Lagrange planetary equations

The Lagrange planetary equations express changes of osculating orbital elements in terms of derivatives of a disturbing function. Their small-eccentricity secular limit becomes a linear equation for complex eccentricity.

If retained Lagrange planetary equations have $\dot{a}=-2(p+q)a{e}^q{C}_r\sin \varphi$ and $\dot{e}=-q{e}^{q-1}{C}_r\sin \varphi$, then $d(e^2)/d\log a=q/(p+q)$. Thus $e^2-[q/(p+q)]\log (a/a_{\mathrm{ref}})$ is constant. A resonantly oscillating orbital eccentricity–semi-major axis trajectory retraces one curve rather than enclosing area in that projection.

For disturbing function $\mathcal{R}=(G{M}_2/a_2)f(\alpha )e\cos \varphi$, $\alpha =a/a_2$, the leading planar Lagrange planetary equations give $\dot{\lambda }=n+n(M_2/M_{\star })eg(\alpha )\cos \varphi$. The derivative with respect to $a$ holds the other osculating orbital elements fixed. If one writes $\lambda =n(t)t+ϵ(t)$, its literal derivative includes $t\dot{n}$; the physical mean-longitude equation cannot be obtained by silently dropping that term. A consistent accumulated-phase parametrization uses $\lambda ={\int }_0^{t}n(s)ds+{ϵ}_{\mathrm{int}}$.

For perturbing acceleration $R\hat{\mathbf{r}}+T\hat{\mathbf{\theta }}$ on an osculating orbital element system with fixed central parameter $\mu$,To prove it, differentiate the specific orbital energy $-\mu /(2a)$, obtaining $\dot{a}=(2a^2/\mu )(R\dot{r}+Th/r)$. Substitute $\dot{r}=\mu e\sin f/h$, $h/r=\mu (1+e\cos f)/h$ and $h^2=\mu a(1-e^2)$. Here $f$ is the true anomaly; a normal perturbing acceleration does no instantaneous work.