THE PULKOVO COOPERATION FOR RADAR AND OPTICAL OBSERVATIONS OF SPACE OBJECTSLMolotov1,2,3,4, A.Konovalenko5, G.Tuccari6, I.Falkovich5, M.Nechaeva7, A.Dementiev7, R.Kiladze8, V.Titenko1,3, A.Agapov3, V.Stepanyants3, Z.Khutorovsky2, S.Sukhanov2, Yu.Burtsev9, O.Fedorov10, V.Abrosimov11, A.Volvach12, A.Deviatkin1, A.Sochilina1, I.Guseva1, V.Abalakin1, V.Vlasjuk13, Liu Xiang14, Yu.Gorshenkov15, G.Kornienko16, R.Zalles17, M.Ibrahimov18, P.Sukhov19, I.Shmeld20, V.Samodourov21, S.Buttaccio6, C.Nicotra6, A.Pushkarev1,12, A.Tsyukh11, V.Nesteruk11, A.Erofeeva16, N.Marshalkina181 Central (Pulkovo) Astronomical Observatory, Russian Academy of Sciences, St.-Petersburg, Russia 2 JSC “Vimpel” International Corporation, Moscow, Russia 3 Keldysh Institute of Applied Mathematics, Russian Academy of Sciences, Moscow, Russia 4 Central Research Institute for Machine Building, Korolev, Russia 5 Institute of Radio Astronomy, National Academy of Sciences of Ukraine, Kharkiv, Ukraine 6 Istituto di Radioastronomia, Noto, Italy 7 Radiophysical Research Institute, N. Novgorod, Russia 8 Abastumani Astrophysical Observatory, Georgian Academy of Sciences, Tbilisi, Georgia 9 Space Force of Russian Ministry of Defence, Moscow, Russia 10 National Space Agency of Ukraine, Kyiv, Ukraine 11 National Control and Space Facilities Test Center, Vitino Village, Sacskiy Region, Ukraine 12 Scientific-research institute “Crimean Astrophysical Observatory”, Simeiz, Ukraine 13 Special Astrophysical Observatory, Russian Academy of Sciences, N. Arkhyz, Karachaevo-Ñherkessia, Russia 14 Urumqi Astronomical Observatory, National Astronomical Observatories, CAS, Urumqi, China 15 Special Research Bureau of Moscow Power Engineering Institute, Moscow, Russia 16 Ussuriysk Astrophysical Observatory, Far-Eastern Branch of RAS, Gornotaeznoe, Primorsky Kray, Russia 17 National Astronomical Observatory of Bolivia, Tarija, Bolivia 18 Ulugh Beg Astronomical Institute, Uzbekistan Academy of Sciences, Tashkent, Uzbekistan 19 Astronomical Observatory, Shevchenko University, Odessa, Ukraine 20 Institute of Astronomy, University of Latvia, Riga, Latvia 21 Puschino Radioastronomy Observatory, P.N. Lebedev Physical Institute, RAS, Puschino, Moscow region, Russia
1. INTRODUCTIONThere is a long history of satellite astrometry observations at the Pulkovo Observatory since
October 10, 1957, when the first photographic frame of the “Sputnik” rocket body was taken
(see Figure 1) and its position was determined. The list of activities included optical
observations, the treatment of measurements, the orbit determination, the development of the
motion theory, and the compilation of a catalogue of geostationary objects.
Fig. 1. The photo frame of the “Sputnik” rocket body taken on October 10, 1957 by Dr. T.P. Kiseleva using the 10-cm telescope AKD. The exposure time is 21 s.
In last years, Pulkovo Observatory has tried to realize the multiform concept of study of
space objects in close collaboration with the Ballistic Center of the Keldysh Institute of
Applied Mathematics and the JSC “Vympel” International Corporation.
2. RADAR AND OPTICAL FACILITIES ON SPACE OBJECT STUDYThe Central Astronomical Observatory at Pulkovo (CAO) is investigating the space objects
on the basis of optical and radar observations. Radar observations are carried out in the
framework of the LFVN that includes the 70-m antenna in Evpatoria with the 6-cm
transmitter facility and the international array of receiving radio telescopes (RT-64 at the Bear
Lakes, RT-32 at Noto, RT-25 at Urumqi, RT-22 at Simeiz, RT-22 at Puschino (Russia), RT-
32 at Ventspils (Latvia)). More detailed information may be found in [1,2]. As a part of this
work, CAO supports the radio astronomical station disposing of the 64-m antenna at the Bear
Lakes (Special Research Bureau of Moscow Power Engineering Institute) near Moscow (see
Figure 2).
Fig. 2. The 64-m dish, receiver cabin, and
apparatus room at the Bear Lakes.
Fig. 3. The specialized satellite telescope SR-220 at Pulkovo Observatory. The optical observations are made in the framework of the PULCOO [2] including the
optical observation stations of many observatories of the former Soviet Union and are
intended to control the most part of geostationary orbit, the telescopes used are as follows:
Zeiss-400 astrograph at Ussuriysk, UAFO; Zeiss-600 at Maidanak, UBAI; Maksutov-700 at
Abastumani; AAO, Zeiss-1000 at Zelenchuk, SAO; AT-64 and 2.6-m ZTSh at Nauchnyi,
CrAO; SR-220 at Pulkovo, CAO; RK-300 at Mayaki, AOSU; Zeiss-600 at Tarija, NAOB and
others). As part of this work, CAO maintains the 22-cm optical telescope SR-220 with the
wide field of view at Pulkovo (see figure 3, it is installed in the top of the AKD telescope,
with which the first satellite photograph frame in 1957 was made ) and prepares the 50-cm
MTM-500 telescope for observations in Kislovodsk, Northern Caucasus.
All necessary software for the CCD-frame processing, ephemeris support, and orbit
determination are developed in CAO, together with the “LAPLACE” analytical theory of
motion of uncontrolled GEO-objects, and with a model of explosions and the space debris
database.
3. RECENT VLBI-RADAR RESULTSThe main directions of the work include the development of the VLBI (very long baseline
interferometry) method for the coordinated and non-coordinated measurements of catalogued
high-orbit space objects, and the adjustment of the beam-park and beam-track techniques for
the search for non-catalogued objects. The three main VLBI principles consist in the
following:
Fig. 4. The cross-spectrum of echo from Cosmos-1366 on the baselines Bear Lakes-
Noto, Urumqi-Noto and Bear Lakes-Urumqi. The fringe rates are measured as
frequencies of spectral maximums: -373:703 Hz, -176:524 Hz and -195:890 Hz,
respectively. VLBR03.1.
Fig. 5. Time dependence of the cross-spectrum maxima of Cosmos-1366 on the
baselines Bear Lakes-Noto (mono), Bear Lakes-Urumqi (mour) and Noto-Urumqi
(nour). VLBR03.1.
The shifts of cross-spectrum maxima, obtained on the baselines between the receiving
antennas, (Fig. 5) with respect to the initial count point 22:23:11 are –3.35 s for Bear Lakes-
Noto, +1.65 s for Bear Lakes-Urumqi and –5.5 s for Noto-Urumqi baselines. Accordingly,
with respect to the Bear Lakes point, the echo signals are ahead in Noto by 2.15 s and delayed
in Urumqi by 5 s. It may be explained by the fact that the reflecting area of the Raduga 9
facility has a narrow beam directivity (about a few degrees wide) and successively passed the
receiving points during the rotation. This fact is demonstrated with respect to the initial orbit
of an object reconstructed from optical data to evaluate the direction of the object rotation
axis. In Table 1 the results of comparisons of precisions of the Doppler shift and fringe rate
measurements are given. The Doppler shift measurements were transformed into the half-
sums of the object radial velocities with respect to the sounding and receiving antennas. The
fringe rate measurements were transformed into the radial velocity differences of the object
with respect to two receiving antennas.
Table 1. The precision of two kinds of VLBI-radar measurements –
the Doppler shift and fringe rate for Cosmos-1366.
One can see that the precision of fringe rate measurements is dozens of times worse
than the precision of Doppler shift data while it should be quite the reverse. It may be explained by insufficient current frequency resolution of the correlator. Nevertheless both
kinds of VLBI-radar measurements may be used for the improvement of the initial orbit of an
object.
The procedures of the beam-park and beam-track searching are adjusted using the
newly designed recording terminals for the e-VLBI named NRTV (Near Real Time VLBI). It
can register the echo-signals on the PC-disks and then transfer them into Internet for further
analysis at the VLBI data processing center. The recorded signals are auto-correlated to the
high frequency and time resolutions, and the obtained data are presented in the form of the
“frequency vs.time” diagram. It is supposed that possible space objects will leave the tracks in
the form of lines on this diagram, and the slope of the line will reflect the value of the Doppler
shift of echo-signals. The beam-park mode (i.e. the fixed beam direction with respect to the
rotating Earth) was used in an attempt to find the LEO objects. The beam track mode (i.e. the
fixed beam direction with respect to the inertial frame) was used in an attempt to detect the
GEO objects. In the beam track mode the antenna beams are slowly moving along the GEO.
During VLBR04.2 in July 2004 the GEO region around the point with coordinates RA. 12h
08m 43s.0, Dec. +00° 50' 45" has been observed. Processing the measurements in this
experiment allowed to clearly detect the echoes from 6 catalogued GEO objects and to
determine the time-moment of the signal maximum, the duration of the beam crossing and the
Doppler shift. A sample of the “frequency vs. time” diagram is shown in figure 6.
Fig. 6. The sample of the “frequency vs. time” diagram for analyzing the beam-track
experiments. On the vertical axis is time from 22:12:31 to 22:16:41 of day 206,
2004. On the horizontal axis are frequencies 247802.734 – 262451.172. The two
points are identified with COSMOS 1961 and TELESAT-5.
4. PULCOO ACTIVITIESThe geographic position and aperture of the telescopes working with PULCOO are presented in figure 7.
Fig. 7. The geographic position and diameter of telescopes working with PULCOO.
In the first place, the PULCOO was organized to improve the ephemerides of the
objects selected as targets for the VLBI-radar experiments. Two other major research
directions are the precise tracking of the GEO-objects in order to develop the dynamical
control method and to search for the small fragments produced by GEO-object explosions on
the basis of the barrier method [5]. There were obtained about 20’000 measurements for the GEO and objects in highly-elliptical orbits in the past year. Also regular observations of the
GEO fragments were carried out. The 64-cm AT-64 and 2.6-m ZTSH telescopes at Nauchnyi
(CrAO) are used to search for the fragments in the barriers calculated by use of the
“LAPLACE” theory. Zeiss-600 in Nauchnyi (SAI MSU), Zeiss-1000 in Zelenchuk (SAO
RAS) and Zeiss-600 in Maidanak (UBAI) are used for follow-up observations of the
fragments. In common 22 fragments of 16m -18.5m were discovered and the orbital parameters
were determined for 25 of them. Some fragments are tracked already on time intervals of
several months. This work is carried out in collaboration with the ESOC (6, 7). The program
of the PULCOO modernization is now in progress. The first stage of the program foresees the
purchase of 10 CCD-matrixes (six matrixes have already been purchased for Nauchnyi,
Pulkovo, Maidanak, Mayaki, Ussuriysk and Abastumani), and the upgrading of three
telescopes (the 50-cm and 1-m telescopes in Pulkovo and the 60-cm telescope in Mayaki).
The measurements are accumulated in the “LAPLACE” space debris database in Pulkovo and
transferred to the “Vympel” International Corporation and Ballistic Center of the Keldysh
Institute of Applied Mathematics, where the Center on collection, processing, and analysis of
information on space debris of the Russian Academy of Sciences was arranged this year.
5. CONCLUSIONSThe Pulkovo Observatory carries out the radar and optical research of high-orbit space objects
in wide cooperation with other institutes and observatories. The Low Frequency VLBI
Network applied for the VLBI-radar experiments has been equipped with the new NRTV
recording terminals that allow to obtain the measurements in quasi-real time using the Internet
for transfer of the VLBI signals from the receiving antennas to the correlation center. The
procedure of the correlation processing was adjusted for the radar echo signals to measure the
Doppler shift and fringe rate. The Pulkovo cooperation of optical observers initiated the
routine observations of space objects practically along the entire geostationary ring. The
“barrier” method of searching for the faint non-catalogued GEO fragments was adjusted. The
potentialities of the PLCOO will increase after finishing the first modernization stage. This
work was supported by the National Space Agency of Ukraine under project “Interferometer”,
by the grant of the Russian Ministry of Education and Science, the INTAS-2001-0669,
INTAS 03-70-567, RFBR 05-02-16832 grants.
Fig. 8. Average magnitude distribution of discovered GEO-fragment.
Fig. 9. Mass-to-area ratio value distributed for 21 fragments.
REFERENCES
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