Let be the cylindrical unit vectors. The surface has an upward normal vector proportional to . If is the vertical component of the normal force, its radial component is . In the stated approximation, vertical acceleration and the vertical driving-force component are neglected, so vertical balance gives . The horizontal contact force is consequently . The projected velocity and its speed are
The driving force is parallel to this velocity, with components and . Use the acceleration in polar coordinates and Newton's second law to obtain
These equations apply where ; at rest the direction of an exactly velocity-aligned drive is not determined.
For a prescribed path, write , . The chain rule gives and . Subtract times the azimuthal equation from the radial equation. The driving force and both cancel:
Thus the constraint for tangentially driven motion on an axisymmetric surface is
The denominator must give a nonnegative squared speed, and the calculation uses . At the polar origin a limiting Cartesian description is appropriate.
For the paraboloid and Archimedean spiral, put
Then, for ,
The branch tending to has positive angular velocity, hence
Since , solve the azimuthal equation for the required force:
This is positive for , consistent with a forward drive. Taking the limit gives
These are the large-time limits of the printed projected equations. Their mechanical approximation has a precise range limitation: on the exact surface, gives , which along this solution grows like . At fixed positive , it is not small as . Thus the requested limits are formal limits of that reduced model; neglect of vertical motion is not a uniform approximation to the full three-dimensional motion all the way to infinity.
For the inverse-square potential , the central force is . The transverse component of acceleration in polar coordinates is therefore zero:
Thus ; for unit mass it is the signed angular momentum perpendicular to the orbital plane. The radial component gives
Consequently
This is the mechanical energy, since the full kinetic energy is and .
For and , the effective potential goes to as and to zero from below as . Its derivative is , so it decreases up to and then increases. Its zero and minimum are
For , is positive and strictly decreasing, with limits at zero and at infinity. It has no minimum at a finite positive radius.
Figure 1.
Attractive and repulsive inverse-square effective potentials and bounded-orbit turning points
. Details.
If , the centrifugal term disappears. For the graph is instead , increasing from to without a minimum; for it remains positive and decreasing. The bounded-orbit calculation below uses the stipulated , which excludes this radial collision case.
In plane polar coordinates, use and . Their derivatives are and . Differentiating gives the velocity and acceleration in polar coordinates:
Both the electrostatic inverse-square force and the drag point radially, so the torque about the origin is zero even though the force depends on radial velocity. The vector angular momentum is constant. For , every position lies in the fixed plane perpendicular to it; if , the trajectory is radial and still lies in a plane. In the nonzero case the transverse equation is , giving
The signed depends on the plane orientation. The stipulated ratio requires .
Set and use primes for differentiation with respect to . Then , and . The radial equation is , so
This damped Binet equation has the general solution, for ,
It is used on the physical interval where . For either sign of , introduce the forward angular distance ; then the exponential is . Thus damping acts forward in time for both orientations, not just when .
For unit mass, the kinetic energy is and the electrostatic potential energy is . Therefore
Using the damped Binet equation,
and multiplication by gives
This is also the drag force times the radial speed. Energy is nonincreasing in time, strictly decreasing while radial motion occurs; a circular trajectory already has constant energy. The sign of alone would be misleading for negative .
To justify circularization under radial inverse-square drag, suppose the forward trajectory remains bounded, . Since and the effective radial potential energy tends to as , the radius is also bounded away from zero. Velocity then stays bounded, so the solution continues for all forward time without collision. Moreover , so . The decaying general solution gives and . Consequently
The tangential motion remains, so the limiting orbit is circular. The convergence is asymptotic; boundedness is needed because a physical solution could otherwise reach and escape rather than complete indefinitely many turns.
Figure 1.
Bounded inverse-square orbit with radial drag approaching a circular orbit, with nonincreasing energy converging to the circular-orbit value
. Details.
The example uses , and , which stays positive. Radial oscillations decay while angular momentum stays fixed.
A central force has no component in the angular direction. The angular component of the acceleration in polar coordinates therefore gives , or
For unit mass, is the signed angular momentum perpendicular to the orbital plane, so its magnitude is conserved. Equivalently, the torque vanishes, which also fixes that plane.
The given potential energy is , whose radial force is : positive is repulsive and negative attractive. The kinetic energy in polar coordinates is , so conservation of energy gives
For and , the effective potential is positive, strictly decreasing from to , and has no stationary point. For , it still tends to at zero, crosses zero at , and has its unique minimum at
It then approaches zero from below. The minimum corresponds to a stable circular orbit. If , the centrifugal barrier disappears; the attractive effective potential is simply and has no minimum.
Figure 1. . Effective potentials with unit angular momentum and k equal to plus or minus one. The attractive minimum and zero are marked. Details.
The perpendicular unit vectors represented by and point radially outwards and transversely in the increasing-angle direction. Reading off their real coefficients in part (b) gives the signed components
These are velocity in polar coordinates and acceleration in polar coordinates. In particular is a transverse speed component; alone is an angular velocity. The moving basis, rather than any extra force assumption, accounts for the additional acceleration terms. At the origin the polar directions themselves are undefined, although the Cartesian velocity and acceleration can remain well defined.
Let be signed displacement along the rails, measured from the centre. The diagram in the original paper shows a guide extending across the centre, so the signed coordinate can pass through zero. Hooke's law gives the radial force . In the rotating reference frame, the radial centrifugal force is . The Coriolis force is perpendicular to the rails and is balanced by their reaction; it has no radial component. Therefore Newton's second law gives
Equivalently, the radial component of acceleration in polar coordinates in the inertial frame is . The radial spring oscillator on a rotating guide has simple harmonic motion only when , with
The angular frequency is in and the frequency in . The critical angular speed is
Strictly this is an upper bound, not an attained maximum for oscillations: at equality , so a displaced object released from rest stays at its displaced position relative to the rails; above it, the central equilibrium is unstable.
A path along a circle can have variable areal velocity. As an illustrative controlled trajectory, keep a point mass on a circle of radius with angle
Its acceleration in polar coordinates and the required net force are
where and are the radial and transverse unit vectors. A circular guide can supply the radial force, while a tangential drive supplies . Hence
For in illustrative units, the three equal time intervals , and sweep areas , and . Their difference comes from the transverse force's positive torque, even though the radius and path shape stay fixed. The area under each areal velocity graph segment equals the corresponding swept area.
Figure 1.
A transverse force gives increasing areal velocity and unequal swept areas in equal times
. Details.
For a differentiable path in plane polar coordinates with , the moving unit vectors are and . Differentiating the position and using proves the displayed velocity. Its signed radial and transverse vector components are and . A second differentiation gives the acceleration in polar coordinates. The complex representatives of the two moving unit vectors are and .