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title: 14. Motion in a central field title: 14. Motion in a central field
--- ---
On reducing the two-body problem to one of the motion of a single body, On reducing the two-body problem to one of the motion of a single body, we arrive at the problem of determining the motion of a single particle in an external field such that its potential energy depends only on the distance r from some fixed point. This is called a central field. The force acting on the particle is $\v{F} = \partial U(r)/\partial \v{r} = - (\dd{U}/\dd{r})\v{r}/r$; its magnitude is likewise a function of $r$ only, and its direction is everywhere that of the radius vector.
we arrive at the problem of determining the motion of a single particle in an
external field such that its potential energy depends only on the distance r As has already been shown in `1/9`, the angular momentum of any system relative to the centre of such a field is conserved. The angular momentum of a single particle is $\v{M} = \v{r}\times\v{p}$. Since $\v{M}$ is perpendicular to $\v{r}$, the constancy of $\v{M}$ shows that, throughout the motion, the radius vector of the particle lies in the plane perpendicular to $\v{M}$.
from some fixed point. This is called a central field. The force acting on the
particle is F = du(r)/dr = - (dU/dr)r/r; its magnitude is likewise a func- Thus the path of a particle in a central field lies in one plane. Using polar co-ordinates $\v{r}$, in that plane, we can write the Lagrangian as
tion of r only, and its direction is everywhere that of the radius vector.
As has already been shown in §9, the angular momentum of any system ```load
relative to the centre of such a field is conserved. The angular momentum of a 1/14.1
single particle is M = rxp. Since M is perpendicular to r, the constancy of ```
M shows that, throughout the motion, the radius vector of the particle lies
in the plane perpendicular to M. see `1/4.5`. This function does not involve the co-ordinate $\phi$ explicitly. Any generalised co-ordinate $q_i$ which does not appear explicitly in the Lagrangian is said to be cyclic. For such a co-ordinate we have, by Lagrange's equation, $(\dd{}/\dd{t}) \partial L/\partial \dot{q}_i = \partial L/\partial q_i = 0$, so that the corresponding generalised momentum $p_i = \partial L/\partial \dot{q}_i$ is an integral of the motion. This leads to a considerable simplification of the problem of integrating the equations of motion when there are cyclic co-ordinates.
Thus the path of a particle in a central field lies in one plane. Using polar
co-ordinates r, in that plane, we can write the Lagrangian as In the present case, the generalised momentum $p_\phi=mr^2\dot{\phi}$ is the same as the angular momentum $M_z=M$ (see `1/9.6`), and we return to the known law of conservation of angular momentum:
(14.1)
see (4.5). This function does not involve the co-ordinate explicitly. Any ```load
generalised co-ordinate qi which does not appear explicitly in the Lagrangian 1/14.2
is said to be cyclic. For such a co-ordinate we have, by Lagrange's equation, ```
(d/dt) aL/dqi = aL/dqi = 0, so that the corresponding generalised momen-
tum Pi = aL/dqi is an integral of the motion. This leads to a considerable This law has a simple geometrical interpretation in the plane motion of a single particle in a central field. The expression $\mfrac{1}{2}r\cdot r\dd{\phi}$ is the area of the sector bounded by two neighbouring radius vectors and an element of the path `1/fig8`
simplification of the problem of integrating the equations of motion when
there are cyclic co-ordinates.
In the present case, the generalised momentum is the same as
the angular momentum M z = M (see (9.6)), and we return to the known law
of conservation of angular momentum:
M = mr2o = constant. =
(14.2)
This law has a simple geometrical interpretation in the plane motion of a single
particle in a central field. The expression 1/2 . rdo is the area of the sector
bounded by two neighbouring radius vectors and an element of the path