Taking the scalar product of the Lorentz force equation with the velocity gives
The triple product vanishes because the cross product is perpendicular to its first factor. Thus the kinetic energy is constant, even if the magnetic field varies with position: magnetic forces do no work.
In cylindrical coordinates, the radial, angular and vertical equations are
For a nonstationary circular orbit with constant and , the first equation gives . Hence its signed angular velocity is . The sign gives the sense of circulation. The zero root describes a stationary transverse position, not a moving circular orbit. A constant vertical velocity can be superposed to produce a helix.
Define the mechanical angular momentum about the axis by . Multiplying the angular equation by gives
For the inverse-radius magnetic field this becomes . Integrating from an initial radius proves
Let and , so that . Since is constant and the total kinetic energy is constant, the transverse speed squared
is also constant. Substituting the angular momentum relation gives the required radial curve:
Only the region is accessible. For , as , and its horizontal asymptote is . Its derivative is . Thus, when , it has a single maximum at . The positive roots of are the turning points obtained from .
For nonzero and , write . When , two turning points occur at
and the radius is confined between them. At , there is only the finite lower turning point ; tends to zero from above and an outgoing particle reaches arbitrarily large radius. For , only the lower turning point remains and the outgoing radial velocity approaches . The sketch shows these three cases and omits inaccessible negative values of from the physical interpretation.
For completeness, if , rises monotonically from to its asymptote; admissible motion then requires and is radially unbound after any inward branch turns. If , is constant; equality gives a circular orbit rather than escape. Above threshold the outgoing branch escapes, whereas an incoming branch reaches the singular axis in finite time and cannot be continued through it without specifying a nonsingular core field. These cases explain why a borderline escape assertion needs an initial-direction qualification.
The transverse escape velocity threshold for radial escape in an inverse-radius axial magnetic field is
For a radial launch at , , and equality permits marginal escape; for , larger transverse speed guarantees radial escape in forward time after any initial inward leg turns. The singular incoming branch is the exception described above. More general launches at equality can instead give the circular exception . A vertical velocity adds to the total speed but cannot pay the transverse escape-energy requirement; if escape merely means unbounded , any nonzero already achieves that. If , transverse motion is force-free and there is no positive escape-speed threshold.
Put . The magnetic field is the curl of the magnetic vector potential. Since does not depend on the differentiated variable ,
Taking the curl under the source integral consequently gives the Biot-Savart law,
Outside the compact source this differentiation is ordinary differentiation of a smooth kernel. For regular volume currents, the locally integrable derivative kernel gives the same formula at interior points.
For the loop, choose positive current circulating counterclockwise as viewed from the positive -axis. Parametrize its source position and directed line element by
At the denominator is the constant , while
The transverse terms integrate to zero around the loop. The Biot-Savart law therefore yields
The magnetic field is axial, with the stated magnitude for ; reversing the electric current reverses its direction.
In vacuum magnetostatics, the two relevant Maxwell equations are
Orient the unit normal from the minus side to the plus side. Integrating Gauss's law for magnetism over a pillbox straddling the current sheet and shrinking its thickness gives .
To obtain the tangential condition, choose an arbitrary tangent unit vector and an infinitesimal rectangle with its long sides of length parallel to on the two sides of the sheet. Orient its surface normal as , so that its plus-side long edge is traversed along . The line integral in Ampère's law tends to . The enclosed electric current tends to . Hence
Because this holds for every tangent direction and the normal jump is zero,
Here , as required for a surface current density.
The force on a current sheet from the mean magnetic field is
The mean removes the sheet's equal and opposite local self-fields, leaving the field that acts on its current through the Lorentz force. Using a one-sided limiting magnetic field would incorrectly include the sheet's own force.
Choose the planar magnetic field convention , so and . The resistive induction equation, with constant magnetic diffusivity and a suitable time-dependent gauge constant removed, reduces to advection and diffusion of this Cartesian magnetic flux function:
For the specified differential rotation, its mth azimuthal Fourier mode obeys
The physical field is the real part of the complex mode. Substitute . A direct radial differentiation gives
On the left, rigid rotation cancels, leaving . Equating the constant and quadratic coefficients yields
The initial condition fixes and , since the constant C was already factored out. Set . Then the exact quadratic-shear magnetic flux solution follows by differentiation:
Indeed and . Also . For an unspecified initial normalization the second formula has a multiplicative constant , but here .
For and , choose . The asymptotic condition is : then tends to the finite constant and . At any fixed s, differentiating A to obtain the magnetic field multiplies it by factors involving and , which have no additional exponential time dependence. Therefore its envelope decays as
Using the paper's magnetic Reynolds number definition gives the precise scaling
Thus the decay time scales as for positive and fixed m. The mechanism is magnetic phase mixing under differential rotation: winding produces progressively fine radial structure on which magnetic diffusion acts efficiently. For negative , choose the square root with positive real part, replacing by in the decay time. If , the initial harmonic mode simply rotates, with , ; there is no shear-enhanced decay. The printed positive-root and Reynolds-number expressions implicitly use .
Write the poloidal magnetic flux function and toroidal amplitude explicitly in spherical components:
Dotting the magnetostatic equilibrium equation with gives . Since all fields are axisymmetric, the poloidal magnetic field is tangent to the contours of in a meridional section. Thus, locally on regular connected flux surfaces, . This is a local flux-surface statement; disconnected surfaces with the same numerical value of need not have the same pressure without further global assumptions.
Taking the azimuthal component of the Lorentz force gives
Its numerator is the meridional Jacobian determinant of and . Vanishing therefore implies locally on the same regular surfaces. Define
A direct curl calculation now gives
Since , the remaining force is
Consequently the spherical magnetostatic pressure balance equation following from the stated physical force balance is
The PDF's displayed scalar equation has the wrong sign and omits for its stated pressure p. This is not corrected by setting , which leaves the sign discrepancy. For example, , , satisfies the stated vector force balance and the corrected scalar equation, because ; it fails the printed scalar equation. One could obtain the printed form by replacing its pressure variable by , but that is not the variable in the given force balance.
Now set , , and . The angular operator gives , so
For the trigonometric form in the question, direct substitution yields
For , this is a solution provided
The same coefficient relation makes the trigonometric pair regular at the origin: . Thus all components of the magnetic field are finite there. With , this explicitly constructs the requested proportional-pressure family; adding does not change force balance. The coefficient c is the one called C in the final sentence of the PDF.
For a confined linear-pressure spherical magnetic equilibrium, the condition that the entire magnetic field vanish on is precisely . In components these conditions read
They eliminate both the radial and meridional components; the toroidal component vanishes too because . For a nontrivial solution with , substituting gives
The last equation selects the allowed nonzero values of . Equivalently, when division is legitimate, ; the undivided equation also handles vanishing denominators correctly. Since , is independent of latitude. In the strictly proportional convention , this is zero. The zero-field solution is a trivial possibility; the displayed conditions describe the nontrivial confined family.
A solar-type main sequence star has a radiative interior and an outer convection zone. Rotating convection and differential rotation continually regenerate its magnetic field by dynamo action. The field is therefore not simply an initially stored field undergoing passive magnetic diffusion. In an alpha-Omega dynamo, the Omega effect winds a poloidal magnetic field into a toroidal magnetic field, while the alpha effect associated with helical motions can regenerate poloidal flux. In a solar dynamo, the Babcock-Leighton mechanism provides another poloidal source through the emergence and dispersal of tilted active regions. Shear near the tachocline and transport through the convection zone help organize the cycle; no single dynamo model is needed to claim that rotation and convection are essential ingredients.
Rotation acts on convective motions through the Coriolis force, altering their correlations and helicity. A useful activity measure is the stellar activity Rossby number, , where is a convective turnover time. At a given stellar structure, faster rotation ordinarily increases rotational influence and produces greater magnetic activity in the unsaturated regime. Young solar-type main sequence stars commonly rotate rapidly and show strong sunspots, flares, and chromospheric and coronal emission, although their initial rotation rates have substantial scatter. Very rapid rotators enter a saturated regime, so activity does not increase without limit as rotation increases. The saturation mechanism is not uniquely fixed by the correlation itself. The observed unsaturated correlation and saturated regime are documented in primary rotation–activity measurements.
The reverse interaction is wind-driven magnetic braking of a solar-type star. An ionized stellar wind is coupled to the star's open magnetic field. Matter carries angular momentum, and the Maxwell stress tensor also transmits a torque. Magnetic coupling provides an effective lever arm comparable to the Alfvén radius, rather than only the stellar radius. Writing for the outward mass-loss rate, a schematic angular-momentum equation is
where a geometry factor can be absorbed into an effective . This lever-arm interpretation follows from the angular-momentum invariant of a magnetized wind; it is the central result of the original magnetized solar-wind calculation. Magnetic braking can be effective despite a small mass-loss rate, because can greatly exceed the stellar radius.
One can derive the familiar rotation-age scaling in a simple unsaturated model. For a radial open field, take , , and . Eliminating gives
If the unsaturated large-scale field satisfies and the other factors vary slowly, this gives with positive K. Approximating I as constant on this part of the main sequence, integration yields
Thus in the late-time part of this approximation. This Skumanich rotation law captures the classic observed secular decline of rotation and magnetic activity; its observational basis is the original rotation and chromospheric-emission analysis. It is a scaling model, not an exact trajectory for every star. With a saturated field, the same simplified wind model instead gives a torque approximately proportional to , so initially rapid rotation can decay more nearly exponentially until the unsaturated regime is reached.
Over the main sequence lifetime, wind loss therefore generally makes the star rotate more slowly, increases its stellar activity Rossby number, and reduces its unsaturated mean activity. Later changes of moment of inertia, wind properties and open-field topology alter the simple power law. Internal transport of angular momentum can also feed the braked envelope from the radiative interior, so surface rotation is not automatically a measure of the entire star's angular momentum. In a star with weak braking, this secular history differs from the ideal cubic-torque model; an age law alone is not a fundamental dynamo equation.
The stellar rotation-activity feedback also acts on shorter time scales. A growing magnetic field exerts a Lorentz force that changes differential rotation and convective motions, extracting kinetic energy and limiting further growth through dynamo quenching. Conversely, varying shear and poloidal regeneration change the magnetic cycle. The present solar-like regime can sustain repeated solar cycles, with polarity reversals and activity modulation superposed on the much slower rotational evolution. Rotation promotes dynamo activity; dynamo-generated fields brake rotation through the wind and react back on the motions that generate them. This coupled feedback explains the broad progression from young, rapidly rotating, strongly active stars toward older, more slowly rotating, less active solar-type stars, while allowing cycles, irregular modulation and different initial histories.
The additional conditions are : incompressible flow and the solenoidal magnetic field constraint. The scalar combines pressure per unit density with magnetic pressure per unit density and any conservative gravitational and centrifugal potentials. In particular, the Lorentz force identity separates magnetic tension from . Adding this latter term to the rotating-flow pressure potential gives the pressure appearing in the stated equation; the Coriolis force remains explicit.
Work in magnetic velocity units , and write for the background shearing sheet flow. Its advective acceleration is zero, and , so the stated quadratic background pressure potential gives an exact balance. A spatially uniform mean magnetic field must evolve as
This is stretching of radial field into azimuthal field by differential rotation.
For the shearing wave phase , advection by the background gives
It vanishes identically if
The changing wavevector describes the shear of initially planar wavefronts. The mean-field stretching and wavevector evolution cancel in the Alfvén frequency:
Hence .
These solutions are exact finite-amplitude disturbances, not merely a linearization. To see this, let and in magnetic velocity units. The divergence constraints give . Thus both real disturbances are pointwise perpendicular to k, whereas all their spatial derivatives are along k. Every quadratic term , , and vanishes, including terms involving conjugate amplitudes. This extends the exact incompressible shearing wave to an exact magnetic shearing wave. The gas pressure can compensate quadratic magnetic-pressure terms even though the combined contains only its stated background and wave harmonic.
The remaining wave terms are therefore precisely
The shear terms arise from perturbations acting on , the magnetic terms from the uniform field acting on the wave, and the last terms from diffusion. Pressure enforces the moving-wavevector velocity constraint: differentiating it gives
Using this pressure leaves invariant. Differentiating in the induction equation similarly leaves it zero. Thus the evolution is consistent with both constraints for initially transverse amplitudes.
Now take positive , so the stipulated condition implies , and take magnetic Prandtl number , with . For a vertical wavevector , use the equal-diffusivity magnetorotational channel form
The two horizontal momentum equations, after adding them, give . Either component then gives . The first induction equation gives . These equations are simultaneously solved by
The second induction component gives the same relation, since . Exponential growth occurs when . The quarter-cycle phase between magnetic and velocity perturbations is required by the factor i in the Fourier equations.
For Keplerian rotation, expanding the local shear gives , hence . Therefore . With and , the growth condition for this prescribed polarization becomes
A weaker field would require a shorter wavelength to retain this mode's selected Alfvén frequency, making diffusive damping too strong. The required wavelength must also fit any actual vertical domain; no vertical boundary conditions are specified here.
The field bound is for the requested equal-component mode, rather than a universal necessary condition for all magnetorotational instability. This distinction matters if all vertical wavelengths are admitted. Indeed, let for a general horizontal polarization. Eliminating its two magnetic amplitudes gives and . Their determinant gives
For a Keplerian disk, . As a concrete counterexample to a universal reading of the bound, in consistent dimensionless units take , , , , and . The positive root gives and , even though . This mode has a different polarization and a much longer wavelength. Real finite-height discs restrict such wavelengths; the PDF supplies no such restriction.
Finally, the horizontally averaged radial flux of azimuthal momentum is the sum of Reynolds stress and magnetic tension stress:
Multiplication by the local radius gives an outward angular-momentum flux. Equal radial and azimuthal velocities give the largest positive product at fixed horizontal kinetic energy, while opposite magnetic components give the largest positive at fixed horizontal magnetic energy. Both follow from . This stress-maximizing magnetorotational channel polarization therefore makes both contributions reinforce outward angular momentum transport. It extracts shear energy at rate , explaining why these correlations are especially effective in driving accretion.
Put , retaining its sign. The Lorentz force equations are
Thus remains invariant when . Also , since a vector is perpendicular to its cross product with the magnetic field. Choose the initial planar velocity along the positive axis and the initial location at . Integration gives
This is a circle centred at with radius . The cyclotron frequency is . Equivalently, choosing this centre as the polar origin gives
The rotation is clockwise viewed from positive when , and reverses when . In the PDF hint, are radial conditions with this centred origin; they do not require zero particle velocity. If , the limiting motion is a straight line instead.
With linear drag, put . The governing equations for damped cyclotron motion become
Taking the scalar product with the velocity gives , hence
For the planar path, let and . Then , so for arbitrary initial planar data
Let . The position relative to this limiting point is
Its radius shrinks exponentially while its angle rotates uniformly: the path is a logarithmic spiral into , not a succession of circles about the original vacuum guiding centre. The weak-drag assumption is , so many revolutions occur before appreciable contraction.
Figure 1.
Undamped circular and weakly damped logarithmic-spiral charged-particle paths in a uniform magnetic field
. Details.
In Cartesian coordinates the magnetic field is . Its divergence is , and all components of its curl vanish. Thus it satisfies the static vacuum magnetic equations and , with no electric current in the region.
Fix clockwise orientation as viewed from above, looking down the positive -axis. Its positive area normal is . The loop's external magnetic flux is therefore
With the opposite normal its flux has the opposite sign. On the circle and clockwise line element is . The Lorentz force element is
The radial terms cancel around the circle, so
This fixes the current/flux/force signs together.
Neglect self-inductance initially, so Faraday's law and Ohm's law give . Including gravity then gives
For and , the terminal solution is with
The general velocity relaxes exponentially to on time scale . In the terminal state , and the Joule-heating rate is
Thus all the lost gravitational potential energy becomes resistive heat when kinetic energy is constant.
Within the zero-inductance approximation as ; finite-speed motion would require an unbounded current. This limit is singular, so it is important to describe the physical ideal-conductor limit separately. With finite self-inductance , the circuit equation is . At , total linked flux is conserved and there is no Joule heating. If initially at , then
This lossless limit of magnetic loop braking has undamped oscillations about , with magnetic energy storing and returning mechanical energy. It has no generic dissipative terminal descent. Thus the vanishing terminal speed is the formal resistive-model limit, not a justification for dropping inductance in a perfectly conducting moving loop.
Linearizing the ideal magnetohydrodynamic induction equation about a static magnetic field and using gives the fluid Lagrangian displacement-generated magnetic field perturbation . The two solenoidal vector field conditions reduce the curl identity to
Its divergence vanishes because it is a curl. Directly, the two products of first derivatives in cancel after exchanging their indices, while the remaining terms differentiate or , both zero. Similarly the integrated linear continuity equation gives , so .
Let be the magnetohydrodynamic total pressure. Magnetostatic equilibrium and the momentum equation in the linearized ideal magnetohydrodynamic equations are
There is no perturbed gravitational potential here because the field is fixed. Multiply by and integrate. The pressure term vanishes by the assumed boundary cancellation and . Thus
where .
Integrate the first magnetic term along , using , then insert the expression for . This gives the positive term and two mixed derivative terms. For clarity, the troublesome term transforms as
The first term on the right cancels the other mixed term. Combining the remaining derivative with the term containing gives
Differentiating the equilibrium relation now combines the gradient of mass density and magnetostatic equilibrium terms:
We obtain the incompressible magnetic displacement energy identity
The two Hessian matrices are real symmetric, making their Hermitian form evaluations real. The last term is a squared norm, and for a nonzero displacement in fluid with positive mass density. Thus . It may be negative, in which case one temporal branch has exponential growth; real squared frequency is not itself a proof of stability.
For the atmosphere with a horizontal magnetic field, has zero Hessian matrix and the equilibrium equation is
Consequently the interchange stability of an incompressible magnetized atmosphere is governed by the numerator
For , the magnetic tension term is zero: these fluid Lagrangian displacements interchange neighboring magnetic field lines without varying along them. A mass density increasing with height gives negative energy and instability; decreasing mass density gives positive energy for these vertical interchanges. If everywhere, the displayed form is nonnegative for every admitted incompressible displacement. If the gradient changes sign, suitably localized divergence-free interchange trials detect an unstable inverted layer; For example, take and , with supported in that layer. Their divergence is zero, and neither component varies along the magnetic field.
For , magnetic field lines are bent. Averaging over a full horizontal wavelength gives the trial Rayleigh quotient
under the stipulated admissible boundary/integrability conditions. It is a trial quotient, not a claim that this displacement is an exact eigenfunction for every profile. mass density decreasing upward is stable here too. For inverted mass density, magnetic tension can stabilize sufficiently short waves along the magnetic field, but does not remove the transverse interchange instability. Locally the two contributions have the familiar scale , with the Alfvén speed .
Consider a local shearing sheet centered at a circular orbit. Take uniform mass density, background velocity , rotation and a weak uniform vertical magnetic field . Here
Use ideal magnetohydrodynamics, neglect viscosity, magnetic diffusion and vertical stratification, and take incompressible axisymmetric disturbances proportional to . They have horizontal velocity and field perturbations. Let be the magnetic perturbation in velocity units, the Alfvén speed and the Alfvén frequency. Magnetic pressure can be included in the perturbation's total pressure; the horizontal Lorentz force for this mode is the magnetic tension term .
Linearizing momentum and induction gives
The term winds a radial magnetic perturbation into an azimuthal one. Omitting it would remove the shear's magnetic energy source and give the wrong stability criterion.
A useful elimination that also covers neutral modes introduces the fluid displacement . Frozen-in flux gives , while the Eulerian perturbation velocity is , , because the displacement samples the gradient of the basic flow. The equations become the spring model of magnetorotational instability:
For the stated time dependence, their determinant is
Thus the ideal magnetorotational dispersion relation is
It follows without dividing by , so the neutral stability boundary is included.
To analyze it, put and . Then
For a hydrodynamically stable rotation law, , the sum of the two roots is positive. Their product is negative precisely when . One squared frequency is then negative, giving an exponentially growing mode and its decaying partner. Therefore the magnetorotational instability, or MRI, has criterion
Angular velocity must decrease outwards, although specific angular momentum may increase outwards and satisfy Rayleigh's circulation criterion. This is why a Keplerian disc can be stable to the axisymmetric hydrodynamic disturbances of Question 2 yet unstable once magnetic coupling is introduced. At zero magnetic frequency the unstable root becomes neutral, while sufficiently large magnetic frequency restores stability. For increasing angular velocity, with , this ideal vertical-field instability is absent.
The growth rate is
For , differentiation with respect to sets , yielding the maximum growth rate of ideal magnetorotational instability:
For Keplerian rotation, , so
Thus the fastest growth is on an orbital timescale. The field strength selects its wavelength, , rather than the maximum ideal growth rate. At fixed , growth does approach zero as ; retaining the finite maximum in that limit requires shorter wavelengths, which magnetic diffusion can eventually exclude. Unstable wavelengths satisfy in this local model. A finite disc must accommodate such a wavelength, so a sufficiently strong field can suppress the available vertical modes through excessive tension.
Physically, a bent field line acts like a spring joining neighboring fluid elements. The inner element rotates faster and pulls the outer element forward, transferring angular momentum outward. The inner element loses angular momentum and moves inward; the outer element gains it and moves outward. In a rotation law with outward-decreasing angular velocity, these motions increase their angular-velocity difference and the magnetic coupling produces further separation. A weak restoring spring therefore creates a feedback instability by enabling angular-momentum exchange. Without that exchange, each displaced element keeps its angular momentum and a positive epicyclic frequency restores its orbit. Strong magnetic tension instead prevents the separation. The free energy is the differential rotation, not the initial magnetic energy.
The instability provides an important route to turbulence and angular momentum transport in sufficiently conducting accretion discs. The radial flux of azimuthal momentum includes the stress
The first term is a Reynolds stress and the second is the magnetic contribution from the Maxwell stress tensor, with the sign appropriate to momentum flux. For the growing branch, take real and positive. The linear equations give and . The last sign follows from . Thus both the velocity and magnetic contributions carry angular momentum outward. The associated energy extraction is . Inward accretion can then accompany outward angular-momentum transport, and dissipation of the resulting fluctuations heats the disc. This gives a physical mechanism behind an effective turbulent-viscosity description such as an alpha disk, whereas microscopic viscosity alone is generally too weak for rapid accretion.
Figure 1.
Finite hydrodynamic swing amplification compared with the growing MRI branch in a Keplerian disc
. Details.
MRI is an exponentially growing magnetic instability of outward-decreasing angular velocity; hydrodynamic shearing-wave amplification is transient and does not by itself establish sustained turbulence. Nonlinear saturation, field regeneration and transport efficiency depend on field geometry, boundaries and thermodynamics. Poor conductivity or important nonideal magnetic effects can suppress or modify the ideal instability, so the local dispersion relation is a mechanism and growth criterion rather than a universal prescription for the saturated stress.
Suppress the common Fourier mode factor and define the transverse and full divergences of the fluid Lagrangian displacement by
The perturbed magnetic field is . Its components are
Thus the magnetic part of the energy integrand is
Use from force balance. The pressure-gradient cross term is
The current term has the azimuthal cross-product component , giving
Every term involving cancels in the sum, including the possibly complex terms. The magnetohydrodynamic energy principle therefore reduces exactly to
For physical and positive adiabatic index , every surviving term is nonnegative. On the admissible displacement domain for the supplied functional, squared ideal-mode frequencies cannot be negative. This is the positive ideal energy of a theta pinch, proving absence of exponentially growing ideal modes. The qualification is stable or marginal, not strictly positive energy for every motion: at , suitable incompressible displacements can have zero energy. As usual, the energy principle presumes regularity and boundary conditions eliminating unwanted surface terms; additional external systems are not part of the given functional.
Use incompressible ideal MHD at scales above the ion skin depth, a strong uniform mean field, and a statistically steady local energy cascade with mean flux per unit mass. Assume balanced counterpropagating wave populations, comparable velocity and magnetic amplitudes in velocity units, and no additional scale-dependent alignment or intermittency correction. Write and introduce the fluctuation Elsässer variables . Their equations are
Only opposite populations distort one another. A single population has no leading nonlinear self-interaction, so the balance assumption is essential to a one-amplitude cascade estimate.
Let denote the typical balanced amplitude and let be coherence lengths relative to the local mean field. The Alfvén wave time and eddy turnover time are
For , one counterpropagating encounter changes the packet fractionally by order . Assume phases decorrelate between encounters. After encounters, random accumulation is of order ; an order-one change requires . The weak wave cascade time is therefore
Weakness by itself does not prove this random walk estimate; phase decorrelation and the interaction geometry are additional assumptions.
For the Iroshnikov-Kraichnan spectrum, impose isotropy, , in addition to . Then and
Hence . A local shell-integrated turbulent energy spectrum has , , so
The isotropy is imposed phenomenologically; a strong guide field actually distinguishes directions and does not force this isotropic picture. The spectrum is not an automatically valid asymptotic result for every strongly magnetized cascade.
For the anisotropic weak Alfvénic cascade, keep approximately fixed while cascading to smaller , and require . This geometry follows from resonant three-wave Alfvén interactions: frequency conservation together with parallel-wavenumber conservation makes one member of an oppositely propagating resonant triad have zero parallel wavenumber, so the propagating modes retain their parallel wavenumber in the leading resonant transfer. Thus there is no leading parallel cascade in this ideal weak-wave ordering. Using the fixed parallel scale,
Therefore . For the one-dimensional perpendicular spectrum, gives
Unlike the isotropic estimate, the parallel length does not decrease with the perpendicular length. Since , the interactions become stronger down the cascade. If at outer perpendicular scale , the weak approximation breaks at . This is the weak-to-strong transition of an Alfvénic cascade.
For Goldreich–Sridhar turbulence, abandon the weak-collision estimate and impose critical balance, . The local cascade is strong, with transfer time of order one eddy turnover time. Then
The parallel scale is set dynamically, not held fixed:
At smaller scales grows, so the eddies are increasingly elongated along the local magnetic field. Strong turbulence does not mean : small transverse amplitudes can still be strong when the eddies are sufficiently anisotropic to satisfy critical balance. Imbalance, alignment or nonlocal interactions would require different cascade reasoning.
Finally, in the usual isotropic hydrodynamic Kolmogorov 1941 theory inertial-range argument, the only relevant dimensional quantities are and . With and , writing forces , . This uses the physical assumptions that outer-scale, viscous and intermittency effects do not supply another leading dependence; dimensions alone are not a proof of those assumptions.
A magnetic guide field supplies the independent speed , and anisotropy adds independent parallel lengths. Even before adding anisotropy, dimensions permit
with arbitrary dimensionless . For example reproduces the isotropic Iroshnikov-Kraichnan spectrum estimate. This dimensional freedom of an MHD spectrum explains why propagation, decorrelation, anisotropy and cascade-time assumptions must select among the spectra: purely dimensional considerations do not select a unique MHD exponent.
Take zero mean flow locally and incompressible fluctuations. Subtracting the averaged induction equation gives
The first-order smoothing approximation omits the second term on the right when solving for , but retains in the mean equation. For a locally uniform, slowly changing mean magnetic field the forcing becomes .
There are two controlled ways to make the omitted fluctuation term small. At small eddy magnetic Reynolds number , diffusion gives , so the omitted is smaller than the retained by . Alternatively, if for the fluctuation response time , then and the short-memory response is perturbative. Mean-field scale separation is additionally required. Merely calling the turbulence weak or assuming that the mean magnetic field is small does not justify the omission.
With homogeneous initial transients removed, the causal linear solution is
Insert this into the electromotive correlation. Isotropy gives , so taking the trace yields the helicity formula for isotropic first-order smoothing:
Using the alternating-tensor sign gives
The minus sign follows from . This derivation specifies the diffusion and correlation weighting, rather than asserting that alpha is proportional to instantaneous helicity for arbitrary turbulence.
If , diffusion over a correlation time is negligible. Define the helicity correlation time by
For an ordinary decaying correlation with nonzero mean kinetic helicity, this gives the familiar estimate
It is the kinetic helicity, not magnetic helicity. Opposite flow handedness reverses the alpha effect. The time-integral formula remains meaningful if the equal-time helicity vanishes or its correlation changes sign, when replacing it by a single positive correlation time may fail. In the same weak-diffusion short-memory approximation the gradient forcing gives ; the two correlation times need not be equal.
In the small-, slowly varying quasistatic regime, diffusion is instead essential. The response gives
For velocity concentrated at wavenumber , this becomes . Its effective memory is the magnetic diffusion time on the eddy scale. The controlled low- setting is developed in Moffatt's analysis of turbulent dynamo action; the causal-response calculation above also covers short-memory turbulence without assuming that diffusion is always negligible.
In mean-field electrodynamics, use Reynolds averaging to write and , with zero-mean fluctuations. Assume the averaging operation commutes with the derivatives and that resolved quantities vary little across an averaging region. Averaging the induction equation then gives
This is the mean-field electromotive force, a vector correlation with units of velocity times magnetic field. The closure problem is to express this correlation in terms of the resolved field.
In the kinematic regime the flow statistics are prescribed, so the response is linear in the mean magnetic field, after independently excited fluctuation transients have decayed. If the mean-field scale is much greater than the turbulent scale , and its evolution is slow compared with the response memory, expand that response in the local mean magnetic field and its gradients:
Without scale separation one generally has a spatially nonlocal and temporally retarded response rather than constant local coefficients.
For homogeneous turbulence the coefficients are independent of position. Invariance under proper rotations makes the rank-two response proportional to , and the isotropic rank-three gradient response proportional to the alternating tensor. Choosing the diffusivity sign convention gives
The alpha effect can regenerate a mean magnetic field, while supplies turbulent magnetic diffusivity. For constant positive , because the magnetic field is solenoidal. Thus the total diffusivity is .
The electromotive vector is a polar vector, whereas the magnetic field is an axial vector. Therefore is a pseudoscalar and changes sign under reflection; is an ordinary scalar. A nonzero isotropic alpha effect requires broken reflection symmetry, such as nonzero kinetic helicity. If “isotropic” includes reflection symmetry as well as rotations, must vanish. The dimensions are and .
The magnetic vector potential gives the upper poloidal magnetic field , and is its toroidal magnetic field; play the same roles below. This representation automatically satisfies . Diffusion acts in both regions. Above the interface the alpha effect converts toroidal magnetic field into poloidal magnetic field, while below it a mean shear converts the poloidal component into toroidal magnetic field. Separating these source regions still allows an alpha-Omega dynamo through diffusion across the interface.
For electromagnetic matching, keep the closure actually represented by these equations. Its retained turbulent mean-field electromotive force is above and zero below: only toroidal-to-poloidal alpha generation is retained. Let the mean velocity be , continuous at the interface, and write the mean electric field as
This yields the specified scalar equations with above and below. In particular, the upper tangential electric component is
where is the scalar toroidal-field amplitude. The other tangential component is .
Assume equal permeability, no imposed singular surface current and ordinary electromagnetic matching. Continuity of the normal magnetic field gives , and tangential magnetic continuity gives and . For the nonzero horizontal Fourier wavenumber used below, normal-field continuity is equivalent to ; the spatially constant potential difference is a gauge freedom. Continuity of , with continuous and , gives the final condition. Thus electromagnetic matching for an alpha-Omega interface is
Continuity of follows from and their time evolution, rather than supplying a fifth independent amplitude condition. A full isotropic mean-field electromotive force would add toroidal alpha induction and an alpha contribution to ; that would be a different bulk and interface problem. Retaining it only in a boundary condition would be inconsistent with the equations being solved here.
Set , without loss of generality for a real wave and its conjugate, and write . Define the two complex vertical wavenumbers and so the upper fields decay as and the lower fields as . The original PDF has a lowercase in the lower phase. The homogeneous upper and lower equations give
Both and have positive real part. Since their squares agree, they must be equal, rather than opposite. Put
so and follow from the equations rather than being assumed in advance.
Suppress the common factor and write
The identity gives the upper forcing equation, while the same operator on gives . Hence
The first and third interface dynamo matching give , . The derivative conditions then give
Thus and . Eliminating the nonzero amplitudes produces the dispersion relation of an equal-diffusivity interface dynamo:
In terms of ,
Each branch has a square root with positive real part and is therefore compatible with vertical localization. The branch with the plus sign is the potentially growing one:
The minus branch has . At the first branch is neutrally oscillatory. The frequency sign follows from the stated convention: positive give propagation in the negative direction. Reversing the coupling sign reverses propagation, while the threshold for the conjugate sign depends on the magnitude of the dynamo number.
Figure 1.
Separated interface-dynamo source layers and the growth threshold at dynamo number 32
. Details.
The equal-diffusivity interface dynamo idealizes a solar configuration in which helical convection regenerates poloidal magnetic field above the tachocline and differential rotation generates strong toroidal magnetic field in or below it. Diffusion communicates the fields between the two regions, closing the feedback loop. This separation is the mechanism emphasized by Parker's interface-wave model. An oscillatory traveling mode gives migrating magnetic patterns and polarity reversals; buoyant toroidal flux can appear as sunspot belts. If is a local latitude coordinate, the direction of their migration depends on the alpha–shear sign and the coordinate orientation.
The magnetic period of this branch is ; polarity reverses after half a period, and activity that depends on field strength rather than sign can repeat on that half-period. This is the qualitative relation between the magnetic solar cycle and its activity cycle. The model does not itself predict the observed period or guarantee equatorward migration: those require actual geometry, transport coefficients and shear signs. Real stars also have diffusivity contrasts, meridional transport, spatially varying regeneration and nonlinear feedback. The kinematic exponential mode describes onset, while saturation and a maintained finite-amplitude cycle require further physics.
For steady electromagnetic fields, Maxwell's equations give and . Introduce a magnetic vector potential with and the permitted Coulomb gauge . The vector identity for the double curl then gives . For localized currents and the decaying solution,
Here follows from harmonicity away from zero and the inward flux of the radial derivative through a small sphere, whose magnitude is one. It verifies the vector Poisson solution componentwise. Moreover steady electric charge conservation gives ; integration by parts confirms the stated potential is divergence-free. Taking its curl, using , proves the Biot-Savart law:
The zero-field condition at infinity selects the magnetic field produced by these currents, excluding an externally imposed homogeneous magnetic field.
At the origin write the source point as . Its current is , so the numerator of the Biot-Savart law is . The radial term cancels after angular integration. Using gives
The inner integral is , as is verified by differentiating . Hence
For , its magnitude is ; it points along for positive azimuthal current , and along for . The limit is , agreeing with direct integration of the infinitely long cylindrical current distribution.
In SI units, the source-free Maxwell equations in vacuum are
Use complex amplitudes with phase and take real parts at the end. The electric divergence equation gives . Faraday's equation gives , so
The magnetic divergence equation follows because . Ampere's equation becomes . Since , a nonzero wave satisfies
Thus both fields are transverse, mutually perpendicular for linear polarization, and obey the vacuum plane-wave dispersion relation.
For the interface let point from the minus side to the plus side and write , similarly for . Applying the integral Maxwell equations to a thin pillbox and a thin loop gives the electromagnetic boundary conditions
Here is the tangential surface current. The jump notation fixes the signs, including the direction of the normal.
For the perfect conductor, take the time-varying interior fields to vanish. Choose positive with . The incident electric field has complex form . To cancel its tangential value at the surface, use the reflected field , whose wavevector points upward. The total vacuum fields are therefore
The sign of each magnetic contribution follows from . At , the electric field is zero and the magnetic field is tangential. The jump conditions yield
For a real incident amplitude this is . It supplies the reflected wave while satisfying the normal-field and tangential-electric conditions. Any independently imposed static interior field is separate from this oscillatory response.
An order parameter distinguishes phases by a macroscopic quantity that changes at the transition. For an Ising model ferromagnet it is the magnetization per Ising spin, . At zero magnetic field the statistical Hamiltonian is invariant under spin inversion symmetry. The disordered phase preserves this symmetry, whereas a selected ordered phase has and a spin-reversed partner with . At finite volume with symmetric boundary conditions the expected value is zero even below the transition; spontaneous magnetization means taking the thermodynamic limit before sending a symmetry-breaking field to zero.
Landau-Ginzburg theory introduces a coarse-grained local order parameter and a symmetry-constrained free-energy functional. For a short-range system with scalar spin inversion symmetry, a useful expansion is
The coefficients vary smoothly with microscopic control parameters at the level of the Landau approximation; normally with . The gradient term penalizes spatial variation. The magnetic field is conjugate to the order parameter, and odd powers at are excluded by spin inversion symmetry. With , the sextic term may be omitted locally; with , a stabilizing positive is essential. The equilibrium uniform order parameter minimizes the local potential , giving
This equation of state follows from minimization, rather than being imposed as an independent assumption. Vector or tensor order parameters and their allowed invariants describe other symmetry classes.
Use for inverse temperature, to distinguish it from the order-parameter critical exponent . In a translation-invariant pure thermodynamic phase, the connected two-point correlation function is
For finite correlation length, at it decays exponentially, possibly with an algebraic prefactor; is the asymptotic exponential decay rate. Below an ordered transition the pure phase is selected by taking the thermodynamic limit before or . A zero-field symmetric mixture of the two ordered phases has a nondecaying connected term and does not describe the usual pure-phase magnetic susceptibility.
Let denote extensive physical free energy and . Since the field contributes to the statistical Hamiltonian, differentiation gives
Expanding the variance and using translation invariance proves the correlation-function susceptibility sum rule:
The sum includes . If the source is instead defined as the dimensionless quantity , the corresponding derivative omits the displayed inverse-temperature factor.
A real-space renormalization group step of length factor uses a local blocking kernel satisfying . For example, a deterministic majority-spin rule assigns one coarse Ising spin to each block; tied blocks can be resolved with equal probabilities. Define the blocked statistical Hamiltonian by
The spacing becomes . All generated interactions, including multispin terms and the field-independent constant, must be retained for an exact transformation. Summing over uses normalization to prove . Iteration gives and .
The coarse probability law is the exact marginal law of these block variables. Indeed, for any coarse observable , its expected value is the microscopic expected value of . A blocking rule that retains the long-wavelength order-parameter mode, with source and observable transformations tracked, therefore retains long-distance response and correlation functions. Their field normalization may change, while their physical length scales and critical singularities do not. Partition-function equality alone would not justify this assertion for an arbitrary kernel that discards all slow variables. Truncating the generated operator family is likewise an approximation.
For the free-energy recursion use dimensionless free energy per site,
in the thermodynamic limit. Exact partition-function invariance gives . If one step sends to , the coefficient records the identity-operator contribution from eliminated fluctuations and normalization. Consequently
Repeated substitution derives the additive free-energy recursion under blocking:
In physical energy units, divide this convention by . The additive term is essential for absolute free energies even when it does not affect the leading critical powers.
A renormalization-group fixed point satisfies . Linearize in scaling coordinates so that . A relevant operator has , an irrelevant operator has , and a marginal operator has with behaviour decided by nonlinear terms. Thus the eigenvalues of the discrete linear map are ; the sign criterion applies to the generator exponents , not to the discrete multipliers. The critical surface is the stable manifold on which every relevant scaling field has been tuned away. Irrelevant coordinates flow to the renormalization-group fixed point along it. A repulsive renormalization-group trajectory leaves the renormalization-group fixed point along an unstable relevant direction, ultimately entering a noncritical phase or another scaling regime.
Figure 1.
Local renormalization-group flow in the zero-field slice: attraction along the critical surface and repulsion in the thermal direction
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To separate the singular free-energy density from its regular background, suppose the eliminated-mode contribution is analytic near the renormalization-group fixed point. Look for an analytic background satisfying . Then satisfies . In linear thermal and field coordinates, an analytic monomial has background coefficient
provided the denominator is nonzero. This explicitly explains when analytic subtraction of an inhomogeneous renormalization recursion works. The printed inhomogeneous equation may describe the free-energy function before this subtraction, or a singular part defined only up to analytic terms. The inhomogeneous sum need not be small compared with the full free energy: an analytic constant can dominate a vanishing singular contribution. It can be omitted in deriving leading singular powers after regular subtraction, provided no renormalization-group free-energy resonance, marginal logarithm or dangerously irrelevant coupling obstructs the homogeneous critical asymptotics. At a renormalization-group free-energy resonance , additive logarithms can remain, so simply dropping the term would miss them.
Suppose there are exactly two relevant scaling fields, thermal and magnetic , with positive exponents , and the remaining fields approach a regular limit. Physical reduced temperature and magnetic field agree with these coordinates to leading order, up to nonuniversal metric factors. The homogeneous scaling hypothesis for critical phenomena is
as an asymptotic scaling equation. Choose to make the thermal argument or . Defining gives
The two functions describe respectively and : approaching the transition from disordered and ordered sides need not give the same function. In particular the ordered zero-field function has one-sided derivatives associated with spontaneous magnetization. Metric factors multiply this formula in different microscopic normalizations.
The correlation length in Bravais lattice units obeys . At , the same choice of gives . Two thermal derivatives of give . One and two field derivatives give, respectively, and , assuming the relevant branch amplitudes are nonzero. At , choose ; then , so . Hence
Simple algebra now gives the Rushbrooke scaling relation and the hyperscaling relation . Also , giving the Widom scaling relation. These statements refer to leading singular contributions with the homogeneous two-field scaling assumptions. Above the upper critical dimension, the quartic coupling is dangerously irrelevant because it is still needed to stabilize the ordered phase; ordinary mean-field critical exponents then satisfy Rushbrooke and Widom but generally not hyperscaling. Marginal logarithms also require qualifications at the upper critical dimension.
For the connected-correlation scaling form , the function tends to a finite nonzero value as and decays exponentially at large , up to powers of , in a massive short-range phase. The scaling ansatz alone does not fix that prefactor. If the usual massive Gaussian field correlation tail applies, matching the powers gives , with a correlation-length-dependent amplitude in fixed by matching the critical scaling form.
In physical coordinates the lattice sum has site-density factor . Its long-distance singular part therefore gives
where is the area of the unit sphere in dimensions. For , finite , an integrable exponential tail and a nonzero integral, the last factor tends to a finite nonzero constant as . Microscopic distances contribute a regular background. Thus , proving the Fisher scaling relation
Equivalently the field has scaling dimension , so its conjugate field has , which gives the same identity from the exponent formulas above.