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#1
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Jimmie D reported Roy Lewallen to write:
"There is no direct way to measure the total power being radiated other than sampling the field at many points in all directions and integrating." That sounds right to me. An approximation is sometimes made by taking 36 samples of field strength in volts per meter at 10-fegrees of azimuth intervals at the same distance from the central antenna system. Each of these sample values is squared and the sum of these squared samples is divided by 36, the number of samples, to get their average. The square poot of this quotient is then the average field strength at that distance from the antenna. A true average signal strength should be the same as the value an isotropic antenna would radiate at a given distance. Knowing the field strength, one could calculate the watts per square meter of the envelope of radiation at a given distance and total the watts per square meter of all the squares to get the total power being radiated. Since 1960, I`ve used the Bird wattmeter satisfactorily to get the total power being delivered by the transmitter and radiated by the antenna. It should be the same if the transmission line and antenna have low losses. It is simply the difference between the forward power indication and the reverse power indication. Many lines and antennas have very high efficiencies. Best regards, Richard Harrison, KB5WZI |
#3
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Owen Duffy wrote:
Firstly you seem to assume that your 36 samples around the azimut circle adequately fulfill Roy's "sampling the field at many points in all directions", surely he mean't all elevation angles as well as all azimuth angles. What is the hourly rental charge on a helicopter? :-) -- 73, Cecil http://www.w5dxp.com |
#4
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Cecil Moore wrote:
Owen Duffy wrote: Firstly you seem to assume that your 36 samples around the azimut circle adequately fulfill Roy's "sampling the field at many points in all directions", surely he mean't all elevation angles as well as all azimuth angles. What is the hourly rental charge on a helicopter? :-) that's what balloons and blimps are for, or model airplanes.. |
#5
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Owen wrote:
"Is that true?" Only for limited conditions. Owen is correct that enough samples must be taken to catch all variations in signal strength, in elevation and azimuth if total radiated power is to be determined. A simple vertical antenna rests on the earth and has a null at its tip. It is far from an isotropic radiator. The sampling I described is done on AM broadcast antennas. Only the wave which travels along the earth is usually of any interest. The minimum distance from the broadcast antenna for any field strength measurements is usually one mile to be sure the far field is being measured. The FCC`s ground wave intensity charts assume that if you have ground conductivity such as sea water, a certain power and antenna efficiency deliver 100 millivolts per meter at a distance of one mile from the antenna. Field intensity in millivolts declines linearly with distance so that at 10 miles you might have 10 mv/m if you have 100 mv/m at one mile.Power is proportional to the square of the voltage. Best regards, Richard Harrison, KB5WZI |
#6
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Richard Harrison wrote:
The FCC`s ground wave intensity charts assume that if you have ground conductivity such as sea water, a certain power and antenna efficiency deliver 100 millivolts per meter at a distance of one mile from the antenna. Field intensity in millivolts declines linearly with distance so that at 10 miles you might have 10 mv/m if you have 100 mv/m at one mile. . . . The attenuation of the ground wave is the same as the free space attenuation? Roy Lewallen, W7EL |
#7
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Roy Lewallen, W7EL wrote:
"The attenuation of the ground wave is the same as the free space attenuation?" No, it is greater. The attenuation of the ground wave is more rapid because the soil has resistance and imposes a loss on the passing wave. In free space, there is no ground loss and the signal loss is from the spreading of the signal which reduces its density. It declines 6 dB (its power is quartered) every time the distance from the transmitter doubles, that is its volts per meter or signal strength is cut in half. Ground waves decrease more rapidly with distance from the transmitter due to imperfect conductivity in the earth`s surface. Loss goes up with the operating frequency and with higher resistivity in the soil. The FCC`s ground-wave field intensity charts cover limited frequency ranges and each curve is for a specific soil conductivity. Best regards, Richard Harrison, KB5WZI |
#8
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Richard Harrison wrote:
Roy Lewallen, W7EL wrote: "The attenuation of the ground wave is the same as the free space attenuation?" No, it is greater. The attenuation of the ground wave is more rapid because the soil has resistance and imposes a loss on the passing wave. . . . I should hope so. That's why your statement that the field strength decreases as the inverse of the distance in the context of AM broadcast measurements at ground level was puzzling. Roy Lewallen, W7EL |
#9
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On Mon, 23 Apr 2007 17:30:20 -0700, Roy Lewallen
wrote: Richard Harrison wrote: Roy Lewallen, W7EL wrote: "The attenuation of the ground wave is the same as the free space attenuation?" No, it is greater. The attenuation of the ground wave is more rapid because the soil has resistance and imposes a loss on the passing wave. . . . I should hope so. That's why your statement that the field strength decreases as the inverse of the distance in the context of AM broadcast measurements at ground level was puzzling. Richard had been reciting decade-for-decade declines of FS faithfully from the FCC charts -over seawater- which he had specifically called out. "Faithfully" except for an inadvertent substitution of decade miles for decade kilometers distance. 73's Richard Clark, KB7QHC |
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