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Basis for Classical , Neoclassical and Anomalous Transports in Torus Plasmas
Heiji Sanuki
中国科学院等離子体物理研究所外籍特聘研究員(2009)and
Visiting Professor of ASIPP and SWIP
Lectures in ASIPP, 2011 and 2012, May~June
Basis for Classical, Neoclassical and Anomalous Transports in Torus Plasmas Heiji sanukiPart 1:
Basis of transport theory, Classical DiffusionPart2-1:Neoclassical Transport in Tokamaks and Helical Systems Part2-2:Fluctuation Loss, Bohm, Gyro-Bohm Diffusion and Convective Loss etc.
Understanding of physics in transport process is one of the key issues associated with confinement improvement and/orDevice performance in fusion plasmas.In this lecture, some fundamental equations and physics involved in transport process are briefly reviewed.
Fluctuation Loss, Bohm, Gyro-Bohm Diffusion and Zonal Flow and GAM
PartII-1 and II-2
References1) Kenro Miyamoto: NIFS-Proc. 80, Chapt.10, pp157~pp1872) Kenro Miyamoto: NIFS-Proc. 88, Chapt.7, pp76~pp81 App. E, pp328~341(in Japanese)3) J. Q.Dong ,H.Sanuki and K.Itoh,PoP(2001),NF(2002,2003) 4) Zhe Gao , H.Sanuki, K.Itoh and J.Q.Dong, PoP(2003,2004,2005)5) Zhe Gao, K.Itoh, H.Sanuki and J.Q.Dong,PoP(2006)6) H.Sanuki and Jan Weiland(1979)7) Jan Weiland ,H.Sanuki and C.S.Liu(1980)8) Lots of references involved in this lectures
Topics (PartII-1)(a)Diffusion caused by Ion Temperature Gradient(ITG) modes ,Two cases, (1) mode overlapping and (2) no overlapping (localized)(b) Simulation Models for Turbulent Plasmas(c) Gyro-Kinetic Particle Simulation Model for trapped electron drift modes(d) Gyro-Kinetic Particle Simulation Model for ITG Modes(e) Full Orbit Particle Model(f) Experimental Observations of Heat Diffusivity(g) Brief View of Gyro-Kinetic and Gyro-Fluid Simulation of ITG and ETG Modes(h) Parameter Dependence of Critical Temperature Gradient associated with Heat Conductivity
Topics(PartII-2)(a)Topics on Zonal Flow and Geodesic Acoustic Mode(GAM)(b) Hasegawa-Mima equation in turbulent plasmas(c) Electromagnetic Drift wave Turbulence and Convective Cell Formation( Weiland-Sanuki-Liu Model)(d)Characteristics of Hasegawa-Mima Equation(e) Zonal Flow Generation Mechanism(f) Self-Regulation and Dynamics for Zonal Flow in Toroidal Systems(g) Overview of Recent Progress in Zonal Flow and GAM Studies(h) Eigenmode Behavior of GAM(i) Experimental Observations in EAST and other Tokamaks
Bohm, Gyro-Bohm Diffusion
Bohm Diffusion
2
2
0
2
0
~~
n
k
k
ke
k
k
kn
ky
n
n
eB
T
n
nkD
In saturation level of turbulence, 1ck
,16
1
)(~ 2
2
2
02
eB
TD
x
kn
nD
eB
cx
kk
n
k
Bohm Diffusion Coefficient
Example: Diffusion caused by ITG modes
References:1) S. Hamaguchi and W. Horton, PF B4,319(1992)2) W .Horton et al., PF 21, 1366(1978)3) F. Romanelli and F. Zonca, PF B5,4081(1993)4) Y. Kishimoto et al., 6th IAEA vol.2 581(1997)
Mode fluctuation potential
p
mt
ii
mn
Lk
qR
rrkRq
s
rq
mn
RR
n
B
B
r
m
B
Bbi
r
mk
Rinzimrzr
11
)()(
1k
1~krate,growth maximumat ,8.0~7.0 ,
)/exp()(),,(
//
//
qR: connection length
Example: Diffusion caused by ITG modes (continued)
skr
nn
m
n
mrqrq
sL
qRr
sOkksRqrrr
mmm
kr
k
pi
im
1~--,
11)()(rq
modeITG for ,
)/(~)/)(/(
1m
2/12/1
//
Case1: mode overlapping
Case2: no overlapping(localized)
Example: Diffusion caused by ITG modes (continued)
Case1: mode overlapping(ITG)
seB
T
s
LrD
rks
Lr
kpi
kg
grpi
g
~~)(
/1~ ,
2
2/1
(Bohm DiffusionType)
Case2: no overlapping ITG(weak shear configuration )
p
i
pp
i
ppik
pi
LeB
T
sL
qR
LeB
T
eBL
Tk
sL
qRrD
sL
qRr
~~)(~ 22
2/1
(Gyro-Bohm DiffusionType)
Note: Diffusion is small around minimum q in negative shear configurations
Simulation Models for Turbulent Plasmas
1) Gyro-Kinetic Particle Simulation Model ( W.W.Lee: PF 26,556 (1983))Example1: “Trapped Electron Drift Mode ( R.D. Sydora: PF B2, 1455(1990))For given parameters:
1,1.0/,1836/
,4/,4/ ,)8006464( 0
eieei
ieizyx
mmm
TTaRLLL
#Time evolution of Intensity of (m,n)=(5,3) mode# Relation between spectrum and frequency
Saturation intensity
Growth rate and mode frequency are in good agreement with linear mode analysis
035.0/ eTe
Simulation Models for Turbulent Plasmas(continued)
1) Gyro-Kinetic Particle Simulation Model ( W.W.Lee: PF 26,556 (1983))Example2: “ITG mode ( S.E. Parker et al.: PRL 71,2042(1993)) δf/f method is applied, adiabaticity is assumed for electronsElectrostatic potential in poloidal cross section at both linear and nonlinear saturation levels
Linear Nonlinear
Experimental Observations of Heat Diffusivity (continued)
Gyrokinetic and gyrofluid simulations of ITG and ETG models
#A.M.Dimits et al. Phys. Plasmas 7(2000)969From the gyrofluid code using 1994, an improved 1998 gyrofluid closer, the 1994 IFS-PPPL model, the LLNL and U.Colorad flux-tube and UCLA (Sydora) global gyrokinetic codes, and the MMM model (Weiland QL-ITG) for the DIII-D Base case.
Good fit scaling to LLNL gyrokinetic results
iLn /(i2vti )15.4[1.0 6.0(LT / R)]
Q (R / LT R / LTeff .)Offset linear dependence
Parameter Dependence of Critical Temperature Gradient
Algebrac formula for critical gradient are proposed associated with electron anomalous transport;
Jenko et al.,PoP(2001), Ryter,PRL(2001), Dong et al.,NF(2003), many other papers
Critical gradients of the SWITG modes in wide parameter regions are evaluated to discuss the possibility of the SWITG instability as a possible candidate to explain anomalous transport( Zhe Gao, H. Sanuki, K. Itoh and J. Q. Dong)(see, SWITG and SWETG PoP(2005) )
The scaling of the critical gradient with respect to temperature ratio, toroidicity, magnetic shear and safety factor are obtianed ( 19th ICNSP and 7th APPTC conference in Nara(July, 2005))
Parameter Dependence of Critical Temperature Gradient(continued)
(J.Q.Dong, G.Jian, A.K.Wang, H.Sanuki and K.Itoh, NF43(2003)1183)
max 1
0.0173 i2 1.95 i 1.18
ckmaxTe
eBR
R
LTe
R
LTe
ct
ETG instability
e DB
0.0173 i2 1.95 i 1.18
c
pe
1
LTe
1
LTe
ct
F(n ,ˆ s ,q)
R
LTe
ct
3.51.07 i 0.5 i
2 , 0.5 i 1.5
2.35 2.59 i , 1.5 i 5.0
i Te Ti
eBcTD eB
Increasing temperature ratio,
i Te Ti
is in favor of suppression of modes due to raising TG criticaland dropping coefficient between maximam growth rate andderivation of TG from critical TG
(up to about 3)
Important comment from view point of control of confinement improvement
Experimental Observations of heat diffusivity
# Ion thermal transport could be reduced to neoclassical level with Internal Transport Barrier(ITB’s) in DIII-D# Electron ITB’s are observed in JET tokamak ECH dominant discharges with
Te Ti 3 # ETG driven insta.
ECH experiments in typical Tokamaks(ASDEX Upgrade,RTP,FTU, TCV,etc.)
All four machines clearly show a strong increase of electron transport above a threshold in
Offset Linear Dependence
R LTe
Experimental Observations in DIII-DExperiment employed off-axis ECH heating to change local value of Heat Pulse Diffusivity Model is proposed
ee TT /
kcriteeeeeeHP
e HkTTTfTTH ])/(2)[(/)( .0
# No clear evidence of an inverse critical scale length on heat diffusivity was observed in DIII-D experiments# More improved theory and experimental fine data are needed
JET ECHExperiment
Simulation Models for Turbulent Plasmas
2) Full Orbit Particle Model:References: 1)R.W.Hockney and J.W.Eastwood,” Coumputer Simulation using Particles”, MacGraw-Hill, New York(1981)This model is characterized by introducing “ Super-particle” and “Shaping Factor” and study wave phenomena with long wavelength
2)H. Naitou: J.Plasma Fusion Res. 74.470(1998)
Some limitations:# Short wavelength modes are hardly studied# CPU time is huge, for 1 Ai t
Simulation Models for Turbulent Plasmas(continued)
2) Full Orbit Particle Model:“Toroidal Particle Code(TPC)”# Study electrostatic turbulence, excluding electromagnetic effect# Using Poisson equation instead of Maxwell equationsReferences: 1) M.J.LeBrun et al., PF B5,752(1993)2)Y. Kishimoto et al. Plasma Phys. Contr. Fusion 40, A&&#(1998)“ ITG mode in tokamak”, electrons are adiabatic fluid ( assumed)
Electrostatic Potential plotin negative shear tokamak
“Discontinuity around minimum -q surface in qusi-stationary state”
--minqq
T opics on Zonal Flow(Convective cell)
Hasegawa-Mima equation in turbulent Plasmas
References1) A. Hasegawa and K. Mima, PF 21,87(1978)2) A.Hasegawa, C.G. Maclennan and Y. Kodama, PF22,2122(1979)
Assumpitons involved in Model:1)Continuity eq. for ions, 2)ion inertia effect parallel to B is neglected, 3) ions: cold, 4) electron : Boltzmann distribution,4) ordering:
1~,~,~1
ni
Ldt
d
T opics on Zonal Flow(Convective cell) (continued1)
Derivation of Hasegawa-Mima eq. in turbulent Plasmas
) (,~
,
ions) (,)ˆ(1
,1
ˆ1
)ions (,0)()(
00 electronsfor
T
e
n
nnnn
forzBtdt
d
dt
d
Bz
Bv
forvnnvt
nvn
t
n
e
i
E×B drift Polarization drift
T opics on Zonal Flow(Convective cell) (continued2)
Derivation of Hasegawa-Mima eq. in turbulent Plasmas
0)1(
,0)1(
22422
22322
xyyxt
yv
xyyxc
t
iss
dsss
(Hasegawa-Mima-Charney equation)
Density gradient is negligible small(Hasegawa-Mima equation) 長谷川―三間的式
Note: This equation has two conservations“Energy conservation” and “vorticity conservation”
Electromagnetic Drift Wave turbulence and Convective Cell Formation(1)
#Convective cell formations( electrostatic ) have attracted much interest from turbulence and related anomalous transportin 1970s and 1980s#Electrostatic convective cell formation based on nonlinear driftwave model (Hasegawa-Mima eq.)(1978)
t
( ˆ ˆ )[(ˆ ˆ z ) ][ ˆ ln
n0
ci
]0
# Electromagnetic convective cell formation based on nonlinear drift Alfven wave model ( Sanuki-Weiland model(J. Plasma Phys.(1980))
me mi 1
me mi
( 2
t2 vA
2 2
z 2 VDi
t
t
)
c
B0
(1k//vA
2
2)t
(yxxy
)
Viscosity term
E B nonlinear term
Characteristics of Hasegawa-Mima Equation
Hasegawa-Mima eq. in turbulent Plasmas
2
ˆ2
ˆˆ2
ˆˆ2
ˆ
11
22322
ˆ1
ˆ)(ˆ
asgiven issolusion A
0ˆ)ˆˆ(ˆ)ˆˆ(ˆ)()ˆˆˆ(
ˆ,,ˆ,ˆ,ˆg,Introducin
,0)1(
k
k
kkttyyxx
yv
xyyxc
t
ysnk
yxxyysnt
isss
dsss
(Hasegawa-Mima-Charney equation)
Non-dimensional form
Characteristics of Hasegawa-Mima Equation (continued)
321
22
23322
1
3,21
032132,
111
1
321
k
case heconsider t we,discussion following In the
))(ˆ)(()1(2
1
~~~~
0process, coupling wavehreeConsider t
~~ ),exp()(
~),(
~
32
kk
kkzkkk
idt
d
kkk
xkittx
kkk
kkkkkkk
kkk
k
kkk
Characteristics of Hasegawa-Mima Equation (continued2)
312
312321
2/122
22,13
3,21
2
22,13
3,212
1
2
22,13
3,211
21
2
321
212,133
323,211
2
3122
, ,0mismatchfrequency if also
and ),( wavesintodecay cascade )( , Since
)4
14(
is rategrowth and unstable becomes mode ,04
0d
g.mismatchinfrequency is )( where
)exp(dt
dA ),exp( .,
)exp(~
~,
~~ excited,strongly is mode If
kkkwavekkk
A
AIf
AAdt
dAi
dt
A
tiAAtiAAdt
dAconstA
tiA
k
iii
Characteristics of Hasegawa-Mima Equation (continued3)
3) and modes(1 ofgain energy toleads mode(2) of lossEnergy
..,.,
~)1( ,
~)1(
as energy mode andnumber gIntroducin
213213
22
22
22
constNNconstNNconstNN
kWkk
kN
WN
ppp
rq
pp
p
pp
kWkW
W
kx- dependence ky- dependence
Linear-nonlinearterm are comparableat k-critical
Zonal Flow in DriftTurbulnce
Characteristics of Hasegawa-Mima Equation (continued4)
22/2/22
22
22
22
222
k
p
)2()exp(
~~)1(
2
1),,(
,)1(
2),( ,)1(
2),(
~)
~(
~)
~(
~)()
~~(
~: ofpart frequency low scale Small
~: ofpart frequency high scale Large
ofdensity power spectrum-k ofEvolution Time
pdxpikktxkn
kdnkk
kktxBkdn
kk
kktxA
ABA
kpkpk
kxy
kyx
yyyxxx
LyLxLxLyLysnLLt
n(k,x,t): Power density of high frequency spectrum of ~
Characteristics of Hasegawa-Mima Equation (continued5)
xycv
k
kkvvk
nkxxk
sE
s
sEdynlk
lkk
kkk
~,
~1
)(
0t
330(1992)Lett.A165, Phys. al.et Dyachenko A.I. Ref.
n:~
of spectrumfrequency high ofdensity Power
22
22
k
Zonal Flow Generation
Recent development in both theory and simulation leads physics involved in zonal flow mechanism more understandableReferences:1) Z. Lin et al., Science 281,1835(1998)2) A.I. Smolyakov et al. PRL 84,491(2000)3) P.N. Guzdar , R.G. Kleva and Liu Chen, Phys. Plasmas 87,459(2001)
Shear flow
Zonal flow
Gyro-kinetic particle simulation(Lin et al.)
(A)shearing effect by zonal flow, (B) no shearing effect
Zonal Flow Generation (continued1)
.0)~
))ˆ~
(()(
,0))ˆ~
((~
))ˆ(((
~)ˆ()ˆ
~(
~)-(1
eqs. decoupled following toreduces eq. Mima-Hasegawa
)1(~,~
),(~ ),(~~
,
:
~)( ,
as modified is responceelectron adiabatic and )0
but ,0(surface magneticon cont. is potential flow Zonal
322
3
0
022s
0
ddsszs
zddzss
dzssdssd
zdddze
de
d
ed
x
zyz
zct
zzc
zcn
nzc
t
OOOT
e
Ordering
T
e
T
e
n
n
k
kk
Zonal Flow Generation (continued2)
,~
2
)1()(k
asgiven isy instabilit almodulationfor condition Unstable
)1(
)(~
2
)1)(1(
)1(
asgiven is rategrowth
.,~
and ),exp( form in thegiven is on termperturbati
and ,~
,~~
excited,strongly is Drift wave If
and ~
,~
,~
for equations coupled 4
)(1 ).cos()(
)sin()sin()(~
)cos()sin()(~
)cos()(~~
Model Coupling Wave4consider weHere
2
0
422
2xc
2222
22
0
222222
2222
224
2
0
0
0
20
0
000d
d
dssys
ss
dsxd
ssxsy
si
yxs
d
zdcdsd
zdsdcd
s
dyzxzz
yzxds
yzxdcyd
v
ck
kc
vkkkk
k
kkc
constt
k
vktxkt
tyktxkt
tyktxkttykt
Zonal flow excitation by drift waveFor
xcx kk
Electromagnetic Drift Wave Turbulence and Convective Cell Formation(4)
Coefficients of NS Equation
s(2 kyvDi kyc0 )(km2 ky
2 ),
U ( vDi c0 )(km2 ky
2 ),
Q (1k//
2vA2
2)ky
2(3km2 ky
2 )
L( vDi c0 )
c
B0
2
,
(km2 ky
2 )
Following the theory by H. Sanuki et al.(1972)
ˆ 1(1) a(t)sech[( g
2p)1 2 a( t)( 2vt)exp( iv
p( vt) i
g
2a2(t)dt
0
t
)
p U
s, g
Q
s, at 2a
Modulational insta. condition
UQ (3km2 ky
2 )0
3
1Elongated structure of Convective cellJ.Weiland, H.Sanuki and C.S.Liu, PoF(1980)
Discovery of new truths by studying the past through scrutiny of the old(温故知新 )
Zonal Flow
Typhoon, Giant Red Spot in Jupiter (Zonal flow)、 El Nino, La Nina、 etc Review of vortics
International J. of Fusion Energy (1977-1985, particularly, 77~78, F1R26)# Hermann Helmholtz(1858)(general)# Winston H. Bostick (Vortex Ring)# D.R.Wells and P.Ziajka (Theory and Experiment) , others
What kind of dynamics determines Structure of Vortices(2D) ? ( unsophisticated question)
lx ly or lx ly or lx ly
Vertex(Convective cell,zonal) Motions in Nature
ACKNOWLEDGMENTS
I would like to acknowledge many collaborators and friends for their continuous and fruitful discussions. This visit is supported
by Prof. Li Jiangang and the Chinese Academy of Sciences 、 Visiting Professor for Senior International Scientists(2009 fiscal year) ,and also supported by Prof. Liu Yong as a guest professor of SWIP.
The present topic is also partially discussed under close collaborations with NIFS( K. Itoh, A. Fujisawa et al.),Tsinghua University (Gao Zhe et al.) and SWIP ( Dong Jiaqi ,Wang Aike
et al.) Finally I would like to acknowledge all friends and staffs, students who take care of lots of arrangements of my visiting ASIPP since my first visit, 1991.