Effects of a guided-field on particle diffusion in - - PowerPoint PPT Presentation
Effects of a guided-field on particle diffusion in - - PowerPoint PPT Presentation
Effects of a guided-field on particle diffusion in magnetohydrodynamic turbulence Yue-Kin Tsang Centre for Astrophysical and Geophysical Fluid Dynamics Mathematics, University of Exeter Joanne Mason Particle transport in fluids Brownian
Particle transport in fluids
Brownian motion observed under the microscope dispersion of pollutants in the atmosphere cosmic ray propagation through the interstellar medium tracing particle trajectories gives alternative view of the structure of the fluid flow — the Lagrangian viewpoint
Single-particle turbulent diffusion
mean squared displacement: |∆ X(t)|2 , ∆ X(t) = X(t) − X(0) Taylor’s formula (1921) for large t:
- X(t) =
X(0) + t dτ V (τ) |∆ X(t)|2] = 2 t ∞ dτ V (τ) · V (0) = 2tD
assume system is homogeneous and stationary and the integral exists
Lagrangian velocity correlation: CL(τ) = V (τ) · V (0) diffusion coefficient: D = ∞ dτ V (τ) · V (0)
Field-guided MHD turbulence + tracers
Motion of a electrically conducting fluid: ∂ u ∂t + ( u · ∇) u = − 1 ρ0 ∇p + (∇ × B) × B + ν∇2 u + f ∂ B ∂t = ∇ × ( u × B) + η∇2 B ∇ · u = ∇ · B = 0
- f : isotropic random forcing at the largest scales
Field-guided MHD turbulence:
- B(
x, t) = B0ˆ z + b( x, t) Evolution of passive tracer particles: d X(t) dt = V (t) = u( X(t), t)
- X(0) =
α
Typical velocity and magnetic fields
hydrodynamic case (ν = η ∼ 10−3) B0 = 1
The hydrodynamic case
−20 −10 10 20 30 −20 −10 10 20 −20 −10 10 20 30 y ν=1.25e−03 , η=1.25e−03 , B0z=0 , Lz=1 , nx=256 , ny=256 , nz=256 x z 200 300 400 500 −40 −20 20 40 time x(t) − x0 200 300 400 500 −30 −20 −10 10 20 30 time y(t) − y0 200 300 400 500 −40 −20 20 40 time z(t) − z0
The field-guided case (B0 = 1)
−5 5 10 −5 5 10 15 −30 −20 −10 10 20 30 y ν=5.00e−03 , η=5.00e−03 , B0z=1 , Lz=1 , nx=128 , ny=128 , nz=128 x z 200 300 400 500 −15 −10 −5 5 10 15 time x(t) − x0 200 300 400 500 −10 −5 5 10 15 time y(t) − y0 200 300 400 500 −40 −20 20 40 time z(t) − z0
transport suppressed in the field-perpendicular direction!
Scaling of mean-squared displacement
100 200 300 400 50 100 150 200
<(∆x)2> <(∆y)2> <(∆z)2)>
hydrodynamic 100 200 300 400 50 100 150 200 field-guided 10
- 2
10
- 1
10 10
1
10
2
elapsed time, t 10
- 4
10
- 2
10 10
2
10
- 2
10
- 1
10 10
1
10
2
elapsed time, t 10
- 4
10
- 2
10 10
2
t2 t2 t t
Dx=0.24 Dy=0.25 Dz=0.25 Dx=0.04 Dy=0.04 Dz=0.26
ballistic limit: ∼ t2 at small time diffusive scaling: ∼ t at large time, (∆x)2 ∼ 2Dxt , etc
Lagrangian velocity correlation function CL(τ) = V (τ) · V (0)
10 20 30 40 50
τ
- 0.05
0.00 0.05 0.10 0.15 0.20
CL,u CL,v CL,w hydrodynamic
10 20 30 40 50
τ
- 0.05
0.00 0.05 0.10 0.15 0.20
field-guided
hydrodynamic: ∼ exp(−τ), short correlation time field-guided: oscillatory, long correlation time how things depend on the guided-field strength B0?
Diffusivity at different (weak) B0 Urms
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dx
hydro 0.1 0.2 0.3 0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dy
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dz
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1
Urms Dx/Dz
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1
Urms Dy/Dz
diffusion is reduced by B0, including the z-direction anisotropic suppression: Dx, Dy Dz strong Urms( B0) reduces the anisotropy in D’s
Diffusivity at different B0
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dx
hydro 0.1 0.2 0.3 1.0 5.0 0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dy
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1 1.2
Urms Dz
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1
Urms Dx/Dz
0.5 1 1.5 2 0.2 0.4 0.6 0.8 1
Urms Dy/Dz
At strong guided-field strength, B0 Urms Dx, Dy are strong suppressed, anomalous behavior of Dz Dx/Dz , Dy/Dz ≪ 1 for the values of Urms studied
Anisotropic turbulent diffusion
0.7 0.8 0.9 1 0.2 0.4 0.6 0.8 1
brms /Urms Dx/Dz
0.7 0.8 0.9 1 0.2 0.4 0.6 0.8 1
brms /Urms Dy/Dz
−1.5 −1 −0.5 0.5 1 0.2 0.4 0.6 0.8 1
log(B 0z /Urms) Dx/Dz
−1.5 −1 −0.5 0.5 1 0.2 0.4 0.6 0.8 1
log(B 0z /Urms) Dy/Dz
Particle trajectories
5 10 −5 5 −5 5 10 15 20 25 y amp=0.1 , ν=1.25e−03 , η=1.25e−03 , B0z=0.2 , Lz=1 , nx=256 , ny=256 , nz=256 x z −15 −10 −5 5 10 15 20 −10 −5 5 10 15 −15 −10 −5 5 10 15 y amp=3 , ν=1.25e−03 , η=1.25e−03 , B0z=0.2 , Lz=1 , nx=256 , ny=256 , nz=256 x z 2 4 6 8 10 −5 5 10 15 −10 −5 5 10 y amp=0.1 , ν=1.25e−03 , η=1.25e−03 , B0z=1 , Lz=1 , nx=256 , ny=256 , nz=256 x z −5 5 10 15 −5 5 10 −20 −15 −10 −5 5 10 y amp=3 , ν=1.25e−03 , η=1.25e−03 , B0z=1 , Lz=1 , nx=256 , ny=256 , nz=256 x z
B0 = 0.2, Urms = 0.25 Dx/Dz = 0.34 B0 = 0.2, Urms = 1.42 Dx/Dz = 0.95 B0 = 1.0, Urms = 0.29 Dx/Dz = 0.24 B0 = 1.0, Urms = 1.39 Dx/Dz = 0.34
Lagrangian velocity correlation
20 40 60 80 100 −0.005 0.005 0.01 0.015 0.02 0.025
B0z =0.2 , Urms =0.25 CL,u CL,v CL,w
5 10 15 20 −0.1 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8
B0z =0.2 , Urms =1.42
20 40 60 80 100 −0.02 −0.01 0.01 0.02 0.03 0.04
B0z =1.0 , Urms =0.29 elapsed time
5 10 15 20 −0.2 0.2 0.4 0.6 0.8 1 1.2
B0z =1.0 , Urms =1.39 elapsed time
Velocity decorrelation time
10
−1
10 10
1
10
2
10
3
U r m s τx/B0
−1 −2
dynamo 0.1 0.2 0.3 1.0 5.0 hydro
10
−1
10 10
1
10
2
10
3
U r m s τy/B0
−1 −2 10
−1
10 10
1
10
2
10
3
U r m s τz/B0
−1 −2 10
−1
10 10
1
10
2
10
3
u r m s τx/B0
−1 −2
dynamo 0.1 0.2 0.3 1.0 5.0 hydro
10
−1
10 10
1
10
2
10
3
v r m s τy/B0
−1 −2 10
−1
10 10
1
10
2
10
3
wr m s τz/B0
−1 −2
A physical picture . . .
wave induces memory into the system wave frequency: τ −1
A ∼ B0
background turbulence removes memory decorrelation time: τu a competition between τA and τu anisotropic diffusion:
brms/Urms ≈ 1 τA ≪ τu Eu(k) ≈ Eb(k)
quantitative theory in development
Summary
study single-particle diffusion in 3D MHD turbulence transport mostly shows diffusive scaling at large time anisotropic suppression of turbulent diffusion by a guided-field (Dx , Dy Dz) competition between waves and background turbulence
−20 −10 10 20 30 −20 −10 10 20 −20 −10 10 20 30 y ν=1.25e−03 , η=1.25e−03 , B0z=0 , Lz=1 , nx=256 , ny=256 , nz=256 x z 200 300 400 500 −40 −20 20 40 time x(t) − x0 200 300 400 500 −30 −20 −10 10 20 30 time y(t) − y0 200 300 400 500 −40 −20 20 40 time z(t) − z0 −5 5 10 −5 5 10 15 −30 −20 −10 10 20 30 y ν=5.00e−03 , η=5.00e−03 , B0z=1 , Lz=1 , nx=128 , ny=128 , nz=128 x z 200 300 400 500 −15 −10 −5 5 10 15 time x(t) − x0 200 300 400 500 −10 −5 5 10 15 time y(t) − y0 200 300 400 500 −40 −20 20 40 time z(t) − z0