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Structural Characterization of Iron Meteorites through Neutron Tomography

机译:中子层析成像技术对铁陨石的结构表征

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In this communication, we demonstrate the use of neutron tomography for the structural characterization of iron meteorites. These materials prevalently consist of metallic iron with variable nickel content. Their study and classification is traditionally based on chemical and structural analysis. The latter requires cutting, polishing and chemical etching of large slabs of the sample in order to determine the average width of the largest kamacite lamellae. Although this approach is useful to infer the genetical history of these meteorites, it is not applicable to small or precious samples. On the base of different attenuation coefficient of cold neutrons for nickel and iron, neutron tomography allows the reconstruction of the Ni-rich (taenite) and Ni-poor (kamacite) metallic phases. Therefore, the measure of the average width of the largest kamacite lamellae could be determined in a non-destructive way. Furthermore, the size, shape, and spatial correlation between kamacite and taenite crystals were obtained more efficiently and accurately than via metallographic investigation.
机译:在本通讯中,我们演示了使用中子层析成像技术对铁陨石进行结构表征。这些材料主要由镍含量可变的金属铁组成。他们的研究和分类传统上是基于化学和结构分析。后者需要对样品的大块进行切割,抛光和化学蚀刻,以便确定最大的滑石片的平均宽度。尽管此方法可用于推断这些陨石的遗传历史,但不适用于小型或珍贵样品。基于冷中子对镍和铁的不同衰减系数,中子断层扫描可以重建富镍(钛铁矿)和贫镍(钾长石)金属相。因此,可以以一种非破坏性的方式来确定最大的金刚石薄片的平均宽度的量度。此外,与通过金相研究相比,更有效,更准确地获得了钾长石和石晶体之间的尺寸,形状和空间相关性。

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