Discovery Research in Magnetic Fusion Energy or “How we learn about magnetic containment and the potential to reduce the cost of fusion energy with alternate configurations” Mike Mauel Columbia University http://www.columbia.edu/~mem4/ ! National Undergraduate Fusion Fellowship Program 13 June 2014 ! The slides for this talk are online at: http://www.apam.columbia.edu/mauel/mauel_pubs/NUF2014-DiscoveryMagFusion.pdf Outline • Columbia University’s plasma physics experiments
• Plasma containment depends upon the shape of the magnetic field
• What can we learn by changing magnetic topology? Examples…
• Stellarator: optimizing the helical plasma torus
• Spheromak: Magnetic self-organization
➡ Levitated dipole: “simplest” axisymmetric magnetic confinement
• Fusion energy needs discoveries to overcome challenges to economic viability
• Over 200 tokamaks and soon there will be ITER… We know a lot about the challenging economics of tokamak-based fusion energy
• Discoveries are needed from creative new scientific investigations (2004)
Columbia University Collaborator Dr. Otto Octavius Stabilize Fusion in NYC… Magnetized Plasma Physics Research at Columbia University
A %XTERNAL TO VESSEL FERRITIC WALL OPTION
• CNT Stellarator FERRITIC MATERIAL
B )N VESSEL FERRITIC WALL OPTION
• HBT-EP Tokamak FERRITIC MATERIAL
• CTX/LDX Dipole Magnetized Plasma Physics Research at Columbia University
• CNT Stellarator
• HBT-EP Tokamak
• CTX/LDX Dipole How Do Magnetic Fields Confine Ionized Matter?
Equations of magnetic confinement… Plasma Pressure (No monopoles) B =0 Plasma ⌅ · (No charge accumulation) J =0 Current ⌅ · (No unbalanced forces) 0 = P + J B ⌅ ⇤ (Magnetostatics) B = µ J ⌅⇤ 0
Magnetic Torus How Do Magnetic Fields Confine Ionized Matter?
Equations of magnetic confinement… Plasma Pressure (No monopoles) B =0 Plasma ⌅ · (No charge accumulation) J =0 Current ⌅ · (No unbalanced forces) 0 = P + J B ⌅ ⇤ (Magnetostatics) B = µ J ⌅⇤ 0 Surfaces of constant Magnetic Torus plasma pressure form nested tori J B = P ⇥ ⇤ B P =0 · ⇤ J P =0 not so easy without · ⇤ symmetry (chaotic fields) Four Plasma Tori
• Axi-symmetric toroid with external poloidal currents (fails)
• Axi-symmetric toroid with internal toroidal current (“levitated dipole” inside the plasma)
• Axi-symmetric toroid with (mostly) external poloidal currents and (mostly) plasma toroidal current (“tokamak”)
• Non-symmetric plasma torus with external helical coils (“stellarator”) How FAILSto make TO CONFINE a magnetic PARTICLES torus?
Coil Current
Toroidal Field from Poloidal Currents How to make a magnetic torus?
Coil Current
Poloidal Field from Toroidal Currents How to make a magnetic torus?
Plasma Current
Combined Toroidal and Poloidal Field (Tokamak) How to make a magnetic torus? 3.3 m
1.7 m
1.8 m
HBT-EP Columbia University
NSTX-U DIII-D PPPL General Atomics Combined Toroidal and Poloidal Field (Tokamak) More than 200 Tokamaks (We know how tokamaks work relatively well.)
ITER Magnetic Fusion Optimization Depends on Shape Fundamentally, the behavior of magnetically-confined plasma depends upon the shape of the magnetic flux tube…
Interchange Instability Bending Field ➠ Effective g How to make a magnetic torus? High q ← Increasing Toroidal Field ← Low q
Fundamentally, the behavior of magnetically-confined plasma depends upon the shape of the magnetic flux tube…
Combined Toroidal and Poloidal Field (Tokamak) How to make a magnetic torus?
Helical Coils (Wound in Place)
+Toroidal Currents
Non-symmetric plasma torus with (mostly) external helical currents (Stellarator) How to make a magnetic torus? Quasi-Isodynamic Torsatron (no parallel currents)
Heliac
Quasi-Symmetry (Like tokamak along helical path)
Non-symmetric plasma torus with (mostly) external helical currents (Stellarator) Why study different magnetic tori?
• Fundamental study • Confinement science, heating, sustainment, heat flux to boundaries, fluctuations, instabilities, complex behaviors of high-temperature matter, magnetized “bright matter” throughout the universe, …
• Fusion energy • Magnetic torus has to “work” and make fusion • Achieve fusion’s promise of safety and environmental attractiveness • Have economically viable applications (like high payload space power and propulsion, non-carbon electrical power on Earth, …) Toroidal Magnetic Configurations Self-Organized
FRC
RFP High Toroidal Field! Low Toroidal Field! High q Low q
ST
Tokamak Dipole
Externally Controlled
NRC BP (Mauel) 19 NRC BP (Mauel) 20 Outline
• Plasma containment depends upon the shape of the magnetic field
• What can we learn by changing magnetic topology? Examples…
• Stellarator: optimizing the helical plasma torus
➡ Levitated dipole: “simplest” axisymmetric magnetic confinement
• Spheromak: Magnetic self-organization
• Fusion energy needs discoveries to overcome challenges to economic viability
• Over 200 tokamaks and soon there will be ITER: what we know about the economics of tokamak-based fusion energy
• Discoveries are needed from creative new scientific investigations
• Columbia University’s plasma physics experiments Levitated Dipole Experiment
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7 Launcher/Catcher MIT Plasma Science & Fusion Center 09/24/2006 11:11 PM
Administration Computers & Networks Calendar Safety Search PSFC Search
8 Channel Plasma Science & Fusion Center
Laser Detection Massachusetts Institue of Technology and RT Controller Electron
Cyclotron Waves
About PSFC Research People Education News & Events Library General Info
The Plasma Science & Fusion Center (PSFC) is recognized as one of the leading university research laboratories in the physics and engineering aspects of magnetic
confinement fusion. 2 m
77 Massachusetts Avenue, NW16, Cambridge, MA 02139 phone: 617-253-8100, [email protected]
http://www.psfc.mit.edu/ Page 1 of 1 Lifting, Launching, Levitation, Experiments, Catching
J. Belcher First Levitated Dipole Plasma Experiment Discover a New Regime by Linking Space and Laboratory Science
• Leveraging space physics to discover a Fast Particles in Space and Lab
new regime: axisymmetric, steady-state, Cassini (Jan 2001) Hot Electron Radio Emission compressibility (ω* ~ ωd), β ~ 1, no field- aligned currents, shear-free, bounce-averaged gyrokinetics, wave-particle dynamics, …
• Magnetospheric configuration but not a “miniature magnetosphere” (high β stability but without polar losses and Hot Electron LDX (Jul 2005) X-Ray Emission field-aligned currents)
• Toroidal magnetic confinement, but not a “miniature fusion reactor” (controlled tests of transport, stability, and self- organization) Our Space Environment is Complex and Highly Variable With Concurrent Plasma Processes and Important Questions to Answer
Van Allen Probes (A&B) Launched August 2012 Discovered New 3rd Radiation Belt (2 MeV e-) then annihilated by passage of interplanetary shock ScienceExpress, Baker, et al., 28 Feb 2013 INNER MAGNETOSPHERIC MODELING WITH THE RICE CONVECTION MODEL
FRANK TOFFOLETTO, STANISLAV SAZYKIN, ROBERT SPIRO and RICHARD WOLF Department of Physics and Astronomy, Rice University, Houston, TX 77005, U.S.A.
Abstract. The Rice Convection Model (RCM) is an established physical model of the inner and middle magnetosphere that includes coupling to the ionosphere. It uses a many-fluid formalism to describe adiabatically drifting isotropic particle distributions in a self-consistently computed electric field and specified magnetic field. We review a long-standing effort at Rice University in magneto- spheric modelingINNER with the MAGNETOSPHERIC Rice Convection Model. MODELINGAfter briefly describing WITH theTHE basic RICE assumptions Electrons andINNER equations MAGNETOSPHERIC that make up the core ofCONVECTION the RCM, we MODELING present MODEL a sampling of WITH recent results THE using the RICE Ions model. We conclude with a briefCONVECTION description of ongoing and MODEL future improvements to the RCM. Key words: magnetosphere-inner,FRANK TOFFOLETTO, numerical STANISLAV modeling, plasma SAZYKIN, convection, ROBERT ring SPIRO current and RICHARD WOLF FRANK TOFFOLETTO,Department of Physics and STANISLAV Astronomy, Rice University, SAZYKIN, Houston, TXROBERT 77005, U.S.A. SPIRO and 180 Semi-collisional FRANKPlasmasphere1.RICHARD Introduction TOFFOLETTO WOLF ET and AL. Ring Current Department of Physics and Astronomy, Rice University, Houston, TX 77005, U.S.A. Earth’s inner magnetosphere is home toTABLE an interesting I variety of particle popula- tions andAbstract. plasmaComparisonThe processes. Rice Convection of equations While Model radiation-belt of (RCM) ideal is MHD an established particles with those physical (> 1MeVenergy)have used model in of the the RCM inner and been elegantlymiddle magnetosphere described that by includes the adiabatic coupling to theorythe ionosphere. developed It uses a in many-fluid the earliest formalism days to describe adiabatically drifting isotropic particle distributions in a self-consistently computed electric Electrons Ions of theIdealfield space MHD and age specified e.g., magnetic (Northrop, field. We 1963), review aRCM this long-standing picture effort can at be Rice disrupted University inby magneto- severe Electrons For eachIons species and invariant energy λ, η is solar-windspheric disturbances modeling with the (Li Riceet Convection al.,1993).Theringcurrent,consistingmainlyof Model. After briefly describing the basic assumptions ∂ρ ∂ conserved along a drift path. ions and∂tand electrons equations(ρv) that in make0 the up 10–200 the core of KeV the RCM, energy( ∂t we presentv range,k(λk a, samplingx,t) carries of) aη recentk large resultsS( fractionηk using) L( the ofηk) Abstract. The∂model.+ Rice∇ We· Convection conclude= with a Modelbrief description (RCM) of ongoing is+ an⃗ and established future⃗ improvements·∇ physical= to the model RCM.− of the inner and the total( particlev )( energyρv) ofj theB magnetosphereP jk B and enoughPSpecifick current Entropy to substantially! middle magnetosphere∂t +⃗·∇ that⃗ includes= ⃗ × ⃗ coupling−∇ to⃗ the× ⃗ ionosphere.=∇ It uses a many-fluidγ formalism2 to affect the∂Key overall words: magnetosphere-inner, magnetic5/3 configuration. numerical modeling, Coexisting2 plasma in convection, the same5 ring/3 region current of spacepV = λ η ( ∂t v )(Pρ− ) 0 P 3 k ηk λk V − ,λk constant ∑ s s describe adiabatically+⃗·∇ drifting isotropic= particle distributions= | in a| self-consistently= computed3 electrics as the radiationB 0P belt and ring current is theart plasmasphere,ofthemagnetic consistingfieldmode mainlyl. of field andparticles specified∇· with⃗ = magnetic energies field.< 1eV.Whiletheplasmaspheredoesnotdirectlyaffectthe We review a long-standing! effort at Rice University in magneto- B µ j Included in magnetic field, but j j . sphericmagnetospheric modeling∇× ⃗ with= themagnetic0 ⃗ Rice Convection field configuration, Model. it After still contains briefly describing most of the⃗ the̸ mass= basick of⃗k assumptions ∂B 1. Introduction and equationsthe magnetosphere. thatE make up⃗ The the plasmasphere core of the RCM, exhibitsIncluded we a present wide implicitly range a sampling in of mapping. interesting of recent plasma results using the ∇× ⃗ =−∂t ! model. Wephenomena concludeEarth’s which with inner affect a magnetosphere brief wave description propagation, is home of toongoing anparticle interesting and loss, future variety and heating improvements of particle processes popula-W( toλk, in thex,t) RCM. 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For example, the per- formanceions of and geosynchronous electrons in the communications 10–200 KeV energy spacecraft range, carries can be a impaired large fraction by the of Specific Entropy! 2 guaranteethe that totalSpecific the particle current energyEntropy density of the! magnetosphere carried by each and enough species currentk,crossedwiththemag- to substantially γ effects of surface charging and the resultant2 arcing in solar panels. MeV outer- pV = λs ηs netic field,affect balances the overall the magnetic gradient configuration.pV ofγ the partial Coexisting pressure in the same for region species of spacek,underthe 3 ∑ belt ‘killer electrons’ constitute another1. Introduction important= ∑ λ space-weathers ηs hazard; they are s assumptionas the that radiation the inertial belt and termsring current in the is3 the momentums plasmasphere, equation consisting mainly are negligible. of In the RCM,particles the adiabatic-compression with energies < 1eV.Whiletheplasmaspheredoesnotdirectlyaffectthe condition takes the form of assuming that Earth’s innerSpacemagnetospheric magnetosphere Science Reviews magnetic107: is175–196, field home configuration, 2003. to an interesting it still contains variety most of the of mass particle of popula- the energy©2003 invariantKluwer Academicλ is Publishers. conserved. Printed Magnetic in the Netherlands. field models used as input to the tions and plasmathe magnetosphere. processes.k The While plasmasphere radiation-belt exhibits a wide particles range of interesting (> 1MeVenergy)have plasma classical RCMphenomena always which assume affect wave propagation,B 0. While particle those loss, and input heating models processes also in generally been elegantly described by the adiabatic⃗ theory developed in the earliest days satisfy a conditionthe ring current andB radiationµ∇ beltj·,thecurrentusedinthemagneticfieldmodelis, populations.= of the space ageBecause e.g., many∇× (Northrop, space-based⃗ = 0 ⃗ assets 1963), are located this picture in the inner can magnetosphere be disrupted and by severe in general,the not underlying constrained ionosphere, to understanding be equal to the the physical sum processes of the RCM-computed that control this partial solar-windcurrents j disturbancesregion;however,someRCMrunsarenowbeingperformedusingamagnetic of space has (Li importantet al. space,1993).Theringcurrent,consistingmainlyof weather implications. For example, the per- ⃗k ionsfield and that electronsformance is consistent of in geosynchronous the with 10–200 RCM-computed communications KeV energy spacecraft currents range, can (Section carries be impaired a 5). largeby As the discussed fraction of effects of surface charging and the resultant arcing in solar panels. MeV outer- thepreviously total particlebelt Faradays ‘killer energy electrons’ law of theconstitute is included magnetosphere another in important the RCM and space-weather enough implicitly, hazard; current through they to are substantially the time- affectdependent the overall mapping magnetic between configuration. ionosphere and Coexisting magnetosphere. in the Like same MHD, region the of RCM space asgenerally the radiation assumesSpace belt Science that and Reviews there ring107: current is175–196, no electric 2003. is the field plasmasphere, component consisting along the magnetic mainly of ©2003Kluwer Academic Publishers. Printed in the Netherlands. particlesfield; however, with energies the RCM< 1eV.Whiletheplasmaspheredoesnotdirectlyaffectthe drift equation includes the effect of gradient-curvature magnetosphericdrifts, which is magnetic equivalent field to writing configuration, a separate it Ohm’s still contains law for most each species of the massk and of theincluding magnetosphere. an extra The gradient/curvature plasmasphere term. exhibits a wide range of interesting plasma phenomena which affect wave propagation, particle loss, and heating processes in the ring current and radiation belt populations. Because many space-based3. assets RCM are Algorithms located in the inner magnetosphere and the underlying ionosphere, understanding the physical processes that control this Figure 1 outlines the essential logical structure of the RCM. This chart elaborates regionthe basic of space scheme has first important proposed space by (Vasyliunas, weather implications. 1970). The For differences example, between the per- formancethe scheme of geosynchronous shown in Figure communications 1 and that given spacecraft by Vasyliunas can be are impaired the additional by the effectsboxes of representing surface charging various and model the inputs resultant and arcing outputs in as solar well as panels. modifications MeV outer- to beltinclude ‘killer such electrons’ effects constitute as self-consistently another important computed space-weather ionospheric conductance. hazard; they The are core of the calculation, in the center of the figure, displays the basic algorithmic timeSpace loop. Science The Reviews RCM steps107: in175–196, time (typically 2003. with steps of 1–5 sec.), iteratively solving©2003 EquationsKluwer Academic (4) and Publishers. (12), with time-dependent Printed in the Netherlands. inputs. Equation (4) is used to advance the particles, using the velocity computed from Equation (1). Equation (1) Self-Organized Mixing: Dye Stirred in Glass CHAPTER 5. MAGNETIC RECONSTRUCTIONS: RESULTS 88 New Regime: High β, Turbulent Self-Organized, Steady-State Supported shot 100805045 Levitated shot 100805046 Self-Organized, Steady-State Profiles atS100805046 High β • 20 kW injected electron cyclotron waves
• Density proportional10.5 GHz on to injected power10.5 GHz off 10.5 GHz on 10.5 GHz off 6.4 GHz off 6.4 GHz off 6.4 GHz on 6.4 GHz on • Plasma2.45 GHz energy on proportional2.45 GHz to offpower 2.45 GHz on 2.45 GHz off • Peak plasma density 1012 cm-3
• Plasma energy 250 J (3 kA ring current)
• Peak β ~ 40% (100% achieved in RT-1)
• Classical fast particles〈Eh〉~ 54 keV
• Peak〈Te〉> 0.5 keV (thermal)
Sustained, dynamic, steady state … • Plasma density and electron pressure naturally approach “canonical” profile shape determined magnetic flux-tube volume, δV. • Density evolves at rates described by bounce-averaged gyrokinetic theory. Time [sec] Time [sec]
Figure 5.1: Overview of supported shot 100805045 and levitated shot 100805046. The top row shows that the heating power profile was the same in both shots. The second row shows that the vessel pressure was similar on both shots. The third row shows that during levitation the change in the magnetic flux measured by a flux loop at the outer mid-plane (diameter 5 m) is nearly a factor of two greater than during supported operation. The last row shows the phase measurement of the 4 chord interferometer: black (77 cm tangency radius), red (86 cm), green (96 cm), and blue (125 cm). The large phase change on the inner chords during levitation show that the electron density is much higher and centrally peaked during levitated operation. The light red and light blue vertical lines indicate the times used in the reconstructions described in the next sections. The vertical black lines mark times when the input power changes. Quantitative Verification of Inward Turbulent Pinch @(¯n V ) @ @(¯n V ) = S + D @t h i @ @ Line Density Shows Strong Pinch (a) Side View With levitated dipole, inward turbulent Onlytransportwith a setsLe vprofileitate devolutionDipole
Levitated
Upper Hybrid Turbulent pinch Resonances from measured Cyclotron fluctuations Resonances