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{110} Slip with {112} slip traces in bcc Tungsten

机译:在密件抄送钨丝中{110}带有{112}滑动痕迹的滑动

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摘要

While propagation of dislocations in body centered cubic metals at low temperature is understood in terms of elementary steps on {110} planes, slip traces correspond often with other crystallographic or non-crystallographic planes. In the past, characterization of slip was limited to post-mortem electron microscopy and slip trace analysis on the sample surface. Here with in-situ Laue diffraction experiments during micro-compression we demonstrate that when two {110} planes containing the same slip direction experience the same resolved shear stress, sharp slip traces are observed on a {112} plane. When however the {110} planes are slightly differently stressed, macroscopic strain is measured on the individual planes and collective cross-slip is used to fulfill mechanical boundary conditions, resulting in a zig-zag or broad slip trace on the sample surface. We anticipate that such dynamics can occur in polycrystalline metals due to local inhomogeneous stress distributions and can cause unusual slip transfer among grains.
机译:尽管可以根据{110}平面上的基本阶跃来理解低温下位错在体心立方金属中的传播,但滑移痕迹通常对应于其他晶体学或非晶体学平面。过去,滑移的特征仅限于事后电子显微镜检查和样品表面滑移痕迹分析。在这里,通过微压缩过程中的原位Laue衍射实验,我们证明了当两个包含相同滑动方向的{110}平面经历相同的解析切应力时,在{112}平面上会观察到清晰的滑动轨迹。但是,当{110}平面受到的应力略有不同时,将在各个平面上测量宏观应变,并使用集体交叉滑动来满足机械边界条件,从而在样品表面产生曲折或较大的滑动轨迹。我们预计,由于局部不均匀的应力分布,这种动力学会在多晶金属中发生,并可能导致晶粒间的异常滑动转移。

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