“…In such cases, the expression (2) for I is easily generalized by the usual replacements x →x, dx → dx in the integrand for a vector x = x 1 , ..., x N of data fluctuations. Furthermore, the integrand (dq/dx) 2 is replaced [6,12] by the sum n (∇q n ) 2 , where ∇ is the gradient operator, for a system that can be in many different states n = 1, ..., N . Finally, as defined in Equation (12), in terms of complex amplitudes ψ n , n = 1, ..., N , the information becomes I = 4N dx n ∇ψ * n · ∇ψ n in problems where the x-space is continuous.…”