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Zeros and poles

Bilateral Z-transform | Unilateral Z-transform | Geophysical definition | Inverse Z-transform | Region of convergence | Examples conclusion | Properties | Relationship to Laplace transform | Process of sampling | Relationship to Fourier transform |


From the fundamental theorem of algebra the numerator has M roots (corresponding to zeros of H) and the denominator has N roots (corresponding to poles). Rewriting the transfer function in terms of poles and zeros

where is the zero and is the pole. The zeros and poles are commonly complex and when plotted on the complex plane (z-plane) it is called the pole-zero plot.

In addition, there may also exist zeros and poles at and . If we take these poles and zeros as well as multiple-order zeros and poles into consideration, the number of zeros and poles are always equal.

By factoring the denominator, partial fraction decomposition can be used, which can then be transformed back to the time domain. Doing so would result in the impulse response and the linear constant coefficient difference equation of the system.


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Linear constant-coefficient difference equation| Output response

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