Appendix 6

Appendix 6. Classical Periodization of the Universe’s Evolution

This Appendix adopts a unified method for computing the radius across all epochs: the present-day comoving radius of the observable Universe, R0, is converted into the proper radius of the same observable region at the epoch of interest with redshift z:
R(z)= Rnow / (1+z)
I emphasize that this is the present-day observable region mapped back in time using the scaling a = 1/(1 + z) [22]. This choice:
– provides smooth matching at epoch boundaries (the end of the previous equals the start of the next in both z and R);
– anchors the values to the reference parameters of Planck 2018 (anchors: zeq and z\* of the last-scattering surface);
– ensures uniformity.
For the earliest stages, where only time t is specified rather than z, the scaling is taken as R ∝ t1/2 (radiation domination) or R ∝ t2/3 (matter domination); the boundaries are again matched to the neighboring epochs where z is already specified.
Rnow, Rstart, Rend – radius today / at the start of the period / at the end of the period (m).
tnow, tstart, tend – time at the start of the period / at the end of the period (s / yr).
Znow, Zstart, Zend – redshift today / at the start of the period / at the end of the period.
Note 22

this is not the Hubble radius, RH​=c/H(z), and not the “particle horizon at that time”.

Appendix 6. Classical Periodization of the Universe’s Evolution

Appendix 6

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