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論文

引張負荷下で単一すべり系が活動するアルミニウム単結晶の延性損傷評価

柴野 純一*; 梶原 堅太郎*; 塚本 拓也*; 河合 紘和*; 三浦 節男*; Zhang, S.*; 菖蒲 敬久

材料, 63(7), p.533 - 538, 2014/07

SPring-8、BL28B2からの白色X線を利用し、アルミニウム単結晶の延性破壊進展挙動の検証を実施した。その結果、以下の2点を明らかにした。(1)延性損傷進展に伴い発生した転移セルの回転は、水辺面内に比べ垂直面内で大きく、特に負荷ひずみ0.05のときのノッチ近傍の角度変化が大変大きく、これは引張負荷によるAl(111)面のすべり活動が転位セルの生成と回転に大きな影響を及ぼしている。(2)転位密度は材料の延性損傷が進むことで全体に増加したが、ノッチ近傍では相対的に低く、これは延性損傷進展によるひずみエネルギーの解放の影響によるものである可能性を見出した。

論文

Evaluation of ductile damage progress of aluminum single crystal with prior activity of single slip system under tensile loading by using synchrotron white X-ray

柴野 純一*; 梶原 堅太郎*; 塚本 拓也*; 河合 紘和*; 三浦 節男*; Zhang, S.*; 菖蒲 敬久; 小林 道明*

Materials Science Forum, 777, p.176 - 181, 2014/02

 被引用回数:1 パーセンタイル:51.86(Materials Science, Multidisciplinary)

A ductile damage progress of an aluminum single crystal with the prior activity of the single slip system under tensile loading was verified by a profile analysis using white X-ray obtained in BL28B2 beam line of SPring-8. In this study, the aluminum single crystal of the purity 6N was used as a specimen prepared in I-type geometry for tensile test. In profile analysis, an instrumental function was defined in consideration both of a divergence by a slit and a response function peculiar to the energy dispersive method. The Gauss component of integral breadth related to non-uniform strain and the Cauchy component of integral breadth related to crystallite size were determined by eliminating the broadening by the instrumental function from the diffraction profile of white X-ray. As a result, the characteristics of ductile damage progress near the notch of the aluminum single crystal were inspected from the distribution of both non-uniform strain and dislocation density.

口頭

The 2024 Noto Peninsula Earthquake and the million year preceding it

Malatesta, L.*; Weiss, N.-M.*; 石村 大輔*; Gailleton, B.*; 西村 卓也*; 高橋 直也*; 塚本 すみ子*; 小松 哲也; 岩佐 佳哉*; 末岡 茂; et al.

no journal, , 

本発表では、令和6年能登半島地震において発生した沿岸部の地形変化、特に隆起分布について着目し、それらと更新世の海成段丘群の高度分布との比較から、過去約100万年間の能登半島におけるテクトニクスや変動地形について考察した。

口頭

The Mw 7.5 Noto Peninsula earthquake illuminates a past shift in tectonic plate boundaries across Central Japan

Malatesta, L.*; Weiss, N.-M.*; 塚本 すみ子*; 末岡 茂; 石村 大輔*; Gailleton, B.*; 西村 卓也*; 高橋 直也*; 片岡 香子*; 小松 哲也; et al.

no journal, , 

On January 1st, 2024, the Mw 7.5 Noto Peninsula earthquake ruptured on a series of coastal offshore reverse faults in the back arc of central Japan. Recent Holocene terraces mapped along the northern coast, where coseismic uplift was greatest on January 1st 2024, suggest that they may be attributable to similar past ruptures. The Peninsula itself is remarkable for its 4767 unique terraces ranging in age from Holocene to 1.02 Ma. We digitized all terraces and recorded the elevation of their landward edge, and derived a rock uplift rate for each based on their age and the corresponding original sea level. The southeast-tilting crustal deformation recorded by the terraces associated with the last two interglacial high stands strongly resembles that caused by the Mw 7.5 earthquake. Older terraces, on the contrary all record a spatially uniform rate of uplift across the Peninsula. We conclude that the faults that caused the most recent earthquake became the dominant structures on the Peninsula over a quarter million year ago. This onset of seismogenic activity informs us about the regional plate tectonics of the area. The boundary separating Eurasia from the North American Plate currently runs south of the Noto Peninsula, linking the cities of Niigata and Kobe along a northeast-striking Tectonic Zone (NKTZ). Immediately east of the Peninsula lies another north-striking Tectonic Line, from Itoigawa to Shizuoka (ISTL). East of the ISTL and north of the NKTZ is the Island of Sado, which terraces also suggest a change in deformation with strong southeast tilting synchronous and similar to Noto. Together, Noto and Sado act as a railroad switch, indicating which of the ISTL or the NKTZ is the active plate boundary. When the ISTL is active, the sites are on different tectonic plates and evolve differently. When the NKTZ takes over, Sado Island becomes part of Eurasia and is more likely to evolve similarly to the Noto Peninsula.

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