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Gyrokinetic Simulations ofTokamak Microturbulence
W Dorland, Imperial College, London
With key contributions from:
S C Cowley F Jenko G W HammettD Mikkelsen B N Rogers C BourdelleW M Nevins D W Ross K HallatschekR Budny E Belli M KotschenreutherJ W Connor E Quataert G D Kerbel
Gyrokinetics is Maturing Rapidly
Ë Mutually benchmarked, nonlinear codes exist
Ë Growing user base of experimentalists and theorists
Gyrokinetics is Maturing Rapidly
Ë Mutually benchmarked, nonlinear codes exist
Ë Growing user base of experimentalists and theorists
Radial correlation functions
from three independentlydeveloped gyrokinetic codes,
run for identical physics
parameters.
W M Nevins, A Dimits, R E Waltz,J Candy, W Dorland
Gyrokinetics is Maturing Rapidly
Ë Mutually benchmarked, nonlinear codes exist
Ë Growing user base of experimentalists and theorists
Ë Improving our understanding of experimental data
Radial correlation functions
from three independentlydeveloped gyrokinetic codes,
run for identical physics
parameters.
W M Nevins, A Dimits, R E Waltz,J Candy, W Dorland
Gyrokinetics is Maturing Rapidly
Ë Mutually benchmarked, nonlinear codes exist
Ë Growing user base of experimentalists and theorists
Ë Improving our understanding of experimental data
Ë Providing guidance for theoretical advances
Radial correlation functions
from three independentlydeveloped gyrokinetic codes,
run for identical physics
parameters.
W M Nevins, A Dimits, R E Waltz,J Candy, W Dorland
First Principles Models Desirable
Ë Outliers valuable -- indicate missing physics
Ë Extrapolation less uncertain
First Principles Models Desirable
Ë Outliers valuable -- indicate missing physics
Ë Extrapolation less uncertain
GLF-23 model(Waltz, Staebler,Dorland, Konings, andKotschenreuther)
vs data from ITERprofile database
J Kinsey
First Principles Models Desirable
Ë Outliers valuable -- indicate missing physics
Ë Extrapolation less uncertain
GLF-23 model(Waltz, Staebler,Dorland, Konings, andKotschenreuther)
vs data from ITERprofile database
J Kinsey
Ë Significant progress over the last nine years.
First Principles Models Desirable
Ë Outliers valuable -- indicate missing physics
Ë Extrapolation less uncertain
GLF-23 model(Waltz, Staebler,Dorland, Konings, andKotschenreuther)
vs data from ITER
profile database
J Kinsey
Ë Worst outliers at high collisionality.
Nonlinear Physics BenchmarkedAgainst Theoretical Predictions
High b Alfvenic turbulence inhomogeneous, stirredplasma shows predictedperpendicular spectrum(and anisotropy, not shown).Here, b = 8 (i.e., 800%).
W Dorland, S C Cowley,G W Hammett and E Quataert
Nonlinear Physics BenchmarkedAgainst Theoretical Predictions
High b Alfvenic turbulence inhomogeneous, stirredplasma shows predictedperpendicular spectrum(and anisotropy, not shown).Here, b = 8 (i.e., 800%).
W Dorland, S C Cowley,G W Hammett and E Quataert
Need theory for inhomogeneous, unstable plasmas!
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilitiesË Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilitiesË Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilities Ë Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilities Ë Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilities Ë Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Equilibrium unstable to primary (linear) instabilities Ë Primaries unstable to secondary instabilities
-----------------------------------------------------------------------------------------------------
Ë Some secondary instabilities have zonal flow component
Ë Zonal flows unstable to tertiary instabilities
Key references: S C Cowley, R M Kulsrud, R Sudan, PF B, (3:2767:1991)J F Drake, et al., PF B, (4:488:1992)M N Rosenbluth, F Hinton, PRL (80:724:1998)B N Rogers, W Dorland, M Kotschenreuther, PRL, (85:5536:2000)W Dorland, F Jenko, M Kotschenreuther, B N Rogers, PRL, (85:5579:2000)
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Parasitic Instability Model
Ë Amenable to analytical treatment
Ë Balances among primaries, secondaries and tertiariesexplain simulation results quantitatively and qualitatively
Ë For example, different kinds of secondaries have
different effects.l Toroidal ITG susceptible to strong secondary -> “weak” transport
l Toroidal ETG susceptible to weak secondary -> “strong” transportl Slab ETG/ITG susceptible to strong secondary -> “weak” transport
Nature of Secondary Instabilities
Contours of electrostatic
potential from simulation of
ETG turbulence
High-n microinstabilities
typically localised to low
field, bad curvature region;extended along field lines
G D Kerbel, W Dorland
Nature of Secondary Instabilities
Contours of electrostatic
potential from simulation of
ETG turbulence
High-n microinstabilities
typically localised to low
field, bad curvature region;extended along field lines
G D Kerbel, W Dorland
Nature of Secondary Instabilities
Contours of electrostatic
potential from simulation of
ETG turbulence
High-n microinstabilities
typically localised to low
field, bad curvature region;extended along field lines
G D Kerbel, W Dorland
Nature of Secondary Instabilities
Radially extended
structures clearly evident
on outboard midplane
Associated with existence
of high amplitude streamertransport
W Dorland, F Jenko
Nature of Secondary Instabilities
What is a secondaryinstability, and how is it
related to pictures like this?
Nature of Secondary Instabilities
What is a secondary
instability, and how is it
related to pictures like this?
Let’s go back in time, and
consider the primaryinstabilities
Nature of Secondary Instabilities
Primary instabilities haveradial widths ~ 1/sqrt(n) and
poloidal widths ~ 1/n
Nature of Secondary Instabilities
Primary instabilities have
radial widths ~ 1/sqrt(n) and
poloidal widths ~ 1/n
Since n >> 1, linear modes look
like ‘streamers’
Nature of Secondary Instabilities
Amplitude of linear
perturbations increases
exponentially in time
Contours of potential are
streamlines of ExB flows whichare increasingly sheared and
thus susceptible to Kelvin-
Helmholtz-like instabilities
Nature of Secondary Instabilities
Amplitude of linear
perturbations increases
exponentially in time
Contours of potential are
streamlines of ExB flows which
are increasingly sheared andthus susceptible to Kelvin-
Helmholtz-like instabilities
Also, gradients in poloidal
direction can be sqrt(n)stronger than radial gradients
if eddies survive long enough
Nature of Secondary Instabilities
Amplitude of linear
perturbations increases
exponentially in time
Contours of potential are
streamlines of ExB flows which
are increasingly sheared andthus susceptible to Kelvin-
Helmholtz-like instabilities
Also, gradients in poloidal
direction can be sqrt(n)stronger than radial gradients
if eddies survive long enough
Secondary growth rate is proportional to primary amplitude
Nature of Secondary Instabilities
ETG secondaries arecomplicated, so
consider ITG secondary
first.
Same view as before.
Secondary breaks upradial flows, tries to
convert them to
poloidal flows
B N Rogers, W Dorland
g, kx spectrum of secondary analytically tractable!
Secondary Instability of ITG Mode
Selected Fourier
harmonic amplitudes vstime in example GK ITG
simulation: collisionless,adiabatic electrons,
electrostatic
Secondary Instability of ITG Mode
Selected Fourier
harmonic amplitudes vstime in example GK ITG
simulation: collisionless,
adiabatic electrons,electrostatic
Primary instability grows
like exp[ g t]
Secondary Instability of ITG Mode
Selected Fourier
harmonic amplitudes vstime in example GK ITG
simulation: collisionless,adiabatic electrons,
electrostatic
Primary instability grows
like exp[ g t]
Secondary instabilities
grow like exp[exp[g t]]
above a threshold…
Secondary Instability of ITG Mode
Growth rate of primaryis constant in time
Growth rate of
secondary increases intime
Secondary Instability of ITG Mode
Growth rate of primaryis constant in time
Growth rate of
secondary increases intime
Growth rate ofsecondary is
proportional to
amplitude of primary
Secondary Instability of ITG Mode
Balance primary and
secondary growth rates to
estimate saturation
amplitude
Secondary Instability of ITG Mode
Balance primary andsecondary growth rates to
estimate saturation
amplitude
Secondary Instability of ITG Mode
Balance primary andsecondary growth rates to
estimate saturation
amplitude
Alternatively, view this as
the physics that
determines the radialmixing length (Cowley)
Secondary Instability of ITG Mode
Balance primary andsecondary growth rates to
estimate saturation
amplitude
Alternatively, view this as
the physics that
determines the radialmixing length (Cowley)
This is not a modulational
instability -- amplitudes aretoo large, orderings
strongly violated
Secondary Instability of ITG Mode
Is the secondaryphysics analytically
tractable?
In the limit of highamplitude primary, low
amplitude secondary,
yes.
Secondary Instability of ITG Mode
Is the secondaryphysics analytically
tractable?
In the limit of highamplitude primary, low
amplitude secondary,
yes.
Best satisfied slightly
before nonlinear break-
up of primary
Secondary Instability of ITG Mode
Analytical treatment
tractable in limit of largeamplitude primary, small
amplitude secondaries
Fully turbulent regime toocomplicated
B N Rogers, W Dorland
Secondary Instability of ITG Mode
Analytical treatment
tractable in limit of largeamplitude primary, small
amplitude secondaries
Fully turbulent regime toocomplicated
Compare theoreticallypredicted secondary
growth rate spectrum with
simulation at t=62.3.
B N Rogers, W Dorland
Secondary Instability of ITG Mode
Secondary growth rate is
much larger than primarygrowth rate
Predicted spectrum in kx
remarkably independent ofprimary mode’s ky
Data taken fromcomplicated nonlinear
simulation
B N Rogers, W Dorland
Secondary Instability of ITG Mode
Agreement in the limit ofthe analytical treatment is
excellent (assumed
simplified primary mode
structure)
Secondary Instability of ITG Mode
Agreement in the limit ofthe analytical treatment is
excellent (assumed
simplified primary mode
structure)
For each kx one must solve
a 2-D eigenvalue problem:in the y (~ poloidal)
direction and along the
field line
Secondary Instability of ITG Mode
Agreement in the limit ofthe analytical treatment is
excellent (assumed
simplified primary mode
structure)
For each kx one must solve
a 2-D eigenvalue problem:in the y (~ poloidal)
direction and along the
field line
Component which is
constant in y and along
field line is special
Secondary Instability of ITG Mode
With trapped particles, part
of the ky = 0 component of
the eigenmode is linearlyundamped in the
collisionless limit; this is
the Rosenbluth-Hinton
zonal flow.
Simulation: M A Beer, G D Kerbel,G W Hammett, W Dorland
Zonal Flows Can Quench Turbulence
Typical spectrum of zonalflows from gyrokinetic
simulation
Strongly peaked at longwavelengths
W M Nevins, W Dorland
Zonal Flows Can Quench Turbulence
Near but above the linear
threshold, Rosenbluth-Hinton zonal flows can
quench turbulence (Dimits)
Zonal Flows Can Quench Turbulence
Near but above the linear
threshold, Rosenbluth-Hinton zonal flows can
quench turbulence (Dimits)
Leads to important
question:Why doesn’t this alwayshappen?Equivalently, what limitsthe zonal flows well abovethe linear threshold?
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Near
Increasing the amplitude of the zonal flows
increases the shear in the zonal flows, whichdecreases the growth rate of the primary
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Near
Increasing the amplitude of the zonal flows
increases the shear in the zonal flows, whichdecreases the growth rate of the primary
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Near
Increasing the amplitude of the zonal flows
increases the shear in the zonal flows, whichdecreases the growth rate of the primary
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Near
Increasing the amplitude of the zonal flows
increases the shear in the zonal flows, which
decreases the growth rate of the primary
Further increases in the zonal flow amplitude lead to
collisionless tertiary instability B N Rogers, W Dorland
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Increasing the temperature gradient slightly
removes window of stability altogether
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
Increasing the temperature gradient slightly
removes window of stability altogether
Although the Rosenbluth-Hinton zonal flows are linearly
undamped, they are unstable to small perturbationsabove a threshold R/LT B N Rogers, W Dorland
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
So far:1. ITG modes linearly
unstable: primary
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
So far:1. ITG modes linearly
unstable: primary
2. Shear-flow instability
limits growth of primary:secondary
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
So far:1. ITG modes linearly
unstable: primary
2. Shear-flow instability
limits growth of primary:secondary
3. Zonal flow component
of secondary quenchesprimary: Dimits shift
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
So far:
1. ITG modes linearlyunstable: primary
2. Shear-flow instability
limits growth of primary:
secondary3. Zonal flow component
of secondary quenches
primary: Dimits shift4. Zonal flows unstable to
tertiary: Stiff transport
at higher R/LT
Zonal Flow Amplitude Limited byCollisionless Tertiary Instability
So far:1. ITG modes linearly
unstable: primary
2. Shear-flow instability
limits growth of primary:secondary
3. Zonal flow component
of secondary quenchesprimary: Dimits shift
4. Zonal flows unstable to
tertiary: Stiff transport
at higher R/LT
What happens with additional physics?
Ion-ion Collisions Damp Zonal Flows,Soften Threshold
Focus analysis on regionbetween linear critical
gradient and effective
nonlinear gradient
Ion-ion Collisions Damp Zonal Flows,Soften Threshold
Ion-ion collisions dampzonal flows and thus
increase turbulent
transport(M N Rosenbluth, F Hinton,P Diamond, Z Lin, W W Lee,
W M Tang, T S Hahm)
Ion-ion Collisions Damp Zonal Flows,Soften Threshold
Ion-ion collisions dampzonal flows and thus
increase turbulent
transport(M N Rosenbluth, F Hinton,P Diamond, Z Lin, W W Lee,
W M Tang, T S Hahm)
Corollary:
Confinement improvement
expected in reactor-sizedtokamaks
Non-adiabatic Electron DynamicsReverse Effect of Collisionality
Trapped electrons causelarge increase in transport
near marginal stability(Y Chen, S Parker;
D Mikkelsen, D W Ross, W Dorland)
Non-adiabatic Electron DynamicsReverse Effect of Collisionality
Trapped electrons causelarge increase in transport
near marginal stability(Y Chen, S Parker;
D Mikkelsen, D W Ross, W Dorland)
Trapped electrons increasegrowth rate of primary, close
zonal flow stability window;
Dimits shift strongly reduced
Non-adiabatic Electron DynamicsReverse Effect of Collisionality
Trapped electrons causelarge increase in transport
near marginal stability(Y Chen, S Parker;
D Mikkelsen, D W Ross, W Dorland)
Trapped electrons increasegrowth rate of primary, close
zonal flow stability window;
Dimits shift strongly reduced
Electron-ion collisions
reduce non-adiabatic
electron response, and thusreduce turbulent transport
Experimental Confirmation ofDimits Shift at High Collisionality
C-Mod H-mode 960116027 at
half radius
IFS-PPPL model overpredictstransport
NonlinearGS2
Simulations
High Collisionality Outlier from ITERProfile Database has Dimits Shift
C-Mod H-mode 960116027 athalf radius
IFS-PPPL model overpredicts
transport
Gyrokinetic simulations show
Dimits shift effect improvesagreement
General geometry, kineticelectrons, Lorentz collisions
D Mikkelsen, M KotschenreutherW Dorland
NonlinearGS2
Simulations
Lowering Collisionality IncreasesPredicted Heat Flux
Lowering overall collision-
ality by factor of 5 increases
predicted transport
IFS-PPPL model
Lowering Collisionality IncreasesPredicted Heat Flux
Lowering overall collision-
ality by factor of 5 increases
predicted transport
Lowering only ion-ion
collisionality by factor of 5
has small effect, near kneeof Dimits shift
IFS-PPPL model
Lowering Collisionality IncreasesPredicted Heat Flux
Lowering overall collision-
ality by factor of 5 increases
predicted transport
Lowering only ion-ion
collisionality by factor of 5has small effect, near knee
of Dimits shift
Results consistent with highcollisionality outliers from
profile database effort
D Mikkelsen, W Dorland
IFS-PPPL model
Gyrokinetic Simulations areStimulating and Guiding
Broad Theoretical Advances
1. Ion-scale physics2. Electron-scale physics
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Profiles from Tore-Supra
Electron Cyclotron Heating
Ion temperature profilesomewhat uncertain
No obvious central particlesource
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Profiles from Tore-Supra
Electron Cyclotron Heating
Ion temperature profilesomewhat uncertain
No obvious central particlesource
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Profiles from Tore-Supra
Electron Cyclotron Heating
Ion temperature profilesomewhat uncertain
No obvious central particlesource
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Profiles from Tore-Supra
Electron Cyclotron Heating
Ion temperature profilesomewhat uncertain
No obvious central particlesource
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Simulations near half-radius
Density gradient observed in
experiment
Focus on TEM+ITG
instabilities
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Simulations near half-radius
Density gradient observed in
experiment
Focus on TEM+ITG
instabilities
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Simulations near half-radius
Density gradient observed in
experiment
Focus on TEM+ITG
instabilities
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Varied ion R/LT around
nominal value
Here, R/LTi increase (to
nominal value) att = 700 causes particle flux
to reverse (pinch)
Trapped electron effect?
K Hallatschek, W DorlandF Jenko, T Hoang
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Varied ion R/LT around
nominal value
Here, R/LTi increase (to
nominal value) att = 700 causes particle flux
to reverse (pinch)
Trapped electron effect?
K Hallatschek, W DorlandF Jenko, T Hoang
Realistic Electron Dynamics AllowsSimulation of Particle Transport
Varied ion R/LT around
nominal value
Here, R/LTi increase (to
nominal value) att = 700 causes particle flux
to reverse (pinch)
Trapped electron effect?
K Hallatschek, W DorlandF Jenko, T Hoang
Passing Electrons Dominate Pinch
Integrated particle flux vspitch angle shows relativecontributions to total flux
Hybrid PIC-fluid models thatassume passing electrons
are adiabatic will miss effect
Direct comparison withexperiment possible
K Hallatschek, W Dorland
Passing Electrons Dominate Pinch
Integrated particle flux vspitch angle shows relativecontributions to total flux
Hybrid PIC-fluid models thatassume passing electrons
are adiabatic will miss effect
Direct comparison withexperiment possible
K Hallatschek, W Dorland
Passing Electrons Dominate Pinch
Integrated particle flux vspitch angle shows relativecontributions to total flux
Hybrid PIC-fluid models thatassume passing electrons
are adiabatic will miss effect
Direct comparison withexperiment possible
K Hallatschek, W Dorland
Secondary physics reduces to
2D eigenvalue problem: alongthe field line, and in the y
direction (perp to B and —y)
Secondary Structure at ri Scales
Secondary Structure at ri Scales
Secondary physics reduces to
2D eigenvalue problem: alongthe field line, and in the y
direction (perp to B and —y)
Shown here are the dominantFourier harmonics of the
solution in the long wavelength
(ITG) limit
Secondary physics reduces to
2D eigenvalue problem: alongthe field line, and in the y
direction (perp to B and —y)
Shown here are the dominantFourier harmonics of the
solution in the long wavelength
(ITG) limit
Note presence of significant
zonal flow component
(constant along field line, ky=0)
Secondary Structure at ri Scales
At re Scales, Secondaries Change
Ë Quickly establish terminology:
Secondary driven by perpendicular shear of
perpendicular flows that are associated with the
primary instability will be the “Rogers” secondary; thishas been the main secondary so far
At re Scales, Secondaries Change
Ë Quickly establish terminology:
Secondary driven by perpendicular shear of
perpendicular flows that are associated with the
primary instability will be the “Rogers” secondary; thishas been the main secondary so far
The secondary driven by perpendicular shear of parallelflows that are associated with the primary instability
will be the “Cowley” secondary; this was the first
secondary identified as potentially important in ITG/ETG
turbulence
Shown here are the dominant
Fourier harmonics of theRogers secondary in the short
wavelength (ETG) limit
Rogers Secondary at re Scales
Shown here are the dominant
Fourier harmonics of theRogers secondary in the short
wavelength (ETG) limit
At small scales, adiabatic ionresponse comes from gyration,
not streaming along field line;
weakens Rogers secondary
Rogers Secondary at re Scales
Shown here are the dominant
Fourier harmonics of the
Rogers secondary in the short
wavelength (ETG) limit
At small scales, adiabatic ion
response comes from gyration,not streaming along field line;
weakens Rogers secondary
Note absence of zonal flowcomponent (constant along
field line, ky=0)
W Dorland, B N Rogers, F Jenko
Rogers Secondary at re Scales
Cowley Secondary at re Scales
If primary instability requiressignificant parallel compress-ibility (e.g., the sheared-slab hemode) the Cowley secondary is
excited
If primary instability requiressignificant parallel compress-ibility (e.g., the sheared-slab hemode) the Cowley secondary is
excited
Shown here are the dominant
Fourier harmonics of the
Cowley secondary in the shortwavelength (ETG) limit
Cowley Secondary at re Scales
If primary instability requires
significant parallel compress-ibility (e.g., the sheared-slab hemode) the Cowley secondary isexcited
Shown here are the dominantFourier harmonics of the
Cowley secondary in the short
wavelength (ETG) limit
Again, note absence of zonal
flow component (constant
along field line, ky=0)S C Cowley, W Dorland
Cowley Secondary at re Scales
If primary instability requiressignificant parallel compress-ibility (e.g., the sheared-slab hemode) the Cowley secondary is
excited
Shown here are the dominant
Fourier harmonics of the
Cowley secondary in the shortwavelength (ETG) limit
Again, note absence of zonalflow component (constant
along field line, ky=0)S C Cowley, W Dorland
Cowley Secondary at re Scales
Cowley Secondary Strong on re Scales
¸ Theoretically predicted:
growth rate; parallel
wavenumber increasing with
the amplitude of the primary
¸ Theoretically predicted:
growth rate; parallel
wavenumber increasing with
the amplitude of the primary
Cowley secondary not
weakened like Rogers at small
scales; breaks up streamerswhen excited
Cowley Secondary Strong on re Scales
¸ Theoretically predicted:
growth rate; parallel
wavenumber increasing with
the amplitude of the primary
Cowley secondary not
weakened like Rogers at small
scales; breaks up streamerswhen excited
Zonal flows irrelevant on rescales because drive is weak
and tertiary is strong
Cowley Secondary Strong on re Scales
Balance of Primaries, Secondariesand Tertiaries Explains Simulations
¸ Foregoing predicts slab
ITG/ETG should be similar (innormalized units) because slab
primary requires parallel
compressibility
Balance of Primaries, Secondariesand Tertiaries Explains Simulations
¸ Foregoing predicts slab
ITG/ETG should be similar (in
normalized units) because slab
primary requires parallelcompressibility
¸ In the limit of constant
curvature, parallel compress-ibility irrelevant to primary, so
normalized ETG saturation
level should be much higher
Balance of Primaries, Secondariesand Tertiaries Predicts Simulations
Major result:
Balance of primary and
secondary growth rates
predicts when highamplitude streamer
transport is found with
simulations
Balance of Primaries, Secondariesand Tertiaries Predicts Simulations
Major result:
Balance of primary and
secondary growth rates
predicts when highamplitude streamer
transport is found with
simulations
Toroidal ETG branch most
dangerous
F Jenko, W Dorland
Experimental Confirmation of Theory?
ETG threshold formulaobtained from GS2
Tore-Supra finds Te profile
is stiff above a criticalgradient
Experimental and theoretical thresholds similar and GK ETG
simulations predict experimental stiffness beyond threshold
F Jenko, G W Hammett W Dorland
NSTX Confinement Consistent withGyrokinetic Predictions
Gyrokinetic analysis of NSTX
discharges indicates long
wavelength instabilities weakor non-existent, but ETG
modes unstable
C Bourdelle, W Dorland, NSTX team
NSTX Confinement Consistent withGyrokinetic Predictions
Gyrokinetic analysis of NSTX
discharges indicates long
wavelength instabilities weakor non-existent, but ETG
modes unstable
TRANSP analysis of NSTX
discharges indicates electrons
are dominant energy loss
channel (not shown)
C Bourdelle, W Dorland, NSTX team
NSTX Confinement Consistent withGyrokinetic Predictions
Gyrokinetic analysis of NSTX
discharges indicates long
wavelength instabilities weakor non-existent, but ETG
modes unstable
TRANSP analysis of NSTX
discharges indicates electrons
are dominant energy loss
channel (not shown)
Detailed results in press
C Bourdelle, W Dorland, NSTX team
Can Higher b and Higher b GradientImprove ST Confinement?
GK analysis of NSTX data suggestsconfirmation of long wavelength
“second microstability” predictions
for STC Bourdelle, G W Hammett
W Dorland, et al.
-db/dr
Can Higher b and Higher b GradientImprove ST Confinement?
GK analysis of NSTX data suggestsconfirmation of long wavelength
“second microstability” predictions
for STC Bourdelle, G W Hammett
W Dorland, et al.
GK simulations of ETG turbulence
indicate 1/b scaling of electron
energy diffusion coefficient in
some regimesF Jenko, W Dorland
-db/dr
Conclusions
Ë First-principles simulation of turbulence in fusion plasmas is
a rapidly maturing area. Gyrokinetic simulations areexplaining experimental data. For example:
1. ETG turbulence identified in NSTX2. ITG turbulence identified in C-Mod
3. TEM-induced particle transport identified in Tore Supra?
Ë Parasitic instability model is a useful theoretical frameworkfor understanding nonlinear simulation results. Competition
among primary, secondary and tertiary instabilities explains
simulation results.
Nonlinear Physics BenchmarkedAmong Independent Codes
GS2 and GENE,
benchmark of heat flux
for toroidal ETGturbulence
F Jenko, W Dorland
Nature of Secondary Instabilities
Primary instabilities haveradial widths ~ 1/sqrt(n) and
poloidal widths ~ 1/n
Since n >> 1, linear modes looklike ‘streamers’
Note: Flux tube simulationstypically ignore radial envelope
because nonlinear coupling
dominates: turbulent radial
correlation length ~ 1/n
Alpha Heating + NeoclassicalTransport + ST = Stable Profiles
Simple alpha power depositionmodel + self-consistent
bootstrap current + small seed
current on axis + neoclassicaltransport + electron energy
transport (possibly strong) in
ST configuration predicted to
yield MHD- and micro-stableprofiles.
W Dorland, M Kotschenreuther
Alpha Heating + NeoclassicalTransport + ST = Stable Profiles
Simple alpha power depositionmodel + self-consistent
bootstrap current + small seed
current on axis + neoclassicaltransport + electron energy
transport (possibly strong) in
ST configuration predicted to
yield MHD- and micro-stableprofiles. Need higher b !
But particle transport problem?
W Dorland, M Kotschenreuther
Experimental Confirmation of Theory?
ETG threshold formula
obtained from approx.
3000 GS2 runs (F Jenko, W
Dorland, G W Hammett)
Experimental Confirmation of Theory?
ETG threshold formula
obtained from approx.
3000 GS2 runs (F Jenko, W
Dorland, G W Hammett)
Smoothly interpolates
analytical results of
Romanelli (toroidal) and
Hahm-Tang (slab)
Experimental Confirmation of Theory?
ETG threshold formula
obtained from approx.
3000 GS2 runs (F Jenko, W
Dorland, G W Hammett)
Smoothly interpolates
analytical results of
Romanelli (toroidal) and
Hahm-Tang (slab)
Tore-Supra finds Te profile
is stiff above a criticalgradient
Linear Physics Benchmarked forWide Range of Problems
Linear micro-
stability calcu-lations for NCSX
with GS2 and
FULL agree
E Belli, G Rewoldt,G W Hammett,
W Dorland
Nature of Secondary Instabilities
Adequate resolution ofradial structures is
challenging, but achievable
Nature of Secondary Instabilities
Adequate resolution of
radial structures is
challenging, but achievable
In normalized units, ETG
transport is much larger
than ITG transport whenstreamers are observed
Nature of Secondary Instabilities
Adequate resolution ofradial structures is
challenging, but achievable
In normalized units, ETGtransport is much larger
than ITG transport when
streamers are observed
The difference can be
traced to differences insecondary and tertiary
physics
W Dorland, F Jenko, B N Rogers