nonlinear instability plasma...
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Graduate School of Energy Science Kyoto University, Japan
Joint ICTP‐IAEA College on Advanced Plasma PhysicsInternational Centre for Theoretical PhysicsTrieste, Italy, 18‐29 August 2014
Nonlinear instability and plasma dynamics
• August 19 : Structure/dynamics of fluctuations in fusion plasmas• August 19 : Nonlinear instability and plasma dynamics• August 21 : Interaction between different scales
Y. Kishimotocollaboration with K. Imadera and J.Q. Li
Planetary environment and fusion plasmas
( )
( ) ( ) ( )
ZF
ZF tot ZF LSS
EE E E
( )
( ) ( ) ( )
ZFZF
ZF turb ZF LSSt ZF LSS
EE E E
• Micro‐turbulences• Macro‐flows
(sometime with low mode)• Large scale structure
World dominated by
No external heatingFully self‐sustained
( )ZFE
( )turbE
( )LSSE
PQ Q
What is the role of ZF and LSS on transport ?
Micro‐scale vortices are embedded in macro‐scale flows
ther
mal
diff
usiv
ity
1
0200 400
2
600
zonal flow
ON
OFF
time
Interaction between flows & fluctuations
g
21
2
xV
gk yy
Shearing decorrelationof turbulence
x
xxx k
x
kysfkyk dk
dkkik
tk
222 , 11
Shearing decorrelation is a local interaction in k space
2'222EVktk
Fluctuation with different time and spatial scales
Meso-scaleMacro-scale Micro-scale
810~510~k
e1
i1
a1
a1 i1 xk
yk
Ion scale
Electron scale
eρ1
Ion scale
[courtesy of Kagei (JAEA)] [Y. Kishimoto et al.’96, PoP ] [Y. Idomura et al.’04, IAEA, NF]
• Coexistence of different scale fluctuations :
θ
r rk
θk
n0
t + n
t + n0v+nv =0
nk
t + n0vk + nk vk
k=k +k = 0
n0
t + Re nkvk
* exp 2k t k
= 0
Flux : nD
Quasi-linear transport due to drift wave (1)
),(~)(),( 0 txnxntxn
),(~)(),( 0 txxtx uuu
kkE -ikk
vk = -i ck kb
B = -i cTi
eB ekTi
kbr + krrb
nk(ExB)
n0 = -i
n0 vkn0k
= - *ik
ekTi
= - *ik r
k2
ekTi
1 - i kk r
dibi vk*: dia-magnetic drift frequency 2
00
00
BennTe
d
Bv
vdj = - cTjejB
1Lpj
= - jvjLpj
= - jvjLnj
1+j
rkbk ˆkˆk rb|| Coupling between ion motion and density gradient (drift wave)
Quasi-linear transport due to drift wave (2)
DB = 116
cTeB
= nkvk r*
k = - n0 cTi
eB kb
*ik
k2
ekTi
2
exp 2kt k
D = - cTieB
kbLn k*i
nkn0
2exp 2k t k
0
cf. nLDn
2icTcf. eB i i i civ
Step size: gyro-radiuscorrelation time : gyration period
TB2
B aB
2
B cf.aD
Quasi-linear transport due to drift wave (3)
D = - cTieB
kbLn k*i
nkn0
2exp 2k t k
poloidal direction
radial direction
Zero transport 0k
k=tan-1 kk r
nk(ExB)
n0 = -i
n0 vkn0k
= - *ik r
k2
ekTi
1 - i kk r
Phase angle between density and potential
nken0
ekTe
1-ik
Quasi-linear transport due to drift wave (4)
Correlation time
BEc
dtd kr ~
2
0
0
BE
Bv
ckk
ckk
r Bcki
BEc
~
Correlation time
generation linear growth rate LkNk
r L Nt t k k kk r steady state
0 NkLk LkNk
ck 1~1~
kk
kc
c
rB
ckD
22 ~~~
annihilation scattering of fluctuation due to various origins
Assuming Markov process
0
1~n r
nn L k
r n r,t +n0 ~ 0
• Mixing length estimate
• Wave breaking estimate
E × B
r
2
2* 0
exp 2 ~b n kr
ncTD k L teB n k
k k k
k
BEc
dtd kr ~
2
0
0
BE
Bv
ckk
ckk
r Bcki
BEc
~Correlation time
kk
kc
c
rB
ckD
22 ~~~
Assuming Markov process 1~ ~b kr
k r
ckB k
0
1 1~ ~ ~k k k
b s r s r n
e nT k k v k L n
*~ ~k kr i 1 1~ ~i Tr
r Lk
1 2
21*2 2~ ~ ~ ~k i i i
i i T i ir r T T
vD k L vk k L L
0 ~ ir
2~ ~k i i
r T
cTDk eB L
0 ~ i Tr L
2~ ~k i
r
cTDk eB
: gyro-Bohm
: Bohm
JT‐60/JET class
ASDEX‐U/JFT‐2Mclass
ITER/ Demo class
ri = 4mma = 2mri /a = 2x10-3
ri = 7mm, a = 1mri /a = 7x10-3
ri = 7mma = 0.35mri /a = 2x10-2
1m 2m 3m 4m 5m 6m
1 2
~ i i
T
cTeB L
2 2 12 1~ ~ s
r n n
eWT k L L
2
~ s
n
WL
~ s
n
WL
Fig.1. Ion heat conductivity vs tokamakminor radius. [Copied from Fig.3 in Ref. [1].
[1] Z. Lin et al., PRL 88, 195004 (2002).
An interesting observation in global gyrokineticsimulations of toroidal ITG turbulence is that forsmall device size plasma, the fluctuations aremicroscopic and local, that transport is diffusive,while the resulting turbulent transport is not gyro-Bohm, shown in Fig.1.[1] The local transportcoefficient exhibits a gradual transition from aBohm-like scaling for small device sizes to agyro-Bohm scaling for future larger devices inthe presence of self-consistent zonal flows.
Fig. 4. Effective heat diffusivity of three global gyrokinetic codes as a function of ρ∗. (copied from Fig.5 in Ref. 3)
[3] Sarazin, et. al, Nucl. Fusion 51 (2011)
tit kk
k rkkArA exp,,ˆa
TB
pB
Weak turbulence : 1nTturb
Strong turbulence: 1~nTturb
Fluctuating filed in confinement device
tit kk
k rkkr exp,,
22
81 BEturb
φ
rB
θ
02
0E B
E Bv
E~* *
x x k kk
nv n v
* *3 32 2x x k k
k
Q pv p v
*~ ~ sin( )x nnu n v
exp( ), exp( )nn n i v v i
Phase difference causes flux :
Particle motion :
eee pendtdv
mn bEb ˆˆ||
Electron motion (parallel to the magnetic field
jv
j||v
πr2
kk ,kk
k
πR2
→ Adiabatic response (simplest case)
e
nmnm T
exnn
,
0,~
Ion motion (perpendicular to the magnetic field
iiii
ii pendtdmn )( 0BvEv
20
0
BE
Bv
200
00
BennTe
d
Bv
cD B
B 2/22
//2
0
00 B
1th order drift
2th order, polarization drift
)(1
0cEp tBvv
tit kk
k rkkr exp,,
nmitrnm
nm exp,,
,
rm
Lmk
2
Rn
Lmk
2
a
TB
pB
Low frequency ion motion
Drift wave caused by drift
0
iii n
tn v
0ˆ~
0
Bcn
tni b
0
yv
t di *
1 1e e sy d y y y s
n n
cT cT vnk v k k keB n x eB L L
tvy dKey point: Density perturbation is in phase with potential, just drift wave
ie
e nTenn ~~
0
ed kv *
Physical picture of slab ITG mode
y
z
p-
p+
x
Ti,e(x)
drift dir.
B
Ey
Ey
Slab ITG: coupling between and ion sound wave
∆
Ti
yBv ˆ12
00
0
xn
neBcT
Benn i
dp
(1 )ee
en iT
0
0
1 )ey d y *
T nω k υ k ω ( iδeB n x
ei nn ~~
Drift wave becomes can be unstable, leading instability
Drift wave : a plasma oscillation propagating along diamagnetic drift direction
If some mechanism may pressure perturbation is out of phase with the potential perturbation, the drift wave becomes “unstable”
//0 0 // / / 0 / /
ˆ ( ) 0e e eie
bm n en p m nt en
Electron drift wave
iδ model :
Collisional electron drift wave: 2 2*
*/ /
ye ei
ce
ki
k
)(1
0cE
ep tB
vv
20
0
BE
Bv
1
cj
jv
j||v
0
pEii ntn
vv i en n
0)1( 22
byt d
xyyx
222 ],[
Hasegawa-Mima equation
2 2(1 ) [ , ] 0dt y
0ee
en n x
T
for zonal flows : =1for others : =0
Turbulence in quasi-two dimensional bounded system
2 21 0dv bt y
Drift wave : Hasegawa-Mima eq.
B
E
n
Conserving quantities 22W :Energy 222U :Enstrophy
ˆEcv zB
pci
c dvB dt
2 2ˆ1 0Rh hv z h ht y
Rossby wave : Charney equation
zρfv Hρgp
g
ˆcg z Hf
v 02p
gH d hf dt
v
With adiabatic election, simplified 3-field equations for ITG mode
2 2
2/ / / /
1 (1 )
1 2 ( )2
in n
D i D
a at L L
p
/ // / / / ip
t
2 cos sinD rf f with
Toroidal curvature for toroidal ITG mode
Parallel compression for slab ITG mode
2
2/ / / / / /
1(1 ) (1 )3
1 8 4 ( )2
ii i
n n
D i D i
p a at L L
p k p
Discussion: Ignoring toroidal curvature and parallel compression term,
reduced to just drift wave; Ignoring toroidal curvature effects, reduced to slab ITG Ignoring parallel compression, reduced to toroidal ITG;
Fluid equation of ITG in tokamak
+
-(A) S=0.2
(B) S=0.1 : weak magnetic shear
[Kishimoto,Li, et al., IAEA ’02]
0
2
4
6
8
10
2 3 4 5 6 7
e/[(
e/Ln)(
cTe/e
B)]
e
s= 0.1
s=0.2(A )
(B )
s=0.4
1 0 -2
1 0 -1
1 0 0
1 0 1
2 3 4 5 6 7
<|d
(z) /d
x|>2 /2
( a )
s= 0 .1
s= 0 .2
e
(B )
(A )
s= 0 .4
Conditional flow generationin high pressure region
( )
( ) ( )
ZF
Z turb ZF
EE E
Energy partition low
fluctuation energy = turbulent part + laminar part
Turbulence dominated by large scale structure
6η 0.1s e
e1
i1
a1
a1 i1 xk
yk
Ion scale
Electron scale
eρ1
Ion scale
turbulence + zonal flow
turbulence
► Emergence of large scale vortices micro scale ETG
ZFMacro
Scale KH
a1
a1
► Mixed turbulence with• micro-scale ETG• ETG driven ZF• ZF driven Large scale structure
Coherency and phase between Ey and n
s = 0.1, e = 3
f (Vte/Ln) f (Vte/Ln) f (Vte/Ln)
f (Vte/Ln) f (Vte/Ln) f (Vte/Ln)
Turbulent plasma Zonal flow dominated plasma
s = 0.1, e = 6
Micro-scale region Macro-scale region
High coherency, but keeping phase relation that produces no transport
turbulence
Zonal flow
total
Change of Magnetic shear (tilting)
Magnetic shear increase
Magnetic shear decreaseIncrease instability free energy
heating
Anomalous nature
Anomalous nature
total
total
turbulence
turbulenceZonal flow
Zonal flowand large scale
structure
Zonal flow
Zonal flow
Zonal flow
turbulence
turbulence
total
total
total
Self‐organization in high pressure state
Linearly more unstable Nonlinearly more stable
[Koshyk-Hamilton, JAS, 01]
Hasegawa-Mima Equation
0φφbyφv
tφ1 2
d2
Charney Equation
0hhzyhv
th1 2
R2
ˆ
wave number10-3
10-2
10-1
100
101
102
0.1 1
<(k
x,y)2 >/
2
kx or k
y
t=400
kx
ky
kx
zonal flow
Comparison of atmospheric zonal flows