Primordial helium response to extra relativistic species Created 2026-10-07 Updated 2026-10-14
With a weak conversion time proportional to and a radiation-era age proportional to , cosmological weak freeze-out occurs at . Extra radiation therefore raises the freeze-out temperature and the neutron-to-proton ratio . Before decay, the primordial helium mass fraction is , giving . A shorter delay through the deuterium bottleneck also leaves more neutrons. After freeze-out, conserve baryon number and evolve the neutron fraction to obtain . A precise abundance requires the weak rates and nuclear-burning history, not merely the number of relativistic species.
At fixed cosmological weak freeze-out temperature and fixed neutron survival factor, neutron-proton chemical equilibrium gives and neutron-limited helium synthesis gives . Differentiating yields the displayed sensitivity. A finite change gives . Increasing the positive mass difference reduces helium production. Changes to the weak conversion rates, neutron lifetime or nuclear history must be supplied separately for a full abundance prediction.
Weak-decoupling temperature estimate Created 2026-10-14 Updated 2026-10-20
In natural units with unreduced Planck mass , the radiation-era Hubble parameter scales as , while a low-energy weak interaction rate scales as . Their equality gives a decoupling scale of order one MeV. Distinct weak processes have distinct rate coefficients: neutrino decoupling and cosmological weak freeze-out of neutron-proton conversion are nearby events, not an identical precise temperature inferred from the power laws alone.