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Effect of Microstructure on Deformation of Polycrystalline MgO
Author(s) -
LANGDON TERENCE G.,
PASK JOSEPH A.
Publication year - 1971
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1151-2916.1971.tb12280.x
Subject(s) - materials science , crystallite , nucleation , microstructure , grain boundary , impurity , plasticity , slip (aerodynamics) , porosity , composite material , metallurgy , grain size , grain boundary strengthening , flow stress , mineralogy , crystallography , chemistry , thermodynamics , physics , organic chemistry
Six types of polycrystalline MgO, one nominally fully dense and the others having porosities of ∼1 to 2%, were tested in compression up to 1400°C. At 1200°C and above, all materials deformed plastically; two of the materials, both porous, also exhibited plastic flow at temperatures down to 800°C, and a third at 1000°C. A qualitative analysis of the microstructures of these materials indicated that the differences in behavior arose primarily because of variations in the size and distribution of pores and in the concentration of impurities at the grain boundaries. It is suggested that the following factors aid plasticity below ∼1200°C: (1) Strong grain boundaries, in the absence of excessive impurities, permit buildup of stress concentrations with consequent nucleation of slip on the {100} system and the extension of slip across the boundaries and (2) clusters of very fine pores within the grains allow some mass accommodation.