Hydrostatic equilibrium plus the ideal gas law is enough to estimate what the center of a star is like, without solving a single differential equation. Astrophysicists call this an order-of-magnitude estimate: replace every derivative by a ratio of typical sizes and keep only the physics.
Why it works
Key idea
Worked examples
Worked example: The Sun's core temperature
- Multiply $G$, $M$ and $m_p$: $GMm_p = 2.22 \times 10^{-7}$ J·m.
- $kR = (1.38 \times 10^{-23})(6.96 \times 10^{8}) = 9.60 \times 10^{-15}$ J/K.
- $T_c \sim 2.3 \times 10^{7}$ K. With $\mu = 0.62$, $1.4 \times 10^{7}$ K.
Answer: Tens of millions of kelvins; models give 15.7 million K.
Worked example: Temperature from pressure and density
- $n = \rho/(\mu m_p) = 1.5 \times 10^{5}/(0.85 \times 1.67 \times 10^{-27}) = 1.06 \times 10^{32}$ m⁻³.
- $T = P/(nk) = 2.5 \times 10^{16}/(1.06 \times 10^{32} \times 1.38 \times 10^{-23})$.
Answer: About $1.7 \times 10^{7}$ K, consistent with the models' 15.7 million K.
Worked example: Bigger stars are only a little hotter inside
- $T_c \propto M/R \propto M/M^{0.8} = M^{0.2}$.
- A 10 $M_\odot$ star: $10^{0.2} = 1.6$.
Answer: Only about 1.6 times the Sun's central temperature, yet, as later topics show, thousands of times its luminosity.
Common mistake