Core temperature along the model clock
Scaled core temperature; the gold line marks the selected time in this demo interval.
AC31 · Heat inside a stellar remnant
How does freezing slow the cooling of a white dwarf? A white dwarf shines by losing stored heat. Freezing releases latent heat, and changes in composition can release more energy. That extra supply slows cooling, so brightness gives an age only after the star’s mass, atmosphere and interior physics are specified.
Drag a probe through a partially crystallized core. Watch a shell release latent heat, then compare a published cooling plateau with the same-mass reference.
Selected independent clock
The section fits the selected core to the view; its actual outer radius is
Source total mass
Scaled core temperature; the gold line marks the selected time in this demo interval.
Scaled energy. Green: sensible heat lost. Blue: latent heat released. Gold: photons emitted.
These are sensible-energy derivatives; latent release is counted separately. At an exact cell melting temperature, the stored derivative uses the solid-side branch.
Published STELUM surface table: one solar mass, standard 30PR30 composition, approximately one-gigayear author smoothing. No internal front or phase fraction is supplied.
Physics tutorial
BackgroundA white dwarf can remain supported by degenerate electrons while losing thermal energy. Its dense ionic material can freeze at a very high temperature, releasing latent heat along the way.
Why it mattersThe cooling light can become a clock only after the mass, envelope and internal energy sources have been specified. This controlled core lets us follow each heat term before comparing a separate published surface sequence.
Start with the essentials
Each is the solid fraction of one mass shell; is its declared latent reservoir. The sensible branch contains ionic and electron heat capacities.
The luminosity comes from the stated Kramers-envelope approximation. This is a model core temperature, not the photospheric effective temperature.
The pure-carbon one-component model freezes at the declared coupling threshold. Denser shells have higher freezing temperatures.
Typical misconceptionDegenerate pressure means the electrons supply all the thermal energy.
Better mental modelPressure support and heat capacity answer different questions. The controlled calculation includes ion and electron thermal terms separately.
Typical misconceptionA front halfway out contains half the core mass.
Better mental modelMass also depends on the radial density profile. The displayed solid mass is integrated over shells, not inferred from the coloured radius.
Typical misconceptionThe long controlled-model time can be appended to a published cooling age.
Better mental modelThe models use different physics and origins. The visible uncalibrated elapsed time is not a stellar-age measurement, and the native sequences retain their own clocks.
Drag the gold probe from the warm liquid into the blue solid.
What to observe: The phase, density and temperature all belong to the selected radial shell and the same saved time.Choose Latent plateau, then compare temperature, released latent energy and radiated energy.
What to observe: The shell can continue supplying light while its temperature remains fixed during the phase change.Choose Debye tail, open Sensible heat capacity and compare the ionic and electron terms.
What to observe: The solid ionic heat capacity falls at low temperature. The electron term is computed separately rather than silently discarded.Open the published plateau, then compare STD, partial and full distillation in the advanced case selector.
What to observe: These are supplied surface sequences with a native origin and about one-gigayear smoothing. They contain no internal front. The controlled core keeps its own uncalibrated clock.The heat and clocks of white dwarfs · Reading path
Articles on this path that use this experiment, followed by the other experiments they suggest.