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Effect of microstructure on deformation of polycrystalline MgO

Effect of microstructure on deformation of polycrystalline MgO
Effect of microstructure on deformation of polycrystalline MgO
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.
0002-7820
240-246
Langdon, Terence G.
86e69b4f-e16d-4830-bf8a-5a9c11f0de86
Pask, Joseph A.
de6df49a-d254-4395-a511-9e52782c9b41
Langdon, Terence G.
86e69b4f-e16d-4830-bf8a-5a9c11f0de86
Pask, Joseph A.
de6df49a-d254-4395-a511-9e52782c9b41

Langdon, Terence G. and Pask, Joseph A. (1971) Effect of microstructure on deformation of polycrystalline MgO. Journal of the American Ceramic Society, 54 (5), 240-246. (doi:10.1111/j.1151-2916.1971.tb12280.x).

Record type: Article

Abstract

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.

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More information

Accepted/In Press date: 1967
Published date: May 1971

Identifiers

Local EPrints ID: 489069
URI: http://eprints.soton.ac.uk/id/eprint/489069
ISSN: 0002-7820
PURE UUID: bf31add6-e084-4753-b4a7-8813fdd5e393
ORCID for Terence G. Langdon: ORCID iD orcid.org/0000-0003-3541-9250

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Date deposited: 12 Apr 2024 16:32
Last modified: 13 Apr 2024 01:38

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Author: Joseph A. Pask

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