Ideal-ion white-dwarf cooling timescale Created 2026-10-25 Updated 2026-11-05
With carbon-ion thermal energy and luminosity , the time between two core temperatures is . Late cooling is slow in this approximation. Extrapolating the formula does not prove a categorical observational absence of ultracool remnants, since atmosphere, crystallization and heat-capacity physics alter the simple model.
Isothermal atmosphere Created 2026-09-28 Updated 2026-11-05
An isothermal atmosphere has the same temperature at every height in the region modeled. With an ideal gas, uniform downward gravity and constant mean particle mass , hydrostatic equilibrium gives and , where the scale height is .
The local gradient is therefore set by a balance: larger thermal energy spreads particles over a greater height, whereas larger particle mass or gravity concentrates them lower down. Measuring the ratio of pressures at two heights yields within this model. A real atmosphere can depart from the exponential law because temperature, composition or gravity changes with height. Being isothermal specifies a thermal profile; it does not independently establish that the fluid is at rest or in hydrostatic equilibrium.
Past exam of the condensed matter physics course of the University of Oxford 2015 1 b Solution 2026-10-25
Pauli exclusion principle prevents most filled electronic states from changing occupation at . Only a shell of width of order around the Fermi energy participates. Since the density of states near that energy is of order per volume and energy, the fraction of active electrons is of order . Their typical change of energy is of order , so the thermal energy increment per volume scales asDifferentiating with respect to temperature gives the electronic heat capacityThe simple shell argument fixes the linear law, not its coefficient. A Sommerfeld expansion using the spin-summed free-electron density of states gives , hence , consistent with the supplied value. The result excludes strong band-structure or interaction corrections and requires a degenerate electron population.
Past exam of the condensed matter physics course of the University of Oxford 2015 1 c Solution 2026-10-25
The Debye model treats the crystal as an isotropic elastic continuum with independent harmonic vibrational modes. There are three acoustic polarizations, approximated by linear dispersions and a common effective speed. A cutoff is chosen to retain modes for atoms. The model neglects anharmonic interactions and the detailed high-wavevector dispersion. In a multi-atom primitive cell, optical branches require additional treatment; copper has one atom per primitive cell even though its conventional cubic cell contains four atoms.
A frequency interval contains, per volume,Each phonon mode has Bose-Einstein distribution occupation . The fixed zero-point energy contributes no heat capacity. Its thermal energy density isFor , extending the upper limit to infinity gives . ThereforeThe cubic law reflects the three-dimensional acoustic mode density proportional to . It is a low-temperature limit, not a valid extrapolation through the classical high-temperature regime.
A protostar forms when a self-gravitating cloud fragment can contract faster than pressure support and energy loss can arrest it. A useful local scale is the Jeans length, , with characteristic Jeans mass and free-fall timefor an initially uniform sphere. Geometry, turbulence and magnetic support change the detailed threshold; none of these estimates asserts that every cloud contracts as a uniform sphere.
While cooling is efficient, compression is nearly isothermal. Then decreases as the density rises, allowing fragmentation. Rotation becomes increasingly important during contraction because a parcel conserving specific angular momentum encounters a centrifugal scale . The resulting accretion disc must transport angular momentum before matter can reach the central object. Infall, a dense accreting interior and an outer envelope can therefore coexist; a protostar is not initially an isolated fixed-mass star.
Increasing optical depth eventually slows radiative cooling. The central gas then becomes less compressible and can form a pressure-supported first core. Molecular hydrogen dissociation absorbs compressional energy and can trigger a second collapse before a compact stellar core is established. Subsequent accretion supplies a luminosity of orderThe retained fraction depends on shock and disc radiation, so this expression is an energy scale rather than a guaranteed luminosity all emerging from the stellar surface.
A central accreting core can be nearly hydrostatic on its short sound-crossing time while its mass, entropy and radius evolve on longer times. A low-mass object is often largely convective because of its opacity and steep radiative temperature gradient; deuterium burning can temporarily contribute to support and moderate contraction. Neither convection nor the timing of deuterium ignition is universal across all masses and accretion histories.
When the main accretion phase ends, gravitational contraction remains an energy source. The virial theorem explains how contraction both heats the interior and supplies radiation: for an ideal-gas-supported object with negligible surface-pressure correction, , so only part of the released binding energy appears as increased thermal energy. The corresponding Kelvin-Helmholtz time isFully convective pre-main-sequence evolution approximately follows a Hayashi track, with decreasing radius and luminosity at comparatively weakly changing effective temperature. Objects developing radiative interiors can follow Henyey tracks. Eventually sustained core hydrogen burning balances the luminosity and the star reaches the main sequence. Massive objects can ignite hydrogen while substantial accretion continues, so “accretion ends, then hydrogen ignites” is not a universal ordering.
A useful structural distinction is therefore between an accretion-powered protostar and a largely fixed-mass pre-main-sequence contraction model. An infrared-bright envelope or disc traces obscured formation and reprocessing of radiation; a schematic evolutionary track should not replace the actual mass- and entropy-dependent stellar-structure problem.
Galaxy formation combines gravitational assembly of dark-matter haloes with dissipative baryonic physics. Primordial density fluctuations supply a statistical seed distribution. In linear theory, each Fourier mode evolves through a growth factor and a scale-dependent transfer function; the power spectrum describes the variance by scale. Radiation pressure, free streaming and the time of horizon entry influence the small-scale transfer, so one should not replace the spectrum by a single universal growing power of time.
When fluctuations become nonlinear, overdense regions collapse, virialize and build larger structures through accretion and mergers. Cold dark matter permits a broad hierarchy of bound haloes. A spherical-collapse threshold and a mass-variance prescription, such as the Press-Schechter formalism, organize an approximate halo abundance; departures from spherical collapse and correlated environments limit its literal interpretation.
Gas falling into a halo is compressed and may be shock-heated toward a virial scaleUnlike collisionless dark matter, it can radiate away thermal energy. A rough cooling time iswhere the denominator specifies a chosen optically thin astrophysical cooling function convention. Cooling is effective for condensation when this time is short compared with the relevant dynamical or supply time. Atomic transitions, molecular processes, ionization state, density and metal abundance matter. A stable virial shock is not obligatory for all accretion: cold dense inflows can supply gas in regimes where shock-heated gas would cool rapidly.
The distinction between a gravitationally assembled massive halo and a radiatively condensing luminous component is fundamental. In the classic two-stage picture, non-dissipative clustering builds potential wells while cooling allows gas to concentrate much further than the halo component.[ref]
Core condensation in heavy halos by Simon D. M. White and Martin J. Rees. 1978 abstract, gravitational clustering plus dissipative gas condensation
Angular momentum inherited from tidal torques and later accretion helps gas settle into a rotationally supported disc after cooling; disc size depends on angular-momentum retention and transport. Locally self-gravitating gas fragments and forms stars. Stellar radiation, winds and supernovae then heat gas, drive turbulence, enrich it with heavy elements and can expel it from shallow potential wells. Metal enrichment can also accelerate later cooling, so feedback is more than a single positive or negative energy term.
Galaxy growth is usefully expressed as a gas-budget competition:Here is the promptly returned stellar mass fraction; unlike the simplification in Question1, a general evolutionary model need not set it to zero. The equation separates newly supplied, converted, expelled and recycled gas rather than assuming that halo mass uniquely fixes stellar mass.
Accreting central black holes can provide radiative and mechanical feedback. Heating a halo, ejecting gas or maintaining a hot atmosphere can reduce fresh fuel; removal of a satellite's gas supply and ram pressure in a surrounding medium provide additional environmental routes. Quiescent galaxy assembly can still add stellar mass through dry mergers, so cessation of star formation is not identical to cessation of all mass assembly.
Mergers and disc instabilities can rearrange morphology and trigger bursts, while smooth accretion can rebuild discs. Cosmological expansion changes the supply and merger environment; accelerated late-time expansion also slows linear growth. A predictive model must connect these mechanisms to the stellar mass function, gas fractions, star-formation histories, sizes, chemical abundances and clustering. Those observables test different pieces of the assembly-and-feedback picture; none alone implies a one-to-one instantaneous relation between galaxy luminosity and total halo mass.
The heat capacity per unit horizontal area is : mass density times specific heat capacity times atmospheric depth. Thus is the rate of stored thermal energy per unit area. The solar constant is the incident radiative flux on a surface normal to sunlight; the ratio of the Earth's intercepting disk area to its spherical area is . The absorbed fraction is , where albedo is the reflected fraction. The outgoing radiative flux is , a Stefan–Boltzmann law with effective radiation factor incorporating the simplified greenhouse effect. Every term therefore has units of power per area.
The albedo curve decreases smoothly, passes through , and approaches at high temperature. At it is , close to when is large. Its derivative isAn ice-covered planet reflects more sunlight than exposed land or ocean. Warming removes reflective ice, lowers albedo, and increases absorbed radiative flux: this is ice-albedo feedback. The parameter controls the sharpness of this transition; the formula is an idealized global response, rather than a local melting law.
Temperature-dependent albedo and the separated fast cooling and slow recovery
. Details. Conservation of thermal energy and Fourier's law give the heat equationsThe density times the specific heat capacity, , is the volumetric heat capacity, and is the thermal conductivity.
The condition holds the left exterior face at a fixed zero reference temperature; does the same for the right exterior face. The condition expresses perfect thermal contact, with no temperature jump at the interface. Finally,expresses continuity of the signed heat flux in the positive direction: the interface neither stores nor produces heat.
A useful microscopic screening estimate compares thermal energy with the buoyant gravitational potential energy over one particle radius. Write and . The sedimentation length is , and the gravitational Peclet number isUsing and requiring givesEquivalently, combining Stokes law speed and diffusion coefficient gives . Buoyancy, not the full polystyrene density, is essential to the estimate. Taking a diameter rather than radius as the comparison length changes the numerical cutoff by an order-one factor.
There is no universal largest particle that stays uniformly suspended indefinitely. If uniformity over a vessel height is required, use , not merely . For example gives a much smaller radius, about 58 nm. Observation time, density matching, convection, particle polydispersity and shape also matter. Independent of sedimentation, electrostatic/steric barriers must prevent aggregation; low ionic strength, suitable surface chemistry and clean solvent can be as important as size.
Past exam of the soft condensed matter course of the University of Cambridge 2014 Paper 1 4 Solution 2026-10-20
Balancing buoyant weight with Stokes drag givesThis needs isolated spherical particles, low Reynolds number and negligible wall corrections. The supplied settling measurement gives , hence . Its Reynolds number is about , consistent with the approximation.
Compare gravitational work over one radius with thermal energy, or use with . The gravitational Peclet number givesBelow this sedimentation-Brownian crossover radius Brownian motion dominates settling on the particle-size scale. It does not eliminate gravity: the sedimentation scale height is . For negligible concentration gradients across a sample height , the stronger condition is . No universal permanently nonsedimenting size follows without a length/time criterion.
Brownian encounters bring small particles into contact; van der Waals attraction can then bind them. Surface charge can create a repulsive barrier through Debye screening of colloid repulsion. For a monovalent salt reservoir with number density of each ionic species, Poisson–Boltzmann theory hasFor , linearization gives , with . If instead means total ion density, the factor two is absent. The planar potential decays as ; a sphere has an additional factor. This mean-field approximation neglects specific adsorption, ion correlations and finite ion size.
DLVO theory adds screened repulsion to dispersion attraction. At small surface separation for equal spheres of radius , a useful schematic form iswith a short-range repulsive core needed outside the continuum model. Low salt can leave a barrier many times , giving kinetic stability. Higher salt shortens the repulsion and can lower or remove the barrier, allowing coagulation into a deep primary minimum. The primary and secondary DLVO minima have different consequences: a shallow secondary minimum permits looser, sometimes reversible aggregation. The surface boundary condition affects ; screening length alone is not a complete measured interaction law. Non-DLVO hydration or steric forces can matter at contact.
Photoionization-recombination thermal balance Created 2026-10-20 Updated 2026-11-05
When the number of photoionizations equals the number of recombinations, and only those processes exchange thermal energy, equilibrium requires . Photon absorption and electron capture have their own spectral weights. The density cancels from this event balance, but the actual equilibrium temperature requires the two energy averages.[ref]
Heating and Cooling of HII regions by Ian Czekala. Photoionization heating and Recombination radiation sections
Recombination cooling of ionized hydrogen Created 2026-10-20 Updated 2026-11-05
In an optically thin plasma, radiative recombination removes the kinetic energy of captured electrons. A radiative recombination photon can also carry the binding energy released when a free electron becomes bound; that part is stored ionization energy, rather than newly removed thermal energy. The kinetic contribution per event is the recombination-weighted electron energy, which need not be .
Equality with mean photoelectron heating requires two balances. If photoionization is the only ionization and heating process, and radiative recombination the only recombination and cooling process, photoionization equilibrium equates their event rates. Separately imposing thermal equilibrium then equates the mean heating energy per ionization to the mean kinetic cooling energy per recombination. Photoionization equilibrium alone does not do this: at the same balanced event rate, unequal energies can still heat or cool the gas. Additional atomic line cooling, collisional ionization or trapping of emitted photons changes the energy accounting.
Thermal energy Created 2026-10-20 Updated 2026-11-05
Thermal energy is a context-dependent name for the microscopic energy associated with a system's thermal state, rather than a separate conserved substance. The characteristic single-particle energy scale is , with Boltzmann constant and absolute temperature . Comparing this scale with an excitation gap or energy barrier helps decide which microscopic processes are thermally accessible.
Under the classical equipartition theorem, each independent quadratic term in the Hamiltonian contributes on average. Three translational terms therefore give per particle of a monatomic ideal gas. Quantum levels can invalidate that count: a degree of freedom with excitation spacing much larger than can remain nearly frozen. A measured heat capacity tests how the stored internal energy changes with temperature; it does not simply count a fixed amount of heat stored in the sample.
White-dwarf cooling 2026-11-05
White-dwarf cooling is the gradual loss of a white dwarf's stored thermal energy after sustained core fusion has ended. Dense degenerate electrons provide most of the pressure support, so luminosity can decline while the star remains mechanically supported.
Cooling depends on core heat capacity, envelope insulation, early neutrino losses and later crystallization processes. A population's luminosity distribution therefore contains age information only through a cooling model and its formation history. Crystallization can delay the decline through latent heat and compositional energy release; luminosity is not a simple universal linear clock.

