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The electromagnetic waves do not need an atmosphere in order to propagate, as you will undoubtedly realize from the fact that space vehicles can transmit radio signals back to earth in a near vacuum But when a radio wave does propagate in the earth s atmosphere, it interacts with the atmosphere, and its path of propagation is altered A number of factors affect the interaction, but it is possible to break the atmosphere into several different categories according to their respective effects on radio signals The atmosphere, which consists largely of oxygen (O2) and nitrogen (N) gases, is broken into three major zones: troposphere, stratosphere, and ionosphere (Fig 2-7) The boundaries between these regions are not very well defined, and change both diurnally (over the course of a day) and seasonally The troposphere occupies the space between the earth s surface and an altitude of 6 to 11 km (4 to 7 mi) The temperature of the air in the troposphere varies with altitude, becoming considerably lower at greater altitude compared with ground temperature For example, a +10 C surface temperature could reduce to 55 C at the upper edges of the troposphere The stratosphere begins at the upper boundary of the troposphere (6 to 11 km), and extends up to the ionosphere ( 50 km) The stratosphere is called an isothermal region because the temperature in this region is somewhat constant, despite altitude changes The ionosphere begins at an altitude of about 50 km (31 mi) and extends up to approximately 300 km (186 mi) The ionosphere is a region of very thin atmosphere Cosmic rays, electromagnetic radiation of various types (including ultraviolet light from the sun), and atomic particle radiation from space (most of these from the sun also), have sufficient energy to strip electrons away from the gas molecules of the atmosphere These freed electrons are called negative ions, while the O2 and N molecules that lost electrons are called positive ions Because the density of the air is so low at those altitudes, the ions can travel long distances before neutralizing each other by recombining Radio propagation on some bands varies markedly between daytime and nighttime because the sun keeps the level of ionization high during.

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If the result returned by the command is a result set, there are several helper functions that can be used to determine what the returned data looks like, and how to handle it These functions are listed and described in Table 14-5 These functions are invaluable in sorting through the result set data returned within the PGresult object The way your program handles the result set data depends on what type of data (if any) is returned The following sections demonstrate how to handle different types of data returned from executing SQL commands in libpq

Coils at Coils at middle of feedpoint ( ) radiators ( ) 1800 950 700 500 360 260 160 75 38 15 2800 1800 1800 1300 950 700 500 160 80 30

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6-13 Shortened or loaded dipole (A) inductors at feedpoint; (B) inductors midway along elements; (C) chart of reactances for coils; (D) commercially available coils; (E) homemade coil based on commercial coil stock

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Other dipoles 159 pose you have about 40 ft available for a 40-m antenna that normally needs about 65 ft for a half-wavelength Because 39 ft is 60 percent of 65 ft, you could use this value as the design point for this antenna Looking on the chart, a 60 percent antenna with the loading coils at the midpoint of each radiator element wants to see an inductive reactance of 700 You can rearrange the standard inductive reactance equation (XL = 628 FL) to the form L H = where L H is the required inductance, in microhenrys F is the frequency, in hertz (Hz) XL is the inductive reactance calculated from the table in Fig 6-13C Example 6-2 Calculate the inductance required for a 60 percent antenna operating on 725 MHz The table requires a reactance of 700 for a loaded dipole with the coils in the center of each element (Fig 6-15B) Solution: L H = = = XL 106 628F (700) (106) (628) (7,250,000) 7 108 46 107 [618] [619] [620] [621] XL 106 628F [617]

Function PQntuples(PGresult *res) PQnfields(PGresult *res)

= 154 H

The -ne operator returns True if the left value and the right value are not identical If the left side of the operation contains multiple values, the operator returns ones that do not match the value on the right

The inductance calculated above is approximate, and it might have to be altered by cut-and-try methods The loaded dipole antenna is a very sharply tuned antenna Because of this fact, you must either confine operation to one segment of the band, or provide an antenna tuner to compensate for the sharpness of the bandwidth characteristic However, efficiency drops, markedly, far from resonance even with a transmission line tuner The function of the tuner is to overcome the bad effects on the transmitter, but it does not alter the basic problem Only a variable inductor in the antenna will do that trick (at least one commercial loaded dipole once used a motor-driven inductor at the center feedpoint) Figures 6-13D and E show two methods for making a coil-loaded dipole antenna Figure 6-13D shows a pair of commercially available loading coils especially designed for this purpose The ones shown here are for 40 m, but other models are also available The inductor shown in Fig 6-13E is a section of commercial coil stock connected to a standard end or center insulator No structural stress is assumed by the coil all forces are applied to the insulator, which is designed to take it

Description Returns the number of records (tuples) in a result set res Returns the number of columns (fields) in a result set res

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