ITU-R REPORT RA 2189-2010 Sharing between the radio astronomy service and active services in the frequency range 275-3 000 GHz《频段在275-3000 GHz无线电天文业务和主动业务之间的共享》.pdf
《ITU-R REPORT RA 2189-2010 Sharing between the radio astronomy service and active services in the frequency range 275-3 000 GHz《频段在275-3000 GHz无线电天文业务和主动业务之间的共享》.pdf》由会员分享,可在线阅读,更多相关《ITU-R REPORT RA 2189-2010 Sharing between the radio astronomy service and active services in the frequency range 275-3 000 GHz《频段在275-3000 GHz无线电天文业务和主动业务之间的共享》.pdf(15页珍藏版)》请在麦多课文档分享上搜索。
1、 Report ITU-R RA.2189(10/2010)Sharing between the radio astronomy service and active services in the frequency range 275-3 000 GHzRA SeriesRadio astronomyii Rep. ITU-R RA.2189 Foreword The role of the Radiocommunication Sector is to ensure the rational, equitable, efficient and economical use of the
2、 radio-frequency spectrum by all radiocommunication services, including satellite services, and carry out studies without limit of frequency range on the basis of which Recommendations are adopted. The regulatory and policy functions of the Radiocommunication Sector are performed by World and Region
3、al Radiocommunication Conferences and Radiocommunication Assemblies supported by Study Groups. Policy on Intellectual Property Right (IPR) ITU-R policy on IPR is described in the Common Patent Policy for ITU-T/ITU-R/ISO/IEC referenced in Annex 1 of Resolution ITU-R 1. Forms to be used for the submis
4、sion of patent statements and licensing declarations by patent holders are available from http:/www.itu.int/ITU-R/go/patents/en where the Guidelines for Implementation of the Common Patent Policy for ITU-T/ITU-R/ISO/IEC and the ITU-R patent information database can also be found. Series of ITU-R Rep
5、orts (Also available online at http:/www.itu.int/publ/R-REP/en) Series Title BO Satellite delivery BR Recording for production, archival and play-out; film for television BS Broadcasting service (sound) BT Broadcasting service (television) F Fixed service M Mobile, radiodetermination, amateur and re
6、lated satellite services P Radiowave propagation RA Radio astronomy RS Remote sensing systems S Fixed-satellite service SA Space applications and meteorology SF Frequency sharing and coordination between fixed-satellite and fixed service systems SM Spectrum management Note: This ITU-R Report was app
7、roved in English by the Study Group under the procedure detailed in Resolution ITU-R 1. Electronic Publication Geneva, 2011 ITU 2011 All rights reserved. No part of this publication may be reproduced, by any means whatsoever, without written permission of ITU. Rep. ITU-R RA.2189 1 REPORT ITU-R RA.21
8、89 Sharing between the radio astronomy service and active services in the frequency range 275-3 000 GHz (2010) TABLE OF CONTENTS Page 1 Introduction 1 2 Atmospheric absorption 2 3 Antenna beamwidth 4 4 RF power generation 7 5 Sharing between active services and radio astronomy . 7 5.1 Terrestrial tr
9、ansmitter into terrestrial radio telescope . 8 5.2 Airborne transmitter into radio telescope . 10 5.3 Satellite transmitter into radio telescope . 11 6 Conclusions 12 1 Introduction Certain characteristics of the frequency range 275-3 000 GHz combine to reduce the likelihood of interference between
10、the radio astronomy service and active services in this range. The purpose of this Report is to present a basic introduction to those characteristics and how they affect potential sharing scenarios. Based on the analysis in this Report, there is little chance for interference to radio telescopes fro
11、m co-frequency terrestrial, airborne, or satellite transmitters, particularly at frequencies above 1 000 GHz. The results of this study are applicable to current and future discussions relating to extending No. 5.565 of the Radio Regulations to frequencies in the 275-3 000 GHz range, and studies rel
12、ated to the advancement of technology at frequencies above 275 GHz1. 1In this Report, “THz frequencies” refers to the range 275-3 000 GHz. 2 Rep. ITU-R RA.2189 2 Atmospheric absorption In the range 275-3 000 GHz, propagation through the Earths atmosphere is strongly affected by absorption due to atm
13、ospheric molecules. The molecular species most responsible for the absorption are oxygen (O2) and water vapour (H2O). Non-resonant absorption creates a general continuum of absorption that steadily increases with frequency, while exceedingly large values of attenuation are found at specific frequenc
14、ies corresponding to natural resonances of the molecules. At sea level, the general continuum of absorption is approximately 5 dB/km at 275 GHz, 300 dB/km at 1 000 GHz, and 4 000 dB/km at 3 000 GHz. At specific molecular resonances in this range, the attenuation can be as large as 550 000 dB/km. Att
15、enuation will decrease with altitude due to lower concentrations of oxygen and water vapour. Figure 1 shows attenuation in dB/km at 4 different altitudes: sea level, 300 m, 1 000 m, and 3 000 m. The curve assumes the 1976 Standard Atmosphere model2,3, with the addition of a column of 2 cm total prec
16、ipitable water vapour with a scale height of 2 km, at a sea-level relative humidity of 50%. The atmospheric parameters were used in the am atmospheric transmission model to compute the absorption curves4,5. Based on the assumed atmospheric characteristics, the following inputs were used in the am mo
17、del: TABLE 1 Assumed atmospheric properties for calculating absorption over a horizontal path of 1 km in length Altitude (m) Temperature (K) Pressure (mbar) Column density of dry air (cm2) Column density of water vapour (cm2) 0 288.15 1013.25 2.55 1 024 3.34 1 022 300 286.20 977.73 2.47 1 024 2.87 1
18、 022 1 000 281.65 898.75 2.31 1 024 2.03 1 022 3 000 268.65 701.09 1.89 1 024 7.45 1 021 2U.S. Standard Atmosphere 1976 U.S. Government Printing Office, Washington DC, http:/ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/19770009539_1977009539.pdf. 3Standard atmosphere calculator available at http:/
19、4Paine, Scott, “The am Atmospheric Model”, Submillimeter Array Technical Memo #152 (Revision 3); available at http:/www.cfa.harvard.edu/spaine/am/. 5Recommendation ITU-R P.676 accurately calculates atmospheric attenuation up to a maximum frequency of 1 000 GHz. The am model is more rigorous for freq
20、uencies above 1 000 GHz. For a consistency check, the data in Fig. 1 and those in Fig. 5 of Recommendation ITU-R P.676 agree well in the region of overlapping frequency coverage. Figure 1 of this Report is based on am for the entire range. Rep. ITU-R RA.2189 3 FIGURE 1 Atmospheric attenuation comput
21、ed over horizontal paths of 1 km at four different altitudes, assuming the atmospheric properties of Table 1. For reference, free-space loss over 1 km is also plotted 0 500 1 000 1 500 2 000 2 500 3 000Attenuation (dB/km)1101001 00010 000100 0001 000 0000 m altitude300 m altitude1 000 m altitude3 00
22、0 m altitudeFree space loss over 1 kmFrequency (GHz)Because atmospheric absorption is a strong factor for terrestrial systems at THz frequencies, calculation of path loss between a transmitter and receiver must include this factor. The signal level at the receiver is: APLGGPPRTTR+= (1) where: PR: th
23、e power at the output port of the receive antenna PT: the power at the input port of the transmit antenna GT: the gain of the transmit antenna in the direction of the receive antenna GR: the gain of the receive antenna in the direction of the transmit antenna PL: the “traditional” path loss between
24、transmit and receive antennas due to geometric spreading and terrain blockage A: the additional loss factor due to atmospheric absorption. All terms are expressed in logarithmic units. Due to extreme atmospheric absorption, typically the only possible interference scenarios involve a transmitter and
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