Guttenfelder, APS-DPP 2014, New Orleans LA
Investigating electromagnetic effects on core transport in Alcator C-Mod H-mode discharges
W. Guttenfelder1, N.T. Howard2, J. Irby3, F.M. Poli1,
A.E. White3, W.F. Bergerson4, D.L. Brower4, J. Candy5, W.X. Ding4, C.E. Kessel1, C. Sung3, S.M. Wolfe3, P. Xu
1 Princeton Plasma Physics Laboratory2 ORISE3 Massachusetts Institute of Technology4 University of California – Los Angeles5 General Atomics
APS-DPP, New OrleansOct. 27-31, 2014
Guttenfelder, APS-DPP 2014, New Orleans LA
Overview & Summary
• Beginning validation of gyrokinetic simulations for high- ITER-like H-mode plasmas in Alcator C-Mod– N=1.3-2.1 H-modes unstable to ITG (r/a~0.5-0.8), sub-dominant microtearing
modes (MTM) also predicted– Baseline nonlinear simulations are dominated by ITG, but ion/electron heat fluxes
do not match experiment– Varying Te & Ti gradients to match fluxes changes balance of ITG vs. MTM,
challenges nonlinear simulations (requires large numerical resolution)
• Characterizing expected importance of electromagnetic effects– Finite reduces predicted ion heat fluxes from ITG by 50%– EM flutter transport contributions are small (1% for heat, 15% for particle flux)
• Using synthetic diagnostic, predict sensitivity of polarimeter diagnostic to ne, Br using synthetic diagnostic– |B/B0| ~ 1% |n/n0|, negligible influence of B on Faraday rotation– Will likely change if predicted character of turbulence changes (ITGMTM) with
gradient variations
2
Guttenfelder, APS-DPP 2014, New Orleans LA
EXPERIMENTAL DETAILS
3
Guttenfelder, APS-DPP 2014, New Orleans LA
Analysis based on ITER-like H-mode discharges with N=1.3-2.1
• ITER-like discharges with 2.5-5 MW ICRH heating (Kessel, NF 2013)
• Using reduced BT=2.6 T to achieve high N and fGW (higher * compared to ITER)
• Dominant electron heating, Te~Ti, no torque (expect low rotation, but no measurement)
• Following transport analysis and gyrokinetic scoping studies around 1.3 s
0
0.2
0.4
0.6
I p (M
A)
0
2
4
n (1
020 m
−3 )
0
2
4
6
PR
F (
MW
)
0
1
2
β N
0
0.5
1
f GW
0 0.5 1 1.50
0.5
1
H98
t (s)
1120717006
1120719005
1120719014
4
Guttenfelder, APS-DPP 2014, New Orleans LA
0 0.2 0.4 0.6 0.8 10
10
20
30
40
ne (1019 m−3)
0 0.2 0.4 0.6 0.8 10
0.5
1
1.5
2
(−) te, (−−) ti (keV)
0 0.2 0.4 0.6 0.8 1
0
1
2
3
4
a/Ln
0 0.2 0.4 0.6 0.8 10
2
4
6
8
a/LT
0 0.2 0.4 0.6 0.8 110
−2
10−1
100
101
(−) νei
(cs/a)
0 0.2 0.4 0.6 0.8 10
0.5
1
1.5
2
(−) βe (%)
0 0.2 0.4 0.6 0.8 11.55
1.6
1.65
1.7
1.75
Zeff
r/a0 0.2 0.4 0.6 0.8 1
0
1
2
3
4(−) q, (−−) s
r/a
1120717006
1120719005
1120719014
TRANSP runs & profiles
• 1120717006 (1300 ms) TRANSP ID 87637
• 1120719005 (1300 ms) TRANSP ID 87632
• 1120719014 (1300 ms) TRANSP ID 87634
• Measured Ti profiles unavailable - scaled i,NCto match neutron rate
– New experiment planned to get Ti, v, and MSE-constrained q profile
• Flat Zeff assumed
• For GYRO sims, keeping D & B (sometimes Mo)
(-) ne, (--) nD
5
Guttenfelder, APS-DPP 2014, New Orleans LA
Fluctuation data available from polarimeter, PCI, TCI and reflectometer for validation with simulations
Guttenfelder, APS-DPP 2014, New Orleans LA
LINEAR GYROKINETICS
7
Guttenfelder, APS-DPP 2014, New Orleans LA
0 0.2 0.4 0.6 0.8 1−1.5
−1
−0.5
0
0.5
1
kθρ
s
ωr (c
s/a)
CMOD 1120719014, 1300 ms
0 0.2 0.4 0.6 0.8 10
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
kθρ
s
γ (cs/a)
r/a=0.5
0.6
0.7
0.8
Initial linear GYRO stability simulations show that ITG dominates r/a=0.6-0.8
• Microtearing modes (MTM) exist for ks<0.4 at r/a=0.5, 0.6– Distinguishable from eigenfunctions/spatial structure (not shown)– Tracking MTM when subdominant using eigenvalue solver (dashed line)
• Clearly distinct dispersion in real frequencies• Similar results for other two shots
8
Linear runs using GYRO
4 kinetic species, D,B,Mo,e(Zeff~1.6)
Electromagnetic(A|| only, e~0.24-0.85%)
Collisions
MTM
ITG
Real frequencies Growth rates
Guttenfelder, APS-DPP 2014, New Orleans LA
Linear ITG weakly stabilized by finite beta (r/a=0.6)
• MTM has threshold at e~0.3% ~ 1/2e,exp, predicts much larger EM fluctuations, |BMTM/B0| ~ 20% of |nMTM/n0|
• Fits for 1120719014 (N=2.1) give a/LTi ~ 1.4a/LTe (r/a=0.6)– a/LTi ~ a/LTe in the other two shots (no ion measurements)
• Let’s investigate sensitivity to gradients
9
0 0.2 0.4 0.6 0.8 1−0.4
−0.2
0
0.2
0.4
0.6
ωr (c
s/a)
βe (%)
0 0.2 0.4 0.6 0.8 10
0.02
0.04
0.06
0.08
0.1
γ (cs/a)
βe (%)
MTM k
θρ
s=0.2
ITG k
θρ
s=0.3
0 0.2 0.4 0.6 0.8 10
0.05
0.1
0.15
0.2
0.25
|δBr|/|δφ|
βe (%)
11207190051120719014
Real frequencies Growth rates
Guttenfelder, APS-DPP 2014, New Orleans LA
ITG stiff with ion temperature gradient (a/LTi),MTM stiff with electron temperature gradient (a/LTe)
• ITG independent of a/LTe
• MTM independent of a/LTi
• MTM much stronger when increasing a/LTe to better match a/LTi~2.7
0 1 2 3−0.8
−0.6
−0.4
−0.2
0
0.2
0.4
0.6
a/LTe
ωr (c
s/a)
CMOD 112071914, 1300 ms
0 1 2 30
0.02
0.04
0.06
0.08
0.1
a/LTe
γ (cs/a)
ITG kθρ
s=0.4
MT kθρ
s=0.2
a/LTi
0 1 2 3−0.5
0
0.5
a/LTi
ωr (c
s/a)
CMOD 112071914, 1300 ms
0 1 2 30
0.02
0.04
0.06
0.08
0.1
a/LTi
γ (cs/a)
ITG kθρ
s=0.4
MT kθρ
s=0.2
a/LTe
10
Real frequencies Growth rates
Guttenfelder, APS-DPP 2014, New Orleans LA
Microtearing present over broad radial region, but always subdominant to ITG
• MTM getting stronger further out in radius, but so is ITG
0.4 0.5 0.6 0.7 0.8−0.5
0
0.5
1
r/a
ωr (c
s/a)
CMOD 112071914, 1300 ms
kθρ
s=0.2
0.4 0.5 0.6 0.7 0.80
0.05
0.1
0.15
0.2
0.25
0.3
r/a
γ (cs/a)
ITG kθρ
s=0.4
MT kθρ
s=0.2
11
Real frequencies Growth rates
Guttenfelder, APS-DPP 2014, New Orleans LA
MTM shows non-monotonic dependence with collisionality, as predicted in core of NSTX & AUG
• Same dependence predicted in core of NSTX [Guttenfelder, 2012] and ASDEX-UG [Doerk, 2012]
• Perhaps expected to be less relevant at lower collisionality(ITER r/a~0.6, e ~ 10-2 cs/a)
0 1 2 3−0.5
0
0.5
νe (c
s/a)
ωr (c
s/a)
CMOD 112071914, 1300 ms
0 1 2 30
0.05
0.1
0.15
0.2
νe (c
s/a)
γ (cs/a)
ITG kθρ
s=0.4
MT kθρ
s=0.2
12
Real frequencies Growth rates
Guttenfelder, APS-DPP 2014, New Orleans LA
NONLINEAR GYROKINETICS
13
Guttenfelder, APS-DPP 2014, New Orleans LA
Initial nonlinear run for 1120719014, 1300 ms, r/a=0.6
• For base case, fluxes dominated by ES contributions (Qi=4.8 MW, Qe=1.9 MW)• Inconsistent with TRANSP analysis (Qi,exp=0.6 MW, Qe,exp=4.4 MW)• Only ~1% EM contribution (~Br) to Qe
14
Nonlinear runs using GYRO3 kinetic species, D,B,e (Zeff~1.6)Electromagnetic (A||, e~0.6%)Collisions
Resolution parametersLx Ly = 125 127 snx ny = 25624 (n=5)ks [min, max] = [0.049, 1.14]krs [min, max] = [0.050, 3.21][n||,n,ne]=[14,8,8]2
0 500 1000−50
0
50
100
150
200
Γe (1019 m−2s−1)
t (a/cs)
0 500 1000
0
2
4
6
8
10
12
Qi (MW)
t (a/cs)
0 500 1000−1
0
1
2
3
4
5
6
Qe (MW)
t (a/cs)
ES
EM
tot
Guttenfelder, APS-DPP 2014, New Orleans LA
Ion heat flux (Qi) decreases ~50% with finite e
• Qe shows weaker dependence, e increases– Heat flux dependence similar to previous studies (e.g. Pueschel, PoP 2008)
• Biggest EM flutter contribution is to particle flux (~15% inward)
15
0 0.2 0.4 0.6 0.8
0
2
4
6
8
Qi (
MW
)
βe (%)
0 0.2 0.4 0.6 0.8−1
0
1
2
3
4
5
Qe (
MW
)
βe (%)
1120719014, 1300 msr/a=0.6
0 0.2 0.4 0.6 0.8−10
0
10
20
30
Γe (
1020
#/s
)
βe (%)
tot
ES
EM
exp
Ion heat flux Electron heat flux Electron particle flux
Guttenfelder, APS-DPP 2014, New Orleans LA
Try to match fluxes by adjusting gradients – 1.2-1.4a/LTegives larger Qe approaching experiment
• But also increases Qi (further from experiment)• Will probably need a corresponding decrease in a/LTi
16
0 1 2 3
0
2
4
6
8
Qi (
MW
)
a/LTe
0 1 2 3−1
0
1
2
3
4
5
Qe (
MW
)
a/LTe
1120719014, 1300 msr/a=0.6
0 1 2 3−10
0
10
20
30
Γe (
1020
#/s
)
a/LTe
tot
ES
EM
exp
Ion heat flux Electron heat flux Electron particle flux
Guttenfelder, APS-DPP 2014, New Orleans LA
0.8a/LTi (for 1.2a/LTe) reduces Qi and e much closer to experiment
• Also brings down Qe significantly (further from experiment)• BUT there are serious numerical resolution problems…
17
0 1 2 3
0
2
4
6
8
Qi (
MW
)
a/LTe
0 1 2 3−1
0
1
2
3
4
5
Qe (
MW
)
a/LTe
1120719014, 1300 msr/a=0.6
0 1 2 3−10
0
10
20
30
Γe (
1020
#/s
)
a/LTe
1.0×a/LTi
0.8×a/LTi
exp
Ion heat flux Electron heat flux Electron particle flux
Guttenfelder, APS-DPP 2014, New Orleans LA
Insufficient resolution for reduced a/LTi simulations
• Pathological peaking at highest ks modes in electron heat flux spectra
18
10−1
100
−0.2
0
0.2
0.4
0.6
0.8
1
1.2
1.4
kθρ
s
Δ(Γ
e/ΓG
B)
/ Δ(k
θρ
s)
10−1
100
10−2
10−1
100
101
102
kθρ
s
Δ(Q
i/QG
B)
/ Δ(k
θρ
s)
10−1
100
100
kθρ
s
Δ(Q
e/QG
B)
/ Δ(k
θρ
s)
1.9092.2912.291
Particle flux spectra Ion heat flux spectra Electron heat flux spectra
Base1.2a/LTe1.2a/LTe, 0.8a/LTi
Guttenfelder, APS-DPP 2014, New Orleans LA
Linear tests for n=90 (ks=0.88) using nonlinear numerical resolution setup show insufficient resolution
• Artificial growth (n=90, ks=0.88) with insufficient resolution, need nx~500 to recover flux-tube results (i.e. ~0, stable mode)
• Seems that it’s necessary to resolve rational surfaces associated with highest ks modes, x/s1/(4sks)~0.25 (nx500)
– rrat/s = 1/sks = 1 (for ks=0.88, q=1.17, s=1.13)– Working on nonlinear simulations
0 50 100 150 200 250
−0.4
−0.2
0
0.2
0.4
0.6
(−−) ωr (−) γ
t
nx=128
256
400
500
19
Guttenfelder, APS-DPP 2014, New Orleans LA
Relative EM amplitude increases linearly with e
• Br/B0 ~ few % of e/Tene/ne0
• Even if turbulence doesn’t change character, expect B to get bigger is polarimeter expected to be sensitive to B fluctutions?
20
0 0.2 0.4 0.6 0.80
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
|δA|||/|δφ|
βe (%)
Σn>0
Σn≥0
Br/B0 = ksA||/sB0~0.3A||/sB0
Guttenfelder, APS-DPP 2014, New Orleans LA
2D fluctuation snapshot (in R,Z)C-Mod 1120719014, 1300 ms
• ne/ne0 Br/B0
21Movie: http://w3.pppl.gov/~wgutten/movies/cmod_nebr_sat.mov
Guttenfelder, APS-DPP 2014, New Orleans LA
SYNTHETIC FARADAY ROTATION
22
Guttenfelder, APS-DPP 2014, New Orleans LA
Utilize synthetic diagnostic to examine sensitivity of polarimeter measurement to n, B
• Interested in interferometry, Faraday rotation and Cotton-Mouton effects• int=cint dL(ne) cFR=2.81710-15 m/T, =118m• FR=cFR2 dL(B||ne) cFR=2.63110-13 1/T• CM=cCM3 dL(B
2ne) cCM=2.45610-11 1/mT2
• Equilibrium ne0(R,Z), B0(R,Z) from Thomson Scattering and EFIT• On right is plot of GYRO ne/ne0 and Br/B vs. R (at Z=0)
– Simulations don’t span entire cross-section, at least use what we’ve got– Would be a little more realistic to run a global simulation, still can’t include pedestal
0.45 0.5 0.55 0.6 0.65 0.7 0.75 0.8 0.85 0.9−1
−0.5
0
0.5
1x 10
−3
R (m)
GYRO fluctuations, Z≈0
(δne/n
e0)/50
(δBr/B)
23
Guttenfelder, APS-DPP 2014, New Orleans LA
Let’s examine equilibrium first
• Using EFIT (in this case actually .geq from TRANSP plasma state)
• Shown are three polarimeter chords (1,2,4) where data was acquired
24
0.4 0.6 0.8 1−0.6
−0.4
−0.2
0
0.2
0.4
0.6
ψ
0.4 0.6 0.8 1−0.6
−0.4
−0.2
0
0.2
0.4
0.6
Bφ
0.4 0.6 0.8 1−0.6
−0.4
−0.2
0
0.2
0.4
0.6
BR
0.4 0.6 0.8 1−0.6
−0.4
−0.2
0
0.2
0.4
0.6
BZ
0.02
0.04
0.06
0.08
0.1
0.12
0.14
0.16
0.18
0.2
0.22
−6
−5.5
−5
−4.5
−4
−3.5
−3
−2.5
−2
−0.4
−0.3
−0.2
−0.1
0
0.1
0.2
0.3
0.4
−0.8
−0.6
−0.4
−0.2
0
0.2
0.4
0.6
Guttenfelder, APS-DPP 2014, New Orleans LA
0.4 0.5 0.6 0.7 0.8 0.9 1 1.1−0.8
−0.6
−0.4
−0.2
0
0.2
0.4
0.6
0.4 0.5 0.6 0.7 0.8 0.9 1 1.10
5
10
15
20
25
dψ/d
l (de
g/m
)
R (m)
ψfr = 11.7874 (deg) ψ
cm = 3.0974 (deg)
Bφ/10
BR
BZ
B⊥/10
B||
ne
FRCM
Calculated equilibrium Faraday Rotation bigger than Cotton-Mouton effect, matches experimental measurement
• FR=cFR2 dL(B||ne) (cFR=2.63110-13 1/T), =118m• CM=cCM3 dL(B
2ne) (cCM=2.45610-11 1/mT2)
• Quantities along polarimeter chord #2 shown, e.g. B||=(BRdR+BZdZ)/dL
• Relatively flat density profile, differential FR and CM phase shift follows B|| and B
2, respectively
• Integrated phase shift (2d) gives FR=11.8 deg, close to exp. FR=11.3 deg
• Shown previously to work well by Bergerson, RSI (2010), Xu thesis (2013)
25
Chord #2
Guttenfelder, APS-DPP 2014, New Orleans LA
Incorporating GYRO fluctuations by interpolating in lab space
• For each polarimeter chord (R,Z), determine corresponding GYRO (r/a, )• Interpolate ne(r/a,) to obtain ne,pol
• Interpolate A||(r/a,) onto a 5-point stencil in (R,Z)• Calculate BR, BZ from A||(RR,ZZ)
– To lowest order in s/R BR=-B/BA||/dZ, BZ= B/BA||/dR• Project along chord to obtain B||,poldL = (BRdR + BZdZ)
0.5 0.6 0.7 0.8−0.2
−0.1
0
0.1
0.2
δne (1020 m−3)
R (m)
0.5 0.6 0.7 0.8−4
−2
0
2
4x 10
−5 δA|| (Wb/m)
R (m)
chord #1
#2
#4
0.5 0.6 0.7 0.8
−60
−40
−20
0
20
40
R (m)
δB||,pol
(G)
26
Guttenfelder, APS-DPP 2014, New Orleans LA
Predicted Faraday rotation dominated by neB||0,Interferometric signal ~300 bigger than Faraday rotation
• (neB||0)~6(ne0B||)• ne~0.11020 m-3 B||~210-3 T• ne0~2.51020 m-3 B||0~310-1 T
27
0.7 0.8 0.9 1 1.1 1.2−0.1
−0.05
0
0.05
0.1
0.15components of synthetic polarimeter signal
t (ms)
deg
FR
~δn⋅B
~n⋅δB
• int=cint dL(ne)• FRcFR2B||0 dL(ne)• cint ~ 300 cFR2B||0
Will estimate sensitivity of Faraday rotation to interferometric contamination due to non-collinearity of two FIR paths
0.7 0.8 0.9 1 1.1 1.2−40
−20
0
20
40
60
t (ms)
deg
synthetic interferometer signals
chord #1
#2
#4
chord #2
Guttenfelder, APS-DPP 2014, New Orleans LA
Simulated synthetic polarimeter phase predicts Faraday rotation fluctuations ~5x smaller than experiment
• Experimental values averaged over 200 ms polarimeter signal (1250-1450 ms)• RMS amplitude ~5x bigger than synthetic
– rms exp = [0.14, ------ ,0.26] degrees– rms syn = [0.029, 0.037, 0.051] degrees
• Possible sources of error: (i) haven’t matched heat fluxes (possible change in turbulence character) (ii) local, not global, simulations, (iii) not simulating edge and/or near-axis, (iv) contamination from interferometric effects, (v) …
281300 1300.1 1300.2 1300.3 1300.4 1300.5 1300.6
−0.6
−0.4
−0.2
0
0.2
0.4
0.6
0.8polarimeter chord #1 measurement
deg
t (ms)
11.3 degree mean subtracted
100
101
102
103
10−13
10−12
10−11
10−10
10−9
10−8
10−7
10−6
f (kHz)
deg2 /H
z
polarimeter power spectra
chord #1
#2
#4
Simulation + synthetic
experiment
Guttenfelder, APS-DPP 2014, New Orleans LA
Future work
• Complete flux-matching simulations with sufficient resolution– Will MTM become a more significant contributor?
• Clarify discrepancy between measured and synthetic polarimeter signal– If not resolved with local flux-matched simulations consider running global
simulations
• Apply synthetic diagnostics for comparison with other available turbulence data (PCI, TCI and reflectometer)
• Possibly run new experiment in 2015 to obtain ion measurements (planned for 2014)
29