Orbit physics in discontinuous fields: openquestions
David Pfefferle1
1The University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia
Mini-course/workshop on the application of computational mathematics toplasma physics
June 24-27, 2019 - Canberra, Australia
VENUS-LEVIS: energetic particles
1 guiding-centre / full-orbit• non-canonical Hamiltonian
formulation (2nd order)• curvilinear coordinates• switching algorithm in high
field-variations
2 supra-thermal populations• NBI, ICRH, fusion alphas• full-f slowing-down / delta-f• ∼ ASCOT, ORBIT,SPIRAL
∂tfhot + v · ∂xfhot + (E + v ×B) · ∂vfhot = C[fhot, fM ] + S(x,v, t)D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 2 / 14
VENUS-LEVIS: energetic particles
1 guiding-centre / full-orbit• non-canonical Hamiltonian
formulation (2nd order)• curvilinear coordinates• switching algorithm in high
field-variations
2 supra-thermal populations• NBI, ICRH, fusion alphas• full-f slowing-down / delta-f• ∼ ASCOT, ORBIT,SPIRAL
Vlasov-Boltzmann via PIC
∂tfhot + v · ∂xfhot + (E + v ×B) · ∂vfhot = C[fhot, fM ] + S(x,v, t)
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 2 / 14
Magnetic confinementCharged plasma particles wrap around magnetic field-lines
helical motion along uniform magnetic field
In uniform magnetic field B =Bez, motion is helical
z = v||t+ z0(xy
)= R(−ωt)ρ⊥ +X
where R(θ) is the rotation matrixaround ez of angle θ
ω = qB/m the Larmor frequency
ρ⊥ = mqBb×v⊥ is the Larmor radius
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 3 / 14
Drifts due to non-uniform field“Grad-B” drift
upward drift due to non-uniform magnetic field
“grad-B” drift fromspatially-varying field-strength |B|
VB =µ
qb× ∇B
B
where µ =mv2
⊥2B
is the “mag-
netic moment”
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 4 / 14
Drifts due to non-uniform field“Curvature” drift
upward drift due to curved magnetic field
curvature drift when field-lines are bending (curved)
Vκ =mv2||
qBb× κ
where κ = b · ∇b is the field-
line curvature
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 5 / 14
Mirror trapping in “magnetic bottles”
consequence of magnetic momentand energy conservation
m
2v2|| + µB = E
where µ =mv2
⊥2B
is the magnetic moment
Mirror devices
• historically first magneticconfinement devices
• suffer from huge losses atboth ends
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 6 / 14
Particle motion in tokamaks
tokamak fields (toroidal + poloidal) ⇒ passing orbits
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 7 / 14
Particle motion in tokamaks
tokamak fields (toroidal + poloidal) ⇒ banana orbits
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 7 / 14
3D makes particle motion complexLack of symmetry results in chaotic dynamics
stellarator 3D fields ⇒ complex motion, detrapping, magnetic wells,. . .
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 8 / 14
Toroidal coordinates in magnetic fusion
• toroidal systems often use chart map
Φ : (0, 1)︸ ︷︷ ︸ρ
× (0, 2π)︸ ︷︷ ︸ϑ
× (0, 2π)︸ ︷︷ ︸ϕ
→M ⊂ R3
x = R(ρ, ϑ, ϕ) cos(ϕ)y = R(ρ, ϑ, ϕ) sin(ϕ)z = Z(ρ, ϑ, ϕ)
R(ρ, ϑ, ϕ) = R0(ϕ) + r(ρ, ϑ, ϕ) cos[θ(ρ, ϑ, ϕ)]
Z(ρ, ϑ, ϕ) = Z0(ϕ) + r(ρ, ϑ, ϕ) sin[θ(ρ, ϑ, ϕ)]
• vector potential (1-form)
A(ρ, ϑ, ϕ) = Aρdρ+Aϑdϑ+Aϕdϕ
• magnetic flux (2-form)B = dA ⇐⇒ B = ∇×A
2π
2π
0
1ρ
ϑ
ϕ
rθ
ϕ
ϕ R Z
x
y
z
Φ
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 9 / 14
Full-orbit curvilinear equations of motion
• u = (u1, u2, u3) = (ρ, ϑ, ϕ) ∈ (0, 1)× (0, 2π)× (0, 2π)
• Lagrangian for single charged particle
L(ui, ui, t) = 12mv · v + qA · v − qΦE
= 12gij u
iuj + qAiui − qΦE
gij = ∂ix · ∂jx is the metric tensor (pullback metric)
• Euler-Lagrange equations yield ∇uu = qm(−dΦE + iuB)]
ui =q
m
(Ei + gijεjklu
k√gBl)
︸ ︷︷ ︸E+v×B
− umunΓimn︸ ︷︷ ︸inertiel forces
where the Christoffel symbol
Γimn = gijΓl,mn Γl,mn = ∂lx · ∂2
mnx
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 10 / 14
Advantages/drawbacksof solving orbits in toroidal coordinates
Advantages:
• mapping forward via Φ is easy, but computing the inverse is not
(ρ, ϑ, ϕ) 7→ x = Φ(ρ, ϑ, ϕ), x 7→ (ρ, ϑ, ϕ) = Φ−1(x)
One could pre-evaluate the inverse on a grid and interpolate, but then it is hard to
ensure ∇ ·B = 0 (and other properties).
• fields are semi-analytic functions (Fourier, splines, polynomials)⇒ high accuracy of derivatives
Drawbacks
• evaluation of metric (Christoffel) prone to numerical error
• integrators (Boris-Buneman?)
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 11 / 14
Orbits in SPEC fields
• interface between MRxMHD equilibrium SPEC and VENUS-LEVIS
(Zhisong, Dean)
• energetic particle confinement in Taylor-relaxed states
Open questions:
• SPEC nested toroidal annuli with ideal interfaces ⇒ discontinuous B
• full-orbit OK, but gyrokinetics KO: reduced kinetic model ?
• numerically integrating across interface ?
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 12 / 14
Particle motion in discontinuous fieldsconstant modulus, sheared field (current sheet)
B = cosαex +
{sinαey z > 0
− sinαey z < 0⇐⇒ j = ∇×B = −2δ(z) sinαex
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 13 / 14
Particle motion in discontinuous fieldsconstant modulus, sheared field (current sheet)
B = cosαex +
{sinαey z > 0
− sinαey z < 0⇐⇒ j = ∇×B = −2δ(z) sinαex
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 13 / 14
Particle motion in discontinuous fieldsconstant modulus, sheared field (current sheet)
B = cosαex +
{sinαey z > 0
− sinαey z < 0⇐⇒ j = ∇×B = −2δ(z) sinαex
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 13 / 14
Conclusions and prospective work
• charged particle motion is governed by magnetic field
• full-orbit motion can be solved in curvilinear coordinates
• SPEC/LEVIS interface underway to study energetic particleconfinement in MRxMHD configurations
• guiding-centre approximation is invalid in discontinuous fields ⇒alternative kinetic models
• numerically integrating through ideal interface
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 14 / 14
Nested toroidal flux surfaces (VMEC)
• prescribing the vector potential to be the 1-form
A = Ψt(ρ)dϑ−Ψp(ρ)dϕ
• magnetic flux is (B = ∇×A)
B = dA = Ψ′tdρ ∧ dϑ+ Ψ′pdϕ ∧ dρ
• field-lines lie on surfaces of constant ρ(x, y, z) = C
dρ ∧B = 0 ⇒ B · ∇ρ = 0
• restricted to those surface, B 6= 0 is the symplectic form for aHamiltonian system
dϑ
dϕ=∂Ψp
∂Ψt=
Ψ′pΨ′t
= ι(ρ)dΨt
dϕ= −∂Ψp
∂ϑ= 0
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 15 / 14
• Ψt is the toroidal flux,
∫P (ρ)
B =
∫∂P (ρ)
A = 2πΨt
• Ψp is the poloidal flux,
∫T (ρ)
B =
∫∂T (ρ)
A = 2πΨp
P
T~B
D.Pfefferle (UWA) Orbit physics ANU/MSI mini-course 16 / 14