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Fourth-year transfer route after the first three years of an eligible Oxford undergraduate degree. Teaching is shared with the MSc in mathematical and theoretical physics course of the University of Oxford. Examined subjects include Groups and representations course of the University of Oxford.
The held 2022 paper uses this title. Its source title and formal code are retained separately from later papers headed advanced quantum field theory for particle physics course of the University of Oxford.
Source bundle pages 111–115. The paper cover establishes 2022; the attachment filename uses 2021.
There are two one-loop Feynman diagrams: the two orders of the labelled photons around a top quark fermion loop, with one Yukawa interaction insertion for the outgoing Higgs boson. They are added, rather than identified by a Feynman-diagram symmetry factor. Each has the same color charge trace .
Figure 1.
The two photon orders and consistent directed loop momenta
. Original Feynman diagrams. Solid arrows show fermion flow and the labelled internal four-momenta. Wavy external lines are incoming photons; the dashed external line is the outgoing Higgs boson. The two panels use independent dummy loop momenta. Details.
In the first routing, traverse the fermion loop from the insertion to the insertion with momentum , then to the Higgs boson insertion with momentum , then back to the insertion with momentum . Conservation at the Higgs boson insertion gives . The second routing exchanges and : its three internal momenta are , and . Reversing the orientation is another way to represent this second ordering. Two vector insertions give no Furry theorem cancellation.
Use Minkowski metric and the convention . Put , , and
The Feynman i-epsilon prescription is understood in subsequent denominators. Contracting the spinor indices around the fermion loop gives the trace
Here is Feynman slash notation. The closed fermion loop sign is , the three interaction vertices contribute , and the three Dirac propagators contribute . Their product, including the color charge trace, is . Thus one ordering has
Multiplying by the incoming polarization vectors and adding the exchanged Feynman diagram gives
The displayed four-dimensional Feynman integral is formal until regularized; subsequent manipulations use dimensional regularization, which permits the required loop momentum shifts.
Set , so and . The physical polarization vectors obey . Write when they agree after contraction with these polarization vectors; terms proportional to or may then be discarded.
The gamma matrix trace identities kill the terms with an odd number of gamma matrices. The remaining three two-momentum terms and the term with three factors of are
In the coefficient the terms linear in cancel, leaving . Among the other terms, the surviving mixed products of and also cancel. Consequently
In the second Feynman diagram, exchange the external labels and change the dummy loop momentum . Its projected numerator and denominator become identical to those of the first Feynman diagram. Hence
With the common factor extracted, the primitive integer coefficients are
Equivalently, extracting only gives and prefactor . A common rescaling of all three coefficients changes the prefactor inversely. The physical scattering amplitude is ; the projected integrand is not an identity for an arbitrary uncontracted off-shell tensor.
Continue the loop momentum to dimensions, keeping and the external physical polarization vectors four dimensional. Introduce Feynman parameters , , denoting this integration triangle by . Completing the square gives
Odd terms in integrate to zero. Lorentz invariance of dimensional regularization gives . The general projected numerator therefore becomes, under the Feynman integral,
Only the term can give an ultraviolet divergence. Define, with the conventional scale factor implicit,
The gamma function formula gives
Thus the pole of the numerator integral, including , is
The coefficients satisfy this condition. A nonzero local divergence would have to be removed by a counterterm. The Ward identity forbids a local term, and the first electromagnetic gauge-invariant coupling with one Higgs boson and two photons has the form , of engineering dimension five. It is not an independent counterterm of the Standard Model, a renormalizable quantum field theory. The top quark contribution is separately electromagnetic gauge-invariant; no additional W boson loop Feynman diagram is needed to cancel this pole.
The finite remainder must still be retained. For ,
Putting before evaluating the divergent Feynman integral would incorrectly set this finite contribution to zero.
Use the Feynman parameters and defined in Solution. With , the finite term just found is . Combining it with the remaining coefficient gives
The other coefficient is . Thus, writing for the Feynman integral without the overall prefactor,
For , the two coefficients must have the corresponding ratio. The mismatch is simply , independent of . Therefore the required relation is
which is satisfied. In the primitive normalization the result is
and the full top quark scattering amplitude, in our stated convention, is
Indeed : replacing either polarization vector by its photon momentum makes the scattering amplitude vanish. This is the Ward identity, expressing electromagnetic gauge invariance. The result also is symmetric under exchange of the two photons. The finite term in Solution is essential for this Ward identity.
As an independent low-energy check, for the Feynman parameter integral is
The coefficient is consequently at leading order. It has the inverse-mass dimension required for an effective coupling. If , this coefficient stays finite in the large- limit at fixed ; that limit increases the Yukawa coupling, so it is not a fixed-coupling heavy-field decoupling limit.
At the stated order the renormalization-group beta function is separable:
Consequently
For a positive initial running coupling, this expression is used on the connected interval containing where its denominator is positive and perturbation theory remains valid.
If , the running coupling decreases at high renormalization scale and tends to zero: this is asymptotic freedom. Decreasing the renormalization scale increases the running coupling, with a formal infrared pole at . Near , perturbation theory fails; the pole alone is not a proof of confinement. Both QCD and the SU(2) weak gauge coupling have this sign for the Standard Model particle content above the relevant thresholds.
If , the running coupling decreases towards low renormalization scale and grows towards high renormalization scale. The formal ultraviolet Landau pole is . The pole signals failure of this perturbative evolution, rather than a controlled physical infinity. The hypercharge gauge coupling and ordinary QED with charged matter have this sign.
If , the running coupling is constant at this order; higher-order terms may still make it run. No Standard Model gauge factor has a vanishing one-loop order coefficient for the usual particle content.
For precise normalization, take and . The Standard Model one-loop gauge coefficients then give
These coefficients use , not . Threshold matching changes the active particle content, so the single constant- expression is applied piecewise across thresholds.
There is one tree-level Feynman diagram: annihilation of the up quark and its antiquark into an -channel gluon, followed by production of the down quark and its antiquark. A gluon interaction vertex preserves quark flavor, so a -channel line joining the incoming up quark to the outgoing down quark is impossible.
Figure 1.
Annihilation and exchange channels with labelled external momenta
. Original Feynman diagrams, with arrows denoting fermion flow. The left panel with and is the distinct-quark flavor process. Both panels with describe Bhabha scattering; both with and describe identical-quark flavor scattering. The wavy internal line stands for the indicated vector mediator. Details.
Let label the initial quark, initial antiquark, final quark, final antiquark color charges. Up to an irrelevant common sign, the scattering amplitude is
The Mandelstam variables are , , , with in the zero-mass limit. The spin sum uses , and the initial spin average contributes . The resulting two gamma matrix traces contract to
The initial color average contributes . Summing final color charges gives the distinct-flavor quark scattering color factor
Therefore
Equivalently for the QCD coupling . There is no initial gluon spin average: the gluon is internal.
The two Bhabha scattering tree-level Feynman diagrams are the two panels of Solution with a photon mediator: -channel annihilation with internal momentum , and -channel exchange with internal momentum . Each interaction vertex preserves the electron species. There is no independent -channel Feynman diagram, since the outgoing electron and Positron are distinguishable.
Removing the color charge factor from Solution and replacing by gives
Crossing symmetry interchanges and for the exchange Feynman diagram, giving
Squaring the sum of the two scattering amplitudes also produces the interference term . The given third term must be this cross term: it has both propagator denominators , whereas a squared individual Feynman diagram has or . With the correct relative fermionic sign, its value is . Thus
The coefficient of the last displayed fraction is positive, but and in the physical scattering region, so this interference is destructive. The relative sign originates in the two possible external fermion contractions; changing an external-state phase changes both scattering amplitudes together.[ref]
Both -channel annihilation and -channel gluon exchange are now allowed. Their spin sum factors are the Bhabha scattering factors with . Their color charge tensors, with the external indices of Solution, are
Each squared term has . The cross term instead has the color average
To evaluate it, use the SU(N) fundamental completeness relation
This follows by completing the orthogonal basis of traceless Hermitian matrices with the identity. Since , it gives , and hence
Multiplying the two squared Bhabha scattering terms by and its cross term by gives
For the SU(3) gauge group, this is
The negative color charge overlap reverses the sign of the QED interference. Since , this cross contribution is positive in the physical region. No additional spinor calculation is needed; all the new information is in the SU(N) fundamental completeness relation.
The Goldstone theorem states that spontaneous breaking of a continuous internal global symmetry in field theory in a local relativistic quantum field theory produces a zero-mass Goldstone boson for each independent broken generator, under the usual positive-state-space and conserved-current hypotheses. For there are symmetry-required Goldstone bosons. This count assumes a Lorentz-invariant vacuum state; nonrelativistic counting can differ.
At the classical level, invariance of the scalar potential gives . Differentiating at a stationary vacuum expectation value yields
These are the Goldstone directions in the scalar mass matrix. Broken generators have , so their independent directions have zero quadratic mass with a canonical kinetic term. The theorem guarantees these modes; it does not exclude further accidental zero-mass modes. A local gauge symmetry is a redundancy and does not meet the physical global-symmetry hypothesis: the Higgs mechanism can instead supply longitudinal particle polarizations of massive gauge bosons.
Put . Completing the square in the scalar potential gives
Since , its global minima form the vacuum manifold
Here denotes the positive square root of the parameter . The origin is a local maximum, not a ground state. Choose . Its stabilizer subgroup is the SO(2) subgroup of rotations in the plane, so the stated SO(3) global symmetry in field theory is spontaneously broken to SO(2).
Write , , . The kinetic terms stay canonically normalized, while the scalar mass matrix is
Equivalently, the quadratic scalar potential is . Therefore the particle masses are
The two angular Goldstone bosons match . The radial displacement changes and costs potential energy, giving the massive Higgs mode. These are tree-level masses; the Goldstone theorem protects the angular zero-mass modes in the exact global theory.
For any fixed , the source contribution obeys , because and . Equality occurs only at when . Thus the global ground state lies on the positive first axis. Minimize there:
For , . For , , so increases strictly from to . There is exactly one root , and it is the unique global minimum. Therefore
This argument selects the true ground state even if the full cubic has additional negative stationary roots.
Expand , , . The source is linear, so it shifts the expansion point but has zero Hessian matrix. The scalar mass matrix is diagonal at the new vacuum expectation value:
Eliminating with the stationary equation gives
All three squared masses are positive. The masses themselves are the positive square roots of these expressions.
The source explicitly reduces the stated SO(3) symmetry to SO(2); the selected vacuum state preserves that remaining SO(2). There is consequently no spontaneously broken exact continuous global symmetry in field theory to which the Goldstone theorem applies. For small , the two angular excitations are pseudo-Goldstone bosons. Their squared masses vanish as , while and .
In unitary gauge the quadratic action is that of a Proca field. Use Minkowski metric and add a source . Integration by parts, dropping the boundary term, gives
With Fourier transform convention , its kernel is
For , introduce the transverse and longitudinal momentum projectors
They obey and as mixed-index linear operators. Hence
The final expression is regular at ; the apparent singularities of the individual projectors have cancelled.
The normalized Gaussian functional integral is evaluated by completing the square with :
The source-independent functional determinant cancels in this ratio. Two source derivatives insert two fields, so the covariant Feynman propagator is , with the Feynman i-epsilon prescription at the physical pole:
This is the Proca propagator. Its pole residue has the three physical particle polarizations of a massive spin-one gauge boson. No additional gauge-fixing term is needed to invert this already gauge-fixed massive quadratic action. In a full interacting Higgs mechanism calculation, any field-dependent unitary gauge measure belongs to the interacting theory; the free quadratic gauge boson propagator above is unaffected.
Solutions to both questions and all nine parts. The two-sphere calculation uses the leading free-draining approximation, with negligible connector drag; the limitations of that approximation are made explicit.
To first order in fluid velocity divided by the speed of light, the Lorentz transformation of electromagnetic fields gives . Applying Ohm's law in the local fluid frame gives . Neglecting the displacement current in Ampère's law, . Substitution in Faraday's law gives
Here is the magnetic diffusivity; the paper's is electrical resistivity, rather than magnetic diffusivity. Expanding the curl with the solenoidal magnetic-field constraint gives the resistive induction equation in its compressible form:
The left side is the material derivative of the magnetic field. The three right-hand terms respectively describe field-line stretching and reorientation, amplification or dilution by compression or expansion, and magnetic diffusion. In particular, compression has and amplifies a field component perpendicular to the compression.
The assumptions are nonrelativistic bulk motion, the low-frequency approximation permitting omission of the displacement current, a conducting-fluid continuum, isotropic local Ohm's law with spatially constant scalar electrical resistivity, constant magnetic permeability , and . Hall, electron-pressure and other non-Ohmic corrections to the generalized Ohm's law are excluded. Incompressible flow is not required: imposing it would remove the compression term.
Let be the total magnetic energy. Multiply the curl form of the resistive induction equation by and integrate over the fixed volume. The identity
follows from the divergence theorem. The stated zero boundary fields remove its surface term. Applying it to the motional and resistive contributions yields the magnetic energy balance in resistive magnetohydrodynamics:
The first term is the negative of the mechanical power delivered to the fluid by the Lorentz force density. It transfers energy between fluid motion and the magnetic field, with either sign. The second is the nonpositive magnetic contribution to Joule heating. A nonzero positive electrical resistivity therefore dissipates magnetic energy at rate ; it does not force the total magnetic energy to decrease when fluid motion supplies a larger positive power.
Choose a magnetic vector potential with . The resistive induction equation permits the evolution equation
A gauge transformation changes by a surface integral of the normal magnetic field, which is zero here. Thus the integrated magnetic helicity has gauge invariance under the stated boundary conditions.
Differentiate both factors in . Use the stated vanishing-boundary assumption to remove the helicity surface flux; this can be implemented in the usual closed-boundary gauge , or by extending the localized field and integrating over all space with sufficient decay. The curl integration by parts identity then gives
The motional term is zero pointwise because . The scalar-potential term integrates to zero by and the boundary condition. The resistive magnetic-helicity balance is therefore
Unlike the resistive magnetic energy contribution, this signed integral need not have a fixed sign.
A magnetic field varying over a length has of order . Consequently, the resistive magnetic energy loss contains two inverse powers of , while the resistive magnetic-helicity balance contains only one. Small-scale gradients can therefore dissipate substantial magnetic energy while retaining an approximately conserved large-scale magnetic helicity.
A dimensionally consistent version is the selective decay bound for magnetic helicity. With , the Cauchy-Schwarz inequality gives
For bounded and bounded, possibly nonvanishing as , the resistive change in magnetic helicity tends to zero, even though resistive magnetic energy loss may remain finite. Magnetic energy is preferentially dissipated, while magnetic helicity is approximately conserved in this bounded-energy, bounded-dissipation limit.
This is not a comparison of quantities with different physical units or a universal ordering of fractional decay rates. For a single Beltrami field satisfying , both integrated quantities have fractional decay rate without fluid motion. The boundedness assumptions and distribution of magnetic helicity across spatial scales matter.
The stress tensor of the incompressible Newtonian fluid is , where is the rate-of-strain tensor. The homogeneous Stokes equations give . Apply the divergence theorem to the fluid between the body and a surrounding sphere . If points from the body into the fluid, the fluid-domain normal on the inner boundary is . Hence
This is the force flux at infinity in Stokes flow. A nonzero resultant force must be supported by a stress of order on a surface of area of order . More precisely, the leading exterior solution is a Stokeslet with force on the fluid :
Thus , and . These are leading generic orders for a translating body with nonzero drag; the integral alone does not determine every angular component, and force-free disturbances may decay faster.
For two Stokes flows in the same fluid domain with the same dynamic viscosity, symmetry of the Newtonian fluid stress tensor and incompressibility give the local reciprocal identity
In index notation, its remaining cross-gradient terms are both . On the remote sphere the integrated reciprocal flux tends to zero: the velocity is , the stress tensor is and the area is . On the body, the no-slip boundary condition makes the two velocities the constants . The Lorentz reciprocal theorem therefore gives
By the Linearity of Stokes flow, the sum of the two velocity-pressure fields satisfies the boundary conditions for body velocity . Uniqueness of the exterior Stokes flow identifies it with the third solution. Since the stress tensor and its surface integral are linear too, ; scalar multiplication follows in the same way. Thus for a fixed-orientation hydrodynamic resistance matrix . Substituting arbitrary in the reciprocal identity yields
The minus sign is natural because viscous dissipation gives for nonzero rigid translation in an otherwise stationary fluid; is a positive-definite matrix.
Use the free-draining approximation: neglect the hydrodynamic interaction between the widely separated spheres and neglect the connector's viscous drag. Stokes law gives for each sphere. Their resultant is
This is the leading two-sphere approximation, not an exact finite-separation hydrodynamic resistance matrix. Writing and , the first Stokeslet reflection gives, if the connector remains negligible,
The negative correction expresses reduced drag from fluid entrainment by the other sphere. A very thin but arbitrarily long rod need not have negligible total drag: its typical transverse drag scales as for rod radius . Thus the simple boxed result uses the intended negligibly dragging connector limit as well as ; the two printed size inequalities alone do not specify a uniform limit in which rod drag vanishes.
Hold the two-sphere object fixed in a uniform stream . In the free-draining approximation, its drag forces are , with . The hydrodynamic torque about is
To make it zero for every incoming-stream direction, choose the hydrodynamic centre of a two-sphere dumbbell:
It lies closer to the larger sphere, whose larger drag requires a shorter lever arm. Uniform translation does not spin an isolated sphere, so no additional isolated-sphere spin torque enters this leading approximation.
Figure 1.
Drag-weighted hydrodynamic centre of two widely separated spheres
. Details.
Finite-separation hydrodynamic interactions and connector drag can change the displayed location; the calculation has the same approximation as part c.
For rotation about the hydrodynamic centre of a two-sphere dumbbell, the sphere centres have velocities . Their resultant drag force in the free-draining approximation is
Each sphere also experiences a spin drag torque, but its isolated rotation causes no net force. Those spin contributions therefore do not alter the cancellation.
This illustrates translation-rotation reciprocal coupling. About any fixed origin, write the fluid's rigid-body force and torque as
The transposed cross-blocks follow from the Lorentz reciprocal theorem. If pure translation causes zero torque about an origin for every , then , hence pure rotation about that origin causes zero force. This implication is general for linear Stokes flow; the existence and leading location of such an origin here use the two-sphere geometry and the approximation in part c.
Solutions to both questions and all nine parts. Part 2(d) contains a false identity in the source; its counterexample and the consistent free-energy balance are supplied.
Start in an inertial frame with the inviscid magnetohydrodynamic momentum equation,
Here is mass density, is the isotropic fluid pressure, is inertial-frame velocity, is electric current density, is the magnetic field, and is gravitational potential per unit mass. In the low-frequency approximation to Ampère's law, . The vector calculus identity
separates the Lorentz force density into magnetic tension and a magnetic pressure gradient. Transform the material acceleration to a rigid frame rotating with constant angular velocity , using the stated frame transformation. The rotating-frame magnetohydrodynamic momentum equation is
The final terms are the Coriolis force and centrifugal force densities; is the velocity relative to the rotating frame, and uses that frame.
This requires a smooth conducting-fluid continuum with nonrelativistic motion, a constant magnetic permeability , the solenoidal magnetic-field constraint, a negligible displacement current and negligible net electric-charge force. Viscous forces and anisotropic fluid stresses are omitted. A time-dependent frame would add an Euler force. Incompressible flow is not needed for this force equation. Finite electrical resistivity does not change its displayed instantaneous magnetic force; the later frozen-field calculation additionally uses ideal magnetohydrodynamics. A differentially rotating fluid does not define a single rigid frame with spatially varying : choose a fixed local reference rate and retain the fluid's shear in .
In an inertial frame, a circular orbit at radius has radial acceleration . Neglecting fluid and magnetic forces gives
In a local rotating frame with , the fluid is instantaneously at rest at the reference radius . The radial centrifugal force then balances the inward gravitational force. Away from , the fluid's nonzero rotating-frame velocity must also be retained; the entire differentially rotating disk is not at rest in that one frame.
Take outward radial force as positive and keep the displaced element's angular rate fixed at . Its imbalance is
Use the equilibrium relation from part b, , and a first-order Taylor expansion:
The absolute values are needed for a magnitude. As printed, the proposed magnitude has a signed right side; it would be negative for outward displacement in a Keplerian disk. For decreasing , the signed imbalance above points outward and therefore amplifies that fixed-angular-rate displacement. This calculation fixes the angular rate, rather than the specific angular momentum; the latter is the conserved quantity for an uncoupled inviscid radial displacement and leads to the Rayleigh centrifugal stability criterion.
Linearized magnetic flux freezing gives the Eulerian magnetic field perturbation
The background is uniform, and incompressibility gives . For a horizontal displacement proportional to , and . Thus the first-order magnetic pressure perturbation vanishes, and the magnetic-tension response to an incompressible displacement is
Bending a field line produces a restoring force proportional to displacement, like a spring obeying Hooke's law. Per unit mass, its squared spring frequency is , where is the Alfvén speed. The equilibrium can be independent of while the perturbation varies with ; neglect of background vertical structure does not set this perturbation's wavenumber to zero.
Work locally at with , and define
Here is the radial epicyclic frequency. Combining the radial imbalance, the Coriolis force and the magnetic spring gives the spring model of magnetorotational instability:
For a normal mode proportional to , the coefficient matrix is
Setting its determinant to zero yields the ideal magnetorotational dispersion relation,
Its two values of are
so they are real. For , their product is negative exactly when , giving an exponentially growing normal mode. Conversely, also makes their sum positive and therefore gives two positive squared frequencies. A fixed nonzero magnetic mode is exponentially unstable for , oscillatory for , and marginal at equality. Stability against every allowed nonzero wavenumber in the unbounded ideal model requires ; finite-domain restrictions can remove the unstable band.
For , the equilibrium relation gives , so and . Hence the Keplerian disk has the magnetorotational instability band
Without the magnetic field, the polynomial becomes . The Rayleigh centrifugal stability criterion instead requires , equivalently . A Keplerian disk satisfies that hydrodynamic criterion. Magnetic coupling therefore destabilizes a disk that has a restoring hydrodynamic epicyclic oscillation; the field couples angular-momentum exchange between elements, rather than acting only as an isolated restoring spring.
Figure 1.
Unstable band and fastest growth of the ideal vertical-field Keplerian mode
. Details.
The plotted maximum is the maximum growth rate of ideal magnetorotational instability, at .
Using the given linear momentum balance, multiply by the velocity and integrate over the fixed volume:
This is integration by parts component by component, or the divergence theorem. The first term is boundary stress power. With component-first velocity gradient , the second is the double contraction .
For a Newtonian fluid, , where is the rate-of-strain tensor and is dynamic viscosity. Incompressibility removes the pressure contribution, and the symmetric tensor is orthogonal to the antisymmetric part of . Therefore
The displayed energy identity follows for the stated linear balance. A full advective momentum equation in a fixed control volume would also contribute an advective kinetic energy flux. The nonnegativity statement here is for a purely Newtonian viscous stress; a viscoelastic stress can exchange stored free energy with the flow.
Let , , and . The configuration equation of the Hookean dumbbell model becomes
Here the paper's denotes the Boltzmann constant . Integrating the second moment equation against and discarding boundary terms at infinite separation gives
For example the spring drift differentiates each factor , while the Laplacian gives . The Hookean dumbbell conformation equation is
In the row-vector convention of , the displayed gradient tensor is , giving exactly the transposes in the requested equation. The dimensionless conformation tensor consequently has upper-convected derivative , with polymer relaxation time . This normalization matters: the unscaled has equilibrium value , rather than .
Write the centre position as and the bead positions as . In the affine velocity field, . The midpoint follows the flow, so its two slip velocities are
Each bead loses mechanical power times its squared slip speed. Adding the two powers proves the drag dissipation of a bead-spring pair:
The factor one half comes from two equal-and-opposite bead slips, not from assigning only one bead a drag force.
The claimed equality does not hold for the printed joint distribution. The original PDF specifies a centered Maxwell-Boltzmann distribution of independent of , with
Since the double average includes number density , evaluating the Gaussian integrals gives
The cross term vanishes because the conditional mean of is zero. In particular, set and take the equilibrium configuration probability density . The left side is , while . This is a counterexample even at thermal equilibrium, so no rearrangement of the earlier conformation tensor equation can prove the printed statement.
The discrepancy is thermal bead drag and heat-bath power: gross viscous loss of microscopic thermal motion is replenished by the thermal bath. It is not identical to mechanical polymer stress power. Moreover, in the earlier configuration continuity equation is a probability current velocity, including a distribution-dependent osmotic drift; it cannot simultaneously be identified with an independently sampled centered Maxwellian velocity.
A consistent overdamped result is the free-energy balance of a Hookean dumbbell. Define and
Differentiate the relative entropy and use the configuration Fokker-Planck probability current . After integration by parts,
The affine osmotic term is . Hence
The polymer stress tensor has in an incompressible flow. It stores or releases free energy as well as dissipating it, so the total stress-work term in part a need not itself be a purely dissipative quantity for this viscoelastic material. Stress power equals only for stationary free energy, and uses the probability-current slip. Neither condition turns the printed independent-Maxwellian average into that expression.
Solutions to both questions and all eight parts. The diffusion coefficient and the amplitude-versus-energy damping convention are stated explicitly; the final rotation calculation uses the supplied isolated-sphere incident flow.
Take the inviscid limit of the Navier-Stokes equation, neglect gravity, and use ideal magnetohydrodynamics. The governing equations are
The continuity equation also gives . Write the first-order magnetic perturbation as and linearize about the uniform stationary background:
For a nonzero-wavenumber plane wave proportional to , the two divergence constraints imply . The longitudinal momentum equation then gives for that mode, and gives for nonzero . Thus the propagating Alfvén wave is transverse. Its two independent transverse directions have the same dispersion relation.
The Linear Alfvén wave equations reduce to
Eliminating either amplitude gives
For , the branch traveling along has and . The opposite branch reverses that amplitude sign. Finite viscosity would additionally damp the motion; it is neglected in obtaining the real ideal dispersion relation.
Subtract the constant equilibrium magnetic energy density. Since , the perturbation densities are
The traveling-wave amplitude relation from part a gives
This is pointwise Alfvén wave energy transport for one traveling wave, not a claim that every superposition or standing wave has pointwise equipartition.
For the real fields written as and similarly for , the period averages are
The factors one half distinguish a sinusoid's peak amplitude from its mean squared value; the same complex-vector convention also covers circular polarization of waves.
In ideal magnetohydrodynamics, the first-order electric field is . Retaining its product with both the background and first-order magnetic field gives the Poynting vector
The first term is transverse and oscillatory, with zero period average. The second is quadratic and transports wave energy. A potential quadratic ideal electric-field term vanishes here because the real traveling-wave fields are parallel or antiparallel.
For the branch, , so
For the opposite branch, its sign reverses. The averaged Poynting flux is the total wave energy density, including equal kinetic and magnetic shares, multiplied by the group velocity. This agrees with Alfvén wave energy transport. Although the flux in this expression is electromagnetic, it supplies the transport of both components of the coupled fluid-field wave.
In this question, the coefficient multiplying is the magnetic diffusivity. Denote it ; it is the paper's , with dimensions of length squared per time. If denotes electrical resistivity, then . The two conventions must not be interchanged.
For an imposed real positive , retain the momentum equation and use
Elimination gives the exact Resistive damping of an Alfvén wave relation
Here is complex because the driving frequency is real. Introduce the dimensionless diffusion parameter . For propagation and attenuation along , choose the square-root branch with . The spatial damping of a driven Alfvén wave is
With the convention , the amplitude decays as . Define its e-folding length and the wavelength . Then
If damping length instead refers to wave energy, the squared amplitude decays twice as fast: and . Stating the convention avoids a factor-of-two ambiguity. The temporal damping rate at fixed real is a different specification from this imposed-frequency problem.
Figure 1.
Weak spatial attenuation of a driven Alfvén wave and its amplitude envelope
. Details.
Expand the given translating-sphere Stokes flow into its Stokeslet and potential dipole parts:
The second parenthesis is and has zero curl outside the sphere. For the first,
Thus the vorticity of translating-sphere Stokes flow is
The result is independent of the irrotational finite-size dipole correction. It holds in the exterior ; the singular solid harmonics are used only outside their source.
Use the force flux at infinity in Stokes flow. With an outward normal from a large sphere, the force on the body is . Let . The leading far-field velocity and pressure are
Their rate-of-strain tensor is
In the Newtonian fluid stress tensor , the isotropic pieces cancel. Consequently,
The second spherical moment integral follows from rotational symmetry and . Since , taking gives the Stokes drag law:
The omitted dipole contributes a surface integral of order and vanishes in this limit. The sign refers to the fluid's drag on the moving sphere.
At the terminal velocity, buoyancy-corrected weight balances the Stokes drag law:
Hence
A denser sphere falls in the direction of ; a lighter one rises. Equal densities give no sedimentation. The calculation assumes negligible fluid Reynolds number, an unbounded fluid, and negligible transient body acceleration after terminal settling. The fluid mass density enters through buoyancy and through the small-Reynolds number condition.
Take positive upward, let sphere A's centre be , and write its downward velocity as , with . At B's centre the displacement from A is . The vorticity of translating-sphere Stokes flow therefore gives
B is held in translation but has zero applied torque. By Faxén's rotational law, it rotates with half the incident vorticity:
Integrating the rotation induced by a passing Stokes sphere along the complete path cancels :
Its magnitude is radians, with direction about the negative axis by the right-hand rule. All instantaneous rotations have this same axis, so the integrated angular velocity gives the net angle without a noncommuting-rotation correction. The result is independent of B's radius in the prescribed incident-flow calculation.
Figure 1.
Angular velocity and cumulative rotation from an isolated sphere passing a torque-free target
. Details.
The inequality ensures no overlap. It does not by itself make mutual hydrodynamic interactions negligible: the stated flow is the isolated-A solution, and a held finite B also disturbs A's flow. Thus the displayed angle is the result for that supplied incident flow, or the leading one-way approximation to separated bodies. A fully coupled two-sphere calculation uses the method of reflections for Stokes flow or an exact pair resistance solution.
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