Finite type system (PDEs)

Definition

A system of PDEs, viewed as a submanifold of the jet bundle EJk, is of finite type if its Vessiot distribution V on E has rank exactly n (the number of independent variables) and is involutive (Frobenius integrable).

Equivalently: the vector fields v1,,vn spanning V satisfy

[vi,vj]=0(modulo V).

Consequence

A finite type system has a finite-dimensional solution space: solutions are determined by a finite set of constants (initial data at a point), rather than by arbitrary functions.

Sketch of why

Why rank >n means arbitrary functions.
If dim(V)>n, at each point pE one must choose which n-plane inside V(p) to continue along. This choice is made continuously at every point of the domain — that is exactly what a function is. Each extra dimension of V above n contributes one arbitrary function to the general solution.

What rank =n with involutivity buys.
When dim(V)=n and V is involutive, there is no choice at each point: the n-plane is uniquely determined by V(p) itself. The Frobenius theorem then guarantees that through each point pE there passes a unique integral manifold.

Why that means finite-dimensional.
Fix a base point x0 in the domain. A solution through x0 is determined by specifying where in the fiber Ex0 one starts — i.e., the values of u and its derivatives up to order k at x0. That fiber has dimension dim(E)n, which is finite. Once the starting point is fixed, Frobenius uniquely propagates the integral manifold everywhere.

Summary. Involutivity kills the pointwise freedom of choosing directions; Frobenius turns the unique distribution into a unique leaf; and a leaf is pinned by finitely many numbers (its starting point in the fiber Ex0).

Context

Most PDE systems are not of finite type — their Vessiot distribution has rank >n and the general solution depends on arbitrary functions. The differential constraint method is one systematic way to produce finite type systems: by appending compatible constraints one shrinks E until dim(V)=n, and finite type is the condition that guarantees a solution submanifold actually exists.