Effective potential explained

The effective potential (also known as effective potential energy) combines multiple, perhaps opposing, effects into a single potential. In its basic form, it is the sum of the 'opposing' centrifugal potential energy with the potential energy of a dynamical system. It may be used to determine the orbits of planets (both Newtonian and relativistic) and to perform semi-classical atomic calculations, and often allows problems to be reduced to fewer dimensions.

Definition

The basic form of potential

Ueff

is defined as: U_\text(\mathbf) = \frac + U(\mathbf), where

The effective force, then, is the negative gradient of the effective potential: \begin\mathbf_\text&= -\nabla U_\text(\mathbf) \\&= \frac \hat - \nabla U(\mathbf)\endwhere

\hat{r

} denotes a unit vector in the radial direction.

Important properties

There are many useful features of the effective potential, such as U_\text \leq E .

To find the radius of a circular orbit, simply minimize the effective potential with respect to

r

, or equivalently set the net force to zero and then solve for

r0

: \frac = 0 After solving for

r0

, plug this back into

Ueff

to find the maximum value of the effective potential
max
U
eff
.

A circular orbit may be either stable or unstable. If it is unstable, a small perturbation could destabilize the orbit, but a stable orbit would return to equilibrium. To determine the stability of a circular orbit, determine the concavity of the effective potential. If the concavity is positive, the orbit is stable: \frac > 0

The frequency of small oscillations, using basic Hamiltonian analysis, is \omega = \sqrt,where the double prime indicates the second derivative of the effective potential with respect to

r

and it is evaluated at a minimum.

Gravitational potential

See main article: Gravitational potential.

Consider a particle of mass m orbiting a much heavier object of mass M. Assume Newtonian mechanics, which is both classical and non-relativistic. The conservation of energy and angular momentum give two constants E and L, which have valuesE = \fracm \left(\dot^2 + r^2\dot^2\right) - \frac,L = mr^2\dot when the motion of the larger mass is negligible. In these expressions,

r
is the derivative of r with respect to time,
\phi
is the angular velocity of mass m,

Only two variables are needed, since the motion occurs in a plane. Substituting the second expression into the first and rearranging givesm\dot^2 = 2E - \frac + \frac = 2E - \frac \left(\frac - 2GmMr\right),\frac m \dot^2 = E - U_\text(r),whereU_\text(r) = \frac - \frac is the effective potential.[1] The original two-variable problem has been reduced to a one-variable problem. For many applications the effective potential can be treated exactly like the potential energy of a one-dimensional system: for instance, an energy diagram using the effective potential determines turning points and locations of stable and unstable equilibria. A similar method may be used in other applications, for instance determining orbits in a general relativistic Schwarzschild metric.

Effective potentials are widely used in various condensed matter subfields, e.g. the Gauss-core potential (Likos 2002, Baeurle 2004) and the screened Coulomb potential (Likos 2001).

See also

Further reading

Notes and References

  1. A similar derivation may be found in José & Saletan, Classical Dynamics: A Contemporary Approach, pgs. 31 - 33