Two body problem: Difference between revisions
Created page with "In astronomy, two body problems normally refer to the study of the gravitational interaction of two celestial objects. == Classic form: planetary/satellite orbit (point mass approximation) == Approximate a star/planet as point mass $M$, and a planet/satellite orbiting around it as point mass $m$. The orbit of the planet in the reference frame of the star satisfies the equation: {{#content:Q1785}} Where $\mu=G(M+m)$. === Derivation === Let $$ \mathbf{r}=\math..." |
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Where $\mu=G(M+m)$. | Where $\mu=G(M+m)$. | ||
The orbit described by the equation is usually elliptical: | |||
[[File:Two-body-problem.ggb]] | |||
=== Derivation === | === Derivation === | ||
Latest revision as of 15:04, 24 September 2026
In astronomy, two body problems normally refer to the study of the gravitational interaction of two celestial objects.
Classic form: planetary/satellite orbit (point mass approximation)
Approximate a star/planet as point mass $M$, and a planet/satellite orbiting around it as point mass $m$.
The orbit of the planet in the reference frame of the star satisfies the equation:
Where $\mu=G(M+m)$.
The orbit described by the equation is usually elliptical:
Derivation
Let
$$ \mathbf{r}=\mathbf{r}_m-\mathbf{r}_M $$
be the vector from $M$ to $m$.
Let $r=|\mathbf{r}|$.
Gravity pulls $m$ toward $M$:
$$ m\ddot{\mathbf{r}}_m=-GMm\frac{\mathbf{r}}{r^3} \text{ (1)} $$
Gravity pulls $M$ toward $m$:
$$ M\ddot{\mathbf{r}}_M=+GMm\frac{\mathbf{r}}{r^3} \text{ (2)} $$
Therefore:
$$ \begin{cases} \ddot{\mathbf{r}}_m=-GM\frac{\mathbf{r}}{r^3} \text{ (1)/m} \\ \ddot{\mathbf{r}}_M=+Gm\frac{\mathbf{r}}{r^3} \text{ (2)/M} \end{cases} $$
The relative acceleration of $m$ according to $M$, $\ddot{\mathbf{r}}$, is
$$ \ddot{\mathbf{r}} = \ddot{\mathbf{r}}_m-\ddot{\mathbf{r}}_M $$
Substitute:
$$ \ddot{\mathbf{r}} = -GM\frac{\mathbf{r}}{r^3} - Gm\frac{\mathbf{r}}{r^3} $$
$$ \boxed{ \ddot{\mathbf{r}} = -G(M+m)\frac{\mathbf{r}}{r^3} } $$
Usually, we note
$$ \boxed{ \mu=G(M+m) } $$