报告地质材料原子探针分析的最佳实践

T. Blum, J. Darling, T. Kelly, D. Larson, D. Moser, A. Pérez-Huerta, T. Prosa, S. Reddy, D. Reinhard, D. Saxey, R. Ulfig, J. Valley
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引用次数: 28

摘要

最近的工作已经建立了原子探针断层扫描(APT)作为一个独特的工具,在地球科学审问材料化学在纳米尺度。在APT中,将端形半径为50 - 100nm的针状试样置于高压下,并通过施加定时电压脉冲(用于导电材料)或激光脉冲(用于半导体和绝缘体)将其组成原子进行场蒸发。电压偏置和小曲率半径产生了一个大的电场,该电场位于针状试样的端面周围,并从端面发散出来;蒸发的离子被局部电场加速,导致来自试样表面不同位置的离子产生不同的轨迹。位置敏感探测器记录了报告地质材料原子探针分析的最佳实践的击中位置
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Best Practices for Reporting Atom Probe Analysis of Geological Materials
Recent work has established atom probe tomography (APT) as a unique tool within the geosciences for interrogat­ ing material chemistry at the nanoscale. In APT, a needle‐ shaped specimen with an end‐form radius on the order of 50–100 nm is held at high voltage, and constituent atoms are field evaporated through application of a timed voltage pulse (for conductive materials) or laser pulse (for semicon­ ductors and insulators). The voltage bias and small radius of curvature produce a large electric field that is localized around, and diverging from, the end surface of the needle‐ shaped specimen; evaporated ions are accelerated by the local electric field, leading to divergent trajectories for ions originating from different positions on the specimen surface. A position‐sensitive detector records both the hit position of Best Practices for Reporting Atom Probe Analysis of Geological Materials
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