ITU-R BS 498-2-1990 Ionospheric Cross-Modulation in the LF and MF Broadcasting Bands - Section 10A-1 - Amplitude-Modulation Sound Broadcasting in Bands 5 (LF) 6 (MF) and 7 (HF)《低频和.pdf
《ITU-R BS 498-2-1990 Ionospheric Cross-Modulation in the LF and MF Broadcasting Bands - Section 10A-1 - Amplitude-Modulation Sound Broadcasting in Bands 5 (LF) 6 (MF) and 7 (HF)《低频和.pdf》由会员分享,可在线阅读,更多相关《ITU-R BS 498-2-1990 Ionospheric Cross-Modulation in the LF and MF Broadcasting Bands - Section 10A-1 - Amplitude-Modulation Sound Broadcasting in Bands 5 (LF) 6 (MF) and 7 (HF)《低频和.pdf(9页珍藏版)》请在麦多课文档分享上搜索。
1、Rec. 498-2 1RECOMMENDATION 498-2IONOSPHERIC CROSS-MODULATION IN THE LF AND MF BROADCASTING BANDS(Question 44/10, Study Programme 44E/10)(1974-1978-1990)Rec. 498-2The CCIR,CONSIDERINGthat excessive radiation towards the ionosphere may result in ionospheric cross-modulation and hence harmfulinterferen
2、ce,UNANIMOUSLY RECOMMENDSthat the maximum permissible radiation at any angle of elevation should be such that annoyance due toionospheric cross-modulation does not exceed that agreed for co-channel interference (see Recommendation 560).ANNEX I*The effects of ionospheric cross-modulation in bands 5 (
3、LF) and 6 (MF) may become a problem of increasingseverity as the power of transmitters continues to increase.1. Detailed experiments on this subject have been carried out within the framework of the EBU in severalcountries, notably in the United Kingdom, in the Federal Republic of Germany Haberkant
4、and Vogt, 1966; Haberkantet al., 1971 and in the Peoples Republic of China CCIR, 1986-90. From these experiments which were carried outwith conventional amplitude-modulation double-sideband transmissions, the following results may be deduced:1.1 The percentage of cross-modulation increases practical
5、ly linearly with the power of the interfering transmitterand also increases with the depth of modulation.Note The percentage of cross-modulation is the percentage by which the carrier of the wanted transmitter is modulatedby the modulating frequencies of the interfering transmitter.1.2 Cross-modulat
6、ion depends primarily on the power radiated by the interfering transmitter in the direction of thereflection point of the wanted signal in the ionosphere.Cross-modulation of percentages less than 10% are directly proportional to the power Knight, 1973; anincrease of 3 dB in the interfering transmitt
7、er power therefore, increases the cross-modulation levels by 6 dB. Thepercentage of cross-modulation is also directly proportional to the depth of modulation of the interfering transmitterKnight, 1973.1.3 The percentage of cross-modulation decreases as the modulating frequency of the interfering tra
8、nsmitterincreases. Laboratory experiments Whythe and Reed, 1973 have shown that the subjective effect of cross-modulationcan be related to co-channel interference. To produce a given subjective grade of impairment, interference resulting fromionospheric cross-modulation requires 6 dB less input sign
9、al-to-interference ratio than does co-channel interference,providing that the cross-modulation is referred to a modulation frequency of 300 Hz.1.4 It should be noted that the studies on the problem of ionospheric cross-modulation carried out by StudyGroup 6 are summarized in Report 574.2. Figure 1 s
10、hows the percentages of cross-modulation measured in many experiments Knight, 1973. Eachmeasurement has been standardized to the value which would have been observed if the interfering transmission hadbeen radiated from a short vertical antenna with a carrier power of 100 kW and amplitude modulated
11、at 300 Hz to adepth of 80%._*This Annex is given for information.2 Rec. 498-2D01-scFIGURE 1 D01 = 22 cm = page pleineRec. 498-2 3Figure 1 includes a semi-empirical curve which shows the greatest percentage of cross-modulation, averagedover a short period, likely to be observed; the condition for thi
12、s is that the wanted signal should traverse the region of theionosphere most strongly illuminated by the interfering transmitter. Figure 1 shows that cross-modulation rises to asecond maximum when the frequency of the interfering transmitter is close to the gyromagnetic frequency. Figure 5shows a ma
13、p giving the value of the gyromagnetic frequency for different parts of the world Laitinen andHaydon, 1950.3. The effects of cross-modulation should be taken into account not only for sky-wave reception, but also forground-wave reception at the edge of the service area when at night the sky-wave is
14、no longer negligible. However, theeffect of cross-modulation is reduced approximately in the ratio of the wanted signal levels, ground-wave to sky-wave,at the receiving point.4. The percentages of ionospheric cross-modulation have been calculated for LF and MF and their dependenceon the powers of th
15、e wanted and unwanted transmitter has been determined. Results of theoretical studies and practicalexperiments have been compared. Shluyger et al., 1976.5. Preliminary conclusionsOn the basis of measurements Haberkant and Vogt, 1966; Haberkant et al., 1971 examples may be given ofthe power-flux leve
16、ls, or the transmitter power as a function of the angle of elevation, which can cause disturbance towanted transmissions.For this purpose, an assumption is first made regarding the tolerable level of the percentage of cross-modulation. According to Recommendation 560 and Report 575, a radio-frequenc
17、y protection ratio of approximately30 dB is agreed for 10% of the time in the case of a fluctuating unwanted signal. Ignoring the effect mentioned in 1.3,the same disturbing effect is produced by 3% cross-modulation for 10% of the time. It has been shown Haberkantet al., 1971 that for frequencies at
18、 the upper end of the MF broadcasting band 6 (MF) this level of cross-modulationmay be produced by a power flux within the E region of the ionosphere of about 2 W/m2(57 dB(W/m2), whichcorresponds to a maximum field strength of 27 mV/m (89 dB(V/m).Assuming a height of 100 km of the reflecting layer (
19、E region), it is possible to calculate the power radiatedfrom various types of antenna which would produce this power flux within the E region. The vertical transmittingantennas that are commonly used show a vertical radiation pattern which depends in a well-defined fashion on the height(expressed i
20、n fractions of the wavelength, ). In particular, such vertical antennas do not radiate at an angle of elevationof 90. Table I Haberkant et al., 1971 indicates, for a number of vertical transmitting antennas at different heights thetransmitter powers to be fed into these antennas to meet the above-me
21、ntioned requirements.TABLE ILength of vertical antenna 0.25 0.25 0.5 0.55 0.64 0.64 (1)Transmitter carrier power(kW)320 340 560 670 370 840(1)First side lobe compensated.It is possible to calculate the dependence of the radiated power on the angle of elevation required to producethe same power flux,
22、 covering the whole range from 0 (horizontal radiation) to 90 (vertical radiation). The results aregiven in Table II.Tables I and II give only approximate values because it is known, from theory, that ionosphericcross-modulation may be influenced by several parameters, such as the frequencies of the
23、 wanted and of the interferingtransmitter (in particular seen in their relationship to the gyro-frequency) and the polarization of emission.The powers given in Tables I and II are examples based on a small number of measurements at a frequencynear the top end of band 6 (MF); they make no allowance f
24、or the change of cross modulation with carrier frequency ofthe disturbing signal, nor do they include the effect of reduced cross-modulation at the higher audio frequencies whichpermits interfering-transmitter powers to be increased by 3 dB.4 Rec. 498-2TABLE IIAngle of elevation 0 10 20 30 40 45 50
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