Past exam of the short options paper shared by Prelims and Parts A and B of the physics course of the University of Oxford / 2018 / S26 / 1 / a

A thin spherical shell of thickness $dr$ has mass $4\pi r^2\rho dr$. Balancing its inward gravitational force with the pressure difference across its faces givesFor a transparent estimate take constant density $\rho =3M_{\odot }/(4\pi R_{\odot }^3)$ and negligible surface pressure. Then $M_r=M_{\odot }{r}^3/R_{\odot }^3$, so integration givesCombining with the ideal gas law and $\mu \simeq 0.6$ yields $T_c\simeq \mu m_{H}G{M}_{\odot }/(2k_B{R}_{\odot })\simeq 7\times 10^6$ K. The less specific virial scaling gives $T_c\sim \mu m_{H}G{M}_{\odot }/(k_B{R}_{\odot })\sim 10^7$ K.

The real Sun is strongly centrally concentrated: a uniform-density model substantially underestimates central pressure and is not a detailed solar model. Its value is a justified scale estimate, while more realistic structure produces central temperatures of order $1.5\times 10^7$ K and central pressures of order $10^{16}$ Pa. Hydrostatic equilibrium alone does not uniquely determine both profiles without an equation of state and a density/thermal model.