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| 1 | Unexpected creep behavior in a rejuvenated metallic glass显示文摘Rejuvenation,bringing metallic glasses(MGs)to the younger and higher energy states,provides an alternative avenue to explore the interplay between the property and microstructures of MGs.In this study,the creep behavior of the Zr_(69.5)Cu_(12)Ni_(11)Al_(7.5)MGs was experimentally examined by controlling the energy state in terms of structural rejuvenation and thermal annealing.It is found that compared to the as-cast counterpart,the annealed MG at a lower energy state exhibits a higher hardness,a smaller displacement,and a lower creep rate due to the decreased free volume and the inhibited activation of the shear transformation zone.Conversely,the rejuvenated MG at a high energy state displays lower hardness and increased free volume content,yet it demonstrates superior creep resistance compared to its as-cast counterpart,which deviates from conventional understanding.This unexpected phenomenon occurs as the initial high-content free volume annihilates during creep,and strain hardening takes precedence over strain softening as the prevailing process during creep deformation,leading to a superior creep performance in extremely rejuvenated MGs. | J.P.Wu Y.Lin F.H.Duan Q.Chen H.T.Wang N.Li J.L.Wen J.Pan L.Liu | 2023 | Journal of Materials Science & Technology2023，，32： | 0 |
| 2 | 利用Pms波分裂研究青藏高原东南缘地壳各向异性及变形情况显示文摘通过分析青藏高原东南缘新部署的密集地震台阵的接收函数得到了该区域的地壳各向异性。所测量的接收函数Pms波的分裂时间分布在0.02~0.88s,平均分裂时间为0.28s,这远大于近震S波分裂得到的云南地区上地壳(15km以上)累积的分裂时间,表明研究区地壳各向异性主要来自中下地壳(15km以下)。各次级块体内的Pms波的快波偏振方向与主压应力方向基本一致,在一些大型走滑断裂带附近,如小江断裂带、红河断裂带和澜沧江断裂带,快波偏振方向与断裂带走向基本平行。分裂时间在小江断裂带两侧表现出东侧小,西侧大的特征。在块体内部,由于韧性的中下地壳发生差异运动,从而引起物质沿运动方向排列,产生各向异性。小江断裂带、红河断裂带和澜沧江断裂带附近地壳中分布的低速带、高泊松比和高热流表明断裂带下方可能存在部分熔融,因此在这些深的大走滑断裂带下方的各向异性快波方向沿着断裂带走向分布,主要是由于矿物和熔体在断裂带的走滑运动下发生定向排列引起,说明走滑运动控制着断裂带下方地壳的变形模式。对比Pms波与SKS波分裂模式,本文更倾向于认为研究区地壳与上地幔变形解耦。 | Y.Cai J.P.Wu L.H.Fang W.L.Wang S.Yi 蔡妍(译) 房立华(校) | 2018 | 世界地震译丛2018，49，2： | 0 |
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