The Physics of Fluids · 1975 · 169 citations · 30 references
EngineeringThree-dimensional EquilibriumFluid MechanicsMagnetized Plasma PhysicsPlasma ScienceMagnetized PlasmaPlasma PhysicsMagnetic PlasmaPlasma ModelingMagnetismPlasma TheoryPlasma SimulationMagnetohydrodynamicsPlasma ConfinementMagnetic MomentMirror Magnetic WellsPhysicsSpecial EquilibriaApplied Plasma PhysicFundamental Plasma PhysicPlasma InstabilityMagnetic ConfinementNon-axisymmetric Plasma ConfigurationsMagnetic FieldFinite-pressure Guiding-center Plasma
Finite‑β plasma equilibrium in mirror wells and toroidal devices can now be solved consistently across all guiding‑center fluid time scales, formulated as a classical magnetostatic system. The authors derive the plasma magnetization from three conservation laws and identify field‑geometry conditions that produce omnigenous equilibria, where all particles on a line drift on a common surface, and provide a brief energy‑principle stability analysis. These omnigenous equilibria enable a straightforward link between particle and fluid descriptions, as demonstrated for finite‑β plasmas in magnetic wells, and exhibit particularly simple stability criteria.
Theoretical and numerical methods now give a complete solution to the problem of finite-β plasma equilibrium in mirror magnetic wells and toroidal devices. The equilibria can be made consistent on all of the progressively longer time scales of the guiding-center fluid model, including the particle magnetic drifts and the Coulomb scattering equilibrium of a neutral injected plasma. The theory of equilibrium in the guiding-center fluid model of a finite-β plasma with an arbitrary, anisotropic pressure tensor can be formulated as a classical magnetostatic system: ∇⋅B = 0, ∇×H = 0, B = H + 4πM(B). The plasma magnetization is found explicitly in terms of three physically distinct components related to the laws of conservation of magnetic moment, of longitudinal invariant, and of the sign of the velocity along B of particles that do not undergo mirror reflection. A condition is derived upon the field geometry whereby a large class of special equilibria can be found in which all particles on a given line drift on the same surface, the omnigenous surface. Such systems allow a specially simple connection between particle and fluid models in the guiding-center fluid theory. The usefulness of the theory is exemplified by application to the problem of a finite-β plasma in a magnetic well. Finally, a brief treatment of stability in terms of the energy principle is given. The omnigenous equilibria have particularly simple stability criteria.
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