For asymptotically Cartesian spatial metrics , unit asymptotic lapse and vanishing asymptotic shift, the curvature term in the bulk gravitational Hamiltonian has variation
The surface variation is finite under the usual differentiable asymptotic falloff and is not removed by simply taking the boundary to infinity. Adding Arnowitt-Deser-Misner energy cancels it and makes Hamilton's equations well defined for allowed variations that need not fix the energy. On the constraint surface, the total Hamiltonian for that time translation equals the boundary energy.
Along Hamilton's equations, spatial derivatives of the Hamiltonian function cancel in its total time derivative. Thus . An autonomous Hamiltonian function is conserved; explicit time dependence generally prevents conservation even though phase space is still preserved.
Transport a phase-space density along Hamilton's equations. The Hamiltonian vector field is and the equation is . Its zero divergence gives volume-preserving transport. For , the density is constant along characteristics; a source is integrated by the Duhamel formula for Hamiltonian transport. This is distinct from the elliptic Liouville equation.
Hyperregular Lagrangian 2026-10-06
A Lagrangian is hyperregular when its fiber derivative, sending a velocity to its conjugate momentum, is a global diffeomorphism from the tangent bundle to the cotangent bundle. This gives a globally defined Legendre transform in mechanics and a global equivalence between the Euler-Lagrange equations and Hamilton's equations. With time dependence this requirement is imposed at each time, with a smooth inverse depending on time.
The Arnold-Liouville theorem concerns a connected compact component of a regular common level of commuting independent smooth functions on a -dimensional symplectic manifold. It states that is a Lagrangian torus, and that a neighbourhood of has action-angle variables
in which every depends only on . If or, more generally, , its Hamiltonian flow satisfies
Angles have period here. The theorem is local near this regular compact component; it does not assert globally defined action-angle variables across singular levels or over an entire base with monodromy.
First, has dimension of a manifold by the submersion theorem. The Hamiltonian vector fields are independent, tangent to , and commute. They span . Moreover
so is a Lagrangian submanifold. Compactness makes these restricted vector fields complete. Their joint flow is an -action on . Its orbits are open because the fields span , so connectedness gives one orbit. The stabilizer of a point is discrete by the inverse function theorem, and
Compactness forces to be a full-rank Euclidean lattice: otherwise an unbounded linear coordinate transverse to its span would descend to the quotient. Thus is an -torus.
Next choose a small ball of regular values near and a neighbourhood of this component which is a product family of compact tori . This local trivialization follows directly by choosing transverse vector fields with and lifting short radial paths in the base; compactness of gives a uniform neighbourhood where their flows exist. Hence deformation retracts onto . The commuting joint flows on nearby fibres have smoothly varying full-rank Hamiltonian period lattices. A basis of their periods can be chosen smoothly on this small ball: continue the return equations from a basis at the central fibre, using their nonsingular vertical flow derivatives and the implicit function theorem. No global choice of lattice basis is needed.
Because and retracts onto , its closed symplectic form is exact on . Choose a one-form with . Let be the smoothly continued cycles represented by the period basis and define the action integrals
For a transverse variation of the fibre, differentiating a cycle integral and using Cartan's magic formula eliminates the integral of the exact term. With the cycle parametrized by the joint-flow time , this gives
Thus
The period matrix is nonsingular, so gives coordinates on the base. The corresponding Hamiltonian vector fields satisfy
Their time- flows return along the basis cycles. They commute because each is a function of the commuting . Consequently they give a free torus action on .
Choose a section over the action-coordinate ball and use this torus action to define angles . Since , the symplectic form takes the form
The closed base two-form is exact on the ball: write , , by the Poincare lemma. Changing the angular origins by removes this term, since . This completes the construction of action-angle variables. The functions are constant on the fibres, so are functions of alone, and Hamilton's equations give the claimed straight-line motion. This proves both the topological and symplectic parts of the Arnold-Liouville theorem.
Take canonical coordinates and . The Hamiltonian system is
In the standard Hamilton's equations and , its Hamiltonian is
An arbitrary function of can be added without affecting the characteristic curves. The Hamiltonian generally depends on time through and need not be conserved along a trajectory.
Let be the cotangent bundle projection. Its canonical one-form on a cotangent bundle is defined intrinsically by , so locally . Choose the position-first symplectic form
It is closed by and nondegenerate, since contraction with is , which vanishes only when both coefficient sets vanish. The intrinsic definition of makes this symplectic form independent of coordinates.
Use the convention . Then the Hamiltonian vector field and the Poisson bracket are
so . Choosing and gives the same equations; choosing only one of these sign changes would reverse the flow.
For the geodesic Hamiltonian, Hamilton's equations give
Put , so . Differentiating gives
Consequently,
Symmetrizing the velocity factors and raising the first index converts this to
These Christoffel symbols are those of the Levi-Civita connection. Thus a Hamiltonian integral curve of a vector field projects to an affinely parametrized geodesic. Conversely, an affinely parametrized geodesic lifts by to an integral curve of a vector field of , since reversing the calculation proves both Hamilton's equations. This is the geodesic flow on the cotangent bundle. The conserved Hamiltonian is half the squared speed, and the zero-energy case gives the constant geodesics.
A quadratic homogeneous polynomial depends only on the symmetric part of its coefficient matrix. Accordingly take its unique symmetric coefficients of a quadratic polynomial, . This is the standard implicit convention in identifying such polynomials with symmetric tensors. If an arbitrary nonsymmetric representative were allowed, the literal equivalence would fail: in Euclidean , , and all other components zero give the zero polynomial, which has zero Poisson bracket with every function, whereas the lowered coefficient array is not a Killing tensor because it is not symmetric.
Lower the indices of the symmetric coefficient tensor using the Riemannian metric. Since ,
Along an affinely parametrized geodesic, metric compatibility and imply
Here parentheses mean normalized symmetrization over all indicated indices. The left side is by the Hamiltonian vector field convention. Therefore a rank-two Killing tensor, defined by symmetry and , gives a quadratic geodesic first integral.
Conversely, if everywhere on , the last cubic expression vanishes for every at every point, because the Riemannian metric identifies tangent and cotangent spaces invertibly. A symmetric trilinear form is determined by its diagonal cubic polynomial: equivalently, compare its coefficients, or polarize the cubic. Hence . This proves both directions:
with symmetry understood on the coefficient representative from the outset. The equivalence is local and does not require geodesic completeness.
For the final construction, the antisymmetric differential two-form is a Killing-Yano two-form. Its defining equation says . Antisymmetry of also says , so the three-index tensor is totally antisymmetric.
The proposed tensor is symmetric, since it is the inner product of the covectors and :
There is a useful geometric proof of its Killing tensor equation. Along any affinely parametrized geodesic, define . Then
The first term vanishes by antisymmetry in , and the second by the geodesic equation. Thus is carried by parallel transport. By metric compatibility, its squared norm is constant, and
Every tangent vector is the initial velocity of a local geodesic, so differentiation at the initial point gives for every . The same cubic-coefficient argument proves
This proves that the square of a Killing-Yano two-form is a rank-two Killing tensor and supplies a nonnegative quadratic geodesic first integral. The argument also explains the conserved quantity: it is the squared norm of a covector that the Killing-Yano two-form makes parallel along every geodesic.