
Dynamics of the particle in a field of elastic forces 
 
473 
we obtain thus Binet’s formula, which allows to solve the inverse problem: to determine 
the central force which, applied upon a given particle, imparts a plane trajectory to it, 
after the law of areas with respect to a fixed pole. Taking into account the equation 
(8.1.4') of the trajectory, we can write 
[]
2
2
() ()
mC
Fff
r
θθ
′′
=− +
 
(8.1.8') 
too, where 
22
/
f θ
′′
≡∂ ∂ . If beforehand a form of F  is not imposed, that one has a 
certain non-determination, taking into account the equation of the trajectory (the 
equation which links 
r  to  θ ); eliminating  θ , one obtains  ()FFr
, form used the 
most times. 
For instance, in case of trajectories to which corresponds the equation 
cos
k
rakbθ=+,    ,, constabk
, 
(8.1.9) 
choosing the fixed point as origin, we get 
22
2
3
(1)
() ( 2)
kk
kab
C
Fr k b
rr
+
+−
⎤
=− + +
⎥
⎦
; 
(8.1.9') 
in particular, these trajectories may be conics with the pole at the focus (
1k =− ) or at 
the centre (
1k = ), Pascal limaçons ( 2k
,  0b
), lemniscates etc. 
1.1.2 Qualitative study of orbits. Bertrand’s theorem 
Usually, the trajectory of a particle in a central field of forces is called orbit (even if 
it is not a closed curve). The relations (8.1.6')-(8.1.6''') determine the orbit and the 
motion on it only if 
r
, 
θ
 and 
t
 are real quantities, hence if  () 0rϕ ≥ ; the apparent 
potential must verify the condition 
() 0Ur h
≥
, which determines the domain of 
variation of 
r , corresponding to the motion of the particle; the solutions of the equation 
() 0Ur h
=  
(8.1.10) 
specify the frontier of the domain. From (8.1.6') one may see that the radial velocity 
vanishes on the frontier (
0r
 ), the angular velocity being non-zero ( 0θ ≠
); if  
we would have 
0θ =
 at a point other than the origin, then the first integral of areas 
would lead to 
0C =
, that is to a rectilinear trajectory; hence, at the respective points 
the velocity is normal to the radius vector. On the frontier, 
()rt  changes of sign, the 
respective point corresponding to a relative extremum for 
()rt . The relation (8.1.2) 
shows that 
()tθ
 has a constant sign, so that  ()tθ  is a monotone function; the integrals 
(8.1.6''), (8.1.6''') must be calculated on intervals of monotony, the sign being  
chosen correspondingly. Let 
min
r  and 
max
r  be the extreme values which may be taken 
by 
r ; the corresponding points on the orbit are called apsides. In this case,