We establish a rigorous, constructive two way equivalence between classical explicit analytic solutions of differential equations (satisfying the Cauchy Kovalevskaya conditions) and the solutions represented by a single unified series derived from the differential algebraic closure. The same equivalence is proved for integral equations (Fredholm, Volterra, nonlinear Hammerstein, singular, stochastic, fractional, exterior, and total integral equations) and the corresponding integral algebraic closure. Moreover, we extend this framework to variational equations (Euler Lagrange equations of analytic functionals, including higher order, fractional, exterior, stochastic, and total variation problems) and inverse variational equations (the problem of reconstructing a functional from a given equation or from a family of solutions). We show that any analytic function that belongs to any of these closures automatically belongs to the others, and that every such function can be expanded in a universal series of the form u (x) = u0 (x) +Φm (c, x) 1/pm ωkmm∈Ipm ψm (x), where ψmm∈I is a complete analytic basis of the linearised operator (differential, integral, or second variation), Φm are elements of the closure built from explicit combinatorial coefficients (Stirling numbers for ODEs, multi index Beta functions for PDEs, sign factors for exterior differential equations, Wiener Poisson chaos coefficients for SDEs, Gamma ratios for fractional integrals, Gaunt coefficients for Legendre expansions, Hilbert matrix entries for Chebyshev bases, chaos contraction coefficients for stochastic integrals, and structure constants for exterior and variational problems). The series converges uniformly on compact sets (or in L2 for stochastic cases, or in L1 for BV limits). The forward direction proves that every analytic (or generalised) solution can be expanded in this unified series; the backward direction shows that any function represented by such a series satisfies a nonzero differential, integral, or variational polynomial that is equivalent (up to a constant factor) to the original equation. Consequently, every classical special function (over 150 examples), every physical equation (over 80 examples), and every Euler–Lagrange equation arising from analytic functionals (including higher order, fractional, exterior, stochastic, and total variation) admits this unified representation.
Liu S (Wed,) studied this question.