At neutrino decoupling, the interaction rate is comparable with the Hubble parameter. Equating the supplied rates gives
Here the Planck mass is the unreduced in natural units, , and the effective number of relativistic energy degrees of freedom is . The supplied rate gives an order-of-magnitude neutrino decoupling estimate; a precise neutron-proton conversion temperature uses its own weak-rate coefficients.
The chemical equilibrium condition for is . With negligible lepton chemical potentials, . The nonrelativistic Maxwell--Boltzmann number density therefore gives
because and the small mass difference can be neglected in the prefactor. This is the neutron-proton chemical equilibrium relation.
For the deuterium equilibrium abundance, because photons have zero chemical potential. The sign convention in the paper is important: , while the positive nuclear binding energy is . Using spin multiplicities , gives
With , , and photon number density , this becomes
Here is a number fraction; the fraction of baryons bound in deuterium is . The formula estimates the onset of the deuterium bottleneck opening while depletion of free neutrons and protons remains small. Because , stable deuterium becomes abundant only far below the positive nuclear binding energy, not simply at .
Let denote cosmological weak freeze-out of the neutron-to-proton ratio, , and let mark efficient nuclear burning. Free-neutron decay after freeze-out gives
Almost every surviving neutron enters helium-4, whose atomic nucleus contains two neutrons and four baryons. Thus neutron-limited helium synthesis gives
A longer neutron half-life leaves more neutrons available, increasing the primordial helium mass fraction. If the longer lifetime reflects weaker weak interactions, the accompanying earlier cosmological weak freeze-out can reinforce that effect.
During radiation domination, whereas the weak conversion rate is proportional to . Hence . Increasing the effective number of relativistic energy degrees of freedom raises , increasing , and shortens the interval for free-neutron decay after freeze-out. Both increase the primordial helium mass fraction while nuclear burning remains efficient. The same reasoning gives the primordial helium response to a varying gravitational constant: larger over this interval produces more helium, with fixed microscopic rates and the approximate Friedmann equation unchanged. Smaller has the opposite effect. A particular varying- model must specify its background expansion and time history; the simple trend must not be extrapolated to changes so large that nuclear burning itself fails.