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Hamilton's principle states that the differential equations of motion for
any physical system can be re-formulated as an equivalent
integral equation. Thus, there are two distinct approaches for formulating dynamical models.
It applies not only to the
classical mechanics of a single particle, but also to
classical fields such as the
electromagnetic and
gravitational fields. Hamilton's principle has also been extended to
quantum mechanics and
quantum field theory—in particular the
path integral formulation
of quantum mechanics makes use of the concept—where a physical system
randomly follows one of the possible paths, with the phase of the
probability amplitude for each path being determined by the action for
the path.
Solution of differential equation
Empirical laws are frequently expressed as
differential equations, which describe how physical quantities such as
position and
momentum change
continuously with
time,
space or a generalization thereof. Given the
initial and
boundary conditions for the situation, the "solution" to these empirical equations is one or more
functions that describe the behavior of the system and are called
equations of motion.
Minimization of action integral
Action
is a part of an alternative approach to finding such equations of
motion. Classical mechanics postulates that the path actually followed
by a physical system is that for which the
action is minimized, or more generally, is
stationary. In other words, the action satisfies a
variational principle: the
principle of stationary action (see also below). The action is defined by an
integral, and the classical equations of motion of a system can be derived by minimizing the value of that integral.
This simple principle provides deep insights into physics, and is an important concept in modern
theoretical physics.
History
Action was defined in several now obsolete ways during the development of the concept.
- Gottfried Leibniz, Johann Bernoulli and Pierre Louis Maupertuis defined the action for light as the integral of its speed or inverse speed along its path length.
- Leonhard Euler
(and, possibly, Leibniz) defined action for a material particle as the
integral of the particle's speed along its path through space.
- Pierre Louis Maupertuis introduced several ad hoc and contradictory definitions of action within a single article,
defining action as potential energy, as virtual kinetic energy, and as a
hybrid that ensured conservation of momentum in collisions.
Mathematical definition
Expressed in mathematical language, using the
calculus of variations, the
evolution of a physical system (i.e., how the system actually progresses from one state to another) corresponds to a
stationary point (usually, a minimum) of the action.
Several different definitions of "the action" are in common use in physics. The action is usually an
integral over time. However, when the action pertains to
fields,
it may be integrated over spatial variables as well. In some cases, the
action is integrated along the path followed by the physical system.
The action is typically represented as an
integral over time, taken along the path of the system between the initial time and the final time of the development of the system:

where the integrand
L is called the
Lagrangian. For the action integral to be well-defined, the trajectory has to be bounded in time and space.
Action has the
dimensions of
[energy]⋅
[time], and its
SI unit is
joule-second, which is identical to the unit of
angular momentum.
Action in classical physics
In
classical physics, the term "action" has a number of meanings.
Action (functional)
Most commonly, the term is used for a
functional 
which takes a
function of time and (for
fields) space as input and returns a
scalar. In
classical mechanics, the input function is the evolution
q(
t) of the system between two times
t1 and
t2, where
q represents the
generalized coordinates. The action
![\mathcal{S}[\mathbf{q}(t)]](https://wikimedia.org/api/rest_v1/media/math/render/svg/6d6bc32eb3214884af1b99e757d7f6481963852a)
is defined as the
integral of the
Lagrangian L for an input evolution between the two times:
![{\displaystyle {\mathcal {S}}[\mathbf {q} (t)]=\int _{t_{1}}^{t_{2}}L[\mathbf {q} (t),{\dot {\mathbf {q} }}(t),t]\,dt,}](https://wikimedia.org/api/rest_v1/media/math/render/svg/24fdfbaa6fca4685638bd172a7eb9ca339f7affb)
where the endpoints of the evolution are fixed and defined as

and

. According to
Hamilton's principle, the true evolution
qtrue(
t) is an evolution for which the action
![\mathcal{S}[\mathbf{q}(t)]](https://wikimedia.org/api/rest_v1/media/math/render/svg/6d6bc32eb3214884af1b99e757d7f6481963852a)
is
stationary (a minimum, maximum, or a
saddle point). This principle results in the equations of motion in
Lagrangian mechanics.
Abbreviated action (functional)
Usually denoted as

, this is also a
functional. Here the input function is the
path
followed by the physical system without regard to its parameterization
by time. For example, the path of a planetary orbit is an ellipse, and
the path of a particle in a uniform gravitational field is a parabola;
in both cases, the path does not depend on how fast the particle
traverses the path. The abbreviated action

is defined as the integral of the generalized momenta along a path in the
generalized coordinates:

According to
Maupertuis' principle, the true path is a path for which the abbreviated action

is
stationary.
Hamilton's principal function
Hamilton's principal function is defined by the
Hamilton–Jacobi equations (HJE), another alternative formulation of
classical mechanics. This function
S is related to the functional

by fixing the initial time
t1 and the initial endpoint
q1 and allowing the upper limits
t2 and the second endpoint
q2 to vary; these variables are the
arguments of the function
S. In other words, the action function
S is the
indefinite integral of the Lagrangian with respect to time.
Hamilton's characteristic function
When the total energy
E is conserved, the
Hamilton–Jacobi equation can be solved with the
additive separation of variables:

where the time-independent function
W(
q1,
q2, …
qN) is called
Hamilton's characteristic function. The physical significance of this function is understood by taking its total time derivative

This can be integrated to give

which is just the
abbreviated action.
Other solutions of Hamilton–Jacobi equations
The
Hamilton–Jacobi equations are often solved by additive separability; in some cases, the individual terms of the solution, e.g.,
Sk(
qk), are also called an "action".
Action of a generalized coordinate
This is a single variable
Jk in the
action-angle coordinates, defined by integrating a single generalized momentum around a closed path in
phase space, corresponding to rotating or oscillating motion:

The variable
Jk is called the "action" of the generalized coordinate
qk; the corresponding canonical variable conjugate to
Jk is its "angle"
wk, for reasons described more fully under
action-angle coordinates. The integration is only over a single variable
qk and, therefore, unlike the integrated dot product in the abbreviated action integral above. The
Jk variable equals the change in
Sk(
qk) as
qk is varied around the closed path. For several physical systems of interest, J
k is either a constant or varies very slowly; hence, the variable
Jk is often used in perturbation calculations and in determining
adiabatic invariants.
Euler–Lagrange equations for the action integral
As noted above, the requirement that the action integral be
stationary under small perturbations of the evolution is equivalent to a set of
differential equations (called the
Euler–Lagrange equations) that may be determined using the
calculus of variations. We illustrate this derivation here using only one coordinate,
x; the extension to multiple coordinates is straightforward.
Adopting
Hamilton's principle, we assume that the Lagrangian
L (the integrand of the action integral) depends only on the coordinate
x(
t) and its time derivative
dx(
t)/
dt, and may also depend explicitly on time. In that case, the action integral can be written as

where the initial and final times (
t1 and
t2) and the final and initial positions are specified in advance as

and

. Let
xtrue(
t) represent the true evolution that we seek, and let

be a slightly perturbed version of it, albeit with the same endpoints,

and

. The difference between these two evolutions, which we will call

, is infinitesimally small at all times:

At the endpoints, the difference vanishes, i.e.,

.
Expanded to first order, the difference between the actions integrals for the two evolutions is
![{\displaystyle {\begin{aligned}\delta {\mathcal {S}}&=\int _{t_{1}}^{t_{2}}\left[L(x_{\text{true}}+\varepsilon ,{\dot {x}}_{\text{true}}+{\dot {\varepsilon }},t)-L(x_{\text{true}},{\dot {x}}_{\text{true}},t)\right]\,dt\\&=\int _{t_{1}}^{t_{2}}\left(\varepsilon {\frac {\partial L}{\partial x}}+{\dot {\varepsilon }}{\frac {\partial L}{\partial {\dot {x}}}}\right)\,dt.\end{aligned}}}](https://wikimedia.org/api/rest_v1/media/math/render/svg/15a9230f1429e88e959690bcc1dcdc98e36b31fe)
Integration by parts of the last term, together with the boundary conditions

, yields the equation

The requirement that

be
stationary implies that the first-order change must be zero for
any possible perturbation ε(
t) about the true evolution:
-
This can be true only if
Euler–Lagrange equation
|
The Euler–Lagrange equation is obeyed provided the
functional derivative of the action integral is identically zero:

The quantity

is called the
conjugate momentum for the coordinate
x. An important consequence of the Euler–Lagrange equations is that if
L does not explicitly contain coordinate
x, i.e.
- if
, then
is constant in time.
In such cases, the coordinate
x is called a
cyclic coordinate, and its conjugate momentum is conserved.
Example: free particle in polar coordinates
Simple examples help to appreciate the use of the action principle via the Euler–Lagrangian equations. A free particle (mass
m and velocity
v) in Euclidean space moves in a straight line. Using the Euler–Lagrange equations, this can be shown in
polar coordinates as follows. In the absence of a potential, the Lagrangian is simply equal to the kinetic energy

in orthonormal (
x,
y) coordinates, where the dot represents differentiation with respect to the curve parameter (usually the time,
t).
In polar coordinates (
r, φ) the kinetic energy and hence the Lagrangian becomes

The radial
r and angular φ components of the Euler–Lagrangian equations become respectively

The solution of these two equations is given by

for a set of constants
a,
b,
c,
d determined by initial conditions.
Thus, indeed,
the solution is a straight line given in polar coordinates.
The action principle
Classical fields
The
action principle can be extended to obtain the
equations of motion for fields, such as the
electromagnetic field or
gravitational field.
The
Einstein equation utilizes the
Einstein–Hilbert action as constrained by a
variational principle.
The
trajectory (path in
spacetime) of a body in a gravitational field can be found using the action principle. For a free falling body, this trajectory is a
geodesic.
Conservation laws
Implications of symmetries in a physical situation can be found with the action principle, together with the
Euler–Lagrange equations, which are derived from the action principle. An example is
Noether's theorem, which states that to every
continuous symmetry in a physical situation there corresponds a
conservation law (and conversely). This deep connection requires that the action principle be assumed.
Quantum mechanics and quantum field theory
In quantum mechanics, the system does not follow a single path whose
action is stationary, but the behavior of the system depends on all
permitted paths and the value of their action. The action corresponding
to the various paths is used to calculate the
path integral, that gives the
probability amplitudes of the various outcomes.
Although equivalent in classical mechanics with
Newton's laws, the
action principle
is better suited for generalizations and plays an important role in
modern physics. Indeed, this principle is one of the great
generalizations in physical science. It is
best understood within quantum mechanics. In particular, in
Richard Feynman's
path integral formulation of quantum mechanics, where it arises out of
destructive interference of quantum amplitudes.
Maxwell's equations can also
be derived as conditions of stationary action.
Single relativistic particle
When relativistic effects are significant, the action of a point particle of mass
m travelling a
world line C parametrized by the
proper time 
is

If instead, the particle is parametrized by the coordinate time
t of the particle and the coordinate time ranges from
t1 to
t2, then the action becomes

where the
Lagrangian is

Modern extensions
The action principle can be generalized still further. For example, the action need not be an integral, because nonlocal actions are possible. The configuration space need not even be a functional space, given certain features such as noncommutative geometry. However, a physical basis for these mathematical extensions remains to be established experimentally.