We performed continuous six frequency 1-22 GHz spectra observations of compact extragalactic sources from 1st to 22nd December, 1997. We used the 600 meter ring radio telescope RATAN-600 (Korolkov & Parijskij 1979; Parijskij 1993) at the Russian Academy of Sciences' Special Astrophysical Observatory, located in Karachaevo-Cherkessia Republic (Russia) near Nizhny Arkhyz and Zelenchukskaya at the North Caucasus. The northern sector of the antenna (a part of the main ring reflector) was used together with the secondary mirror of cabin No. 1. Six broad band receivers are located at this movable cabin. The cabin moves along 150 meter long rails in order to be placed in the focus of the antenna system at different elevations. The main (meridional) transit method of observation was employed. Accuracy and reliability of these spectra measurements were essentially higher than earlier experiments conducted at the RATAN-600 due to the following improvements made to the receivers, antenna control system and the procedure of observations.
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nh | ![]() |
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TphysLNA, | TLNA, | Tsys, |
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cm | GHz | GHz | K | K | K | mK | |
1.4 | 2 | 21.65 | 2.5 | 15 | 23 | 77 | 3.5 |
2.7 | 2 | 11.2 | 1.4 | 15 | 18 | 70 | 3 |
3.9 | 2 | 7.70 | 1.0 | 15 | 14 | 62 | 3 |
7.7 | 1 | 3.90 | 0.6 | 15 | 8 | 37 | 2.5 |
13 | 1 | 2.30 | 0.4 | 310 | 35 | 95 | 8 |
31 | 1 | 0.96 | 0.12 | 310 | 21 | 105 | 15 |
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1.4 | 8
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8
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13
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2.7 | 16
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17
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24
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3.9 | 23
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26
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39
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7.7 | 48
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53
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1
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13 | 1
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1
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1
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31 | 3
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3
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5
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We used a new set of broad band receivers at the wavelengths of 1.4, 2.7, 3.9, 7.7, 13 and 31 cm with low noise HEMT amplifiers (LNA), cooled to a temperature of 15 K at the four shortest wavelengths (Berlin et al. 1997, 1993). Parameters of radiometers and antenna beams are given in Tables 2, 3.
Table 2 lists wavelengths ;
numbers
of feedhorns nh; exact central frequencies
;
band
widths
;
physical temperatures of the LNA
TphysLNA; noise temperatures of the LNA
TLNA; total noise temperatures of systems
Tsys, including the antenna noise at middle elevations;
rms noise temperature sensitivities of the system
for a one second integration time.
Dual-feedhorn receivers are beam-switched. Single-feedhorn
receivers have a noise-added, gain-balanced mode of operation.
Linearly polarized systems were available at all frequencies:
horizontal at 7.7 cm and vertical at other wavelengths.
Table 3 gives half power beam widths (HPBW) in right ascensions HPBWRA and declinations HPBWDec = rHPBWRA, for various elevations. The values of HPBWRA were obtained from our measurements. Ignoring the aberration effects, we estimated the factor r using theoretical simulations of the RATAN-600 beam by Esepkina et al. (1979) and their experimental testing by Temirova (1983). A map of the knife-like beam of the RATAN-600 northern sector is known to have different shapes of contours cross-sections at high and low power levels. In the absence of aberrations, the shapes can be described as ordinary elliptical contours (elongated on declinations) at half power level and higher levels. The contours are transformed to "the elongated eight" at lower levels or to "a dumb-bell" at 0.1 normalized power level (see Esepkina et al. 1979 for details).
The full permanent automatic control of 225 elements of the main ring reflector was achieved using the new control system of the antenna (Zhekanis 1997; Golubchin et al. 1995). Errors in position of each element of the main reflector, if present, were recorded in order to check the quality of the antenna surface for each observation. The positioning of cabin No. 1 with the secondary mirror was measured from one of the eight geodetic reference points, located every 20 meters along the rails. The accuracy of semi-automatic positioning of the cabin directed towards the focus was again checked by us some minutes before each observation. If an error of more than 2 mm with respect to a value given in the schedule was found, it was corrected.
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Figure 1: Example of a full multifrequency scan for 4C 39.25, observed on 16 December 1997 with 0.1 second integration time |
All horns of the radiometers are horizontally located and form a
new configuration, which is an optimal one for decreasing transversal
aberrations. Observations were carried out in the main meridian
(transit mode). As a result, a response to an object is obtained due to
its horizontal scanning by the antenna beam because of the daily rotation of the Earth (see an example of 4C 39.25 full scan on
Fig. 1; the moment of culmination is at
here).
The total duration of each six frequency observations was usually about
five minutes, and included also two sets of noise temperature
calibration for 30-40 seconds before and after the passing of the
source. The data acquisition system (Chernenkov &
Tsibulev 1995) controls radiometers and records
the output signals. After each observation, the main ring reflector and
the cabin No. 1 with receivers and the secondary mirror were
repositioned for observation of the next source on a new elevation.
We have optimized the observational schedule, using new software
(Zhekanis & Zhekanis 1997). To increase the
reliability of results by final averaging of the spectra, we endeavoured
to include each source in the schedule two or more times during the set
and each flux density calibrator in more than 70% of the days. The
typical number of sources observed in a 24 hour observing session was
about 80 in the optimized schedule. Several breaks in observations
occurred because of weather conditions (snow-falls or unusually low
temperatures
C), nine hours of technical maintenance per
week, etc. As a result, the total number of successful observations was
about 1450 during 21 days, or about 69 observations per day on average
and 2.6 spectra per source during the set (formal averaging). In 20%
of the sources the spectra have been measured only once.
Copyright The European Southern Observatory (ESO)