In contrast to Chapter 6.3, where the degradation of the drain current is directly fit by (6.1), the drain current is now first converted to an approximate threshold voltage shift using the simple OTF1 relation derived in Appendix A.1
Note that is obtained at stress-level with a delay and is thus not equal to [40], resulting in an offset of the relative degradation. Also, the conversion (6.3) ignores any potential degradation in the mobility and is thus affected by an as-of-yet unknown error [108, 41]. The threshold voltage is extracted at , which yields . Then is fit by
| (6.4) |
In order to circumvent issues with the logarithmic fit caused by offset data due to the uncertainty in , the parameter is included. Besides, it is tried to fit the data to a power-law of the form
| (6.5) |
Again, the parameter is introduced to account for the offset in .
Interestingly, it turns out that the logarithmic fit (6.4) is always possible, while the power-law fit (6.5) produces reasonable results for high temperatures and high only. In that high-stress regime, power-law exponents around are obtained. For weaker stresses, the exponent in (6.5) tends towards zero, which corresponds to a first-order Taylor expansion of (6.5) on a logarithmic scale. As such, in this regime the power-law fit (6.5) becomes equivalent to the logarithmic fit (6.4).
This behavior is illustrated in Fig. 6.15 and Fig. 6.16. The data obtained from the harshest stress conditions (, , and ) gives a stable fit with . For the other extreme case (, , and ) the fitting algorithm gives an exponent of practically zero. For the case of the non-converging exponent the logarithmic and power-law fits coincide.
Consequently, the power-law fit only makes sense for high temperatures and/or high , as displayed in Fig. 6.17. There, the extracted for short-term stress is roughly one third of the often reported of the long-term behavior.