Presentation is loading. Please wait.

Presentation is loading. Please wait.

Vibrationdata 1 Unit 6a The Fourier Transform. Vibrationdata 2 Courtesy of Professor Alan M. Nathan, University of Illinois at Urbana-Champaign.

Similar presentations


Presentation on theme: "Vibrationdata 1 Unit 6a The Fourier Transform. Vibrationdata 2 Courtesy of Professor Alan M. Nathan, University of Illinois at Urbana-Champaign."— Presentation transcript:

1 Vibrationdata 1 Unit 6a The Fourier Transform

2 Vibrationdata 2 Courtesy of Professor Alan M. Nathan, University of Illinois at Urbana-Champaign

3 Vibrationdata 3 Unit 6a Many, many different equations for Fourier Transforms.......... 1. Mathematician Approach 2. Engineering Approach Even within each approach there are many equations.

4 Vibrationdata 4 Continuum of Signals Stationary vibration signals can be placed along a continuum in terms of the their qualitative characteristics. A pure sine oscillation is at one end of the continuum. A form of broadband random vibration called white noise is at the other end. Reasonable examples of each extreme occur in the physical world. Most signals, however, are somewhere in the middle of the continuum.

5 Vibrationdata 5 Frequency Example

6 Vibrationdata 6 Resolving Spectral Components The time history appears to be the sum of several sine functions. What are the frequencies and amplitudes of the components? Resolving this question is the goal of this Unit.

7 Vibrationdata 7 Equation of Previous Signal At the risk of short-circuiting the process, the equation of the signal in Figure 1 is The signal thus consists of three components with frequencies of 10, 16, and 22 Hz, respectively. The respective amplitudes are 1.0, 1.5, and 1.2 G. In addition, each component could have had a phase angle. In this example, the phase angle was zero for each component. Thus, we seek some sort of "spectral function" to display the frequency and amplitude data. Ideally, the spectral function would have the form shown in the next figure.

8 Vibrationdata 8

9 Vibrationdata 9 Textbook Fourier Transform The Fourier transform X(f) for a continuous time series x(t) is defined as where -  < f <  The Fourier transform is continuous over an infinite frequency range. Note that X(f) has dimensions of [amplitude-time].

10 Vibrationdata 10 Textbook Inverse Fourier Transform The inverse transform is Thus, a time history can be calculated from a Fourier transform and vice versa.

11 Vibrationdata 11 Magnitude and Phase Note that X(f) is a complex function. It may be represented in terms of real and imaginary components, or in terms of magnitude and phase. The conversion to magnitude and phase is made as follows for a complex variable V.

12 Vibrationdata 12 Real Time History Practial time histories are real. Note that the inverse Fourier transform calculates the original time history in a complex form. The inverse Fourier transform will be entirely real if the original time history was real, however.

13 Vibrationdata 13 Fourier Transform of a Sine Function The transform of a sine function is purely imaginary. The real component, which is zero, is not plotted.

14 Vibrationdata 14 Characteristics of the Continuous Fourier Transform 1. The real Fourier transform is symmetric about the f = 0 line. 2. The imaginary Fourier transform is antisymmetric about the f = 0 line.

15 Vibrationdata 15 Characteristics of the Continuous Fourier Transform This Unit so far has presented Fourier transforms from a mathematics point of view. A more practical approach is needed for engineers ………

16 Vibrationdata 16 Discrete Fourier Transform n An accelerometer returns an analog signal. n The analog signal could be displayed in a continuous form on a traditional oscilloscope. n Current practice, however, is to digitize the signal, which allows for post- processing on a digital computer. n Thus, the Fourier transform equation must be modified to accommodate digital data. n This is essentially the dividing line between mathematicians and engineers in regard Fourier transformation methodology.

17 Vibrationdata 17 Discrete Fourier Transform Equations The Fourier transform is The corresponding inverse transform is

18 Vibrationdata 18 Discrete Fourier Transform Relations Note that the frequency increment  f is equal to the time domain period T as follows The frequency is obtained from the index parameter k as follows where k is the frequency domain index  t is the time step between adjacent points

19 Vibrationdata 19 Nyquist Frequency The Nyquist frequency is equal to one-half of the sampling rate. Shannon’s sampling theorem states that a sampled time signal must not contain components at frequencies above the Nyquist frequency. Otherwise an aliasing error occurs.

20 Vibrationdata 20 Half Amplitude Discrete This is the imaginary component of the transform. The real component is zero.

21 Vibrationdata 21 Previous Fourier Transform Plot Note that the sine wave has a frequency of 1 Hz. The total number of cycles is 512, with a resulting period of 512 seconds. Again, the Fourier transform of a sine wave is imaginary and antisymmetric. The real component, which is zero, is not plotted.

22 Vibrationdata 22 Spectrum Analyzer Approach Spectrum analyzer devices typically represent the Fourier transform in terms of magnitude and phase rather than real and imaginary components. Furthermore, spectrum analyzers typically only show one-half the total frequency band due to the symmetry relationship. The spectrum analyzer amplitude may either represent the half-amplitude or the full-amplitude of the spectral components. Care must be taken to understand the particular convention of the spectrum analyzer. Note that the half-amplitude convention has been represented in the equations thus far.

23 Vibrationdata 23 Full Amplitude Fourier Transform The full-amplitude Fourier transform magnitude would be calculated as

24 Vibrationdata 24 Full Amplitude Fourier Transform Note that k = 0 is a special case. The Fourier transform at this frequency is already at full-amplitude. For example, a sine wave with an amplitude of 1 G and a frequency of 1 Hz would simply have a full-amplitude Fourier magnitude of 1 G at 1 Hz, as shown in the next figure.

25 Vibrationdata 25

26 Vibrationdata 26 Full Amplitude Fourier Transform Time History Example

27 Vibrationdata 27 Full Amplitude One-Sided

28 Vibrationdata 28 Unit 6a Exercise 1 Convert the following complex number into magnitude and phase: x = 5 + j 9 Use program EngMath.exe

29 Vibrationdata 29 Unit 6a Exercise 2 A time history has a duration of 20 seconds. What is the frequency resolution of the Fourier transform?

30 Vibrationdata 30 Unit 6a Exercise 3 Recall file white.out from Unit 5. Take the Fourier transform using program fourier.exe. Plot both the FT_half.out and Ft_full.out files. How does the amplitude vary with frequency?

31 Vibrationdata 31 Unit 6a Exercise 4 Plot the half-sine time history hs.txt. Then take the Fourier transform. How does the amplitude vary with frequency?

32 Vibrationdata 32 Unit 6a Exercise 5 1. Generate white noise time history using generate.exe Std dev = 7 0 to 20 sec Sample rate = 500 10000 samples Output filename = seven.dat 2. Take Fourier transform. Call ft_full.out into EasyPlot (continued on next page)

33 Vibrationdata 33 Unit 6a Exercise 5 (continued) Call ft_full.out into Excel 1. Multiply each spectral magnitude by 0.707 to convert from peak to RMS. 2. Square each spectral RMS value to convert to mean square. 3. Sum the mean square values. 4. Take the square root of the sum. 5. The result is the standard deviation from the frequency domain. 6. Take the standard deviation of seven.dat in the time domain. The standard deviation from the time domain should be the same as that from the frequency domain


Download ppt "Vibrationdata 1 Unit 6a The Fourier Transform. Vibrationdata 2 Courtesy of Professor Alan M. Nathan, University of Illinois at Urbana-Champaign."

Similar presentations


Ads by Google