Author:
Xu Guanghai,Mates T. E.,Clarke D. R.,Ma Qing,Fujimoto Harry
Abstract
AbstractThe SiO2/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 SiO2/TiN interface using Imaging Secondary Ion Mass Spectroscopy (SIMS) after immersion in water containing radioactive tracers, 2D and 18O. Analysis of images formed using 2D and 18O revealed that both diffuse along the interface with a diffusivity of (6 ±2)×10−13 cm2/sec, a value about 104 times faster than the bulk diffusion in the SiO2 dielectric.
Publisher
Springer Science and Business Media LLC
Cited by
2 articles.
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1. Interface Fracture;Annual Review of Materials Research;2003-08
2. Atomic mass spectrometry;Journal of Analytical Atomic Spectrometry;2000