Classical Local Fields and Actions
A local field equation is only part of a classical field theory. The action, admissible configurations, boundary data, and initial-value formulation must fit together. This chapter develops that package for the free models used in quantization.
Enter this chapter
Section titled “Enter this chapter”Begin with Fields, Configurations, Dimensions, and Local Dynamics to identify the variables and scales. If varying an action is already familiar, start with the boundary page to check which variations are actually allowed.
Topics
Section titled “Topics”- Fields, Configurations, Dimensions, and Local Dynamics — Specifies the fields, parameters, dimensions, and local ingredients of a model.
- The Action Principle and Field Equations — Derives Euler–Lagrange equations from stationary action.
- Boundaries, Variations, and Well-Posed Actions — Determines whether the surface variation is compatible with the prescribed data.
- Hamiltonian Initial Data and Phase Space — Tests the Legendre map and identifies canonical variables or constraints.
- Classical Symmetries, Currents, and Stress Tensors — Relates concrete continuous symmetries to currents and energy–momentum.
How the ideas fit together
Section titled “How the ideas fit together”Integration by parts produces both the field equations and a boundary contribution. The equations hold for interior variations; the surface term decides which boundary conditions or additional boundary action make the full problem stationary. A boundary term can leave the bulk equations unchanged while changing the variational problem and its charges. See Harlow and Wu 2020, § 2.
The Hamiltonian construction asks a different question: can velocities be recovered from momenta? If the velocity Hessian is singular, the momenta obey constraints. Writing a formal Hamiltonian does not eliminate that singularity, and quantization must retain the resulting restrictions.
Review the chapter
Section titled “Review the chapter”For the free scalar density , what links the action and initial-data descriptions?
Solution
Varying with compatible boundary data gives . On a constant-time slice, and the Hamiltonian density is . Hamilton’s equations reproduce the same wave equation; the positive kinetic Hessian makes the Legendre map invertible.
Where to go next
Section titled “Where to go next”Continue to Canonical Quantization and the Free Scalar to turn this phase-space example into an operator algebra and vacuum representation.