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Title: Prsentation PowerPoint


1
3D modelling of edge parallel flow asymmetries
P. Tamainab, Ph. Ghendriha, E. Tsitronea, Y.
Sarazina, X. Garbeta, V. Grandgirarda, J. Gunna,
E. Serrec, G. Ciraoloc, G. Chiavassac aAssociati
on Euratom-CEA, CEA Cadarache, France bEuratom-UKA
EA Fusion Association, Culham Science Centre,
UK cUniversity of Provence/CNRS, France
2
Strong poloidal asymmetries in parallel Mach
number measured on all machines
Expected situation symmetrical parallel
flow parallel Mach number at the top M u//
/cs 0
Experimental results asymmetrical flow M0.5
at the top universal phenomenon (X-point and
limiter)
Asakura, JNM (2007)
3
Hard to reproduce with transport codes without
any ad-hoc hypothesis
  • Modelling attempts with 2D transport codes
    Erents, Pitts et al., 2004
  • evidence for influence of drifts (ExB and
    diamagnetic)
  • ad-hoc strong ballooning of radial transport
    necessary to recover experimental amplitudes

D?LFS / D?HFS 200
Zagorski et al., 2007
4
TOKAM-3D a new numerical tool able to tackle
consistently this kind of issue
3D - full torus
closed open field lines
limiter
simulated region
  • 3D fluid drift equations B. Scott, IPP 5/92,
    2001
  • density, potential, parallel current and Mach
    number M
  • Bohm boundary conditions in the SOL
  • flux driven, no scale separation gt Turbulence
    Transport

5
3D drift fluid equations
ExB advection
continuity
curvature
parallel dynamics
diffusive transport
charge
vorticity definition
parallel momentum
parallel current
6
Neoclassical vs turbulent regime
D?/DBohm ?
1
t
?
?
  • high D? neoclassical equilibrium with drifts
    gt only large scale effects
  • low D? turbulent regime gt impact of small
    scales

7
Neoclassical regime growth of poloidal
asymmetries even without turbulence
  • neoclassical equilibrium with ExB and
    diamagnetic drifts
  • non-zero Mach number at the top M0.25
  • uniform D? ? not linked to poloidal distribution
    of radial transport
  • mechanism combination of global ExB drift and
    curvature

8
Is that enough to recover experimental results?
  • larger amplitude than that found in previous
    studies but still lower than experiments
  • radial extension in the SOL not deep enough

? p/2 (top)
r/a 1.07
The answer seems to be NO there must be
something else
9
Edge turbulent transport can generate large
amplitude poloidal asymmetries
Density n
  • no limiter gt previous large scale drifts effect
    not included
  • low diffusion D? /DBohm0.02
  • gt turbulent transport

10
90 of the flux at the LFS
  • Mach number at the top Mtop0.35

?LFS ?r / ?tot ?r 0.9
  • asymmetry due to ballooned transport

HFS
LFS
M
lt?rgt
11
How do these two mechanisms overlap in a complete
edge simulation?
  • turbulent regime in closed open flux surfaces
  • filament-like structures generated in the
    vicinity of the LCFS and propagate in the SOL

12
The superposition of both mechanisms allows a
recovery of experimental features
  • experimental large amplitudes Mtop0.5 recovered
    even in far SOL
  • good qualitative and quantitative agreement with
    experimental data

13
SUMMARY / CONCLUSION
  • Parallel flows poloidal asymmetries
  • confirmation of the existence of 2 distinct
    mechanisms
  • large scale drifts gt coupling between ExB,
    curvature and the limiter
  • ballooning of turbulent radial transport gt
    coupling between turbulent scales and curvature
  • superposition of both mechanisms leads to good
    agreement with experimental data without
    requiring ad-hoc hypotheses

14
The TOKAM-3D Model
  • Fluid modeling with no scale separation
  • 3D fluid drift equations matter, charge,
    parallel momentum, parallel current (generalized
    Ohms law) Scott, IPP 5/92, 2001
  • isothermal closure in current version

15
3D drift fluid equations
ExB advection
continuity
curvature
parallel dynamics
diffusive transport
charge
vorticity definition
parallel momentum
parallel current
16
Geometrical dependances
Impact of field inversion and of limiter position
  • 3 identical cases limiter poloidal shift and B
    reversal (?B drift sign)

LFS
HFS
(Bx?B)ions
M0
Bottom, normal ?B
17
Return parallel flow mechanism driven by ExB
and curvature
  • step 1 establishment of large poloidal ExB
    drift at LCFS
  • step 2 curvature effects trigger symmetric
    inhomogeneities
  • step 3 ExB drift advects the density and breaks
    the symmetry

ExB
18
Origin of the Mach number asymmetry
ExB drift curvature plays a major role
  • step 1 establishment of large poloidal ExB
    drift at LCFS

?r? sign changes gt drift direction does not
change with field direction
LCFS
?
?
?
r
r
r
Bottom, normal ?B
Bottom, reverse ?B
Equatorial, normal ?B
19
Origin of the Mach number asymmetry
ExB drift curvature plays a major role
  • step 1 establishment of large poloidal ExB
    drift at LCFS
  • step 2 curvature effects trigger symmetric
    inhomogeneities

No curvature effect at equatorial plane
LFS
top
N
N
N
?
?
?
Bottom, normal ?B
Bottom, reverse ?B
Equatorial, normal ?B
20
Origin of the Mach number asymmetry
ExB drift curvature plays a major role
  • step 1 establishment of large poloidal ExB
    drift at LCFS
  • step 2 curvature effects trigger symmetric
    inhomogeneities
  • step 3 ExB drift advects the density and breaks
    the symmetry

LFS
top
ExB
ExB
N
N
N
?
?
?
Bottom, normal ?B
Bottom, reverse ?B
Equatorial, normal ?B
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