An alpha-squared dynamo may use a tensorial alpha effect rather than an isotropic coefficient. For constant alpha tensor and magnetic diffusivity , a steady nonzero Fourier mode with wavevector satisfies and . Anisotropy can change both the critical alpha magnitude and the preferred wavevector direction.
For an isolated bounded conductor of uniform magnetic diffusivity , contained in a sphere of radius and matched to a decaying potential field in an insulating exterior, dynamo action requires maximum stretching rate . Here bounds the largest eigenvalue of the rate-of-strain tensor throughout the flow and time. Use fluid boundary conditions eliminating the stretching boundary term, for example a no-slip boundary condition, and no imposed energy input. The proof combines the magnetic free-decay spectral bound with the magnetic energy equation. This is a necessary condition, not a sufficiency criterion; changing magnetic boundary conditions changes the spectral constant.
Hartmann number 2026-10-06
The Hartmann number measures the strength of magnetic coupling relative to viscous and resistive effects in a channel:
Here is the channel half-width, the kinematic viscosity, the magnetic diffusivity and the electrical conductivity. In Hartmann flow, large produces thin magnetic-viscous wall layers and a flatter, slower core for fixed pressure gradient.
For constant alpha tensor and positive magnetic diffusivity , the steady anisotropic alpha-squared dynamo equation is
For a nonzero Fourier mode with wavevector , this becomes . Rotational symmetry of the alpha tensor in the horizontal plane lets us set , with . The component equations are
Substitute the first and third into the second. A nonzero steady amplitude requires . Conversely, this relation supplies a nonzero amplitude through the same component equations, and the solenoidal magnetic-field constraint is automatically satisfied. Thus the steady-mode condition is
For the first form, no division by is needed. The quotient applies when that denominator is nonzero, in particular for and .
Put and . The derivative of is
For , the derivative changes from negative to positive at . For it is nonnegative throughout the allowed half-line and the minimum is at . Therefore the optimized uniaxial alpha dynamo threshold is
Both expressions agree at . If the horizontal boundary conditions permit , a nonzero mode instead has and the infimum is zero as ; it is not attained by a nonzero wavevector. The exactly uniform mode has no diffusive or alpha curl term and must be treated separately.
Let be the rate-of-strain tensor of an incompressible flow, and let be the supremum over the conductor of its largest eigenvalue. State Backus' necessary condition for dynamo action with its magnetic boundary conditions: an isolated bounded conductor of uniform positive magnetic diffusivity , surrounded by an electrical insulator with a decaying potential exterior field, and no imposed magnetic field or boundary energy input. For definiteness take a no-slip boundary condition on the fluid, which eliminates the stretching surface term. If the conductor lies within a sphere of radius and , a necessary condition for a nondecaying dynamo is
The constant is the free-decay spectral bound for an insulating exterior, not a universal constant for every magnetic boundary condition. The condition is necessary, not sufficient, and involves maximum stretching rather than an rms velocity.
To see both the condition and the growth-rate bound, include exterior magnetic energy:
This follows from the resistive induction equation and integration by parts, with the stated boundary assumptions. The magnetic free-decay spectral bound is . For a sphere its lowest mode is the dipolar poloidal free-decay mode; enclosing a smaller conductor gives the same valid lower bound. Since , we obtain
Integrating this differential inequality gives decay whenever . More generally the exponential rate of the field norm, rather than of its squared energy, satisfies
Simply discarding the nonnegative resistive dissipation already proves the requested maximum-strain bound. The energy exponent is twice the field-amplitude exponent.
For the alpha-Omega dynamo model, write , , and . Direct differentiation gives
For , use the weighted energy estimate for two coupled modes and form the positive weighted norm . The inequality gives
For each fixed and model parameters, this norm is equivalent to the amplitude norm; its square-root exponential rate is therefore bounded by , uniformly over all admissible . Maximizing over gives
The exponent is also achievable in order of magnitude. Choose the admissible constant . The growing eigenvalue of the two-component system has real part . Its maximum occurs at and equals . Thus the bounded-modulation alpha-Omega growth estimate has the scaling
This means the maximum over allowed modulations and wavenumbers, not that every bounded modulation grows; supplies no regenerating alpha coupling.
The Omega effect rapidly makes toroidal field from poloidal field, but exponential dynamo action also requires the slower alpha effect to regenerate the poloidal component. The coupled amplification rate is of order rather than ; shortening the wavelength to increase it also increases magnetic diffusion as . Their optimal balance gives and growth . The Backus' necessary condition for dynamo action estimate controls stretching alone and does not incorporate this regeneration bottleneck. A shear without regeneration can give transient amplification but not this sustained exponential feedback.
Use Faraday's law and the solenoidal magnetic-field constraint . In the nonrelativistic, single-fluid approximation, neglect Hall and other nonideal electromotive terms and use the moving-conductor moving-conductor Ohm law, . Infinite electrical conductivity with finite current gives , hence
This is the ideal magnetohydrodynamic induction equation. For comparison, neglecting displacement current in Ampère-Maxwell equation gives ; with uniform finite electrical conductivity it produces magnetic diffusion , where the magnetic diffusivity is . The ideal approximation requires a large magnetic Reynolds number . Dropping displacement current is useful for this finite-conductivity comparison, but Faraday's law and the ideal Ohm relation already suffice for the ideal induction equation.
Expanding the curl and using the solenoidal magnetic-field constraint gives the material derivative form
Combine this with mass conservation, , to obtain
Now parametrize a material curve by a fixed label : obeys . Differentiating with respect to shows that its tangent evolves by . This is exactly the same linear ordinary differential equation as for . Initially parallel tangents remain parallel by uniqueness, with a label-dependent proportionality factor constant along each particle trajectory. Thus magnetic field lines are transported as material curves, wherever the field and fluid flow are smooth and the field is nonzero. This is the field-line form of magnetic flux freezing.
For the flux statement, take a material surface and let , . Both tangents obey . Its oriented material surface element is . Differentiating the cross product, rather than assuming its transport rule, gives
Equivalently, , with . Contracting this derived rule with the induction equation gives a pointwise cancellation:
Integrating over the fixed material labels therefore proves conservation of flux through an open material surface:
The surface need not be closed; its boundary is carried with the fluid. The result follows from material transport, rather than from the zero flux through a closed surface.
For a homologously shrinking cloud, write and keep its shape factors fixed. Conserved mass gives ; conserved magnetic flux gives . Thus the gravitational and magnetic energies scale as
where are dimensionless geometry factors. Both grow in magnitude as , so collapse cannot reduce magnetic support relative to gravity while the mass-to-flux ratio is frozen. With negligible gas pressure, contraction lowers the combined potential energy only when its coefficient of is negative. Consequently a necessary critical mass-to-flux ratio condition is
Here denotes the magnitude of the conserved threading flux. The numerical coefficient depends on geometry and boundary conditions; the scaling argument does not determine it or make the condition sufficient in the presence of other support.
For adiabatic pressure support during gravitational collapse, . The pressure-support scale is , so relative to either gravity or magnetic energy,
Pressure becomes more important as decreases if , equally important in scaling if , and less important if . In particular, a monatomic perfect gas with becomes increasingly pressure supported. For isothermal pressure support during gravitational collapse, the isothermal equation of state gives , so is constant and : isothermal pressure becomes less important during collapse. The same comparisons hold against magnetic support because its energy has the same scaling as gravity.
Use the fully developed flow branch of Hartmann flow. Translation invariance along the walls makes the velocity and induced magnetic field functions of alone. Incompressible flow and zero normal velocity at the walls give and hence . The zero divergence of the magnetic field makes constant, equal to the imposed . There is no forcing in ; the homogeneous -components obey the same coupled viscous-resistive equations as the -components, with zero boundary data. Multiplying them by and , integrating by parts and adding gives
Thus , establishing the asserted forms on this fully developed flow branch. This is a symmetry reduction of the steady channel model, rather than a claim that every possible flow in a channel is translation invariant.
The current density and Lorentz force density are
The advective acceleration vanishes because acts on fields independent of . The -component of the magnetohydrodynamic momentum equation therefore gives
The -component must also balance: it requires . Hence a compatible pressure is ; the specified streamwise pressure gradient does not require the ordinary pressure to be uniform in . This accounts for the magnetic pressure of the induced field.
The resistive induction equation with constant magnetic diffusivity gives . Since , its curl has -component . Steadiness consequently gives
Finally the no-slip boundary condition gives , and the normal magnetic field boundary condition gives . The coupled equations and all wall conditions follow directly from momentum balance and magnetic induction.
For a solenoidal vector field and constant magnetic diffusivity , the magnetic induction equation is
It combines Faraday's law with the moving-conductor relation for electrical conductivity, neglecting displacement current. With incompressible flow, its advective form is .
Resistive magnetohydrodynamics retains finite magnetic diffusivity in the coupled evolution of a conducting fluid and its magnetic field. The resistive induction equation allows field diffusion relative to the fluid, while the magnetohydrodynamic momentum equation includes the Lorentz force density. It contrasts with the zero-diffusivity limit of ideal magnetohydrodynamics.