Mechanics of particles and systems Orbital mechanics Theorem
Lagrange's planetary equations
Builds on Orbital perturbationOsculating orbitOrbital elementsGradient
Statement
Let and let a body move by where the disturbing function is a smooth function and is its gradient in . Assume that the osculating orbit stays elliptic with and . Let and the mean anomaly be its orbital elements, and let be the mean motion. Write as a function of these elements and , with partial derivatives in taken at fixed . Then the elements satisfy
Remarks
The proof is Lagrange's method of variation of constants. The elements are functions of that are constant along Kepler motion, so along the perturbed motion their derivatives are linear in the perturbing acceleration. Computing the Poisson brackets of the elements, or equivalently the Lagrange brackets, gives the coefficients above. Without the term the right sides vanish, except , which is uniform motion on a fixed ellipse. Example: averaging the term of the Earth's potential over one orbit and inserting it in the equation for gives the classical regression of the node of a satellite. The factors and show why the equations break down for nearly circular or nearly equatorial orbits; other sets of elements are used there. For forces that do not come from a potential, such as drag, one uses Gauss's form of the equations instead.
Going deeper
For a student
The equations are the starting point of secular perturbation theory: one averages over the fast mean anomalies and studies the slow evolution of the remaining elements. In the averaged system , so the semi-major axis is constant to first order, which is the Laplace–Lagrange result behind the classical stability arguments. They are a Hamiltonian system in disguise; in Delaunay variables they take canonical form.
Reading path
To understand this page from the ground up, read these 11 pages in order. The foundations come first.
Show the path as a graph
- no evidence level
- Euclidean space object
- Function concept
- Orbital elements concept
- Orbital perturbation concept
- Osculating orbit concept
- Total derivative concept
- Function of several variables concept
- Differentiable function of several variables concept
- Partial derivative concept
- Gradient concept
- Lagrange's planetary equations statement
Further reading
About this page
| Tag | EGYH1Z6SF2 |
|---|---|
| URI | m2://EGYH1Z6SF2 |
| Kind | statement, theorem |
| Writing | W0 stub |
| MSC | 70F15, 70M20, 70H09 |
| Status | This copy of the site has no build data. Run m2 status EGYH1Z6SF2. |
| About | Orbital perturbation |
| Uses | Orbital perturbation, Osculating orbit, Orbital elements, Gradient |
| Changed | 3 November 2026 |
Markdown · JSON · Edit on GitHub
What this page needs for W1
- an inventory row: the row of the inventory that the node accounts for (0 of 1)
- a source with a locator (0 of 1)
The writing levels say how complete the text of a page is. They do not measure its truth.
What links here
No page links to this page yet.