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Bilateral Z-transform

Geophysical definition | Inverse Z-transform | Region of convergence | Examples conclusion | Properties | Relationship to Laplace transform | Process of sampling | Relationship to Fourier transform | Linear constant-coefficient difference equation | Zeros and poles |


Читайте также:
  1. Inverse Z-transform
  2. Unilateral Z-transform

History

The basic idea now known as the Z-transform was known to Laplace, and re-introduced in 1947 by W. Hurewicz as a tractable way to solve linear, constant-coefficient difference equations.[1] It was later dubbed "the z-transform" by Ragazzini and Zadeh in the sampled-data control group at Columbia University in 1952.[2][3]

The modified or advanced Z-transform was later developed and popularized by E. I. Jury.[4][5]

The idea contained within the Z-transform is also known in mathematical literature as the method of generating functions which can be traced back as early as 1730 when it was introduced by de Moivre in conjunction with probability theory.[6] From a mathematical view the Z-transform can also be viewed as a Laurent series where one views the sequence of numbers under consideration as the (Laurent) expansion of an analytic function.

Definition

The Z-transform, like many integral transforms, can be defined as either a one-sided or two-sided transform.

Bilateral Z-transform

The bilateral or two-sided Z-transform of a discrete-time signal x[n] is the formal power series X(z) defined as

where n is an integer and z is, in general, a complex number:

where A is the magnitude of z, j is the imaginary unit, and is the complex argument (also referred to as angle or phase) in radians.


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