Homework 7 solutions#
1. Electron heat capacity#
We want to find the specific heat of degenerate non-relativistic electrons and compare to that of the ions in a white dwarf to see if we were justified in neglecting their contribution when we did white dwarf cooling.
import numpy as np
We’ll use unyt
to keep track of units for us. This uses SymPy underneat to symbolically track the units we attach to quantities.
import unyt as u
In a previous homework, we found:
We’ll write this as:
with
and
Let’s compute these
h = 6.63e-27 * u.erg * u.s
m_u = 1.67e-24 * u.g
m_e = 9.11e-28 * u.g
k = 1.38e-16 * u.erg / u.K
alpha = h**2 / (20 * m_e) * (3 / np.pi)**(2./3.)
alpha
unyt_quantity(2.33951736e-27, 'erg**2*s**2/g')
beta = 40 * np.pi**2 / (3 / np.pi)**(4./3.) * m_e**2 / h**4 * k**2
beta
unyt_quantity(3.43404019e+21, 'g**2/(K**2*erg**2*s**4)')
Now, we know that for non-relativistic electrons,
and
so
and
If we take typical conditions in a white dwarf, we can evaluate this
rho = 1.e7 * u.g / u.cm**3
T = 1.e7 * u.K
mu_e = 0.5
cv_e = 3 * alpha * beta * T / rho**(2./3.) / (mu_e * m_u)**(1./3.)
cv_e
unyt_quantity(551430.44751741, 'cm**2/(K*s**2)')
cv_e.to("erg/g/K")
unyt_quantity(551430.44751741, 'erg/(K*g)')
We see that for the electrons,
For the ions, in class we found that
we can evaluate this for a carbon white dwarf (\(\mu_I = 12\)):
mu_I = 12
cv_ions = 1.5 * k / (mu_I * m_u)
cv_ions
unyt_quantity(10329341.31736527, 'erg/(K*g)')
We see that we have
so \(c_{v,ions} \gg c_{v,e}\), justifying our assumption in class.
2. WD cooling#
Another assumption we made when we did white dwarf cooling was to assume that the radiative layer was thin. Here we’ll check that.
We showed that the radiative layer behaves like a polytrope with an equation of state:
with \(n_\mathrm{eff} = 13/4\).
Let’s start with hydrostatic equilibrium:
where \(M_\star\) is assumed to be the constant mass of the star (the layer does not have significant masss).
Using the chain rule, we can write:
and from our EOS, we see \(\nabla^{-1} = 1 + n_\mathrm{eff} = 17/4\).
Now we use the ideal gas law to replace \(P/T = \rho k /(\mu m_u)\), giving
We can integrate this from the transition radius (where \(T = T_c\)) to the surface of the star
which gives
we can take the surface temperature to be 0, giving
with \(l = R_\star - r_\mathrm{tr}\) as the layer thickness.
This gives
Let’s put in numbers
M = 0.6 * u.solar_mass_cgs
R = 0.012 * 7.e10 * u.cm
G = 6.67e-8 * u.dyne * u.cm**2 / u.g**2
g = G * M / R**2
g.to("cm/s**2")
unyt_quantity(1.12778349e+08, 'cm/s**2')
Tc = 1.e8 * u.K
mu = 12
l = 17./4. * k * Tc / (mu * m_u * g)
(l/R).to("dimensionless")
unyt_quantity(0.03089337, 'dimensionless')
We see that for \(T_c = 10^7~\mathrm{K}\) the layer is indeed thin.
We also see that if we increase \(T_c\) by a factor of 10, then \(l \sim R_\star\), so our approximation is no longer as good.
3. Hot-CNO#
We want to estimate the energy release from hot-CNO burning. As discussed in class, the rate becomes limited by the decays of \({}^{14}\mathrm{O}\) and \({}^{15}\mathrm{O}\). These have half-lives of
we’ll denote these as \(\tau_{14}\) and \(\tau_{15}\) here.
a.#
In equilibrium, we have:
and a \(\beta\)-decay reaction has the form:
so equilibrium means that
and since \(Y = X/A\), we have
We define \(Z_\mathrm{CNO} = X_{14} + X_{15}\), so \(X_{15} = Z_\mathrm{CNO} = X_{14}\), giving:
solving for \(X_{14}\), we have
b.#
Again using equilibrium, we have
where the “+4” comes from the fact that 4 H are consumed each time a single \({}^{14}\mathrm{O}\) is consumed.
Using the result above, we see
This reaction also produces a single \({}^{4}\mathrm{He}\), so
The energy release per reaction is \((28.3 - 2.03)~\mathrm{MeV}\) or \(4.2\times 10^{-5}~\mathrm{erg}\)
Therefore the total energy rate is