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In Situ Erosion Study of Kapton Using Novel Hyperthermal Oxygen Atom Source

机译:基于新型超热氧原子源的Kapton原位侵蚀研究

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摘要

A novel hyperthermal oxygen atom source has been used to perform in situ erosion of Kapton surfaces at room temperature, and these surfaces have been examined using x-ray photoelectron spectroscopy before and after exposure to different fluences of oxygen atoms and then after exposure to air. The data indicate that the initial attack site is the carbonyl portion of the Kapton by reaction with atomic oxygen to form carbon dioxide, which desorbs. The oxygen-to-carbon-atom ratio decreases from 0.23 to 0.11 during a 24-h exposure to a hyperthermal oxygen-atom flux of about 1.4 X 10~(14) atoms/cm~2-s. Following the 24-h oxygen-atom exposure, the sample was exposed to air for 3 h. The oxygen, nitrogen, and carbon concentrations return to values similar to those obtained before the oxygen-atom exposure due to reaction with molecular oxygen in the air. Previous data from space and ground simulations indicate an increase in the surface oxygen content with exposure to atomic oxygen and then air before analysis. The results obtained demonstrate that it is necessary to examine the chemical effects of oxygen-atom degradation of Kapton without air exposure before surface characterization.
机译:一种新型的超热氧原子源已被用于在室温下对Kapton表面进行原位侵蚀,并且在暴露于不同浓度的氧原子之前和之后以及暴露于空气之后,使用X射线光电子能谱检查了这些表面。数据表明,最初的攻击部位是Kapton的羰基部分,通过与原子氧反应形成二氧化碳,从而解吸。在暴露于约1.4 X 10~(14)个原子/cm~2-s的超热氧原子通量24小时期间,氧-碳-原子比从0.23降低到0.11。在氧原子暴露 24 小时后,将样品暴露在空气中 3 小时。由于与空气中的分子氧反应,氧、氮和碳浓度恢复到与氧原子暴露前相似的值。先前来自空间和地面模拟的数据表明,在分析之前,暴露于原子氧和空气中,表面氧含量会增加。所获得的结果表明,在表面表征之前,有必要检查Kapton在不暴露空气的情况下氧原子降解的化学效应。

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