may follow. The initiation and growth of cracks from pores has been considered by Sammis & Ashby (1986): that from small angled cracks is analysed by Nem

frenzy

Brittle-to-ductile transitions in polycrystalline non-metallic materials,teristic strength and brittle or ductile deformation behaviour of crystalline solids is determined by the nature of their atomic bonding and crystal structure. Thus Frost & Ashby (1982) have recognized 21 isomechanical groups in their study of deformation mechanism maps to represent the plasticity a

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