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3D modelling of edge parallel flow asymmetries. P. Tamain ab , Ph. Ghendrih a , E. Tsitrone a , Y. Sarazin a , X. Garbet a , V. Grandgirard a , J. Gunn a , E. Serre c , G. Ciraolo c , G. Chiavassa c a Association Euratom-CEA, CEA Cadarache, France
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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 aAssociation Euratom-CEA, CEA Cadarache, France bEuratom-UKAEA Fusion Association, Culham Science Centre, UK cUniversity of Provence/CNRS, France
Strong poloidal asymmetries in parallel Mach number measured on all machines M~0 expected M measured M M=+1 M=-1 [courtesy J. Gunn] Expected situation: symmetrical parallel flow parallel Mach number at the top: M = u// /cs ~ 0 Experimental results: asymmetrical flow M~0.5 at the top universal phenomenon (X-point and limiter) [Asakura, JNM (2007)]
Hard to reproduce with transport codes without any ad-hoc hypothesis M~0.5 HFS LFS M=+1 M=-1 [Gunn & al., JNM (2007)] • 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: DLFS / DHFS ~ 200 [Zagorski et al., 2007]
TOKAM-3D: a new numerical tool able to tackle consistently this kind of issue SOL edge centre • 3D fluid drift equations [B. Scott, IPP 5/92, 2001] • density, potential, parallel current and Mach numberM • Bohmboundary conditions in the SOL • flux driven, no scale separation => Turbulence + Transport 3D - full torus closed + open field lines limiter simulated region
3D drift fluid equations ExB advection continuity curvature parallel dynamics diffusive transport charge vorticity definition parallel momentum parallel current
“Neoclassical” vs turbulent regime 8.10-2 D/DBohm ~ * 1 t • high D: “neoclassical” equilibrium with drifts => only large scale effects • low D: turbulent regime => impact of small scales
Neoclassical regime: growth of poloidal asymmetries even without turbulence 1 HFS LFS 0.5 M>0 0 M=0 -0.5 M<0 -1 Parallel Mach number M • neoclassical equilibrium with ExB and diamagnetic drifts • non-zero Mach number at the top: M~0.25 • uniform D not linked to poloidal distribution of radial transport • mechanism: combination of global ExB drift and curvature
Is that enough to recover experimental results? HFS Top LFS LCFS 1 0.25 0 Parallel Mach number Parallel Mach number 0 -1 40 100 θ 160 Minor radius r/ρL • larger amplitude than that found in previous studies but still lower than experiments • radial extension in the SOL not deep enough θ = π/2 (top) r/a = 1.07 The answer seems to be NO: there must be something else…
Edge turbulent transport can generate large amplitude poloidal asymmetries M 1 <rturb>t,, poloidal up/down (m=1,n=0) asymmetry in spite of strongly aligned structures <rdiff>t,, 0 r Density n • no limiter => previous large scale drifts effect not included • low diffusion: D /DBohm=0.02 => turbulent transport
90% of the flux at the LFS LFS HFS 0.4 0 90% of total flux -0.4 • Mach number at the top: Mtop~0.35 LFS r / tot r ~ 0.9 • asymmetry due to ballooned transport: HFS LFS M <r>
How do these two mechanisms overlap in a complete edge simulation? HFS LFS HFS LFS N M • turbulent regime in closed + open flux surfaces • filament-like structures generated in the vicinity of the LCFS and propagate in the SOL
The superposition of both mechanisms allows a recovery of experimental features • experimental large amplitudes Mtop~0.5 recovered even in far SOL • good qualitative and quantitative agreement with experimental data
SUMMARY / CONCLUSION • TOKAM-3D: • new generation of edge codes: 3D transport & turbulence across LCFS success of fully consistent approach • on-going development for model and code improvements • Parallel flows poloidal asymmetries: • confirmation of the existence of 2 distinct mechanisms: • large scale drifts => coupling between ExB, curvature and the limiter • ballooning of turbulent radial transport => coupling between turbulent scales and curvature • superposition of both mechanisms leads to good agreement with experimental data without requiring ad-hoc hypotheses
The TOKAM-3D Model buffer zone periodic buffer zone Fluid modeling with no scale separation • 3D fluid drift equations : matter, charge, parallel momentum, parallel current (generalized Ohm’s law) [Scott, IPP 5/92, 2001] • isothermal closure in current version
3D drift fluid equations ExB advection continuity curvature parallel dynamics diffusive transport charge vorticity definition parallel momentum parallel current
Geometrical dependances HFS LFS HFS LFS M=0 (BxB)ions M=0 (BxB)ions Bottom, reverse B Equatorial, normal B Impact of field inversion and of limiter position • 3 identical cases: limiter poloidal shift and B reversal (B drift sign) HFS LFS (BxB)ions M=0 Bottom, normal B
‘Return parallel flow’ mechanism driven by ExB and curvature HFS LFS LCFS M// r top LFS N top LFS ExB N • 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
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 => drift direction does not change with field direction LCFS r r r Bottom, normal B Bottom, reverse B Equatorial, normal B
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
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