Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 63 2 Solution Created 2026-10-03 Updated 2026-10-14
In the radiative layer, take the enclosed mass to be , the transported luminosity to be , and the mean molecular weight to be constant. The envelope's own gravity is neglected. Divide the hydrostatic and radiative temperature equations, and then eliminate density using the gas equation of state:Put and . For , integration givesDefining and yieldsIn the relevant positive-exponent case, writing produces the stated form whenever this integration constant is nonnegative. The exceptional values excluded above lead to logarithms: gives , gives , and both zero give .
For radiative-envelope convection matching, compute the logarithmic gradient of the pressure relation:At the marginal boundary, the Schwarzschild criterion equates this with the ideal-gas adiabatic gradient . HenceThe positive real notation requires a nonnegative bracket; a general signed is the safer integration constant otherwise. For the later case and a monatomic gas, this bracket is , so is of the same order as .
Deep below the convective boundary, with the temperature-power term dominating , the pressure law becomes . Differentiating this approximation and using hydrostatic balance givesThe general temperature is a term proportional to plus a boundary-dependent constant. Well inside the boundary radius, where that term dominates, it reduces toThe inverse-radius profile is an inner approximation, not an assertion that the boundary term vanishes everywhere.
Now take , so , . Then , , and define so that . The luminosity supplied by the thin burning layer isBecause the integral is strongly concentrated near and , the outer term is negligible. ThusThe factor , rather than merely , is essential since the specified energy-generation rate is per unit mass. This integration uses the deep radiative profile as a leading thin-shell approximation.
Crucially, is not independent of luminosity. Its defining relation givesSubstitution into the shell integral therefore yields . The degenerate-core relation gives , soThis degenerate-core shell-burning mass-luminosity relation is specific to the adopted opacity, burning exponent and structural approximations.
Removing some envelope mass while retaining the hydrogen-burning shell and the deep-envelope regime leaves the leading luminosity approximately unchanged at fixed core mass. The envelope can instead change the radius and effective temperature. This independence is not valid for arbitrarily complete stripping: removing the fuel or the pressure-confined shell structure quenches or modifies shell burning, and the assumed giant model then fails.
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 63 3 a Solution Created 2026-10-03 Updated 2026-10-14
Write and for the number densities of nickel-56 and iron-54. Both nuclei contain 28 neutrons, while their proton numbers differ by two. Dividing the positive-exponential nuclear statistical equilibrium formulas printed in the PDF therefore gives the nickel–iron nuclear equilibrium ratioThe neutron-density factors cancel. contains the isotope-dependent statistical and translational mass factors suppressed in the supplied proportionality; it is constant in this simplified calculation. The TeX conversion incorrectly reverses the exponential sign, so the PDF sign is essential here.
In the specified restricted composition, equality of total proton and neutron numbers meansConsequentlyDifferentiation, with the suppressed prefactors held constant, givesUsing the paper's supplied signed energy difference producesWith that negative value, tends to zero at both temperature endpoints, increases below this temperature and decreases above it. At the stationary point , so it is indeed a maximum for the printed toy data.
There is a genuine physical-data qualification: the stated negative energy difference is inconsistent with interpreting as the conventional positive total nuclear binding energy of these actual isotopes. Using atomic masses, whose electron masses cancel in this reaction,The masses used are , and , from NIST hydrogen masses, NIST iron masses and NIST nickel masses. Small electronic binding corrections do not change the sign. With a positive , the simplified above is strictly decreasing for and has no finite maximum. Thus the numerical maximum follows from the supplied negative parameter, not from consistent physical binding energies; changing the TeX sign to recover a maximum would not repair the PDF's data.
Nuclear statistical equilibrium is appropriate when the relevant forward and inverse strong or electromagnetic reactions are fast compared with changes of temperature, density and composition. It is useful in sufficiently hot late silicon-burning material and in the hottest explosive burning regions of massive stars. Some burning zones reach only quasi-equilibrium, and cooling or expansion eventually freezes the abundances out; an equilibrium expression cannot by itself predict the full ashes when these timescale conditions fail. Temperature, density, conserved baryon number and the electron fraction in stellar matter must all be specified. Negligible free-particle contributions in bulk bookkeeping are not the same as exactly zero free densities in the equilibrium formula.
Strong and electromagnetic reactions preserve total charge and baryon number, so they conserve the proton-to-neutron ratio. Weak reactions need not: electron capture and beta-plus decay convert protons into neutrons and lower it. Such conversions occur in hydrogen-burning networks and in the nitrogen-to-neon chain during helium burning. At high density in advanced stellar cores and core collapse, electron capture becomes particularly important; neutrino emission also affects energy and lepton loss. Beta-minus decay changes the ratio in the opposite direction and can compete during later relaxation. Nuclear equilibrium for strong reactions does not automatically imply weak equilibrium or a fixed proton-to-neutron ratio throughout all stellar evolution.
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 63 3 b Solution Created 2026-10-03 Updated 2026-10-14
Use for the neon-22 mass fraction, temporarily keeping it distinct from the earlier metallicity. Let be the baryon density, ignoring small nuclear mass defects. Equal masses of carbon and oxygen giveCarbon-12 and oxygen-16 each have equal proton and neutron numbers, while neon-22 has ten protons and twelve neutrons. The total proton and neutron numbers per baryon are consequentlyHenceThe equal carbon/oxygen mass split cancels from this result: any mixture of these two symmetric nuclei has the same electron fraction. Taking the paper's metallicity symbol to mean gives its requested expression.
The literal pre-helium-burning nitrogen interpretation, however, needs a correction. Each initial nitrogen-14 nucleus receives two alpha particles, including eight additional baryons, before becoming neon-22; the intervening beta-plus decay also emits a neutrino. Thus, if the entire original metallicity is nitrogen-14 with mass fraction , conservation of the number of seed nuclei givesThis is neon-22 neutron excess from nitrogen-14. The two expressions are compatible only when their arguments are distinguished: the displayed law uses the final neon mass fraction, not literally the earlier nitrogen mass fraction. Treating those fractions as equal is an extra simplifying approximation, not a consequence of the stated capture chain.
A radioactively powered Type Ia supernova light curve rises to a broad maximum over roughly weeks as energy deposited in expanding ejecta diffuses out, then declines over the following weeks and months. Its power comes predominantly from the nickel-56 decay chain, first nickel to cobalt and then cobalt to iron. Gamma rays and charged decay products deposit heat, which is reprocessed into optical and infrared radiation. At later times, declining cobalt decay power and increasing gamma-ray escape shape the tail. It is not sustained nuclear fusion in the expanding ejecta. The amount of radioactive nickel, photon diffusion time and deposition efficiency all matter, so an uncorrected fixed luminosity is only an idealization.
For the requested two-isotope yield calculation, assume the same total processed iron-group mass, namely as inferred from the zero-neon reference. Treat the final freeze-out ashes as nickel-56 and iron-54, neglecting residual light particles and additional weak neutronization. If is the nickel mass fraction, conservation of electron fraction givesSince , this reduces to the metallicity dependence of nickel-56 yieldUnder the paper's intended identification ,If instead denotes the earlier nitrogen mass fraction, retaining the actual capture stoichiometry gives and . The same temperature and density do not alone fix a total burned mass; equality of that mass is also implicit in the comparison. The two-isotope assumption is a bulk-ash approximation, not a complete equilibrium network with all free particles identically absent.
For otherwise comparable explosions, approximate the peak luminosity by a quantity proportional to the radioactive nickel mass. Let be the true distance to an extremely low-neon event, and use the solar calibration . Its measured flux is , but the inferred standard-candle distance isThe source is intrinsically brighter than the calibration, so the distance is underestimated by about , conventionally described here as about . Equivalently, , consistent with the supplied rounded factor . Using the literal nitrogen metallicity instead gives about a underestimate. These are conditional composition effects in this simplified model; real Type Ia distance estimation also standardizes light-curve shape and color.
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 68 2 Solution Created 2026-10-03 Updated 2026-10-14
A passive disk is heated predominantly by intercepted stellar radiation, rather than by its own viscous dissipation. A rough luminosity criterion, ignoring geometric factors, isThe intrinsic accretion disk luminosity is of order , with additional accretion energy potentially released at the stellar surface. The local test is more precise: absorbed irradiation must dominate the viscous flux at the radius being considered. For an ordinary steady Keplerian accretion disk, sufficiently far outside its inner edge,where is the irradiation grazing angle of a disk. Reflection, very small incidence angles and shadowing can invalidate a simple total-luminosity comparison. The following calculation assumes an illuminated, absorbing surface.
At a point on the upper surface, the outward unit normal in the meridional plane is proportional to , and a light ray from the point source is directed along . Its flux through the upper face is the incident inverse-square flux times minus their scalar product:For a thin disk with small surface slope this becomesThe tangent slope and ray slope differ by . Positive incidence requires disk flaring, , and an unobstructed ray from the star. A negative value of the formula would mean that direct illumination of this face is absent, not that it receives a negative heating flux. The hierarchy makes the finite angular size of the star negligible here.
Let , so the ideal gas equation of state gives the isothermal sound speed . In the stellar vertical gravitational potential, hydrostatic equilibrium has vertical acceleration , where . Integration of gives a Gaussian atmosphere with disk scale heightConsequently satisfies . Substitute this into the stipulated Stefan–Boltzmann law and the irradiation flux:Here specifies surface height in units of disk scale height and is unrelated to the wind-energy fraction in the preceding solution. This separable differential equation integrates exactly toIf the thin-disc solution is formally matched to , then , givingIt follows that the flaring passive disk asymptotic isThis applies in the thin intermediate region , in addition to the point-source and stellar-gravity assumptions. The corrections are of relative order . In particular, the printed hierarchy must still be accompanied by the initial thin-disc condition : if , radii larger than cannot satisfy that approximation. The matching at is an extrapolation used to set an integration constant; the derivation is not a valid treatment of a thick surface at itself.
Identify the stellar surface temperature with its effective radiating temperature, so that luminosity of a spherical blackbody gives . The given stellar surface scale height has , hence . Substituting into yieldsThus a small stellar surface scale height leaves a wide interval above and below in which the thin disk flaring law can apply. The point-source approximation imposes the stronger lower cutoff obtained from :This cutoff is still much smaller than when . The full interval is therefore , whenever these bounds overlap. An assumed thickening radius must lie above the lower cutoff for all of the original approximations to hold simultaneously. The stellar luminosity-temperature relation is essential to the final comparison; independent arbitrary values of and would not imply it.
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 80 1 Solution Created 2026-10-03 Updated 2026-10-14
Use the flat-surface Boussinesq approximation, with small thermal expansion, constant properties, negligible surface deformation, and constant surface tension. The top is impermeable and shear-free, while the solid walls are no-slip. Temperature-dependent surface tension would introduce a separate Marangoni stress, which is not included in this buoyancy-driven model. The stated time scale requires to mean thermal diffusivity; if the material property given is a dimensional thermal conductivity , use .
Take positive downwards and define the nondimensional streamfunction by , . Velocity is scaled by , streamfunction by , and temperature is measured from the cold-end surface value. Define the Prandtl number and horizontal-length Rayleigh number bywhere is the thermal expansion coefficient. Put , and let . Taking the curl of the Boussinesq equations eliminates pressure and gives the full nonlinear vorticity-temperature systemThe buoyancy sign follows from the downward coordinate: warmer fluid has body acceleration .
Choose the same streamfunction constant, zero, on the connected boundary. The mechanical and thermal boundary conditions areThe upper stress-free boundary condition reduces to , since there already gives . An arbitrary additive constant in changes only the reference hydrostatic pressure.
In steady infinite-Prandtl-number convection, momentum inertia disappears but thermal advection remains:For a shallow lake, with fixed as , the leading interior temperature is . This is an outer solution: it does not satisfy the insulated sidewall derivative right at . The leading global conductive solution, which resolves those end regions, isIt is harmonic, has , and satisfies the insulated sides and bottom. Away from sidewall layers of horizontal width it reduces to with exponentially small end corrections. These layers also turn the flow and enforce the sidewall no-slip boundary condition.
In the shallow interior the dominant momentum derivatives are vertical, so . Integrating with the surface and bottom conditions gives the shallow horizontal convection with an insulated bottom solution, with :Surface flow is toward the colder end, with a deeper return flow. The depth-integrated volume flux is zero because . The bulk expressions apply away from the turning regions, not unchanged on the vertical walls. A useful small-advection condition in the end layers is , automatic for fixed Rayleigh number in the stated thin limit.
The heat flux in these units is . For the leading bulk temperature, the horizontal transport through a vertical section per unit out-of-plane width isThus leading advective horizontal transport vanishes: both layers have the same temperature at a given , and their opposing volume fluxes cancel. The leading conductive transport is from the hot end toward the cold end. In dimensional form it is per unit width. Heat enters through the warmer portion of the maintained upper surface and leaves through its colder portion, with the conductive end adjustments particularly important near the two insulated sidewalls. It cannot enter through the insulated sides or bottom.
For the advection correction in shallow horizontal convection, set in the bulk. Since and , the steady heat equation gives . The conditions and imply and henceFor example the bottom bulk temperature is . The correction makes the returning deeper fluid slightly colder. Its horizontal advective heat transport isThus the transport including this bulk correction is , both terms directed toward the colder end.
Vertical transport must distinguish local flux from net transport. In the leading interior , whereas the temperature correction gives a local downward conductive flux . The end circulation gives an upward advective transport: with impermeable sidewalls and , integration by parts gives . It compensates that downward conduction. More generally, steady heat conservation and insulated sides give , and the insulated impermeable bottom sets the constant to zero. ThereforeThere is no net vertical heat transport through the lake, despite its local recirculating heat flux and its nonzero horizontal heat transport.
Past exam of the mathematics course of the University of Cambridge 2009 iii Paper 80 4 Solution Created 2026-10-03 Updated 2026-10-14
Let be the particle radius and the supercooling. Use spherical symmetry, constant thermal properties, equal phase densities , and negligible fluid advection. Let be latent heat per unit mass, the liquid specific heat, its thermal conductivity and its thermal diffusivity. The exterior temperature satisfies the radial heat equationwith for , and as .
The Gibbs-Thomson effect gives curvature-induced melting-temperature depression. For a spherical interface writewhere is solid-liquid interfacial energy per area and the factor two is the sphere's curvature . Here in the thermodynamic formula is an absolute temperature. The notation also permits a given measured capillary coefficient without requiring its microscopic derivation.
In the one-phase Stefan problem, the solid has no internal heat flux and the Stefan condition isThe sign follows from heat balance: positive outward liquid heat flux releases latent heat as the solid grows. If the solid's thermal storage is retained, its temperature instead satisfies its own radial heat equation, , and . The two-phase condition is . It reduces to the one-phase condition in the quasistatic limit because a regular harmonic temperature inside a sphere is spatially constant. An initial solid temperature profile is additional data for a fully time-dependent two-phase problem.
Two reciprocal Stefan number conventions are common. The large parameter appropriate to the requested slow-interface limit is the latent-to-sensible heat ratioIt measures the energy required for phase change relative to cooling or heating by the supercooling. The often-used sensible-to-latent definition is . Thus “large Stefan number” here means large , not large in that other convention.
The thermal diffusion time for scale is , whereas the interface time is . More explicitly, with , and slow time , the liquid equation isFor , temperature therefore equilibrates before the radius changes appreciably. The quasistatic spherical Stefan problem with capillarity has a harmonic exterior temperature, fixed by its interface and far-field values:The small initial diffusion adjustment is omitted at this order. Inserting into the Stefan condition givesThis is the critical radius for a supercooled spherical seed. For , the interface is warmer than the liquid and loses heat, driving growth. For , its curvature-depressed interface temperature is colder than the liquid, so heat enters and the solid melts. At , the uniform temperature supplies an equilibrium radius. It is unstable, since the radius-velocity derivative there is . For a growing particle with , increases asymptotically as .
For a subcritical particle the radius decreases monotonically and remains below . HenceIt cannot remain positive beyond , proving finite-time extinction of a subcritical spherical seed. The exact extinction time in the reduced model is obtained by separating variables:With , this isNear disappearance, the capillary term dominates and , so . For , the lifetime is ; it diverges logarithmically as , consistently with the unstable equilibrium. The threshold and lifetime above are conclusions of the specified large- quasistatic continuum model, rather than an assertion that its approximation is uniform through every finite- shrinking-interface transient.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 60 4 iii Solution Created 2026-10-03 Updated 2026-10-14
Metal absorption lines depend on the temperatures, ionization states and luminosity weights of the contributing stellar populations, as well as their stellar metallicity. A young stellar population dominated by hot luminous stars can have weak metal absorption lines even at substantial abundance, so weak lines alone do not establish low metallicity, an aspect of the age-metallicity degeneracy.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 67 2 Solution Created 2026-10-03 Updated 2026-10-14
Introduce a constant filament bending modulus , which sets the mechanical force scale. The filament has intrinsic curvature of an elastic filament , and its actual signed curvature in a small-slope Monge representation is . To quadratic order one may identify material arc length with in , whileAt fixed positive extension force, the mechanical potential is bending energy minus . Replacing by leaves, up to a force-dependent constant,Its first variation isThe higher-order Euler-Lagrange equation is thereforeFor a Fourier transform relation, take a periodic bulk segment, or a long-filament bulk approximation with negligible endpoint contributions; these are necessary boundary conditions because the question specifies no filament end conditions. Using , every nonzero wavenumber obeysA zero displacement mode is an arbitrary translation. In a periodic representation a constant intrinsic-curvature mode contributes a constant bending cost but no bulk slope, so it does not contribute to the following deficit. The Parseval identity givesFor clarity about finite normalization, on a periodic interval of length define , . Then the equivalent exact quadratic-order formula isThis is force-extension of an intrinsically curved filament, determined by its particular fixed shape rather than by a thermal orientation entropy.
For an ensemble with quenched intrinsic curvature, first minimize each realization and then average the last expression, replacing by its ensemble mean. For stationary bulk disorder, let be the power spectrum, normalized so that its correlation is . The measurable mean deficit per unit projected length isIf the curvature is smooth enough that the second spectral moment is finite, one can take the large-force limit under this integral, obtaining the smooth-curvature high-force extension lawFor a stationary ensemble the integral is . Equivalently, the bulk slope is ; a plot of the mean deficit against measures the mean squared intrinsic-curvature gradient, if is known. The law is a smooth-curvature bulk result, not a universal law for every random filament. For example, ideal white intrinsic-curvature disorder with has an infinite second spectral moment; retaining the full integral instead gives in that ideal continuum model.
Endpoint conditions also matter. If each end is moment-free and has no transverse applied force, the natural conditions from the variation areat each end. These can produce a free-end curvature boundary layer of width . For a constant intrinsic filament curvature , integration of the higher-order Euler-Lagrange equation with zero transverse force gives and henceThe last formula follows by integrating , and tends to , despite the vanishing bulk curvature gradient. Thus a finite free-ended measurement must include or suppress endpoint bending before interpreting a bulk fit.
For the freely jointed chain, rigid links have independent orientations, so the restoring force is entropic. Let now denote absolute temperature, and with Boltzmann constant . In the usual three-dimensional chain, a segment at polar angle has force energy . Its angular canonical partition function and the full chain partition function areDifferentiating with respect to yields the exact mean projected displacementHere is the Langevin function; this is force-extension of a three-dimensional freely jointed chain, in the fixed-force canonical ensemble. At high extension, , soThus the smooth quenched-curvature bulk deficit falls as , whereas the three-dimensional freely jointed chain deficit falls as and depends explicitly on temperature. The distinction is mechanical straightening of a fixed intrinsic shape versus orientational entropy; thermal bending fluctuations of a stiff filament have not been included in the first calculation.
If the comparison chain is also restricted to two dimensions, it is a planar freely jointed chain rather than the three-dimensional model. In this case,The last identity follows directly by differentiating the integral defining ; and are Modified Bessel functions of the first kind. At large the angular weight is proportional to , giving . Consequently : the same inverse-force exponent, with half the three-dimensional coefficient. Both versions assume inextensible links and forces below the regime where the links themselves stretch.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 72 1 Solution Created 2026-10-03 Updated 2026-10-14
Write and . When the ice sphere grows by volume , it consumes liquid volume . The difference is expelled from the fixed cavity. Thus mass conservation fixes the outward Darcy flux in the surrounding porous medium:The Darcy law and implyMatching at the cavity wall, whose internal pressure is uniform, givesThe solid and liquid pressures are equal when the Gibbs--Thomson relation is neglected; nevertheless the coexistence temperature changes with their common pressure because their specific volumes differ. Along coexistence, equality of chemical potentials givesHence the common-pressure melting-point slope is . To first order in the pressure change,The multiplying this coefficient is absolute temperature, approximately for water; a temperature difference may equally be measured in kelvin or degrees Celsius. Substituting the numerical value from the Celsius scale into a thermodynamic denominator would be incorrect.
In the quasi-stationary thermal conduction approximation, neglect advective heat transport and use the stated effective conductivity outside the sphere. The radial Laplace equation gives the bounded solid temperature and the liquid/porous-region temperature:This treats the exterior as a uniform conducting medium, as required by the printed reduction; distinct cavity and porous-medium conductivities would give an additional thermal resistance. There is no solid-side heat flux in the bounded quasi-stationary solution. The Stefan condition therefore becomesEliminate and to obtainFor , and , this isThe pressure follows either from the Darcy flux or the Stefan condition:In particular : rising pressure progressively reduces the available undercooling. This is spherical freezing inside a porous cavity, whose fixed hydraulic outlet radius distinguishes it from freezing directly through a porous matrix.
For the idealized zero-radius start, integration givesA finite seed replaces the right side by its difference from the initial value. The reduction ends when the sphere fills the cavity.
For , hydraulic drainage is easy and the pressure feedback is small throughout the cavity. The leading expressions areThis is ordinary conduction-controlled spherical solidification, with a completion time asymptotic to .
For , distinguish the initial crossover from the pressure-dominated regime. At , equivalently , the same square-root growth applies and . At , equivalently ,The interface approaches , the pressure approaches the finite coexistence value , and growth becomes hydraulically limited. The leading completion time is . The cube-root approximation is not valid at the instant of nucleation, where the initial square-root regime must be retained.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 72 2 Solution Created 2026-10-03 Updated 2026-10-14
Use the one-sided thermal conduction model encoded by the requested dispersion relation: neglect solid-side perturbation heat flux, take equal phase densities, and let the normal point from solid into liquid. Write the isotropic linear kinetic undercooling law using the solidification attachment mobility :Here is solid-liquid surface energy, is the sum of principal curvatures, and is absolute temperature. Positive curvature convex into liquid lowers the equilibrium freezing temperature through the Gibbs--Thomson relation. The planar base state has .
Set and defineThe paper's is the latent-to-sensible heat ratio, the reciprocal of the common Stefan number convention. Below, velocities, lengths and growth rates are dimensionless in these scales. In the travelling coordinate , the liquid heat equation gives , while the bounded solid steady field is constant. Matching a decaying liquid profile to the Stefan condition givesThe kinetic undercooling condition is . ThusThe speed is constant for , determined by and the attachment coefficient in the specified scales. Thermal diffusivity sets the exponential decay length , not the selected speed. Including solid-side perturbation conduction would change the stability equation below.
For linear stability analysis, corrugate the interface to and write the liquid perturbation as . The liquid heat equation requiresFor this graph the linearized curvature is . Evaluate the temperature on the displaced interface: its perturbation is . The kinetic undercooling law therefore givesLikewise the derivative evaluated at the displaced surface is , with . The Stefan condition at perturbation order readsElimination proves the one-sided kinetic solidification dispersion:The destabilizing term comes from a protrusion encountering colder liquid; capillarity and kinetic relaxation oppose it.
At , and the base liquid has no thermal contrast generated by latent heat. The interface obeys : positive surface energy damps all nonzero modes, while is neutral at this order. Here the thermal perturbation amplitude vanishes, so the auxiliary decay exponent is immaterial to that pure kinetic relaxation. At , and the formal limit givesFor it has a negative real branch and no growing branch; at the interface branch is neutral. Strictly, is a singular endpoint of the travelling profile: no finite-width stationary exponential connects to the far-field value zero. These stability statements describe the limit of the travelling-front model.
For , assume at small wavenumber. ExpandSubstituting into the dispersion relation cancels on both sides and givesAt the capillary stability threshold for a kinetic freezing front , continuing the same expansion gives : the nonzero long waves are damped even at threshold.
For large wavenumber, multiply the dispersion relation by and eliminate using the thermal equation. The exact algebraic form isIt prevents the uncontrolled replacement when itself is of order . In the usual small-capillarity range the leading results areFor the second result, set in the cubic; its quadratic-order balance gives . Thus positive capillarity stabilizes sufficiently short waves. If also and , the useful reduced approximation isits finite terms should not be treated as a uniform expansion for arbitrary fixed .
For completeness, large dimensionless capillarity has different balances. At , and . For , , so . At , the real branch reaches : for its growth rate is , and for that endpoint is exact. For at this boundary, or for , the selected real- normal mode ceases to exist at sufficiently large wavenumber; the full diffusion problem includes a thermal continuous spectrum and cannot be assigned a real isolated interface growth rate by this ansatz there. Indeed, writing the bulk thermal perturbation as reduces its heat equation to , whose half-line diffusion modes have decay rates for . The thermal branch endpoint is . Loss of a damped isolated interface mode is not a morphological instability.
The approximate instability condition is already clear from the long-wave coefficient: , equivalently . In fact it is exact for growing modes of the present one-sided model. At , let , so . The right side of the dispersion relation becomesFor real , the residual is strictly increasing, sinceTherefore a unique positive root exists precisely when . For , the unstable band isThere are no unstable oscillatory roots hidden by this real-root test. Indeed, if and , the thermal equation implies . For , the imaginary parts of the two equations would require , contradicting . Thus growing modes have real and real .
The sketch shows zero capillarity approaching the positive plateau , weak capillarity giving a positive band followed by short-wave damping, and threshold/stronger capillarity giving damping at every nonzero wavenumber. The zero-wavenumber mode is a translation. As with fixed positive , both the unstable bandwidth and the positive growth rates shrink to zero; the small-wavenumber expansion is not uniform in that limit.
Past exam of the mathematics course of the University of Cambridge 2010 iii Paper 72 4 Solution Created 2026-10-03 Updated 2026-10-14
Take and , with the liquidus referenced to the pure-water melting point. The solid-liquid segregation coefficient means that newly formed ice contains no salt. A steady sharp front producing only pure ice cannot remove the incoming solute flux. More explicitly, in the liquid the steady solute flux is , whereas in pure solid it is zero. Interfacial salt conservation would require , a contradiction. An equilibrium mushy layer avoids this by carrying concentrated pore liquid down to the eutectic region, where a salt-bearing solid assemblage can form.
Use equal densities and common downward translation velocity . Write for the liquid fraction; here is the solid fraction. Local liquidus equilibrium in the mush requiresAbove a stationary roof , the liquid advection-diffusion equation is , with solutionThe marginal equilibrium at a mush-liquid boundary condition is , hence . Matching the temperature and liquidus at the roof givesA positive equilibrium mush requires ; otherwise this positive-thickness construction does not apply.
Including solute diffusion in the liquid pore space, the steady solute flux in the mush isThus . Inserting and the value of yieldsThis is the diffusive steadily pulled equilibrium mush. Omitting the diffusive contribution would give a different solid-fraction distribution.
The imposed temperature and local liquidus coincide throughout the mush. In the liquid put . Their difference iswith equality and matching first derivatives at the roof. The inequality follows because the derivative of is . Thus the liquid is not constitutionally supercooled. In the phase diagram, the pore-liquid trajectory follows the liquidus from the eutectic composition to , then curves into the liquid region and approaches as height increases. Pure-ice crystals have composition zero; the trajectory denotes the liquid composition, not the bulk mush composition.
After pulling stops, the imposed temperature keeps the pore-liquid composition fixed wherever the material remains mush. Solute conservation becomesBecause , this reduces toThe method of characteristics uses and . HenceThese are the solute-diffusion characteristics in a fixed-temperature mush; their validity is local to the coexisting solid–liquid region.
For an explicit initial-data solution, define , and , so . A characteristic through has initial footWhile that foot lies in the original mush and no phase boundary has removed the point,This recovers the initial distribution and shows that interior ice fraction increases as salt diffuses upward from colder, more concentrated pore liquid.
If one simply transports the initial zero-solid-fraction level, implies the printed formal lawOn the physical concentration branch , this is , so . It starts moving above immediately.
This formal continuation cannot be the physical mush–liquid roof of a column sealed to salt by the membrane. The no-flux constraint in a fixed-temperature mush is at the membrane. At a smooth zero-fraction equilibrium roof, however, and , giving . Moreover the formal roof has left the membrane-bounded domain. The printed interface law is incompatible with a salt-impermeable membrane when interpreted as the physical roof. Its derivation above is a characteristic extrapolation; it does not enforce the stated boundary condition. If “impermeable” were intended to block bulk flow but allow salt diffusion, a different boundary condition would need to be specified.
The closed-column physical sketch is consequently different. Salt transported upward accumulates below the membrane and produces a liquid brine cap; the cap composition need not lie on the liquidus at every height. Its lower boundary can have a finite jump in solid fraction, so it need not follow the initial zero-fraction characteristic. Near the cold solid base, zero salt supply from below requires the liquid fraction to vanish, and a pure-ice region develops. In the surviving mush, the characteristic formula increases relative to its initial value. An intermediate profile therefore has pure ice at the bottom, a remaining mush with elevated solid fraction, and liquid at the top. The plotted intermediate roof is schematic, not claimed to obey the inconsistent formal law.
Initial, intermediate and final solid fractions in a salt-sealed column
. Details. One can characterize the final state quantitatively if the solid base also admits no salt diffusion, as in the usual pure-solid/no-solid-diffusion closure. In a stationary column, solute flux is constant and is zero at the sealed roof. A finite-width equilibrium mush would have , forcing everywhere in that region; it therefore cannot remain mush. The final state is pure ice for and a uniform-composition liquid cap for . At their boundary,The cap is liquid because above its base. The fixed external thermal field can supply or remove the heat involved; this is a solute-budget determination rather than an isolated enthalpy budget.
The final salt budget of a sealed mush column determines . Initiallysince . Conservation requires . Writing the final cap depth , the equation and its unique positive root areThe initial salt integral is less than , so and ; the resulting remains on the ice–brine branch above the eutectic. If the basal eutectic region is instead allowed to exchange solute with the column, this salt budget must include that flux and the numerical final height is not fixed by the printed data alone. No universal physical follows from the interior characteristic equation without the cap and basal boundary conditions.
Past exam of the mathematics course of the University of Cambridge 2010 ii Paper 3 15D Solution Created 2026-09-24 Updated 2026-10-14
For a nonrelativistic particle, . The Gaussian integral yieldsIndeed , which combines with to give the prefactor. For the two species this givesChemical equilibrium imposes . If the two massless bath species have zero chemical potentials, then ; their masses alone do not imply this chemical-potential condition.
Weak reactions such as , with leptons treated as relativistic, interconvert neutrons and protons. Negligible lepton chemical potentials give approximately , since their degeneracies and masses are nearly equal. Equilibrium favors protons increasingly as temperature falls. But the weak reaction rate decreases faster than the expansion rate and eventually falls below it: cosmological weak freeze-out prevents the ratio from following its equilibrium exponential to zero. Free neutrons subsequently decay, reducing the frozen ratio further.
In Big Bang nucleosynthesis, cooling eventually makes deuterium survive photodissociation. Nuclear reactions then build helium through deuterium and the light intermediate nuclei, locking almost all surviving neutrons into stable helium-four. Neglecting binding-energy corrections and taking , each helium nucleus uses two neutrons and two protons, so andFor example gives a helium mass fraction , with the remaining baryons predominantly hydrogen.
Past exam of the mathematics course of the University of Cambridge 2012 iii Paper 61 1 i Solution Created 2026-10-03 Updated 2026-10-07
The first relation is vertical hydrostatic equilibrium. In a thin disc, the central object's gravity near the midplane is ; the pressure gradient balances it. The second is an equation of state combining ideal gas pressure with isotropic radiation pressure. Write , so and ; is the Stefan-Boltzmann constant and the mean molecular weight in proton-mass units.
The third is local energy balance: the increase of upward radiative flux with height equals viscous dissipation. Here is dynamic viscosity, not mean molecular weight. A Keplerian disc has shear , so its heating rate is . The fourth is optically thick radiative diffusion, with opacity per unit mass and diffusion directed down the temperature gradient. Midplane symmetry gives and oppositely directed fluxes from the two faces. The four relations express vertical force balance, gas–radiation thermodynamics, local heating, and diffusive cooling.
Past exam of the mathematics course of the University of Cambridge 2012 iii Paper 63 1 c Solution Created 2026-10-03 Updated 2026-10-14
Keep the fixed stellar homology profile, so that and . Solving the partially degenerate equation of state for the central temperature giveswhere and are positive constants. The ion mean molecular weight is distinct from the total-particle mean molecular weight used in part (a).
Set . The expression in parentheses is a concave quadratic in . Its maximum occurs atSubstitution gives the contraction-limited central temperatureAt this point electron degeneracy pressure supplies half the required central pressure. Further contraction increasingly goes into the density-dependent degeneracy term rather than heating the ions. The formula applies along the positive-temperature part of the idealized homologous sequence; a negative value beyond it is not a physical temperature.
For sufficiently small mass, this maximum never reaches the temperature needed for sustained hydrogen burning. Such an object stays below the hydrogen-burning minimum mass and becomes a cooling brown dwarf, rather than an ordinary main sequence star. Some such objects burn their initial deuterium, but that finite reservoir does not provide lasting hydrogen burning.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 48 2 c Solution Created 2026-10-03 Updated 2026-10-20
Photon decoupling is a dynamical loss of frequent scattering, distinct from the chemical conversion of charged particles into neutral atoms. Before recombination, Thomson scattering on free electrons keeps photons coupled to the baryon plasma. The physical scattering rate isin units with . Define the approximate decoupling temperature byEquivalently the photon mean scattering time becomes comparable to an expansion time. A refined last-scattering definition uses the optical depth and the maximum of the visibility function; it need not coincide exactly with the local rate criterion. As falls, scattering becomes inefficient, ordinarily after the half-ionized recombination stage, so .
Residual electron freeze-out concerns the remaining ionized fraction. The Saha equation presumes sufficiently rapid forward and reverse reactions to maintain chemical equilibrium. Real recombination is slowed by radiative bottlenecks and expansion; the free-electron fraction can therefore exceed its equilibrium value. Eventually the effective recombination rate per free electron, roughly , falls below . The remaining electrons cannot all find and recombine with protons within an expansion time. A small nonzero residual fraction survives while the Saha prediction decreases exponentially toward zero.
The sketch shows this lag and residual floor. Its kinetic curve and the position of the decoupling marker are schematic: the data supplied determine the equilibrium curve, but not a quantitative recombination history or an exact . Determining those needs the expansion history and atomic transition rates. The horizontal axis decreases toward the right to follow cosmological cooling.
Saha equilibrium and a schematic delayed recombination curve, with recombination and photon-decoupling temperatures marked during cooling
. Details. Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 53 2 a Solution Created 2026-10-03 Updated 2026-10-07
Use the notation throughout, with optical depth increasing inward and for an outward ray. This removes the change in argument order used in the printed surface-intensity notation. Multiplying the radiative transfer equation by its integrating factor givesIntegrating from the surface to a deeper boundary yieldsFor a semi-infinite atmosphere with no exponentially growing homogeneous term, the boundary term vanishes as . The formal solution of the radiative transfer equation is thereforeThe usual deep-atmosphere boundary condition is necessary; a first-order differential equation alone does not fix the emerging specific intensity.
For a linear source function, the zeroth and first exponential moments give . Equivalently , the Eddington-Barbier relation. If the source rises inward, rays near the limb sample cooler, shallower layers, producing limb darkening.
For the finite polynomial, put and integrate each term. Repeated integration by parts gives , so the polynomial source function moments for emergent intensity giveThe limiting grazing-ray specific intensity is . If the displayed polynomial is only a local Taylor approximation to a more general source, this formula applies to that approximation and a source-function remainder also contributes; a finite local expansion is not automatically an exact description at every optical depth.
For a constant source in an overlying layer of optical thickness , the radial ray has the exact transfer relationExpanding the exponentials gives the constant source transfer through a thin layer:This finite-layer result does not require the specific intensity below the layer to equal its source function. The sign of already distinguishes emission from absorption.
An absorption line forms when a bound-bound transition increases opacity at selected frequencies. In a photosphere whose temperature decreases outward, optical depth of order one at the line frequency occurs higher than at a nearby continuum frequency. In an absorption-dominated region in local thermodynamic equilibrium, the source is the Planck function; the cooler line-forming layer then emits less specific intensity than the deeper continuum-forming layer. The result is a dark spectral feature. Scattering and departures from LTE modify the source, so this temperature-gradient picture is a useful mechanism rather than a universal identity for every line.
Two distinct situations can produce emission lines. First, a heated chromosphere has an outward temperature rise, so an optically thick line can sample gas hotter than the continuum photosphere beneath it. Secondly, a hot optically thin circumstellar envelope or stellar wind emits line photons through collisional excitation or recombination, with no comparably bright background along all rays; its added line flux can exceed the underlying continuum. Winds of hot luminous stars can also give a mixture of emission and absorption across a Doppler-broadened line profile. These examples explain the change in specific intensity through either an enhanced source function or additional emitting material.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 53 2 b Solution Created 2026-10-03 Updated 2026-10-07
The high luminosity-to-mass ratio makes radiative acceleration and atmospheric departures from the simple approximations important. For an illustrative fully ionized hydrogen-rich composition with electron-scattering opacity , the stellar electron-scattering Eddington factor isThus electron scattering alone removes roughly half of the effective surface gravity. It is below the Eddington luminosity, so electron scattering alone does not prove that a hydrostatic atmosphere is impossible. Line opacity can provide substantially more radiative acceleration and can drive a stellar wind.
For a plane-parallel atmosphere, the geometrical condition is that the line-forming region be thin compared with the radius. In a simple isothermal photospheric estimate, the atmospheric scale height isThis is plane-parallel validity from pressure scale height. The mass and luminosity alone do not specify or the atmospheric temperature, so they cannot decide the geometry uniquely. For example, if and , the luminosity relation gives and . Plane-parallel geometry could then be adequate for deep weak photospheric lines. It would still fail for lines formed over an extended wind, and a cooler, more extended supergiant needs a separate geometrical assessment. This numerical example is conditional, not an additional datum about the stated star.
LTE requires collisions and local thermal processes to establish the relevant excitation and ionization populations at the local gas temperature. In the dilute outer layers of a luminous hot star, radiative transition rates can dominate collisions, and the radiation field arriving from other depths is not the local Planck function. A non-LTE stellar atmosphere should therefore use statistical equilibrium with radiative and collisional rates coupled to transfer. Deep layers may approach LTE, but surface ionization balances and abundance-sensitive spectral lines are particularly susceptible to departures. An LTE abundance can be systematically wrong even when a plane-parallel approximation is geometrically good.
A static atmosphere requires velocities to be negligible where the diagnostic lines form. Massive luminous stars commonly have line-driven outflows, so static models cannot represent wind-formed profiles or their mass density and velocity gradients. A hydrostatic approximation can still be useful below the sonic region if the chosen lines form there, provided radiative acceleration is included in the effective gravity. Large outflows call for spherical moving-atmosphere models rather than merely a changed abundance in a static model.
The three assumptions cannot be accepted on the quoted mass and luminosity alone. LTE is especially doubtful in the outer layers; wind-sensitive abundance diagnostics require non-LTE moving models, and geometry must be checked through atmospheric extension and line-formation depth. Reliable stellar chemical abundances should be supported by observed wind signatures, temperature and gravity constraints, and agreement between several suitable ionization stages or weak photospheric lines.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 53 3 Solution Created 2026-10-03 Updated 2026-10-14
The supplied rate law gives a local logarithmic temperature sensitivity, evaluated at fixed number densities. Since ,Thus a power law here describes the tangent logarithmic slope near the chosen temperature, not an exact power law over all temperatures. For the three reactions, the factors are , and , respectively. At the local temperature exponent of a thermonuclear reaction givesHence , , and . The larger reduced mass for reaction 34 produces the last inequality. Composition changes contribute separately to an evolving reaction rate; they are held fixed for this derivative.
For the effective proton-proton reaction network, let the event rates beThe factors of one half count identical pairs once. Event 11 consumes two protons and makes one deuteron; event 21 consumes a deuteron and a proton and makes helium-3; event 33 consumes two helium-3 nuclei and makes one helium-4 nucleus and two protons. Under the stipulated fast-capture approximation, event 34 consumes helium-3 and helium-4 and supplies one mass-seven nucleus, and event 17 consumes that lithium-7 nucleus and a proton and makes two helium-4 nuclei. ThereforeFor closure, . The stoichiometry conserves , the baryon number density at fixed volume. In particular the mass-seven capture produces two helium-4 nuclei, not one.
The beryllium-to-lithium step is electron capture. Eliminating beryllium assumes that its capture flux tracks its production on the slow evolutionary timescale. More generally one retains and ; setting the former to zero gives the effective equation used above. Fast capture relative to slow evolution alone would not prove that lithium exceeds beryllium: if both reach steady state their ratio is . The mass-seven abundance assertion is thus part of the stipulated schematic limit, not a consequence to impose on every detailed solar model.
The enormous separation between the one-second deuterium destruction time and the other stated timescales justifies deuterium quasi-equilibrium in proton-proton burning:Substitution givesThe approximation is to the rapidly adjusting intermediate abundance, not to the slow proton abundance.
Near the centre the helium-3 relaxation time is also short compared with solar age and with the timescale of significant hydrogen evolution. Put , and . For slowly varying background quantities, the stable positive root of gives the helium-3 equilibrium abundanceThe other root is negative and unphysical. The production-minus-destruction function decreases strictly with positive , so this is the unique attracting equilibrium. For , with the background held fixed during relaxation,Dropping the quadratic perturbation term gives the helium-3 relaxation timeIf the equilibrium itself evolves slowly, an additional forcing term appears; tracking is accurate when this drift is small over one relaxation time. The given central value years is much shorter than the roughly -year age of the Sun.
To estimate the temperature for helium-3 freeze-out, take the cooler pp-I-dominated regime and keep the background proton mass density approximately fixed for this order-of-magnitude scaling. ThenUsing the local exponents four and sixteen, this gives and , not : the equilibrium abundance changes with temperature. Normalizing at the central temperature givesSetting this equal to solar age yieldsThis is the requested power-law estimate. The exponents were evaluated locally at the central temperature, so extrapolation over this large range is approximate. Keeping the supplied full exponential rate factors in the same fixed-density pp-I estimate giveswhich gives about . Thus the robust scale is a few million kelvin, roughly six to seven million in these estimates. A unique precise solar transition temperature cannot be obtained from the given numbers without the mass density, composition and pp-II contribution as functions of radius.
Finally, use mass fractions . The hydrogen mass fraction is depleted most strongly in the central burning region, so increases outward and approaches the nearly unprocessed envelope value. Convective mixing makes the outer envelope composition approximately uniform.
In the hot core helium-3 is quickly destroyed and remains close to its small equilibrium abundance. Moving outward, its destruction rates fall much faster than its production rate, so the equilibrium ratio rises. Where the relaxation time becomes comparable with solar age the abundance ceases to follow that rising equilibrium. Farther out, production itself becomes too slow to accumulate much helium-3, so falls again toward the envelope value. The result is a broad off-centre maximum, rather than a central maximum. These are the solar hydrogen and helium-3 abundance profiles requested by the sketch.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 66 1 c Solution Created 2026-10-03 Updated 2026-10-07
Choose real eigenfunctions with . For positive modes, self-adjointness and integration by parts diagonalize the energy:At temperature , the canonical ensemble is a product of centered Gaussian distributions. The equipartition theorem, with Boltzmann constant , givesThe resulting thermal covariance of an elastic filament isFor an unnormalized eigenfunction of squared L2 norm , divide its summand by . This normalization factor cannot be absorbed silently into the modal variance.
For clamped boundary conditions at both ends, the inverse of has Green function, for ,It is cubic on each side of , satisfies the four clamped conditions, has continuous first two derivatives, and has unit jump in its third derivative. Thus , and its eigenfunction expansion is the sum above. In particular,These finite variances require removal of every zero-energy filament mode. An unconstrained free-free elastic filament can translate and tilt at no energy cost; a torqued-torqued elastic filament can translate. Their unrestricted Boltzmann distributions are not normalizable, so the full displacement variance is undefined. Fix those rigid degrees of freedom before applying the positive-mode formula.
Past exam of the mathematics course of the University of Cambridge 2013 iii Paper 69 5 Solution Created 2026-10-03 Updated 2026-10-07
Use the well-mixed natural ventilation model for a distributed floor source. Let the building height be , its volume be , its temperature excess be , and the exterior mass density be . Let be the coefficient of thermal expansion, so reduced gravity is . Convert the total heat input to the temperature-volume flux , where is specific heat capacity. If the quoted heat flux is per floor area, first multiply it by that area.
For effective opening area for pressure-driven ventilation, define the equal-opening hydraulic coefficient such that the signed throughflow obeys , with the total driving pressure divided by mass density. In the effective-area convention of question 6, each opening has discharge , so . The usual physical-area orifice law instead gives ; that prefactor does not affect the stability conclusions.
Set and . Positive denotes entry at the floor and exit at the roof. hydrostatic pressure and wind combine to giveBecause the inflowing air is at exterior temperature in either direction, the heat budget isThe well-mixed ventilation temperature balance at steady state is thereforeAll roots must satisfy and their appropriate flow-direction inequality; squaring a pressure relation without imposing those conditions could add spurious branches.
The assisting case has a unique positive solution and it is stable. For opposing wind, define . There is always one solution with , a buoyancy-dominated upward flow. Below , the heat-removal curve is . It is zero at both endpoints, and its maximum occurs at :For there are two downward-flow roots as well as the upward-flow root. Equivalently, setting and , the equilibrium curve isFor linear stability analysis of the opposing-wind ventilation bistability, linearize the heat budget: the eigenvalue is . The cooler downward root has and , so it is stable. The warmer downward root has and , so it is unstable and separates the two basins. The upward root has and is stable. At the two downward roots merge at a saddle-node bifurcation; above that value only the upward equilibrium remains.
For ventilation switching under wind and heating changes, increasing wind pressure or decreasing heat input both reduce , so both can create the pair of wind-driven equilibria. They nevertheless have different physical and transient effects. On the hot upward branch, implicit differentiation of shows that increasing increases , while decreasing decreases . Both reduce the upward ventilation rate, but only a wind change shifts .
Under slow parameter variation, a state follows its current stable branch while that branch persists; the upward branch does not disappear when wind increases or heating decreases. A sufficiently large abrupt wind increase can raise beyond the current temperature and place that state below the new unstable threshold, causing flow reversal and cooling towards the wind-dominated equilibrium. A jump insufficient to cross its basin boundary returns to the upward equilibrium.
At fixed , reducing a still-positive heat input cannot force an initially upward-flow state through : at that boundary the temperature balance has . Thus heat reduction alone does not cause that reversal in this model. Conversely, decreasing wind or increasing heat from the stable downward branch eventually destroys it at the fold and forces a switch to the upward branch, giving history dependence. Wind strengthening and heat reduction have the same effect on the steady dimensionless control parameter, but not the same temperature change or switching dynamics. These stability statements use quasi-steady opening flow and a single well-mixed temperature; other stratification or airflow-inertia models require their own stability analysis.




