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Interfacial diffusivity of moisture along a SiO_2/TiN interface measured using imaging secondary ion mass spectroscopy (SIMS)

机译:沿SiO_2 / TiN界面的水分界面扩散率,使用成像二次离子质谱法(SIMS)测量

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The SiO_2/TiN interface is prone to sub-critical decohesion by crack extension along the interface when exposed to moisture. As with conventional sub-critical crack growth in bulk silica, the rate of decohesion is dependent on both the relative humidity and the strain energy release rate. One of the unusual observations we have noted is that the decohesion velocity of narrow strips is highly sensitive to the exposure time in the humid environment, suggesting that the moisture diffuses into the interface ahead of the propagating decohesion crack, causing a form of hydrolytic weakening of the interface. In seeking to establish the origin of this behavior, we report measurements of moisture diffusion along the SiO_2/TiN interface using Imaging Secondary Ion Mass Spectroscopy (SIMS) after immersion in water containing radioactive tracers, ~2D and ~(18)O. Analysis of images formed using 2~D and ~(18)O revealed that both diffuse along the interface with a diffusivity of (6+-2)x10~9-13) cm~2/sec, a value about 10~4 times faster than the bulk diffusion in the SiO_2 dielectric.
机译:当暴露于湿气中时,SiO_2 / TiN界面容易因沿界面的裂纹扩展而发生亚临界脱粘。与块状二氧化硅中常规的亚临界裂纹增长一样,内聚速率取决于相对湿度和应变能释放速率。我们注意到的异常观察之一是,窄条的脱粘速度对在潮湿环境中的暴露时间高度敏感,这表明水分在传播的脱粘裂纹之前扩散到界面中,从而导致水合形式的水解减弱。接口。为了寻求确定这种行为的根源,我们报告了在浸入含有放射性示踪剂,〜2D和〜(18)O的水中后,使用成像二次离子质谱(SIMS)对沿着SiO_2 / TiN界面的水分扩散进行的测量。对使用2〜D和〜(18)O形成的图像进行分析后发现,两者均沿界面扩散,扩散率为(6 + -2)x10〜9-13)cm〜2 / sec,约为10〜4倍快于SiO_2电介质中的体扩散。

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