Practical_Antenna_Handbook_0071639586

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C h a p t e r 2 : r a d i o - W a v e P r o p a g a t i o n 11 A. Wave amplitude at point A versus time t. A 1 s t make the analogy to radio waves more realistic, the wave must be generated in a continuous fashion, as shown in Fig. 2.2A: A ball is dipped up and down at a cyclic rate, successively reinforcing new wave crests on each dip. New waves continue to be generated at point A as long as the ball continues to oscillate up and down. The result is a continuous wave train spreading out through the water. Perhaps the most important point to note about the water-wave analogy is that careful observation of individual water molecules (if that were possible) a small distance from the ball would show little or no net horizontal movement or displacement of any specific molecule sideways across the surface of the water. Nonetheless, a clearly visible wavefront travels outward from the point where the ball was dropped. Similarly, the motion of a radio wave does not require that electrons travel with it. To the contrary, we shall see in our discussion of basic antennas that maximum radiation occurs at right angles to the direction of travel of electrons along a wire antenna! There are two fundamental properties of all waves that are important to our study of radio waves: frequency (f) and wavelength (l).The frequency is the number of oscillations (or cycles) in the wave’s amplitude per unit of time. Since the fundamental unit of time is universally accepted to be the second, frequency is often expressed as the number of cycles per second (cps). If the time between successive positive peaks at any single point in space is 0.5 s, as suggested by Fig. 2.2A, exactly two complete amplitude cycles of the wave occur in 1 s, so the frequency of the wave created by the oscillating ball is 2 cps. Note that we can make the measurement from consecutive observable points elsewhere on the waveform, such as negative peaks, zero crossings, etc. At one time, frequencies (along with the frequencies of other electrical, mechanical, and acoustical waves) were expressed in cycles per second but, in honor of Heinrich Hertz, the unit of frequency was renamed the hertz (Hz) many years ago. Since the units are equivalent (1 Hz = 1 cps), the wave in Fig. 2.2 has a frequency of 2 Hz. Because the frequencies best suited for efficient radio propagation are so high, they are usually expressed in kilohertz (kHz = 1000s of Hz), megahertz (MHz = 1,000,000s of Hz), or gigahertz (GHz = 1,000,000,000s of Hz). Thus, the frequency of WBZ in Boston, operating near the mid- B. Wave amplitude at time t versus distance. A B d Figure 2.2 A bobbing ball on a string demonstrates continuous wave generation. (A) Wave amplitude at point A versus time t. (B) Wave amplitude at time t versus distance d.

12 p a r t I I : F u n d a m e n t a l s dle of the AM broadcasting band, can be properly expressed as 1,030,000 Hz, 1030 kHz, or 1.03 MHz, all of which are equivalent and equally correct. While radio receiver tuning dials in North America are usually calibrated in kilohertz or megahertz, in Europe and the rest of the world it is not uncommon to find radio dials calibrated in meters, the universal unit of wavelength, as well as in frequency. In radio work, wavelength is expressed in meters or its subunits, such as when talking about millimeter waves. The wavelength of any wave is the physical distance between adjacent corresponding points of a spatial waveform, measured at the exact same time. In Fig. 2.2B the wavelength (l) is drawn as the distance between successive negative peaks in any direction from the source, but we could also measure the wavelength from the distance between successive positive peaks, or between any two corresponding features on successive waves as we move outward from the source in a straight line. Wavelength is proportional to the reciprocal of the frequency. The relationship is given by fl = v, where f is the frequency in Hz, l is the wavelength in meters, and v is the velocity of propagation in meters per second (m/s). In each case, v depends on certain characteristics of the medium (water, air, etc.). In water at room temperature, the velocity of a sound wave is typically 1482 m/s, or about 4861 ft/s—just a bit less than a mile per second. In air, however, sound waves travel at about 343 m/s, or 1125 ft/s. In contrast, radio waves in free space propagate at the speed of light—approximately 300,000,000 m/s (or 186,000 mi/s) in free space and almost exactly the same in the earth’s atmosphere. For historical reasons, the lowercase letter c is usually used to represent the speed of light. Thus: c 300,000,000 f = = λ λ (2.1) where f is in hertz (Hz), l is in meters (m), and c is in meters per second (m/s). For convenience, these equations are often recast with frequency in kilohertz or megahertz: 300,000 f (kHz) = (2.2) λ f (MHz) = 300 (2.3) l Thus, a wavelength of 300 m corresponds to a frequency of 1 MHz (the middle of the AM broadcast band), while a wavelength of 10 m corresponds to 30 MHz (just above what we call the amateur 10-m band, which lies between 28.0 and 29.7 MHz). Note When a wave of any type—be it a mechanical wave, sound wave, or radio wave—passes from one linear medium to another, only its wavelength changes, not its frequency. Thus, a radio signal having a wavelength of 40 m in free space may have a wavelength of, say, only 30 m in one of the solid-dielectric transmission lines discussed in Chap. 4. A 1-kHz tone in the air will still be a 1-kHz tone in water. The place where the water-wave analogy falls down most profoundly is in the implied need for a medium of propagation. Water waves propagate by actually moving

C h a p t e r 2 : r a d i o - W a v e P r o p a g a t i o n 11<br />

A. Wave amplitude<br />

at point A versus time t.<br />

A<br />

1 s<br />

t<br />

make the analogy to radio waves more realistic, the wave must be generated in a continuous<br />

fashion, as shown in Fig. 2.2A: A ball is dipped up and down at a cyclic rate,<br />

successively reinforcing new wave crests on each dip. New waves continue to be generated<br />

at point A as long as the ball continues to oscillate up and down. The result is a<br />

continuous wave train spreading out through the water.<br />

Perhaps the most important point to note about the water-wave analogy is that<br />

careful observation of individual water molecules (if that were possible) a small distance<br />

from the ball would show little or no net horizontal movement or displacement of<br />

any specific molecule sideways across the surface of the water. Nonetheless, a clearly<br />

visible wavefront travels outward from the point where the ball was dropped. Similarly,<br />

the motion of a radio wave does not require that electrons travel with it. To the<br />

contrary, we shall see in our discussion of basic antennas that maximum radiation occurs<br />

at right angles to the direction of travel of electrons along a wire antenna!<br />

There are two fundamental properties of all waves that are important to our study<br />

of radio waves: frequency (f) and wavelength (l).The frequency is the number of oscillations<br />

(or cycles) in the wave’s amplitude per unit of time. Since the fundamental unit of<br />

time is universally accepted to be the second, frequency is often expressed as the number<br />

of cycles per second (cps). If the time between successive positive peaks at any single<br />

point in space is 0.5 s, as suggested by Fig. 2.2A, exactly two complete amplitude cycles<br />

of the wave occur in 1 s, so the frequency of the wave created by the oscillating ball is<br />

2 cps. Note that we can make the measurement from consecutive observable points<br />

elsewhere on the waveform, such as negative peaks, zero crossings, etc.<br />

At one time, frequencies (along with the frequencies of other electrical, mechanical,<br />

and acoustical waves) were expressed<br />

in cycles per second<br />

but, in honor of Heinrich Hertz,<br />

the unit of frequency was renamed<br />

the hertz (Hz) many<br />

years ago. Since the units are<br />

equivalent (1 Hz = 1 cps), the<br />

wave in Fig. 2.2 has a frequency<br />

of 2 Hz.<br />

Because the frequencies best<br />

suited for efficient radio propagation<br />

are so high, they are usually<br />

expressed in kilohertz (kHz<br />

= 1000s of Hz), megahertz (MHz<br />

= 1,000,000s of Hz), or gigahertz<br />

(GHz = 1,000,000,000s of Hz).<br />

Thus, the frequency of WBZ in<br />

Boston, operating near the mid-<br />

B. Wave amplitude at time t<br />

versus distance.<br />

A<br />

<br />

B<br />

d<br />

Figure 2.2 A bobbing ball on a<br />

string demonstrates continuous<br />

wave generation. (A) Wave amplitude<br />

at point A versus time t. (B) Wave<br />

amplitude at time t versus<br />

distance d.

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