3.3 Complex Symmetry Properties

Figure 3.3b. Symmetry properties of an odd function, o(t).
Figure 3.3a. Symmetry properties of an even function, e(t).

The symmetry properties inherent in complex Fourier transform pairs are very useful in practical applications. Symmetry refers to the even and odd parts of s(t) or S(f) in the time or frequency domains, respectively. A function, e(t) has even symmetry if it is a mirror image (symmetric) about the zero axis, i.e., e(-t) = e(t); a function has odd symmetry if the reflection about zero has an opposite sign (antisymmetric) where o(-t) = -o(t). Even and odd symmetries are illustrated in Figure 3.3a and b, respectively.

An arbitrary function, s(t) can always be separated into odd and even parts. These parts are, in general, complex, which leads to several complex, symmetry combinations for the Fourier transform pairs as described by Bracewell (1965). We need not consider all of them because everything we deal with in applied geophysics is real in the time (or space) domain. Such signals transform into functions that have real, even parts and imaginary, odd parts in the frequency domain. Figure 3.4a shows these relations nicely using the visualization technique presented by Bracewell (1995) which allows both real and imaginary parts of a function to be plotted on one graph in either domain.


A function whose real part is even and imaginary part is odd, is called a Hermitian function irrespective of whether it’s in the time or frequency domain. Such a function in the frequency domain would have an amplitude spectrum that is even and a phase spectrum that is odd. Since a real function in the time (or space) domain generates a Hermitian function in the frequency domain, real geophysical signals, s(t) that are even have Fourier transforms that are real and even (Figure 3.4b). And, a signal, s(t) that’s real and odd has a Fourier transform that’s imaginary and odd (Figure 3.4c). Knowledge of these complex symmetries is very useful in practical applications of spectral analysis.

Figure 3.4a. Symmetry properties of Fourier transform pairs when a real signal, s(t) is arbitrary, neither even nor odd. The Fourier transforms are: Hermitian. Double-ended arrows indicate Fourier transform pairs.
Figure 3.4b. Symmetry properties of Fourier transform pairs when a real signal, s(t) is is an even function. The Fourier transforms are: real, even. Double-ended arrows indicate Fourier transform pairs.
Figure 3.4c. Symmetry properties of Fourier transform pairs when a real signal, s(t) is is an odd function. The Fourier transforms are: imaginary, odd; respectively. Double-ended arrows indicate Fourier transform pairs.

SAGE SAYS:

Knowledge of the Hermitian property of the Fourier transform of real geophysical signals tells us that the complex results at positive and negative values in the frequency domain are not independent. They have real, even and imaginary, odd symmetries.