Abstract:
MOS capacitance measurements are very fundamental characterization methods for MOS and FET structures. This paper discusses the effects of a finite bias sweep rate on qua...Show MoreMetadata
Abstract:
MOS capacitance measurements are very fundamental characterization methods for MOS and FET structures. This paper discusses the effects of a finite bias sweep rate on quasi-static and high-frequency (HF) capacitance-voltage (C-V) measurements. As typically measured, a finite sweep rate causes the transition region from inversion to depletion of the quasistatic C-V curve to be shifted by several tenths of a volt along the bias voltage axis. The physical origin of this shift as well as a model to account for the effect is discussed. In order to understand quasi-static MOS C-V measurements and to extract fundamental parameters such as substrate doping density and polysilicon depletion effects from C-V measurements, these bias sweep rate effects must be understood and taken into account.
Published in: IEEE Transactions on Electron Devices ( Volume: 44, Issue: 6, June 1997)
DOI: 10.1109/16.585558
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- IEEE Keywords
- Index Terms
- Sweep Rate ,
- Quasi-static Capacitance ,
- Bias Voltage ,
- polySia ,
- Doping Density ,
- Solid Line ,
- Electron Density ,
- Surface Charge ,
- Negative Voltage ,
- Depletion Region ,
- Edge Region ,
- Theoretical Curves ,
- Poisson Equation ,
- Electron Injection ,
- Forward Bias ,
- Gate Bias ,
- High-frequency Data ,
- Constant Bias ,
- Inversion Layer ,
- Strong Inversion
Keywords assist with retrieval of results and provide a means to discovering other relevant content. Learn more.
- IEEE Keywords
- Index Terms
- Sweep Rate ,
- Quasi-static Capacitance ,
- Bias Voltage ,
- polySia ,
- Doping Density ,
- Solid Line ,
- Electron Density ,
- Surface Charge ,
- Negative Voltage ,
- Depletion Region ,
- Edge Region ,
- Theoretical Curves ,
- Poisson Equation ,
- Electron Injection ,
- Forward Bias ,
- Gate Bias ,
- High-frequency Data ,
- Constant Bias ,
- Inversion Layer ,
- Strong Inversion