The following are arguments showing that the LRL vector is conserved under central forces that obey an inverse-square law.
Direct proof of conservation A central force \mathbf{F} acting on the particle is \mathbf{F} = \frac{d\mathbf{p}}{dt} = f(r) \frac{\mathbf{r}}{r} = f(r) \mathbf{\hat{r}} for some function f(r) of the radius r. Since the angular momentum \mathbf{L} = \mathbf{r} \times \mathbf{p} is conserved under central forces, \frac{d}{dt}\mathbf{L} = 0 and \frac{d}{dt} \left( \mathbf{p} \times \mathbf{L} \right) = \frac{d\mathbf{p}}{dt} \times \mathbf{L} = f(r) \mathbf{\hat{r}} \times \left( \mathbf{r} \times m \frac{d\mathbf{r}}{dt} \right) = f(r) \frac{m}{r} \left[ \mathbf{r} \left(\mathbf{r} \cdot \frac{d\mathbf{r}}{dt} \right) - r^2 \frac{d\mathbf{r}}{dt} \right], where the momentum \mathbf{p} = m \frac{d\mathbf{r}}{dt} and where the triple cross product has been simplified using
Lagrange's formula \mathbf{r} \times \left( \mathbf{r} \times \frac{d\mathbf{r}}{dt} \right) = \mathbf{r} \left(\mathbf{r} \cdot \frac{d\mathbf{r}}{dt} \right) - r^2 \frac{d\mathbf{r}}{dt}. The identity \frac{d}{dt} \left( \mathbf{r} \cdot \mathbf{r} \right) = 2 \mathbf{r} \cdot \frac{d\mathbf{r}}{dt} = \frac{d}{dt} (r^2) = 2r\frac{dr}{dt} yields the equation \frac{d}{dt} \left( \mathbf{p} \times \mathbf{L} \right) = -m f(r) r^2 \left[ \frac{1}{r} \frac{d\mathbf{r}}{dt} - \frac{\mathbf{r}}{r^2} \frac{dr}{dt}\right] = -m f(r) r^2 \frac{d}{dt} \left( \frac{\mathbf{r}}{r}\right). For the special case of an inverse-square central force f(r)=\frac{-k}{r^{2}}, this equals \frac{d}{dt} \left( \mathbf{p} \times \mathbf{L} \right) = m k \frac{d}{dt} \left( \frac{\mathbf{r}}{r}\right) = \frac{d}{dt} (mk\mathbf{\hat{r}}). Therefore, is conserved for inverse-square central forces \frac{d}{dt} \mathbf{A} = \frac{d}{dt} \left( \mathbf{p} \times \mathbf{L} \right) - \frac{d}{dt} \left( mk\mathbf{\hat{r}} \right) = \mathbf{0}. A shorter proof is obtained by using the relation of angular momentum to angular velocity, \mathbf{L} = m r^2 \boldsymbol{\omega}, which holds for a particle traveling in a plane perpendicular to \mathbf{L}. Specifying to inverse-square central forces, the time derivative of \mathbf{p} \times \mathbf{L} is \frac{d}{dt} \mathbf{p} \times \mathbf{L} = \left( \frac{-k}{r^2} \mathbf{\hat{r}} \right) \times \left(m r^2 \boldsymbol{\omega}\right) = m k \, \boldsymbol{\omega} \times \mathbf{\hat{r}} = m k \,\frac{d}{dt}\mathbf{\hat{r}}, where the last equality holds because a unit vector can only change by rotation, and \boldsymbol{\omega}\times\mathbf{\hat{r}} is the orbital velocity of the rotating vector. Thus, is seen to be a difference of two vectors with equal time derivatives. As described
elsewhere in this article, this LRL vector is a special case of a general conserved vector \mathcal{A} that can be defined for all central forces. \begin{align} 2\xi p_\xi^2 - mk - mE\xi &= -\Gamma, \\ 2\eta p_\eta^2 - mk - mE\eta &= \Gamma, \end{align} where is a constant of motion. Subtraction and re-expression in terms of the Cartesian momenta and shows that is equivalent to the LRL vector \Gamma = p_y (x p_y - y p_x) - mk\frac{x}{r} = A_x.
Noether's theorem The connection between the rotational symmetry described above and the conservation of the LRL vector can be made quantitative by way of
Noether's theorem. This theorem, which is used for finding constants of motion, states that any infinitesimal variation of the
generalized coordinates of a physical system \delta q_i = \varepsilon g_i(\mathbf{q}, \mathbf{\dot{q}}, t) that causes the Lagrangian to vary to first order by a total time derivative \delta L = \varepsilon \frac{d}{dt} G(\mathbf{q}, t) corresponds to a conserved quantity \Gamma = -G + \sum_i g_i \left( \frac{\partial L}{\partial \dot{q}_i}\right). In particular, the conserved LRL vector component corresponds to the variation in the coordinates \delta_s x_i = \frac{\varepsilon}{2} \left[ 2 p_i x_s - x_i p_s - \delta_{is} \left( \mathbf{r} \cdot \mathbf{p} \right) \right], where equals 1, 2 and 3, with and being the -th components of the position and momentum vectors and , respectively; as usual, represents the
Kronecker delta. The resulting first-order change in the Lagrangian is \delta L = \frac{1}{2}\varepsilon mk\frac{d}{dt} \left( \frac{x_s}{r} \right). Substitution into the general formula for the conserved quantity yields the conserved component of the LRL vector, A_s = \left[ p^2 x_s - p_s \ \left(\mathbf{r} \cdot \mathbf{p}\right) \right] - mk \left( \frac{x_s}{r} \right) = \left[ \mathbf{p} \times \left( \mathbf{r} \times \mathbf{p} \right) \right]_s - mk \left( \frac{x_s}{r} \right).
Lie transformation Noether's theorem derivation of the conservation of the LRL vector is elegant, but has one drawback: the coordinate variation involves not only the
position , but also the
momentum or, equivalently, the
velocity . This drawback may be eliminated by instead deriving the conservation of using an approach pioneered by
Sophus Lie. Specifically, one may define a Lie transformation in which the coordinates and the time are scaled by different powers of a parameter λ (Figure 9), t \rightarrow \lambda^{3}t , \qquad \mathbf{r} \rightarrow \lambda^{2}\mathbf{r} , \qquad\mathbf{p} \rightarrow \frac{1}{\lambda}\mathbf{p}. This transformation changes the total angular momentum and energy , L \rightarrow \lambda L, \qquad E \rightarrow \frac{1}{\lambda^{2}} E, but preserves their product
EL2. Therefore, the eccentricity and the magnitude are preserved, as may be seen from the
equation for A^2 = m^2 k^2 e^{2} = m^2 k^2 + 2 m E L^2. The direction of is preserved as well, since the semiaxes are not altered by a global scaling. This transformation also preserves
Kepler's third law, namely, that the semiaxis and the period form a constant . == Alternative scalings, symbols and formulations ==