The Madison Dynamo Experiment: magnetic instabilities...

of 38 /38
February 28, 2001 The Madison Dynamo Experiment: magnetic instabilities driven by sheared flow in a sphere Cary Forest Department of Physics University of Wisconsin

Embed Size (px)

Transcript of The Madison Dynamo Experiment: magnetic instabilities...

  • February 28, 2001

    The Madison Dynamo Experiment: magnetic instabilities driven by sheared flow in a sphere

    Cary ForestDepartment of PhysicsUniversity of Wisconsin

  • February 28, 2001 2

    Planets, stars and perhaps the galaxy all have magnetic fields produced by dynamos

    Solar prominences and x-rays from sunspots

    Magnetic fields observed inM83 spiral galaxy

    Glatzmaier Roberts simulation of geodynamo

  • February 28, 2001 3

    Outline• What are dynamos?• Some models of astrophysical and geophysical dynamos• The Madison dynamo experiment• Questions for experiments to study

  • February 28, 2001 4

    Physics of magnetic field generation

    1. Charged particles moving in a magnetic field experience the Lorentz force

    2. The motional EMF generates a current

    3. Currents produce a magnetic field

  • February 28, 2001 5

    Dynamos generate magnetic energy from mechanical energy• this is easy if you allow yourself

    the luxury of using insulators and solid conductors

    • in a conductor, currents are generated by motion across a magnetic field

    feedback

  • February 28, 2001 6

    • plasmas or liquid metals • Magnetohydrodynamics: systems are describe by two

    vector fields:– the magnetic field, is generated by electrical currents in the conducting fluid

    In astrophysical dynamos the conductors are simply connected (no insulators) and can flow

    Induction Resistivediffusion

    -The velocity field evolves according to Navier-Stokes + electromagnetic forces

  • February 28, 2001 7

    • in a fast moving, or highly conducting fluid, magnetic field lines are frozen into the moving fluid

    • transverse component of field is generated and amplified• finite resistance leads to diffusion of field lines

    Fluid flow can amplify and distort magnetic fields

    0

  • February 28, 2001 8

    Cartoon of a laminar geodynamo driven by convection and differential rotation

    Differential rotationgenerates Bφfrom dipole

    Thermal convection in rotatingsphere generates cyclonic

    eddies which produce dipole field from Bφ

    Dipole field reinforcesinitial magnetic field

    pB RmBφ ∼

  • February 28, 2001 9

    The kinematic dynamo problem• Start with a sphere filled with a uniformly conducting fluid of

    conductivity σ, radius a, surrounded by an insulating region

    • Find a velocity field V(r) inside the sphere, which leads to growing B(r,t)

    • Ignore the back-reaction of magnetic field on flow

  • February 28, 2001 10

    The kinematic dynamo problem (continued)• Transform to dimensionless variables:

    • Since its linear in B, use separation of variables:

    • Solve eigenvalue equation for given V(r) profile

    ( ), ) λ=∑ B rB(r i iti

    t e

    m0 axRm aVσ=µ

    2

    02

    1

    1ˆ ˆ ˆˆ

    ∂ =∇× × + ∇µ σ∂∂ =∇× × + ∇∂

    B V B B

    B V B B

    t

    Rmt

    21λ =∇× × + ∇B V B Bi i iRm

  • February 28, 2001 11

    Solution technique involves solving induction equation using spherical harmonic basis functions

    ( ) ( ) ( ) ( )( ) ( ) ( ) ( )

    m m m mn n n n

    m m m mn n n n

    ˆ ˆt r Y , s r Y ,

    ˆ ˆT r Y , S r Y ,

    θ ϕ θ ϕ

    θ ϕ θ ϕ

    = ∇ × + ∇ × ∇ ×

    = ∇ × + ∇ × ∇ ×

    V r r

    B r r

    Since fields are incompressible, use vector potential formulation, based on spherical harmonics (Bullard and Gellman, 1954)

    Integration over angles and selection rules produce a coupled set of differential equations, which are solved numerically, using finite differences in the radial direction

    ( ) ( ) ( ) ( )

    ( ) ( ) ( ) ( ) ( )

    2

    2 2 2

    2

    2 2 2

    1

    1

    ,

    ,

    n nS RmS S t S S s T S s S S

    r r r

    n nT RmT T t T T t S T s T T s S T

    r r r

    γ γγγ γ α β γ α β γ α β γ

    α β

    γ γγγ γ α β γ α β γ α β γ α β γ

    α β

    λ

    λ

    +∂ − − = + + ∂

    +∂ − − = + + + ∂

    ∑Solutions for complex eigenvalues are found using inverse iteration

  • February 28, 2001 12

    Growing magnetic fields are predicted for simple flow topologies in a sphere

    • induction equation is solved numerically

    • flow fields are axisymmetric • growth rate depends upon

    m0 axRm aVσ=µconductivity X size X velocity

  • February 28, 2001 13

    Numerical search is used to find optimized velocity profiles forgiven flow topology• Radial function is

    parameterized and search algorithm is used to find low Rmcrit

    ( )

    ( )

    220

    2 22

    220

    2 22

    1

    1

    tt t

    t

    ss s

    s

    r rl lt ( r ) exp( )

    r r w

    r rl ls ( r ) exp( )

    r r wε

    −= − + −

    −= − + −

  • February 28, 2001 14

    Optimized solutions have low critical Rm

  • February 28, 2001 15

    Can these flows be produced in a laboratory?• How big and how much power is required?• Is this simply an linear eigenmode problem in a

    turbulent/mechanically homogeneous system?• Estimates suggest 100 kW, and a=0.5 m with sodium

    should provide Rm=100

  • February 28, 2001 16

    The Dynamo Experiment• 1 m diameter• 200 Hp • sodium• Rm=200

  • February 28, 2001 17

    Why sodium?• the control parameter is the magnetic Reynolds number

    – quantifies relative importance of generation of B field by velocity and diffusion (decay) of B due to resistive decay of electrical currents

    – must exceed critical value for system to self-excite• Sodium is more conducting than any other liquid metal

    (melts at 100 C)– Rm = 120 for a=0.5 m, Vmax=15 m/s

    m0 axRm aVσ=µ conductivity X size X velocity

  • February 28, 2001 18

    Dimensionally identical water experiment is used to create flows and test technology• Laser Doppler velocimetry is

    used to measure vector velocity field

    • Measured flows are used as input to MHD calculation

    • Full scale, half power

  • February 28, 2001 19

    Measurements at discrete positions are used to find radial profile functions for input to eigenvalue code

  • February 28, 2001 20

    Data are fit by profile functions

  • February 28, 2001 21

    Simple baffles and Kort nozzles produce T2S2 flows

  • February 28, 2001 22

    Measured water flows extrapolate to an experimental dynamo in the sodium experiment

  • February 28, 2001 23

    Flows are turbulent and large scale velocity field varies on resistive time scales

    • Large scale velocity field varies with time– Mechanically homogeneous

    • Magnetic eigenmode analysis is only valid on correlation time of velocity fluctuations

    • Turbulence from small scales may play important role

  • February 28, 2001 24

    Flow should be linearly unstable some fraction of the time• Assume mean flow is bounded

    by rms fluctuation levels• Specific geometry corresponds

    to a family of flow profiles• Some fraction of flow profiles

    self-excite• Monte-Carlo analysis shows

    estimates fraction of time in growing phase

    • Temporal intermittency for dynamo?

  • February 28, 2001 25

    Sodium laboratory is 20 miles from Water laboratory (remember high school chemistry)

    Physics Department

    Liquid sodium laboratory

  • February 28, 2001 26

    Molten sodium laboratory is operational• A new laboratory has been constructed for housing the

    dynamo experiment

  • February 28, 2001 27

  • February 28, 2001 28

    The Dynamo Experiment will address several dynamo issues experimentally• Do dynamically consistent flows exist for kinematic

    dynamos?• How does a dynamo saturate?

    – role of Lorentz force on fluid velocity• What role does turbulence play in a real dynamo?

    – energy equipartition of velocity fields and magnetic fields– enhanced electrical resistivity– current generation

  • February 28, 2001 29

    Back-reaction and saturation is due to non-linearities in MHD Equations • Induction equation by itself is linear in B

    – If V is given, linear solutions can be found (kinematic dynamo problem)

    • Induction equation is non-linear if V is affected by B• Navier-stokes is nonlinear in V and JxB

    – V is naturally turbulent– JxB force modifying V we can call the back-reaction

  • February 28, 2001 30

    What happens as the magnetic field energy grows?• Simulations show a strong back-reaction when b=v• Turbulent flows can be strongly modified

    2 2

    0

    1 12 2

    v bρµ

    = %%

  • February 28, 2001 31

    Nonlinear effects in mean-field electrodynamics• α-effect as derived is a kinematic treatment• Treatment did not include back-reaction of induced

    magnetic field on velocity fluctuations

    ( )( )

    ( )( )

    ( )

    0

    0

    23 1

    t

    corr

    corr

    t

    d

    t dt

    B

    t t

    δ

    δ

    τα

    στρ

    δ

    δ−∞

    −∞

    ×

    ′ ′= ∇ × ×

    ⋅∇×≈ ⋅∇× − ⋅∇×

    ×

    ′ ′= ∇ ×

    =

    ×

    +

    E = + v b

    b v B

    v vv v b b

    v b

    v b B

    %%

    %

    % %% %

    %

    %

    %

    %

    %

    See Gruzinov and Diamond’s quasilinearTreatment of backreaction term

  • February 28, 2001 32

    MHD turbulence introduces effects beyond scope of laminar DynamoTheory for Experiments to Study

    – equipartition between magnetic and kinetic energy is predicted for small scales

    – resistivity enhancement due to mixing of magnetic fields on small scales is predicted

    – Currents can be generated by helical velocity fluctuations on small scales

  • February 28, 2001 33

    The β-effect: eddies move flux

    ( )( ) ( )0

    2

    0

    1

    1 3corr

    T ,

    σ α β

    µ σβ σ α

    τσσ β

    µ σβ

    = × − ∇×

    ⇒ + = ×

    ⇒ = ≈+

    J E + V B + B B

    J E + V B + B

    v

    Will there be a turbulent modification to Rm-crit in experiments?

    01T

    RmRm

    µ σβ⇒ =

    +

  • February 28, 2001 34

    Measured turbulence levels already indicate resistivity enhancement may be important• Turbulence levels are measured

    on small experiment

    0

    2

    1

    3

    T

    corr

    σµ σβ

    τβ

    =+

    ≈ v

  • February 28, 2001 35

    Experiment to measure β-effect• Use transient techniques to

    estimate resistivity (measure electrical skin depth of system)

    • Use ω-effect to measure Rm with applied poloidal field

    zB Rm Bϕ =

  • February 28, 2001 36

    Experiment to measure turbulent α-effect• Apply toroidal field. If toroidal

    current is observed, symmetry breaking fluctuations must be responsible

    • Increase B and look for modifications to a-effect

    • Study role of large scale B on small scale fluctuations (saturation through Alfven effect)

    21 corr Bα

    στρ

    ⋅∇×≈

    +

    v v% %

  • February 28, 2001 37

    Summary• water experiments have demonstrated flows which may

    lead to dynamo action• sodium laboratory facility is completed

    – sodium experiment is under construction – sodium operation is imminent

    • initial experiments will search for growing eigenmodes and evaluation of role of turbulence

  • February 28, 2001 38

    Thanks to:

    • The David and Lucille Packard Foundation

    • The Sloan Foundation• NSF• The Research Corporation• The DoE

    Roch Kendrick, Jim Truit Rob O’Connell, Cary ForestErik Spence, Mark Nornberg