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Show that the equation for hydrostatic equilibrium, Eq. ( 6 ), can also be written in terms of the optical depth $\tau,$ as \[\frac{d P}{d \tau}=\frac{g}{\bar{K}}\] This form of the equation is often useful in building model stellar atmospheres. $$\frac{d P}{d r}=-G \frac{M_{r} \rho}{r^{2}}=-\rho g$$

   Show that the equation for hydrostatic equilibrium, Eq. ( 6 ), can also be written in terms of the optical depth $\tau,$ as
\[\frac{d P}{d \tau}=\frac{g}{\bar{K}}\]
This form of the equation is often useful in building model stellar atmospheres.
$$\frac{d P}{d r}=-G \frac{M_{r} \rho}{r^{2}}=-\rho g$$
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An Introduction to Modern Astrophysics
An Introduction to Modern Astrophysics
Bradley W. Carroll,… 2nd Edition
Chapter 11, Problem 1 ↓

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The optical depth $\tau$ is defined as the integral of the absorption coefficient $\kappa$ over a path length $dr$, i.e., $d\tau = \kappa \rho dr$, where $\rho$ is the density of the medium.  Show more…

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Show that the equation for hydrostatic equilibrium, Eq. ( 6 ), can also be written in terms of the optical depth $\tau,$ as \[\frac{d P}{d \tau}=\frac{g}{\bar{K}}\] This form of the equation is often useful in building model stellar atmospheres. $$\frac{d P}{d r}=-G \frac{M_{r} \rho}{r^{2}}=-\rho g$$
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Key Concepts

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Opacity
Opacity represents the degree to which matter obstructs or scatters the passage of radiation, and it is often characterized by a mean or average value (such as the Rosseland mean opacity) in stellar atmospheres. This averaged opacity connects the density of the material to its radiative properties, enabling the transformation of the hydrostatic equilibrium equation into a form involving optical depth. This is crucial for simplifying the modeling of radiative transfer in stars.
Optical Depth
Optical depth is a dimensionless measure that quantifies the transparency of a medium to radiation. It is defined as the integral of the absorption coefficient along the path of the radiation, and a higher optical depth means that photons are more likely to be absorbed or scattered before escaping the medium. In stellar atmospheres, it is used as an independent variable to describe the radiative transfer process, linking the physical properties of the medium to the observed spectrum.
Hydrostatic Equilibrium
Hydrostatic equilibrium is the balance between the inward gravitational force and the outward pressure gradient within a star or any self-gravitating fluid body. This condition ensures that the star or atmosphere remains stable rather than collapsing or dispersing. It is mathematically expressed by the equation dP/dr = -?g, where P is pressure, ? is density, and g is the local gravitational acceleration.

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