5.3 Sampling Rate And Alias Signals
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Statutory Documents - IMO Publications and Documents - Circulars - Maritime Safety Committee - MSC/Circular.616 – Evaluation of Free-Fall Lifeboat Launch Performance – (22 June 1993) - Annex – Evaluation of Free-Fall Lifeboat Launch Performance - Section 5 – Measuring And Filtering Acceleration Forces - 5.3 Sampling Rate And Alias Signals

5.3 Sampling Rate And Alias Signals

  5.3.1 Any discussion of sampling rate and signal aliasing, must include a discussion of the frequency content of the signal being measured. In the case of free-fall lifeboats, the signal being measured is the acceleration force time-history. The acceleration force time-history, which is the variation of the acceleration force with time, can be decomposed into a combination of sine and cosine curves of varying amplitudes and frequencies. This concept is represented mathematically as:

The term h(t) is the amplitude of a resultant time-history at time t. The time-history is T seconds in duration. The quantities aj and bj are the amplitudes of the cosine and sine curves, respectively, associated with frequency f j. n different frequencies, and associated amplitudes, are included in the analysis.

  5.3.2 To obtain a more intuitive understanding of the significance of this equation, consider the curves presented in Figure 5.3. Shown on this figure are two sine curves and one cosine curve of different amplitudes and frequencies. The 2 hz and 20 hz signals are sine curves with amplitudes of 1.5 and 0.5, respectively. The 6 hz signal is a cosine curve with an amplitude of unity. The amplitude of the combined signal at any particular time is equal to the sum of the amplitudes of the three other curves at that same time. For this particular example, then, the amplitude of the combined signal at any time is:

When considering Equation 5.2, recall that the frequency in radians is equal to 2π times the frequency in Hertz.

Figure 5.3 A Signal that is a Combination of Three Sinusoids

  5.3.3 By using principles from calculus of complex variables, Equation 5.1 can be reduced to a form in which frequency and its associated amplitude are more readily apparent, namely:

where

The term Ai is the amplitude of the resultant sinusoid and θi is the phase angle. With the equation presented in this form, there is a single amplitude associated with each frequency. For the example presented in Figure 5.3, a plot of the frequency content versus amplitude is shown in Figure 5.4. The frequency content of the combined curve is 2, 6, and 20 hz .

Figure 5.4 Frequency Content of Example Problem

  5.3.4 Selection of a data sampling rate requires knowledge of the highest frequency that is of significance in the analysis to be performed as well as the magnitude of other frequencies with significant amplitudes present in the system being measured. Let us first deal with the highest frequency that is important in the analysis. If the sampling rate is not rapid enough an aliased signal (a false signal) such as that shown in Figure 5.5 will be returned. In Figure 5.5 the actual signal is a sine curve with an amplitude of 1.5 and a frequency of 15 hz. This sine curve was "sampled" every 60 milliseconds; these data points are indicated by the solid boxes. By sampling at this slow rate, an apparent signal with a frequency of 1 ⅔ hz and an amplitude of 1.5 was obtained. The apparent signal is significantly different than the actual signal and as such is probably of very little value. In this particular case, the actual signal increases in an opposite direction from the apparent signal. Starting at time t=0, the actual signal initially increases positively whereas the apparent signal initially increases negatively.

Figure 5.5 Apparent Signal from a Signal that Was Sampled at too Slow a Rate

  5.3.5 Clearly, the sampling rate must be rapid enough to properly describe a signal oscillating at the highest important frequency. Although the general shape of a sinusoid can be described with as few as two data points, more data points provide a more reliable description of the shape. As shown in Figure 5.6, four data points provide a reasonable description of the shape of a sine (or cosine) curve. More data points will describe the curve better but five points generally provide an adequate description. A good “rule of thumb" often used in experimental measurement is that a signal should be sampled at a rate which will enable a sinusoid with a frequency five times greater than that of importance to be adequately described. As such, the minimum sampling rate is generally 20 times the highest important frequency. If, for example, 20 hz is the highest frequency to be considered, the data should be sampled 400 times per second (4 samples per cycle times 20 cycles per second times 5).

Figure 5.6 Minimum Number of Data Points Required to Describe a Sinusoid

  5.3.6 One problem does however, arise in experimental measurement of mechanical or structural systems. Very often high frequency vibration is present. In free-fall lifeboat systems, such vibration occurrs when the lifeboat slides along the launch ramp and again when it impacts the water. If the amplitude of the vibration is significant, the sampled signal can be an alias of the true signal (small amplitude, high frequency vibration is not a concern). An alias signal can be observed in Figure 5.7. In this example, the important frequency is 2 hz with an amplitude of 2.0. This is the "true' signal" shown on the figure. There was 15 hz unoise" with an amplitude of 1.5 that was superimposed over the true signal. The resulting signal is the actual signal shown on Figure 5.1; the actual signal is that which will be measured even though it contains the unwanted high frequency data. If the actual signal is sampled enough (about 20 times the highest frequency) the unwanted frequencies can be later removed through filtering. If, however, the signal is not sampled rapidly enough to properly describe these high frequencies, the data will be aliased, the high frequency data is falsely translated into the low frequency data. The apparent curve in Figure 5.7 was obtained by sampling the data at 16 ⅔ hz; such a rate is adequate for the true signal but is not adequate for the high frequency noise. As such, the apparent signal resembles the true signal but the amplitude is different; the apparent signal is erroneous and may lead to improper conclusions about the behavior of the system. A signal should therefore be sampled at a rate quick enough to describe large amplitude, high frequency vibration that may be present. After a signal has been sampled, there is little that can be done to remove the aliased power (Press, et. al., 1988). If this results in an excessively high sampling rate, anti-aliasing filters can be used to limit high frequencies in the signal before it is sampled.

Figure 5.7 An Alias of a True Signal

  5.3.7 Experience with free-fall lifeboats has indicated that sampling rates in the order of 600–800 hz are adequate to provide a reliable acceleration force time-histories that has negligible aliasing. Such rates have been used on both GRP and aluminum boats with free-fall heights as high as 30 meters. Care should be taken, however, to properly mount the accelerometers on rigid parts of the boat. If the accelerometers were placed in the middle of a large flat panel, for instance, this sampling is probably not rapid enough.


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