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Radio Wave Reflections from the Earth

Ground-wave transmission is affected by the surface of the earth. This is also true for sky-wave transmission involving more than a single hop. The earth is not a perfect conductor.

Certain of the electrical constants16 of the surface of the earth of importance in radio transmisison are as follows:

Type of Terrain

Dielectric

Constant (Inductivity)

Conductivity e.m.u.

Absorption factor at 50 miles, 1000 kilocycles

Sea water

81

4.64 X 10-11

1.0

Pastoral, rich soil, low hills, midwest

14

3 X 10-13

0.50

Pastoral, medium soil, medium hills, east

13

6 X 10-14

0.09

Rocky soil, steep hills, Xew England

14

2 X 10-14

0.025

City, industrial area, average

5

1 X 10-14

0.011

The dielectric constants given are with respect to air as unity. The conductivity values are in electromagnetic units and can be converted to mhos by multiplying by 109. The absorption factor is the ratio of the actual field intensity to the field intensity with no absorption16 and indicates which terrain is the poorest, sea water being assumed perfect. These constants are determined by studying radio transmission, although it is possible to make direct measurements.17

If the ground were a perfect conductor, then the reflection of radio waves by the surface of the earth would be somewhat as explained in Chapter 6 for a transmission line. The electric field at the surface of a perfect conducting plane must be zero because there can be no voltage drop over such a surface. The reflected electric component must reverse to cause cancellation. From a study of these phenomena,3 it is concluded, theoretically, that a horizontally polarized wave is reflected from a perfectly conducting surface with a 180° phase shift and that a vertically polarized wave is reflected without a phase shift.

Since the earth is not a perfect conductor, the theoretical situation just described may not exist. Studies of wave reflection under actual conditions have been made.17 Both the ratio of the amplitude of the incident to reflected wave and the phase shift vary with the conductivity and the dielectric constant of the earth and with the frequency and angle of incidence. These values can be calculated17 or taken from curves.18



Last Update: 2011-05-18