Tautological one-form explained

T*Q

of a manifold

Q.

In physics, it is used to create a correspondence between the velocity of a point in a mechanical system and its momentum, thus providing a bridge between Lagrangian mechanics and Hamiltonian mechanics (on the manifold

Q

).

The exterior derivative of this form defines a symplectic form giving

T*Q

the structure of a symplectic manifold. The tautological one-form plays an important role in relating the formalism of Hamiltonian mechanics and Lagrangian mechanics. The tautological one-form is sometimes also called the Liouville one-form, the Poincaré one-form, the canonical one-form, or the symplectic potential. A similar object is the canonical vector field on the tangent bundle.

To define the tautological one-form, select a coordinate chart

U

on

T*Q

and a canonical coordinate system on

U.

Pick an arbitrary point

m\inT*Q.

By definition of cotangent bundle,

m=(q,p),

where

q\inQ

and

p\in

*Q.
T
q
The tautological one-form

\thetam:

*Q
T
mT

\to\R

is given by\theta_m = \sum^n_ p_i \, dq^i,with

n=dimQ

and

(p1,\ldots,pn)\inU\subseteq\Rn

being the coordinate representation of

p.

Any coordinates on

T*Q

that preserve this definition, up to a total differential (exact form), may be called canonical coordinates; transformations between different canonical coordinate systems are known as canonical transformations.

The canonical symplectic form, also known as the Poincaré two-form, is given by\omega = -d\theta = \sum_i dq^i \wedge dp_i

The extension of this concept to general fibre bundles is known as the solder form. By convention, one uses the phrase "canonical form" whenever the form has a unique, canonical definition, and one uses the term "solder form", whenever an arbitrary choice has to be made. In algebraic geometry and complex geometry the term "canonical" is discouraged, due to confusion with the canonical class, and the term "tautological" is preferred, as in tautological bundle.

Coordinate-free definition

The tautological 1-form can also be defined rather abstractly as a form on phase space. Let

Q

be a manifold and

M=T*Q

be the cotangent bundle or phase space. Let \pi : M \to Qbe the canonical fiber bundle projection, and let \mathrm \pi : TM \to TQ be the induced tangent map. Let

m

be a point on

M.

Since

M

is the cotangent bundle, we can understand

m

to be a map of the tangent space at

q=\pi(m)

:m : T_qQ \to \R.

That is, we have that

m

is in the fiber of

q.

The tautological one-form

\thetam

at point

m

is then defined to be\theta_m = m \circ \mathrm_m \pi.

It is a linear map\theta_m : T_mM \to \Rand so \theta : M \to T^*M.

Symplectic potential

The symplectic potential is generally defined a bit more freely, and also only defined locally: it is any one-form

\phi

such that

\omega=-d\phi

; in effect, symplectic potentials differ from the canonical 1-form by a closed form.

Properties

The tautological one-form is the unique one-form that "cancels" pullback. That is, let

\beta

be a 1-form on

Q.

\beta

is a section

\beta:Q\toT*Q.

For an arbitrary 1-form

\sigma

on

T*Q,

the pullback of

\sigma

by

\beta

is, by definition,

\beta*\sigma:=\sigma\circ\beta*.

Here,

\beta*:TQ\toTT*Q

is the pushforward of

\beta.

Like

\beta,

\beta*\sigma

is a 1-form on

Q.

The tautological one-form

\theta

is the only form with the property that

\beta*\theta=\beta,

for every 1-form

\beta

on

Q.

Proof.
For a chart

(\{qi\}

n
i=1

,U)

on

Q

(where

U\subseteq\Rn),

let
i\}
\{p
i,q
n
i=1
be the coordinates on

T*Q,

where the fiber coordinates
n
\{p
i=1
are associated with the linear basis

\{dqi\}

n
i=1

.

By assumption, for every

{q}=(q1,\ldots,qn)\inU,

\beta = \sum^n_ \beta_i(\mathbf)\,dq^i,or\mathbf=(q^1,\ldots,q^n)\ \stackrel\ (\underbrace_,\underbrace_)).It follows that\beta_*\left(\frac\Biggl
_\mathbf\right) =\frac \Biggl_+ \sum^n_\frac\Biggl_ \cdot \frac\Biggl_which implies that(\beta^*\,dq^i)\left(\right)_\mathbf=dq^i\left[\beta_*\left({\partial/\partial q^j}\right)_\mathbf{q}\right] =\delta_.

Step 1. We have\begin(\beta^*\theta)\left(\partial / \partial q^i\right)_\mathbf&= \theta\left(\beta_*\left(\partial/\partial q^i\right)_\mathbf\right) = \left(\sum^_p_jdq^j\right)\left(\beta_*\left(\partial/\partial q^i\right)_\mathbf\right) \\&= \beta_i(\mathbf) = \beta\left(\partial/\partial q^i\right)_\mathbf.\end

Step 1'. For completeness, we now give a coordinate-free proof that

\beta*\theta=\beta,

for any 1-form

\beta.

Observe that, intuitively speaking, for every

q\inQ

and

p\in

*
T
qQ,
the linear map

d\pi(q,p)

in the definition of

\theta

projects the tangent space

T(q,p)T*Q

onto its subspace

TqQ.

As a consequence, for every

q\inQ

and

v\inTqQ,

d\pi_(\beta_ v) = v,where

\beta*q

is the instance of

\beta*

at the point

q\inQ,

that is,\beta_ : T_qQ \to T_T^*Q.Applying the coordinate-free definition of

\theta

to

\theta\beta(q),

obtain(\beta^*\theta)_qv=\theta_(\beta_v) = \beta(q)(d\pi_(\beta_ v)) = \beta(q) v.

Step 2. It is enough to show that

\alpha=0

if

\beta*\alpha=0,

for every one-form

\beta.

Let\alpha = \sum^n_ \alpha_(\mathbf,\mathbf)\,dq^i + \sum^n_ \alpha_(\mathbf,\mathbf)\,dp_i,where
\alpha
pi
,\alpha
qi

\inCinfty(\Rn x U,\R).

Substituting

v=\left(\partial/\partialqi\right)q

into the identity

\alpha(\beta*v)=0

obtain\alpha(\partial / \partial q^i)_ + \sum^n_(\partial \beta_j / \partial q^i)_\cdot \alpha(\partial / \partial p_j)_ = 0,or equivalently, for any choice of

n

functions

pi=\betai(q),

\alpha_(\mathbf,\mathbf) + \sum^n_ \partial p_j / \partial q^i \cdot \alpha_(\mathbf,\mathbf) = 0.Let

\beta=

n
\sum
j=1
j,
c
jdq
where

cj=const.

In this case,

\betaj=cj.

For every

q\inU

and

cj\in\R,

\alpha_(\mathbf,\mathbf)\bigl
_^ = 0.This shows that
\alpha
qi

(p,q)=0

on

\Rn x U,

and the identity\sum^n_ \partial p_j / \partial q^i \cdot \alpha_(\mathbf,\mathbf) = 0must hold for an arbitrary choice of functions

pi=\betai(q).

If

\beta=

n
\sum
j=1
jdq
c
jq

j

(with

{}j

indicating superscript) then

\betaj=

j,
c
jq
and the identity becomes\alpha_(\mathbf,\mathbf)\bigl
_^ = 0,for every

q\inU

and

cj\in\R.

Since

cj=pj/qj,

we see that
\alpha
pi

(p,q)=0,

as long as

qj0

for all

j.

On the other hand, the function
\alpha
pi
is continuous, and hence
\alpha
pi

(p,q)=0

on

\Rn x U.

So, by the commutation between the pull-back and the exterior derivative,\beta^*\omega = -\beta^* \, d\theta = -d (\beta^*\theta) = -d\beta.

Action

If

H

is a Hamiltonian on the cotangent bundle and

XH

is its Hamiltonian vector field, then the corresponding action

S

is given byS = \theta(X_H).

In more prosaic terms, the Hamiltonian flow represents the classical trajectory of a mechanical system obeying the Hamilton-Jacobi equations of motion. The Hamiltonian flow is the integral of the Hamiltonian vector field, and so one writes, using traditional notation for action-angle variables:S(E) = \sum_i \oint p_i\,dq^iwith the integral understood to be taken over the manifold defined by holding the energy

E

constant:

H=E=const.

On Riemannian and Pseudo-Riemannian Manifolds

If the manifold

Q

has a Riemannian or pseudo-Riemannian metric

g,

then corresponding definitions can be made in terms of generalized coordinates. Specifically, if we take the metric to be a mapg : TQ \to T^*Q,then define\Theta = g^*\thetaand \Omega = -d\Theta = g^*\omega

In generalized coordinates

(q1,\ldots,q

n,q
1,\ldots,q

n)

on

TQ,

one has\Theta = \sum_ g_ \dot q^i dq^jand \Omega = \sum_ g_ \; dq^i \wedge d\dot q^j +\sum_ \frac \; \dot q^i\, dq^j \wedge dq^k

The metric allows one to define a unit-radius sphere in

T*Q.

The canonical one-form restricted to this sphere forms a contact structure; the contact structure may be used to generate the geodesic flow for this metric.

References