advsemi_lec8 2013-05-14
TRANSCRIPT
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Advanced
Semiconductor
Devices
Lecture 8
Advanced
Semiconductor
Devices
Lecture 8
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V. Ariel 2013 Advanced Semiconductor Devices Lecture 8
Lecture outline
Review
Three-terminal MOS structure
Quasi-Fermi potential
Regions of operation
Accurate modeling of three-terminal MOS capacitor
Surface potential
Inversion charge
Pinchoff voltage
MOSFET transistor
Charge-sheet model
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Three-terminal MOS structure
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Three-terminal MOS structure energy bands
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Three-terminal MOS structure - charges
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Three-terminal MOS structure regionsof operation
Depletion:
Weak inversion:
Moderate and strong inversion:
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Three-terminal MOS structure basic equations in depletion and inversion
From charge and potential balance
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Three-terminal MOS structure basic equations in depletion and inversion
Define
Then
Depletion weak inversion:
Moderate and strong inversion:
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Surface potential in moderate and stronginversion
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Approximation for surface potential inmoderate and strong inversion
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Approximation for MOS capacitance inmoderate and strong inversion
MOS capacitance in general
MOS capacitance in moderate and strong inversion
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Depletion
Condition for depletion
Approximation for gate voltage in depletion
(similar to two-terminal MOS structure)
Can neglect inversion charge!!!
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MOS Capacitor in depletion
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Weak inversionWeak inversion is defined as
Consequently
Need to pay attention to terms of the order of
Note that inversion charge contribution is mostly importanton the border with moderate inversion
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On the border of moderate inversion
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Charges in depletion and weakinversion
Obtained approximation where the first term is the regular
contribution of the depletion charge while the second term
is due to the inversion charge on the border of moderate
inversion
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Surface potentialin depletion and weak inversion
Approximating for gate voltage for small
Re-arranging
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Depletion and linear approximations of the surface potential
MOS capacitance in depletion andweak inversion
Linear approximation
Depletion approximation
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Need to account for both depletion charge and inversion
charge in weak inversion
MOS Capacitor in depletion andweak inversion
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Using approximations for the surface potential
MOS capacitance in depletion andweak inversion
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Depletion and weak inversion
MOS capacitance in all regions of operation
Moderate and strong inversion
The model is fully analytic with explicit dependence on applied
voltages
The model is physics based, all parameters have physical
meaning and can be determined from experimental MOS capacitor
measurements
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The new approximation of MOS capacitor is accurate!!!
MOS capacitance in depletion andweak inversion
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MOS capacitance at different VCB
terminal biases
VCB
= 0V
VCB
= 0.5V
VCB
= 1V
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Depletion and weak inversion
MOS surface potential in all regionsof operation
Moderate and strong inversion
The model is fully analytic with explicit dependence on applied
voltages
The model is physics based and accurate since surface potential
is an integral function of MOS capacitance
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Surface potential at different VCB
terminal biases
VCB
= 0V
VCB
= 0.5V
VCB = 1V
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Semiconductor charges in allregions of operation
Since we have a model of surface potential in all regions of
operation, we can easily calculate semiconductor charges
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Inversion charge at different VCB
terminal biases
VCB
= 0V
VCB = 0.5V
VCB
= 1V
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Increasing bulk potential reduces inversion charge
Body effect
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Inversion disappears for large VCB
Pinchoff voltage
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Assume large L and W
Also assume IG
= 0 and IB
= 0
Long-channel MOS transistor (MOSFET)
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Regions of inversion are determined by the most heavily
inverted terminal (usually source)
MOSFET regions of inversion
Depletion weak inversion:
Moderate and strong inversion:
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Drain current in different regions of inversion
MOSFET regions of inversion
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All voltages measured with respect to bulk
Body reference
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All voltages measured with respect to source terminal
Convenient because measure drain voltage vs source voltage
Source reference
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Basic equations along MOSFET channel
All equations depend on the gate voltage, channel voltage,
and surface potential
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Surface potential along MOSFET channel
Depletion and weak inversion
Moderate and strong inversion
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Basic assumptions for current calculation
DC operation
Horizontal electric field is much smaller than the vertical
electric field Gradual channel approximation
Channel length is much larger than pn-junction depeletionregions around source and drain
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Charge-sheet model
Inversion layer charge is approximated as a layer of charge
of zero thickness at semiconductor surface
Current consists of drift and diffusion components
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Charge-sheet model: basics
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Charge-sheet model: constant mobility
Assume that mobility is constant along the channel (???)
Use
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Charge-sheet model comparison
Lines: charge-sheet model
Dots: full semiconductor equation solution
We have an approximate analytical model of surface potential
which should lead to similar accuracy as charge-sheet model