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540 ⏐⏐⏐ SINUSOIDAL ALTERNATING WAVEFORMS<br />

Height<br />

Height<br />

Sand<br />

Distance<br />

(a)<br />

Average height<br />

Sand<br />

Same<br />

distance<br />

(b)<br />

FIG. 13.34<br />

Effect of distance (length) on average value.<br />

Height<br />

Sand<br />

Height<br />

Distance<br />

(a)<br />

Average height<br />

Sand<br />

Same<br />

distance<br />

(b)<br />

Ground level<br />

FIG. 13.35<br />

Effect of depressions (negative excursions) on<br />

average value.<br />

If the distance parameter includes a depression, as shown in Fig.<br />

13.35(a), some of the sand will be used to fill the depression, resulting<br />

in an even lower average value for the landscaper, as shown in Fig.<br />

13.35(b). For a sinusoidal waveform, the depression would have the<br />

same shape as the mound of sand (over one full cycle), resulting in an<br />

average value at ground level (or zero volts for a sinusoidal voltage over<br />

one full period).<br />

After traveling a considerable distance by car, some drivers like to<br />

calculate their average speed for the entire trip. This is usually done by<br />

dividing the miles traveled by the hours required to drive that distance.<br />

For example, if a person traveled 225 mi in 5 h, the average speed was<br />

225 mi/5 h, or 45 mi/h. This same distance may have been traveled at<br />

various speeds for various intervals of time, as shown in Fig. 13.36.<br />

By finding the total area under the curve for the 5 h and then dividing<br />

the area by 5 h (the total time for the trip), we obtain the same result<br />

of 45 mi/h; that is,<br />

area under curve<br />

Average speed � �� (13.25)<br />

length of curve<br />

A1 � A2 Average speed ��<br />

5 h<br />

(60 mi/h)(2 h) � (50 mi/h)(2.5 h)<br />

�����<br />

5 h<br />

225<br />

� � mi/h<br />

5<br />

� 45 mi/h<br />

Equation (13.25) can be extended to include any variable quantity, such<br />

as current or voltage, if we let G denote the average value, as follows:<br />

algebraic sum of areas<br />

G (average value) � ��� (13.26)<br />

length of curve<br />

Speed (mi/h)<br />

70<br />

60<br />

50<br />

40<br />

30<br />

20<br />

10<br />

A1 A2 Average speed<br />

0 1 2 3<br />

Lunch break<br />

4 5 6 t (h)<br />

FIG. 13.36<br />

Plotting speed versus time for an automobile excursion.<br />

The algebraic sum of the areas must be determined, since some area<br />

contributions will be from below the horizontal axis. Areas above the<br />

axis will be assigned a positive sign, and those below, a negative sign.<br />

A positive average value will then be above the axis, and a negative<br />

value, below.<br />

The average value of any current or voltage is the value indicated on<br />

a dc meter. In other words, over a complete cycle, the average value is

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