un:virial-theorem
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| ====== Virial theorem ====== | ====== Virial theorem ====== | ||
| - | If a bound system of particles is in steady (time-averaged) equilibrium, | + | The **virial theorem** |
| + | For a star, galaxy, or molecular cloud in steady equilibrium, | ||
| - | We start from the scalar virial \(G \equiv \sum_i \mathbf{r}_i \!\cdot\! \mathbf{p}_i\). Differentiating twice and time-averaging over many dynamical times for a system whose size does not grow without bound (\(\langle \ddot{G}\rangle = 0\)) gives | + | {{: |
| + | |||
| + | Starting from hydrostatic equilibrium, | ||
| $$ | $$ | ||
| - | \left\langle | + | \frac{dP}{dr}=-\rho(r)\frac{G\,M(r)}{r^{2}}, |
| + | $$ | ||
| + | multiply by the spherical volume element | ||
| + | $$ | ||
| + | \int_{0}^{R}4\pi r^{3}\frac{dP}{dr}\,dr=-\int_{0}^{R}4\pi r^{3}\rho(r)\frac{G\, | ||
| $$ | $$ | ||
| - | \begin{equation} | + | **Left-hand side (pressure term).** Integrate by parts: |
| - | \boxed{\,2\langle K\rangle + \left\langle \sum_i | + | $$ |
| - | \end{equation} | + | \int_{0}^{R}4\pi r^{3}dP=\Big[4\pi r^{3}P\Big]_{0}^{R}-\int_{0}^{R}12\pi |
| + | \approx-3\!\int_{0}^{R}4\pi r^{2}P\,dr=-3\!\int P\,dV, | ||
| + | $$ | ||
| + | where \(P(R)\simeq 0\). | ||
| - | For Newtonian | + | **Right-hand side (gravity |
| $$ | $$ | ||
| - | \Omega \equiv | + | -\int_{0}^{R}4\pi r^{3}\rho\,\frac{G\,M}{r^{2}}\,dr |
| + | = -\int_{0}^{R}\frac{G\, | ||
| + | \equiv \Omega , | ||
| $$ | $$ | ||
| - | Hence, for self-gravitating systems, | + | which is the (negative) **gravitational potential energy**. |
| + | Equating both sides gives the pressure–gravity balance: | ||
| \begin{equation} | \begin{equation} | ||
| - | \boxed{\,2\langle K\rangle | + | 3\!\int P\,dV+\Omega=0. |
| \end{equation} | \end{equation} | ||
| - | —a result that holds for any bound, steady system interacting via \(1/r^2\) gravity (angles denote time averages). | + | For an **ideal gas** the thermal kinetic energy is \(K=\tfrac{3}{2}\!\int P\,dV\), hence |
| + | \begin{equation} | ||
| + | 2K+\Omega=0, | ||
| + | \end{equation} | ||
| + | the virial theorem in its standard energy form. | ||
| + | |||
| + | ===== Satellites and stars ===== | ||
| - | **Example (circular orbit):** a satellite of mass \(m\) around a mass \(M\) at radius \(r\) has \(v^2=GM/ | + | A satellite of mass \(m\) in a circular orbit around a mass \(M\) at radius \(r\) obeys |
| $$ | $$ | ||
| - | E_k=\tfrac12 m v^2=\tfrac12 \frac{G M m}{r}, | + | K=\tfrac12 m v^{2}=\tfrac12\,\frac{G M m}{r}, |
| - | E_p=-\frac{G M m}{r}, | + | \Omega=-\frac{G M m}{r}, |
| $$ | $$ | ||
| - | so | + | so that |
| \begin{equation} | \begin{equation} | ||
| - | \boxed{\, | + | K=-\tfrac12\, |
| \end{equation} | \end{equation} | ||
| - | in agreement | + | consistent |
| - | --- | + | {{https:// |
| - | **Derivation from hydrostatic equilibrium | + | A **star without an internal nuclear source** behaves analogously: |
| + | As the star shrinks: | ||
| + | | ||
| + | | ||
| - | For a spherical | + | Thus a self-gravitating gas has **negative specific heat**: losing energy can raise its temperature. |
| + | During stellar birth the contracting cloud spins up and heats until pressure and rotation counter gravity; during late stages, core contraction again heats the gas and ignites progressively heavier fuels. | ||
| + | When nuclear power equals surface losses, the star reaches **true equilibrium**—hydrostatic balance | ||
| + | |||
| + | ===== Clusters of galaxies ===== | ||
| + | {{https:// | ||
| + | |||
| + | The virial theorem also yields the **total mass** of a galaxy cluster from member velocities. | ||
| + | For \(N\) identical galaxies (mass \(m\)), | ||
| $$ | $$ | ||
| - | \frac{dP}{dr}=-\rho(r)\frac{G | + | 2\sum_i \tfrac12 m v_i^{2}-\sum_{i\neq j}\frac{G |
| $$ | $$ | ||
| - | Multiply by the volume element \(4\pi r^3\,dr\) and integrate from \(0\) to \(R\): | + | Rearranging, |
| $$ | $$ | ||
| - | \int_0^R 4\pi r^3 \frac{dP}{dr}\,dr | + | m\sum_i v_i^{2}-G m^{2}\sum_{i\neq j}\frac{1}{r_{ij}}=0. |
| - | = -\int_0^R 4\pi r^3 \rho(r)\frac{G M(r)}{r^2}\,dr . | + | |
| $$ | $$ | ||
| - | Integrate | + | Multiplying |
| $$ | $$ | ||
| - | \int_0^R 4\pi r^3 dP | + | N m\!\left[\frac{1}{N}\sum_i v_i^{2}\right] |
| - | =\Big[4\pi r^3 P\Big]_0^R - \int_0^R 12\pi r^2 P\,dr | + | -\frac{G(Nm)^{2}}{2}\!\left[\frac{1}{N(N-1)/ |
| - | \approx -3\!\int_0^R 4\pi r^2 P\,dr | + | |
| - | = -3\!\int P\,dV , | + | |
| $$ | $$ | ||
| - | where the surface term \((4\pi R^3 P(R))\) vanishes for negligible external pressure. | + | With \(M\equiv Nm\) (total mass) and defining |
| - | + | \begin{equation} | |
| - | Rewrite the **right** side using \(dM=4\pi r^2\rho\,dr\): | + | M\,\langle v^{2}\rangle-\frac{G M^{2}}{2}\,\langle r_{ij}^{-1}\rangle=0, |
| - | $$ | + | \end{equation} |
| - | -\int_0^R 4\pi r^3 \rho\frac{G M}{r^2}\,dr | + | hence the **virial mass** |
| - | = -\int_0^R \frac{G M(r)}{r}\,dM(r) | + | |
| - | = \Omega | + | |
| - | $$ | + | |
| - | because | + | |
| - | + | ||
| - | Equating both sides gives the **pressure–gravity identity** | + | |
| \begin{equation} | \begin{equation} | ||
| - | \boxed{\,3\!\int P\,dV + \Omega = 0\,} \tag*{} | + | M=\frac{2\,\langle v^{2}\rangle}{G\,\langle r_{ij}^{-1}\rangle}. |
| \end{equation} | \end{equation} | ||
| - | For an ideal gas, the internal | + | Only the **line-of-sight** component \(v_{\text{los}}\) is observed. |
| + | Assuming isotropy, | ||
| $$ | $$ | ||
| - | K = \tfrac{3}{2}\!\int P\,dV . | + | \langle v^{2}\rangle=3\,\langle v_{\text{los}}^{2}\rangle |
| $$ | $$ | ||
| - | Insert this in the previous box: | + | Thus the virial theorem |
| - | \begin{equation} | + | |
| - | \boxed{\,2K + \Omega = 0\,} \tag*{} | + | |
| - | \end{equation} | + | |
| - | — the virial theorem | + | |
| ===== Insights ===== | ===== Insights ===== | ||
| - | The virial theorem | + | The virial theorem |
| - | | + | * In stars: |
| - | * From hydrostatic equilibrium, | + | |
| - | * Heating a star (increasing | + | * The negative |
| ===== Inquiries ===== | ===== Inquiries ===== | ||
| - | - Starting from \( \frac{dP}{dr}=-\rho | + | - Starting from \( \frac{dP}{dr}=-\rho\,G M(r)/r^{2} \), derive |
| - | - Use \(2K+\Omega=0\) | + | - Explain physically how \(2K+\Omega=0\) |
| - | - For a cluster | + | - Using the cluster |
un/virial-theorem.1761422338.txt.gz · Last modified: by asad
