Math 2.0

Mechanics of particles and systems Orbital mechanics Theorem

Lagrange's planetary equations

Builds on Orbital perturbationOsculating orbitOrbital elementsGradient

Statement

Let μ>0\mu > 0 and let a body move by r′′=−μ r∥r∥3+∇rℛ(r,t),r'' = -\frac{\mu\, r}{\norm{r}^3} + \nabla_r \mathcal{R}(r, t), where the disturbing function ℛ\mathcal{R} is a smooth function and ∇r\nabla_r is its gradient in rr. Assume that the osculating orbit stays elliptic with 0<e<10 < e < 1 and 0<i<π0 < i < \pi. Let a,e,i,Ω,ωa, e, i, \Omega, \omega and the mean anomaly MM be its orbital elements, and let n=μ/a3n = \sqrt{\mu / a^3} be the mean motion. Write ℛ\mathcal{R} as a function of these elements and tt, with partial derivatives in aa taken at fixed MM. Then the elements satisfy dadt=2na∂ℛ∂M,\frac{da}{dt} = \frac{2}{na} \frac{\partial \mathcal{R}}{\partial M}, dedt=1−e2na2e∂ℛ∂M−1−e2na2e∂ℛ∂ω,\frac{de}{dt} = \frac{1 - e^2}{n a^2 e} \frac{\partial \mathcal{R}}{\partial M} - \frac{\sqrt{1 - e^2}}{n a^2 e} \frac{\partial \mathcal{R}}{\partial \omega}, didt=cos⁡ina21−e2sin⁡i∂ℛ∂ω−1na21−e2sin⁡i∂ℛ∂Ω,\frac{di}{dt} = \frac{\cos i}{n a^2 \sqrt{1 - e^2} \sin i} \frac{\partial \mathcal{R}}{\partial \omega} - \frac{1}{n a^2 \sqrt{1 - e^2} \sin i} \frac{\partial \mathcal{R}}{\partial \Omega}, dΩdt=1na21−e2sin⁡i∂ℛ∂i,\frac{d\Omega}{dt} = \frac{1}{n a^2 \sqrt{1 - e^2} \sin i} \frac{\partial \mathcal{R}}{\partial i}, dωdt=1−e2na2e∂ℛ∂e−cos⁡ina21−e2sin⁡i∂ℛ∂i,\frac{d\omega}{dt} = \frac{\sqrt{1 - e^2}}{n a^2 e} \frac{\partial \mathcal{R}}{\partial e} - \frac{\cos i}{n a^2 \sqrt{1 - e^2} \sin i} \frac{\partial \mathcal{R}}{\partial i}, dMdt=n−1−e2na2e∂ℛ∂e−2na∂ℛ∂a.\frac{dM}{dt} = n - \frac{1 - e^2}{n a^2 e} \frac{\partial \mathcal{R}}{\partial e} - \frac{2}{na} \frac{\partial \mathcal{R}}{\partial a}.

Remarks

The proof is Lagrange's method of variation of constants. The elements are functions of (r,r′)(r, r') 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 ∇rℛ\nabla_r \mathcal{R} the right sides vanish, except dM/dt=ndM/dt = n, which is uniform motion on a fixed ellipse. Example: averaging the J2J_2 term of the Earth's potential over one orbit and inserting it in the equation for Ω\Omega gives the classical regression of the node of a satellite. The factors 1/e1/e and 1/sin⁡i1/\sin i 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 ℛ\mathcal{R} over the fast mean anomalies and studies the slow evolution of the remaining elements. In the averaged system ∂ℛ/∂M=0\partial \mathcal{R} / \partial M = 0, 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.

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Each page uses the pages above it. The colour of the bar on a box shows how strong the evidence is, and the box also gives it as text. The list has the same pages.
  • no evidence level
  1. Euclidean space object
  2. Function concept
  3. Orbital elements concept
  4. Orbital perturbation concept
  5. Osculating orbit concept
  6. Total derivative concept
  7. Function of several variables concept
  8. Differentiable function of several variables concept
  9. Partial derivative concept
  10. Gradient concept
  11. Lagrange's planetary equations statement

Further reading

  1. Web https://en.wikipedia.org/wiki/Perturbation_(astronomy)
About this page
TagEGYH1Z6SF2
URIm2://EGYH1Z6SF2
Kindstatement, theorem
WritingW0 stub
MSC70F15, 70M20, 70H09
StatusThis copy of the site has no build data. Run m2 status EGYH1Z6SF2.
AboutOrbital perturbation
UsesOrbital perturbation, Osculating orbit, Orbital elements, Gradient
Changed3 November 2026

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