Slip System Partitioning as a Possible Mechanism for Ultrafine Grain Formation in Fe-3%Si Bicrystals
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概要
- 論文の詳細を見る
An Fe–3%Si bicrystal was deformed in compression to a strain of 0.9 at ambient temperature. In the interior of deformation bands, characteristic band structures with high orientation gradients and low and high angle boundaries were formed during straining. Furthermore, isolated ultrafine grains were found in the matrix of the deformation bands. The morphology and crystallography of the ultrafine grains indicate that they are caused by slip system partitioning, i.e. local activity of a highly stressed slip system that is different from the active slip system in the surrounding crystal volume.
- 社団法人 日本鉄鋼協会の論文
- 2008-08-15
著者
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TSUZAKI Kaneaki
Structural Metals Center, National Institute for Materials Science
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Dorner Dorothee
Structural Metals Center National Institute For Materials Science
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ADACHI Yoshitaka
Structural Metals Center, National Institute for Materials Science
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Tsuzaki Kaneaki
Structural Metals Center National Inst. For Materials Sci.
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Tsuzaki Kaneaki
Steel Research Center National Inst. For Materials Science (nims)
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Tsuzaki Kaneaki
Structural Metals Center National Institute For Materials Science
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Tsuzaki Kaneaki
Doctoral Program In Materials Science And Engineering University Of Tsukuba
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Tsuzaki Kaneaki
Steel Research Center National Institute For Materials Science
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Tsuzaki Kaneaki
National Institute For Materials Science Tsukuba
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Tsuzaki Kaneaki
Frontier Research Center For Structural Materials National Institute For Materials Science
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Tsuzaki Kaneaki
Frontier Research Center For Structural Materials National Research Institute For Metals
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Adachi Yoshitaka
Structural Metals Center National Institute For Materials Science
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Tsuzaki Kaneaki
Structural Materials Unit, Research Center for Strategic Materials, National Institute for Materials Science (NIMS)
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- PREFACE
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