Simula'ng Plasma Turbulence
- D. R. Hatch
ICTP Oct 2018
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Simula'ng Plasma Turbulence D. R. Hatch ICTP Oct 2018 1 - - PowerPoint PPT Presentation
Simula'ng Plasma Turbulence D. R. Hatch ICTP Oct 2018 1 Turbulence 2 Turbulence: Enduring Fascina'on and Challenge Da Vinci `Turbulence is the most important unsolved problem of classical physics.' - Richard Feynman - 3 Turbulence:
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`Turbulence is the most important unsolved problem of classical physics.'
Da Vinci
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‘When I die and go to Heaven there are two maOers on which I hope for
quantum electrodynamics and the other is the turbulent mo'on of fluids. And about the former I am really rather
Da Vinci
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Millenium Prize: Existence and Smoothness of Navier Stokes ‘This is the equa'on which governs the flow of fluids such as water and air. However, there is no proof for the most basic ques'ons one can ask: do solu'ons exist, and are they unique? Why ask for a proof? Because a proof gives not
Da Vinci
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How long can rolling waters remain impure?
Dye in Pipe Flow
transpor'ng par'cles, momentum, heat, etc.
flow or molecular diffusion (typically factor of ~Re faster—i.e. 104-107!)
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εk ∝k−5/3
Kolmogorov
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Large scales Small scales
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q è 0, incompressibility, etc.
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– G. G. Howes et al. ApJ, (2006). – A. A. Schekochihin et al. ApJS, (2009).
– G. G. Howes, et al. Phys. Rev. Le/., (2011). – J. M. TenBarge et al. Physics of Plasmas, (2012). – D. Told et al. Phys. Rev. Le/. (2015).
– J. M. TenBarge, et al. Physics of Plasmas (2014). – M. J. Pueschel,, et al. ApJS, (2014).
– Tatsuno et al. Phys. Rev. Le/. (2009) – Banon-Navarro et al. Phys. Rev. Le/. (2011) – Teaca et al. Phys. Rev. Le/. (2012) – Hatch et al. Phys. Rev. Le/. (2011,2013)
– AstroGK (based on fusion code GS2) – GENE – Others
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vE = E × B B2
2 2
2 1 B B B B q v m v
j j d
∇ × =
⊥
Outboard Side of Torus Ion Temperature Gradient Instability (ITG)
Mike Beer - Thesis
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Outboard Side of Torus Ion Temperature Gradient Instability (ITG)
vE = E × B B2
2 2
2 1 B B B B q v m v
j j d
∇ × =
⊥
+
−
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+ + + + + + + + +
Outboard Side of Torus Ion Temperature Gradient Instability (ITG)
vE = E × B B2
2 2
2 1 B B B B q v m v
j j d
∇ × =
⊥
+
−
εk ∝k−5/3
Kolmogorov
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Large scales Small scales
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Hydrodynamic turbulence: Navier Stokes equation è Kolmogorov picture:
Saturation è Energy drive at large scales balances with dissipation at small scales. k Drive Dissipation Inertial Range
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2
2 v
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Q=gradient drive C=collisional dissipa'on k Drive Dissipation Inertial Range Contrast:
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Q=gradient drive C=collisional dissipa'on Small scales develop in velocity space even at drive scales in real space. èScale range of drive and dissipaHon overlap!
(Also a cascade at higher k Banon Navarro, PRL, 2011.)
∂ ˆ fn ∂t = ηiiky π
1 4
k2
⌅
2 ¯ φδn,0 iky π
1 4
¯ φδn,0 ηiiky ⇧ 2π
1 4
¯ φδn,2 ikz π
1 4
¯ φδn,1 ikz ⇤⇧n ˆ fn1 + ⇧ n + 1 ˆ fn+1 ⌅ νn ˆ fn + ⌦
k
xky kxk⇥ y
⇥ ¯ φk ˆ fn,kk. Hermite representa'on:
f(v) =
⇤
⌦
n=0
ˆ fnHn(v)ev2
Equa'ons: DNA code: Reduced GK model: As simple as possible while s'll capturing dynamics of interest. Hatch et al PRL ’13 Hatch et al JPP ’14 Hatch et al NJP ‘16
p = π1/4 √ 2 ˆ f2 + π1/4 2 ˆ f0 u = π1/4 √ 2 ˆ f1 φ = D(k⊥) ˆ f0
Simple rela'ons between moments and Hermites
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∂ε(f)
k,n
∂t = ηiQkδn,2 − Ck,n − J(φ)
k δn,1
+Jk,n−1/2 − Jk,n+1/2 + N (f)
k,n, n,2 νnε(f) k,n −ν⊥(kx,y / kmax)8
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−ν⊥(kx,y / kmax)8
ε(f )
k,n = 1
2π1/2| ˆ fk,n|2
Gyrokine'c energy in Hermite space: Energy evolu'on equa'on:
ε = c0n−1−αe−n/nc
Vary collisionality: constant power law, changing nc Varying driving gradients and collisionality
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n
νn1/2
∂ ∂n⟨kz⟩n √nεn = −νnεn − αεn
Compare Schekochihin et al. JPP 2016