ASTR 498N Lecture 8
The way forward
(online at www.astro.umd.edu/~drabin/)
Doroga k Zvjozdam Otkrita.
The way to the stars is open.
Sergei Koroljov
The equations of stellar evolution
(O&C §10.5)
We’ve already derived two of the four equations of
static stellar structure, expressing mass conservation and hydrostatic
equilibrium. Although we still need to
assemble more ingredientsconcerning the generation and transport of energy
let’s write down a full set of evolution equations
to get an overall sense of the enterprise at hand.
We’ll consider only spherically symmetric stars, in which all physical variables are constant on spherical shells of constant radius (or internal mass). We also assume the star does not rotate.
What does it mean to specify stellar structure?
We will consider the instantaneous structure of a
star to be specified if the following structural variables are known as functions of r or M :

Pressure P(r) or P(M)
Density ρ(r) or ρ(M)
Temperature T(r) or T(M)
Mass or radius M(r) or r(M)
Luminosity L(r) or L(M)
Composition X(r) or X(M)
where X is an n-vector
of element mass fractions with . Since M and L are variables,
we’ll need to use other symbols (
and
)
for the total mass and luminosity of the star; for notational consistency,
we’ll also use
for the total radius. These choices are not universal. For example, some authors use m or Mr
in place of M, or Lr or
in place of L.
How many differential equations will be required?
There are n +
5 structural variables. Of the n composition
variables, only n1 are independent because they sum to unity. We’ll show below that nuclear reaction
rates determine n
1 independent equations of the form
, leaving five structural variables. The pressure equation of state, P = P(ρ,T,
X), provides one relationship these remaining variables. We therefore expect to need four
differential equations in addition to the composition equations.
The differential equations
Conservation of mass
Conservation of momentum
We earlier derived this in the form where the left hand side vanishes: hydrostatic equilibrium. If the pressure gradient does not exactly balance the gravitational force on the shell, the shell accelerates (Newton’s law). Note that the time derivative of r = r(M) implies a Lagrangian rather than Eulerian description.
Conservation of energy
Write the first law of thermodynamics as , where δ is an infinitesimal Lagrangian
change in a shell of mass dM, luminosity dL, and volume dV. Substitute for the thermodynamic quantities
to obtain
Using and
, we can rewrite this as
So, for an infinitesimal change over δt,
For the static case (d/dt = 0), this just says that the luminosity dL added by shell dM is due to the energy generation rate per unit mass. From the thermodynamic relation TdS = dE + pdV for quasistatic changes, the equation can also be expressed as
where S is the entropy per unit mass.
Energy transport
In Lecture 5, we used dimensional arguments to show, using only the hydrostatic equilibrium equation and the perfect gas equation of state, that a star is much hotter at the center than it is near the surface. From thermodynamics, we know that heat flows from higher to lower temperatures, the more so as the temperature gradient increases. Thus, we expect that our fourth differential equation will relate the flow of energy to the temperature gradient: dT/dr = f(L,…). The form of this relationship will depend upon the dominant mode of energy transport. We’ll find that when all the energy is transported by radiation,
radiative
transport
where is a suitably
frequency-averaged (Rosseland mean) opacity.
An equation of similar form can be used when conduction is important, as
in white dwarfs. This is not
surprising, since optically thick radiative transport (photon “collisions”) and
heat conduction (particle collisions) are both diffusive, random-walk
processes.
However, we will also show that, when the temperature gradient exceeds a critical value known as the adiabatic gradient, the dominant mode of energy transport switches from radiation to convection (think of water coming to a boil when heated strongly from below). Convection is so efficient that usually only a tiny “superadiabatic” temperature gradient is necessary to transport all the luminosity of a star, in which case, to an excellent approximation, the convective temperature gradient has the adiabatic value and
convective transport
where Γ2 (ρ,T, X) coincides, for an ideal gas, with γ ≡ Cp/Cv, a ratio of specific heats. For a monatomic ideal gas, γ =5/3. The adiabatic approximation to the convective temperature gradient is not good near the surface of a cool star, where a substantially superadiabatic gradient may be required to transport enough flux.
Only one of the two equations for dT/dr is used at a given place and time. If the gradient predicted by the radiative transport equation exceeds the adiabatic gradient, the convective equation applies. The convective gradient is still related to luminosity in the sense that a larger gradient transports more heat, but (dT/dr)ad = f(L,…) is a very weak function of L (or, conversely, the heat flux is a very strong function of the superadiabatic gradient).
Composition changes
Recall that XZ is the fraction by mass of element Z: XZ = mZnZ/ρ. It is most convenient to use the Lagrangian description, XZ = XZ (M,t), because then, if there is no particle diffusion between mass shells, only nuclear reactions can change XZ. Then
Let rjk give the rate, per unit volume and time, at which nuclear reactions transform nuclei of type j to type k. The concentration of nucleus Z is increased by reactions rjZ that create Z and decreased by reactions rZk that destroy Z:
where the sums are over all Z. In practice, the number n of transmuting elements that play a significant role in influencing stellar structure at any one time is usually small. However, if one is tracking elemental or isotopic abundances per se, n may need to be large.
This expression of the composition equations is
purely formal, in that we know nothing as yet about the reaction rates rjk(ρ,T, X). In fact, we won’t develop the composition equations furtherour
interest in the reaction rates will center on their role in the energy
equation. However, it is important to
understand that, although much can be learned from sequences of static stellar
models (stellar structure), the composition equations are an essential
ingredient of stellar evolution.
Timescales
We’ve previously introduced three important
timescalesdynamical, thermal (Kelvin-Helmholtz), and nuclear
that are arranged in a hierarchy:
In the Sun, for example, τdyn ~ 1 hr, τth ~ 106.5 y, τnuc ~ 1010.5 y.
If the star changes only on timescales much longer than τdyn, the momentum equation reduces to the hydrostatic (mechanical) equilibrium equation
With the exception of pulsating stars, we will not consider situations in which the time-dependent momentum equation is required.
If the star changes only on timescales much longer than τth, the energy equation reduces to
and the star is in thermal equilibrium. The combination of mechanical and thermal
equilibrium is sometimes known as complete equilibrium.
Unlike mechanical equilibrium, which is a good approximation for all but
the most dynamic phases of stellar evolution, thermal equilibrium is not a good approximation during many evolutionary phasesfor example, during pre-main sequence evolution when
the star derives energy from gravitational contraction rather than nuclear
burning.
The nuclear timescale is quite longlonger than the estimated age of the solar
system. Therefore, we do not expect
that the Sun is in nuclear equilibrium.
The equations of static stellar structure
In the approximation of complete equilibrium, the evolution equations separate into two groups: the structure equations, involving only spatial derivatives, and the composition equations, involving only time derivatives. Thus, if X(M) is specified at some time t, the structure equations form a complete set of ordinary differential equations that determine the spatial structure of the star. Here are the structure equations: