Axisymmetric magnetic winding Created 2026-10-05 Updated 2026-10-06
For prescribed axisymmetric differential rotation , the ideal magnetohydrodynamic induction equation and Gauss's law for magnetism giveThe poloidal field is unchanged while rotational shear generates a toroidal magnetic field. For time-independent , the toroidal component grows linearly until neglected dynamical feedback becomes relevant.
Cross-helicity conservation law Created 2026-09-28 Updated 2026-10-05
Let be the cross-helicity density. The ideal magnetohydrodynamic induction equation implies . Dotting the momentum equation with eliminates the Lorentz force density, since it is perpendicular to the magnetic field. The material derivative of is thereforeUsing for specific enthalpy and specific entropy , together with Gauss's law for magnetism, converts this toThe source vanishes when magnetic field lines lie in constant-specific entropy surfaces, in particular in a homentropic flow. Integrating over a volume conserves its total cross-helicity only if the boundary flux also vanishes. This local law is derived in Ogilvie's astrophysical fluid dynamics notes.
For nonresonant incompressible normal modes of a uniform-density shear flow with aligned uniform magnetic field, let , and . The normal displacement is . The linearized horizontal equations and incompressibility give . Substituting the ideal magnetohydrodynamic induction equation into normal momentum gives the displayed conservative equation. Across a zero-thickness shear layer, continuity of and of supplies the interface conditions. They express common normal displacement and continuous perturbed magnetohydrodynamic total pressure, avoiding undefined products of distributional shear gradients.
Elsässer variable 2026-10-06
For an incompressible flow with constant mass density, the Elsässer variables are , where is the Alfvén velocity. Adding and subtracting the Euler momentum equation and ideal magnetohydrodynamic induction equation yields , with and . Thus each field is transported by the other, a useful way to expose interactions of oppositely directed Alfvén waves.
Ideal magnetohydrodynamic equations 2026-10-06
The smooth ideal-MHD system couples mass conservation, momentum, adiabatic pressure transport and the ideal magnetohydrodynamic induction equation, subject to the solenoidal magnetic-field constraint. Without gravity it is a quasilinear partial differential equation system. Across shocks, conservative total energy replaces smooth adiabatic pressure transport.
Ideal magnetohydrodynamic momentum equation 2026-10-06
The inviscid magnetohydrodynamic momentum equation balances inertia, pressure, gravitational acceleration and Lorentz force density. The magnetic force separates into magnetic tension and magnetic pressure. It is coupled to the continuity equation and the ideal magnetohydrodynamic induction equation.
The magnetic nonrelativistic limit neglects displacement current and uses , , . Under a Galilean transformation , , its consistent field transformations are , and . Indeed and , giving covariance of the induction equation. The full charge-current transformation has ; neglecting its convective correction belongs to the magnetic quasineutral approximation, not exact relativistic electrodynamics. With , the combination is invariant. Vanishing electric field in the fluid rest frame therefore gives the ideal magnetohydrodynamic induction equation.
For an axisymmetric poloidal magnetic field , the ideal magnetohydrodynamic induction equation gives , after fixing the time-dependent additive constant in . A regular axial reference makes the enclosed magnetic flux. This scalar statement of magnetic flux freezing holds even when rotation also produces a toroidal magnetic field.
Moving-conductor Ohm law 2026-10-06
In the nonrelativistic scalar-conductivity approximation, neglecting Hall and other nonideal electromotive effects, . The ideal finite-current limit gives and hence the ideal magnetohydrodynamic induction equation.
Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 36 3 a Solution Created 2026-10-03 Updated 2026-10-14
Choose a magnetic vector potential with , and define the total magnetic helicity byThe value is unchanged by a single-valued gauge transformation , becauseHere both the solenoidal magnetic-field constraint and the tangent boundary field are essential. In a multiply connected domain, choose the vector potential by extending the tangent field by zero to all space and fixing its decay there, or fix the equivalent circulation convention. This avoids silently varying the non-gradient harmonic ambiguity of a vector potential on the restricted domain.
The ideal magnetohydrodynamic induction equation permitsDifferentiating and using integration by parts for curl,The volume product vanishes algebraically, the gauge flux vanishes since , and the last boundary term vanishes since . Thus magnetic helicity is conserved even though viscosity dissipates mechanical energy.
Through magnetic flux freezing, magnetic field lines move with the fluid and retain their linkage during every smooth ideal motion. For two thin closed flux tubes carrying fluxes , their mutual contribution is , where is their linking number; self-contributions measure twisting and writhing of the tubes. This explains the topological content of magnetic helicity. Conservation of this one scalar is a consequence of the frozen structure, not a complete description of all that structure.
Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 36 3 b Solution Created 2026-10-03 Updated 2026-10-14
Let be the kinetic energy, the magnetic energy and :Dot the magnetohydrodynamic momentum equation with and integrate. Incompressibility and the zero boundary velocity remove the advective and pressure work. The viscous term integrates to . ThusThe ideal magnetohydrodynamic induction equation gives, with no boundary contribution,The Lorentz force density therefore transfers energy between the field and the fluid without creating total energy. Since and on the boundary, another integration by parts gives , where is vorticity. The viscous magnetic-relaxation energy identity isThe conserved nonzero magnetic helicity prevents all the field energy from disappearing. Fix a bounded inverse-curl convention for the magnetic vector potential, so that . The Cauchy-Schwarz inequality gives the magnetic-energy lower bound from helicity,Consequently decreases to a finite positive limit andUnder the intended regular long-time interpretation of smooth vorticity, the dissipation cannot keep producing peaks of fixed height and arbitrarily short duration. More precisely, if is uniformly continuous, uniformly continuous integrable dissipation tends to zero proves . The Poincaré inequality and the identity above then imply .
To identify the asymptotic state, suppose the regular relaxation has a limit, or work on a compact invariant limiting set on which the energy is continuous. On such a set the energy is constant, so the displayed identity forces , and the zero boundary velocity forces . The induction equation is then stationary, and the momentum equation becomesThis is magnetostatic equilibrium, with nonzero field allowed and required here by conserved magnetic helicity. It is not necessarily a force-free magnetic field: a pressure gradient can balance the magnetic force. If the field develops a current sheet, equilibrium is understood with the corresponding interface force balance.
There is a mathematical qualification to the smoothness premise. Smoothness at each finite time alone does not prove uniform long-time bounds, uniform continuity of dissipation or convergence to one limiting field. The energy calculation proves finite total dissipation unconditionally for a smooth solution; the settling conclusion is the regular-relaxation argument just given. A rigorous global convergence theorem requires that additional long-time control. In particular, smooth vorticity does not require smooth electric current density in the limiting state.
Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 42 2 Solution Created 2026-10-03 Updated 2026-10-14
The magnetohydrodynamic total pressure isThe Lorentz force has been split into the gradient of magnetic pressure and the remaining magnetic tension term. An appropriate boundary model is impermeable, perfectly conducting stationary cylindrical walls with no initial normal magnetic flux: at . In an inviscid fluid this is a slip condition, not a no-slip condition on or . It also makes the tangential ideal electric field vanish at the walls. Take perturbations periodic in and periodic or Fourier-resolved in ; the wall reaction supplies the normal pressure force without an extra prescribed pressure value.
Write the steady velocity and magnetic field as and . They satisfy both divergence constraints. Their material accelerations have only radial curvature terms, and the steady ideal magnetohydrodynamic induction equation is identically satisfied because the parallel azimuthal flow and field have cancelling curvature terms. The radial momentum equation isHence the most general such equilibrium isIts gas pressure is ; on a bounded annulus the additive constant can be chosen to keep it positive. Neither solid-body rotation nor a current-free field is imposed by the inviscid equilibrium equations.
For the linear stability calculation, put , , and define . Use axisymmetric normal modes proportional to . Denote the velocity amplitudes by and the magnetic amplitudes in velocity units by . Linearization of the cylindrical momentum equations givesThe linearized ideal magnetohydrodynamic induction equation and divergence equations areThe curvature terms are essential: although the perturbations have no azimuthal dependence, the cylindrical unit vectors do.
For , . Introduce the radial Lagrangian fluid displacement by . The azimuthal amplitudes reduce toConsequently the radial and vertical equations, combined with the incompressible flow constraint, givewhere the Michael criterion for axisymmetric toroidal-field interchange coefficient isFor , the required single displacement equation is thereforeThe same differential equation holds for , which is a constant multiple of .
Set . Multiplication by and integration by parts with the wall conditions gives the global variational form of the Michael criterion:The denominator is strictly positive for a nonzero displacement, so every mode's is real. If everywhere, no exponentially growing mode exists. Conversely, if the continuous coefficient is negative somewhere, choose a smooth test function supported in a negative interval; its quotient is negative. For sufficiency, let be the positive Sturm-Liouville operator with Dirichlet boundary conditions and let multiply by . The generalized mode equation is equivalent to the compact operator and self-adjoint operator problem . The negative test quotient guarantees a negative eigenvalue and therefore a growing solution . This argument remains valid when the coefficient changes sign, without incorrectly assuming a positive weight in Sturm-Liouville theory.
Thus, for any fixed nonzero vertical wavenumber,Equality is marginal. When , the incompressible flow constraint and both rigid-wall conditions force the radial velocity to vanish, so that special case has no radial interchange mode. When the field vanishes, the coefficient reduces to , recovering the Rayleigh centrifugal stability criterion.
For a Keplerian disk, . If , the toroidal interchange field threshold in a thin Keplerian disk isFor ordinary radial gradients on the scale , the Alfvén speed must therefore be comparable to the orbital speed. A field on the gas pressure scale has in a thin disk, and cannot normally meet this condition. Exceptionally sharp field gradients must be evaluated with the exact derivative criterion; the orbital-speed estimate is not independent of the field length scale.
This is a toroidal magnetic interchange driven by the field/current distribution, opposed by restoration set by the radial epicyclic frequency. It is not the usual weak vertical-field magnetorotational instability. In the vertical-field problem, a nonzero bends magnetic field lines and couples displaced fluid elements, allowing decreasing to supply rotational kinetic energy even when . Here the axisymmetric perturbation has no scalar variation along the purely toroidal background field, and no such weak-field coupling: a sufficiently adverse toroidal-field gradient, rather than merely , is required. Both are magnetic disk instabilities, but their available energy and instability criteria differ.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 64 2 Solution Created 2026-10-03 Updated 2026-10-14
Use the adiabatic form of ideal magnetohydrodynamics: heat conduction and external heating are absent, so . Infinite electrical conductivity and zero viscosity alone would not remove the thermal source terms on the cover page. If those terms are retained, the energy equation below must acquire on its right-hand side.
Expanding the continuity equation gives its conservative form . Using it to expand the conservative momentum derivative givesFor , the Lorentz force density is the divergence of the magnetic Maxwell stress tensor:Combining these identities with momentum balance provesThe dyadic stress contains both magnetic tension and magnetic pressure; the sign in the flux is fixed by moving the magnetic force to the left.
For the energy equation, first dot momentum balance with and add the adiabatic internal-energy equation. The continuity equation converts their material derivatives into conservative derivatives, while . The result isThe ideal magnetohydrodynamic induction equation gives the magnetic counterpart. In fact,Thus the outward Poynting vector is , and magnetic work cancels the fluid work. Finally, the continuity equation impliesAdding all three identities gives ideal magnetohydrodynamic energy conservation in the required local form:whereThe magnetic energy coefficient is , as in the original PDF. For a self-consistent, time-dependent gravitational field this local balance should not be confused with a global self-gravitating energy integral: the latter uses gravitational field energy, or the familiar one-half factor in after the field is eliminated.
Work in the shock frame of a thin planar discontinuity, with normal speed . A smooth gravitational potential has no finite jump through a vanishingly thin front; its advected contribution cancels using the common mass flux. Integrating the conservation laws gives constant normal mass, momentum and energy fluxes, together with the normal-field and tangential-electric-field conditions of the ideal magnetohydrodynamic shock conditions.
For a parallel magnetohydrodynamic shock, and . The magnetic solenoidal constraint makes the same on both sides. The normal momentum flux is ; its magnetic term is therefore identical upstream and downstream. The Poynting vector is zero because . Hence the nontrivial jumps are exactly the Rankine-Hugoniot conditions for a perfect gas:with specific enthalpy . Physically, motion along the straight field neither bends it nor compresses its transverse flux. The field consequently provides no changed stress or energy flux in this purely parallel geometry. This conclusion does not apply to a shock that develops a transverse magnetic field.
For a perpendicular magnetohydrodynamic shock, the magnetic field is tangential and the velocity normal. Steady induction makes continuous, while the continuity equation makes continuous. Dividing gives the magnetic flux freezing relationPut , so and . Constant normal momentum flux now reads . Substitution givesThe magnetic correction is negative for compression: part of the incoming ram pressure builds magnetic pressure instead of thermal pressure.
Here the Poynting vector has normal component . Divide the constant energy flux by the nonzero mass flux to obtainWith , this gives the second expression for downstream pressure:In this expression is the only downstream unknown. Equating the two pressure expressions and multiplying by yieldsup to an overall minus sign, where andThe discarded factor is the unchanged state, not a compressive shock. This derives the polynomial for the compression ratio of a perpendicular magnetohydrodynamic shock without omitting its trivial branch.
For the usual physical adiabatic index , is strictly increasing for positive , has , and has one positive root. Sincethat root is greater than one precisely when . The necessity is not limited to : for any , eliminating using givesFor , positive downstream pressure requires when . Moreover,The bracket is positive throughout , even when . The exactly cold unmagnetized limit gives the familiar strong-shock upper compression ratio directly. Thus the physical compressive branch requiresThe PDF's final denotes this same incoming speed . The right side is the squared speed of a perpendicular fast magnetosonic wave: the upstream flow must be super-fast-magnetosonic so that this compressive signal cannot run upstream against the incoming flow. At equality the shock amplitude vanishes into a characteristic disturbance.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 64 3 Solution Created 2026-10-03 Updated 2026-10-14
Use , and primes for derivatives. Time dependence is , so exponential growth means . The constant mass density and incompressible velocity giveAll magnetic factors below use the source convention .
Linearizing the ideal magnetohydrodynamic momentum equation, the advective perturbation is . The magnetic force is , whose component vanishes. Thus the three component equations areIn particular the vertical equation has the pressure-gradient and magnetic signs printed in the PDF.
The incompressible ideal magnetohydrodynamic induction equation can be written . Linearizing it givesFor , these areThe term is essential: a perturbed vertical magnetic component is stretched by the background shear flow. Differentiating these amplitudes and using incompressibility also verifies .
For completeness, substitution into all three momentum equations giveswhere is the vertical vorticity amplitude. Multiplying the equation by and subtracting times the equation eliminates pressure:Therefore, away from ,This is the nonresonant reduction relevant to the instability calculation. Division at the Alfvén wave resonance would be invalid. For a concrete counterexample to an unrestricted reading, take constant , , , and , with all other amplitudes zero. Every smooth solves the original linear system, but need not vanish. These transverse resonant waves do not drive . A genuinely growing mode in a real background has complex and cannot satisfy either or on the real axis. This explains exactly when the requested reductions may be used.
On that nonresonant branch, multiply the horizontal equations by and and add. Incompressibility gives , soCombining incompressibility with vorticity, multiply its first equation by and subtract times the definition of . This givesConsequentlySubstitute this and the derivative of the displayed pressure relation into vertical momentum. Multiplication by givesExpanding the second derivative once gives exactly the requested vertical-velocity equation:
To take the discontinuous-layer limit without multiplying distributions, introduce . It is proportional to the normal displacement: the material kinematic condition is , so . Since , . The same equation becomes the displacement equation for a parallel magnetic shear flowThe physical interface condition is continuity of , because both fluids move the same interface. For constant on each side, away from resonance the coefficient is constant and nonzero, so . Requiring decay at infinity and matching yieldsThe exponent is , as in the actual PDF; the converted TeX's there is a transcription error.
Integrate the conservative displacement equation across a layer of thickness . Its undifferentiated term has an integral tending to zero, while the derivative givesEquivalently, the perturbed magnetohydrodynamic total pressure is and is continuous. With and , a nontrivial amplitude requiresThis is also the rigorous thin-layer integration of the original vertical equation, after combining the derivative terms before taking the limit.
Put and . Completing the square gives the dispersion relationFor both interface frequencies are real, so there is no exponentially growing interface mode. Above that threshold, the growing sign has growth rate . This is magnetic stabilization of an equal-density vortex sheet: magnetic tension from bending the field overcomes the kinetic shear driving Kelvin-Helmholtz instability. Equality is marginal and the strict stable condition avoids its double-root degeneracy. The case has no streamwise shear drive and has the neutral interface frequency ; the nonzero-frequency elimination should be interpreted by the original equations or a limiting displacement formulation in that case. The horizontal affects the exponential decay length through , but not the stated threshold.
Past exam of the mathematics course of the University of Cambridge 2003 iii Paper 65 1 i Solution Created 2026-10-03 Updated 2026-10-14
Write horizontal components with a subscript . The steady ideal magnetohydrodynamic induction equation gives . Since , its horizontal components implyThus is a spatial constant. A vanishing axial electric field, , is needed to infer horizontal alignment. It is satisfied, for example, if the constant electric field vanishes at a boundary or at infinity. With this additional condition and , define the magnetohydrodynamic mass loading by , and put . ThenThe steady continuity equation and the solenoidal magnetic-field constraint giveAlso . Using the vector identity for the curl of a cross product, together with and , its curl is . HenceThese are steady planar ideal-MHD field-line invariants: both quantities are constant along a magnetic field line.
The zero-electric-field condition does not follow from the printed stationarity assumptions alone. Constant , , and , with , satisfy every displayed ideal magnetohydrodynamics equation but have perpendicular horizontal velocity and magnetic field. Their is nonzero, so no give the stated decomposition. The field-line decomposition is valid on the branch; as an unrestricted implication, the first claim has this counterexample. The subsequent calculations use that branch.
Past exam of the mathematics course of the University of Cambridge 2005 iii Paper 71 2 Solution Created 2026-10-03 Updated 2026-10-14
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 toIts 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 areThere 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 . Thuswhere .
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 asThe first term on the right cancels the other mixed term. Combining the remaining derivative with the term containing givesDifferentiating the equilibrium relation now combines the gradient of mass density and magnetostatic equilibrium terms:We obtain the incompressible magnetic displacement energy identityThe 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 isConsequently the interchange stability of an incompressible magnetized atmosphere is governed by the numeratorFor , 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 quotientunder 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 .
Past exam of the mathematics course of the University of Cambridge 2006 iii Paper 70 2 c Solution Created 2026-10-03 Updated 2026-10-14
For fixed volume define and . Differentiate and use the ideal magnetohydrodynamic induction equation. The vector identitythen gives the general balanceThe volume term is the work done by the magnetic force on the fluid, with the opposite sign for magnetic energy. Under the force-free assumption of part (b), it vanishes, leaving the requested boundary expression. Without that assumption, or another reason for zero net Lorentz work, a boundary-only balance is not generally valid.
For an axisymmetric boundary its normal has no azimuthal component. The differential rotation is tangential, so , and . Therefore . A thin axisymmetric tube between neighboring flux labels carries flux . Its exit endpoint contributes and its entry endpoint contributes . Pair the endpoints, counting each once, to obtainThe endpoint convention fixes the sign. Include each connected tube segment through once; a field line with no boundary crossing contributes nothing. This is magnetic-energy injection by differential boundary rotation. A common angular velocity at both ends produces no such injection.
Past exam of the mathematics course of the University of Cambridge 2007 iii Paper 65 2 c ii Solution Created 2026-10-03 Updated 2026-10-14
For the circular MHD wave polarization, is constant. Choose any constant , put and takeThis gives a circularly polarized nonlinear Alfvén wave of arbitrary amplitude. All fields depend only on , and , so and . Constant mass density and pressure then satisfy continuity and the adiabatic pressure equation, and because is constant.
The remaining ideal magnetohydrodynamic induction equation and transverse magnetohydrodynamic momentum equation areSince on the traveling profiles and , both identities hold exactly when . The longitudinal magnetohydrodynamic momentum equation holds because is constant. The circularly polarized wave is therefore an exact nonlinear solution even though the fluid is compressible. Compressibility permits mass density changes; it does not require every possible motion to compress the gas.
Past exam of the mathematics course of the University of Cambridge 2007 iii Paper 65 2 c i Solution Created 2026-10-03 Updated 2026-10-14
Take , and . The transverse ideal magnetohydrodynamic induction equation and magnetohydrodynamic momentum equation are satisfied by , , with constant mass density. However, the longitudinal magnetohydrodynamic momentum equation also requiresHere is not constant. Balancing its gradient would requireThe adiabatic pressure equation instead gives , since this velocity is divergence-free and has no component along the spatial variation. No choice of removes the spatially varying time derivative. Thus a nontrivial finite-amplitude linearly polarized sinusoidal Alfvén wave is not an exact pure traveling wave in a compressible ideal fluid. The magnetic-pressure obstruction to a linearly polarized Alfvén wave is quadratic in , so the wave is a valid linear approximation and drives a compressive response at higher order. In an incompressible model pressure is a constraint variable; it is not governed by the same compressible adiabatic evolution law.
Allowing longitudinal flow and varying mass density does not rescue a regular one-dimensional periodic traveling solution with precisely this transverse magnetic field. To see this, let and use the traveling coordinate. Integrated continuity, induction and transverse momentum givewhere are constants. Eliminating givesAt any zero of , finite mass density and velocity require the right side to vanish. Wherever , the coefficient then vanishes and fixes , constant; continuity fixes , and adiabatic entropy transport fixes . The longitudinal magnetohydrodynamic momentum equation again contradicts the varying . The alternative makes transverse momentum force constant. Trivial cases such as or are excluded from the nontrivial wave conclusion.