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  1. 400 金属材料研究所
  2. 東北大学研究所報告. A集, 物理学・化学・冶金学

Microstructures of Deformation and Fracture of Cementite in Pearlitic Carbon Steels Strained at Various Temperatures(Metallurgy)

http://hdl.handle.net/10097/28051
http://hdl.handle.net/10097/28051
ef81bac7-e4e7-4290-8dec-202a51a34c32
名前 / ファイル ライセンス アクション
KJ00004394163.pdf KJ00004394163.pdf (155.6 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-05-02
タイトル
タイトル Microstructures of Deformation and Fracture of Cementite in Pearlitic Carbon Steels Strained at Various Temperatures(Metallurgy)
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ departmental bulletin paper
著者 INOUE, Akihisa

× INOUE, Akihisa

INOUE, Akihisa

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OGURA, Tsugio

× OGURA, Tsugio

OGURA, Tsugio

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MASUMOTO, Tsuyoshi

× MASUMOTO, Tsuyoshi

MASUMOTO, Tsuyoshi

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抄録
内容記述タイプ Abstract
内容記述 In order to make clear the effect of temperature on deformation and fracture of cementite in steels, observations by transmission electron microscopy were made on cementite in carbon steels strained in tension at various temperatures ranging from -196 to 700℃. Hardly any plastic deformation of cementite was detected at -196 and -78℃. It was confirmed that above room temperature cementite in steel can deform due to dislocation slip and that the deformation becomes easier as the temperature increases. Slip in cementite at room temperature and at 300℃ seems to be confined to only (100) or (001). Dislocations observed at room temperature and at 300℃ were mostly isolated and straight. Above 400℃ (100), (010), (001), and some {110} planes are all operative slip planes. Dislocation loops, dipoles, cusps, and networks were frequently found. These observations indicate that double slipping and the interaction of dislocations can occur and that the deformability of cementite above 400℃ is very large. An appreciable degree of dynamic recovery was detected above 500℃. The fracture of cementite at -196 and -78℃ occurred in a cleavage manner along some crystallographic planes such as (110), (100) or (210) . Above room temperature fracture occurred along an activated slip plane and was preceded by some amount of slip on that plane. Above 400℃ cementite fracture, caused by joining of voids, formed along an activated slip plane was frequently observed.
書誌情報 Science reports of the Research Institutes, Tohoku University. Ser. A, Physics, chemistry and metallurgy

巻 27, p. 87-88, 発行日 1979
ISSN
収録物識別子タイプ ISSN
収録物識別子 00408808
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00836167
フォーマット
内容記述タイプ Other
内容記述 application/pdf
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
出版者
出版者 Tohoku University
資源タイプ
内容記述タイプ Other
内容記述 紀要類(bulletin)
登録日
日付 2008-05-02
日付タイプ Created
公開日(投稿完了日)
日付 2008-05-02
日付タイプ Created
発行日
日付 1979
日付タイプ Created
フォーマット
内容記述タイプ Other
内容記述 155559 bytes
更新日
日付 2010-01-27
日付タイプ Created
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